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diff --git a/.gitattributes b/.gitattributes new file mode 100644 index 0000000..6833f05 --- /dev/null +++ b/.gitattributes @@ -0,0 +1,3 @@ +* text=auto +*.txt text +*.md text diff --git a/31994-8.txt b/31994-8.txt new file mode 100644 index 0000000..4391e19 --- /dev/null +++ b/31994-8.txt @@ -0,0 +1,1390 @@ +The Project Gutenberg EBook of The Forests of Mount Rainier National Park, by +Grenville F. Allen + +This eBook is for the use of anyone anywhere at no cost and with +almost no restrictions whatsoever. You may copy it, give it away or +re-use it under the terms of the Project Gutenberg License included +with this eBook or online at www.gutenberg.org + + +Title: The Forests of Mount Rainier National Park + +Author: Grenville F. Allen + +Release Date: April 15, 2010 [EBook #31994] + +Language: English + +Character set encoding: ISO-8859-1 + +*** START OF THIS PROJECT GUTENBERG EBOOK FORESTS OF MT RAINIER NAT. PARK *** + + + + +Produced by Greg Bergquist and the Online Distributed +Proofreading Team at https://www.pgdp.net (This file was +produced from images generously made available by The +Internet Archive/American Libraries.) + + + + + + + +Transcriber's Note + +The punctuation and spelling from the original text have been faithfully +preserved. + + + FORESTS OF MOUNT RAINIER + NATIONAL PARK + + [Illustration] + + DEPARTMENT OF THE INTERIOR + OFFICE OF THE SECRETARY + 1916 + +For sale by the Superintendent of Documents, Government Printing Office, +Washington, D.C. Price, 20 cents. + + + + +PUBLICATIONS ON MOUNT RAINIER NATIONAL PARK SOLD BY THE SUPERINTENDENT +OF DOCUMENTS. + + +Remittances for these publications should be by money order, payable to +the Superintendent of Documents, Government Printing Office, Washington, +D.C., or in cash. Checks and postage stamps can not be accepted. + +Features of the Flora of Mount Rainier National Park, by J.B. Flett. +1916. 48 pages, including 40 illustrations. 25 cents. + + Contains descriptions of the flowering trees and shrubs in the + park. + +Mount Rainier and Its Glaciers, by F.E. Matthes. 1914. 48 pages, +including 26 illustrations. 15 cents. + + Contains a general account of the glaciers of Mount Rainier and of + the development of the valleys and basins surrounding the peak. + +Panoramic view of Mount Rainier National Park, 20 by 19 inches, scale 1 +mile to the inch. 25 cents. + + + + +THE FORESTS OF MOUNT RAINIER NATIONAL PARK. + +By G.F. ALLEN, _United States Forest Service_. + + + + +GENERAL STATEMENT. + + +The remarkable development of the forests about the base of Mount +Rainier results from climatic conditions peculiarly favorable to tree +growth. The winters are mild and short. The ocean winds that pass +through the gaps of the Coast Range are laden with moisture which falls +in the form of rain or snow on the west slope of the Cascades. The trees +are nourished by this moisture through a long season of annual growth, +and form an evergreen forest which is, in some respects, the most +remarkable in the world. This forest, distinguished by the extraordinary +size and beauty of the trees and by the density of the stand, extends +into the deep valleys of the rivers which have their sources in the +glaciers. On the dividing ridges and in the upper stream basins the +composition and character of the forest change with the increasing +severity of the climate. + +The distribution of the different species of trees according to the +intervals of altitude at which they occur separate the forests of the +Mount Rainier National Park into different types. The lines of +separation are to some extent also determined by complex conditions of +slope, exposure, and moisture. The successive forest belts are uniform +in the composition of their central areas, but blend and overlap where +they come together. + +The low valleys of the main and west forks of White River, of the +Carbon, the Mowich, the Nisqually, and the Ohanopecosh are covered with +a dense and somber forest of fir, hemlock, and cedar. The trees, pushing +upward for light, are very tall and free from limbs for more than half +their height. Their tops form a continuous cover which the sunshine +rarely penetrates, and on which the light snows of early winter fall and +melt, without reaching the ground. Even in midsummer the light is soft +and shaded, and the air cool and humid. In the wintertime the young +growth is sheltered from wind and the severity of the cold is tempered +by the protecting mountain ranges. Saved from fire by the uniform +dampness of the air the trees grow until they decay and fall from old +age. They are succeeded by the suppressed younger trees. The forest +remains mature, not uniformly sound and vigorous, yet not decreasing as +a whole in size and volume. Individuals perish, but the character of the +forest is constant. The deep alluvial soil covered with moss and decayed +vegetation nourishes a luxuriant tangled undergrowth of vine maple, +willow, and devil's-club. The forest floor is covered with a deep layer +of decayed vegetation and is encumbered with fallen and mossy logs and +upturned stumps. The explorer who leaves the trails must be a strong and +active man if he can carry his pack 6 or 8 miles in a long summer day. + +Ascending from the river bottoms to the lower slopes of the dividing +ridges the forest becomes more open and the trees are smaller. Salal, +Oregon grape, and huckleberry bushes take the place of the taller +undergrowth of the valleys. Up to 3,000 feet the Douglas fir and the +hemlock still are the dominant species. Above this altitude new species +are found intermingled with the trees typical of the lowland, but +forming a distinct forest type. The noble and amabilis fir appear, +sometimes growing in pure stands, but more often associated with the +Douglas fir and western hemlock at the lower limits of the type, and +with alpine fir and mountain hemlock at the upper limit. + +Nearly all the trees of this type have deep and wide-spreading roots +which serve to hold in place the surface deposit of volcanic pumice +which covers the slopes of the mountain. Evidence afforded by the after +effects of forest fires in other parts of the Cascades indicates that +the destruction of the forest on the mountain sides is followed by +erosion. Heavy rains and the melting of the upper snow banks by warm +Chinook winds combine to produce a surface run-off that denudes the +steeper declivities down to the underlying bedrock. + +At elevations above 4,500 feet the lowland trees have disappeared +entirely. Subalpine species adapted to withstand the burden of deep snow +take their place. Mountain hemlock, alpine fir, and Engelmann spruce +grow singly and in scattered groups or form open groves alternating with +grassy parks and rocky ridges. The symmetrical outline of the slender +pyramidal crowns and rapidly tapering trunks of the spruce and alpine +fir trees that stand singly on the greensward of the open parks bring to +mind the closely trimmed cultivated evergreens that adorn city parks and +lawns. Their lower branches reach the ground and the tops terminate in +slender upright spires. + +As timber line is approached tree growth is confined to dwarfed and +flattened mountain hemlocks, alpine firs, and the white-bark pines +firmly rooted among the crevices of the rocks. + +The extreme limit of tree growth on Mount Rainier is 7,600 feet above +sea level. There is no well-defined timber line. Scattered clumps of low +stunted trees occur up to 7,000 feet. A few very small and flattened +mountain hemlocks grow above this elevation. A very large part of the +area above 4,500 feet consists of glaciers, talus slopes, barren rocky +peaks, and open parks. Basins at the heads of canyons in the high +mountains are usually treeless, on account of the great depth of snow +which accumulates in them during the winter. On the steep, smooth upper +inclines the snow banks frequently slip and form slides which acquire +momentum as they rush down the mountain side and break and carry away +large trees. Repeated snowslides in the same place keep the slopes +nonforested, and their track is marked by light green strips of brush +and herbage. + +The transition of the forest from its lowland to its extreme alpine type +is one of the most interesting features of a visit to the mountain. +Entering the park at the western boundary close to the Nisqually River +the road skirts the base of the lightly timbered spurs and passes into a +forest of large and old Douglas fir and western hemlock. Red cedars grow +along the streams that cross the road. Little yew trees and vine maples +mingle with the young conifers that form the undergrowth; the gloom of +the forest is occasionally relieved by the white bark of alders and the +smooth gray stems of the cottonwoods that grow on the sandy bank of the +Nisqually. After the road crosses the Rainier Fork, noble fir and +amabilis fir appear, but the Douglas fir and western hemlock are still +the prevailing species. + +Above Longmire Springs the noble and amabilis fir, mixed with western +hemlock, become the dominant type. The trees are shorter and the +branches heavier. Mountain ash and yellow cypress grow on the margin of +the mountain streams. Huckleberry bushes take the place of the taller +undergrowth of the valley. + +Above Narada Falls the forest is more open, and the trees are still +smaller. Mountain hemlock and alpine fir succeed the trees of the lower +slope. Little glades and mountain meadows are seen. They become larger +and more numerous and the traveler soon enters the open park of Paradise +Valley, in which are but scattered groves of trees. The same successive +altitudinal types are met in ascending to Moraine and Grand Parks by way +of the Carbon Valley, and in following the Mowich watershed, Crater +Lake, and Spray Park routes. + +Approaching the park from the east the routes pass through open western +yellow pine forests and western larch stands. Since Mount Rainier is +west of and apart from the summit line, these species which are peculiar +to the eastern slope are not found within the limits of the park. + + + + +EFFECTS OF FIRE. + +[Illustration: FIG. 1.--Whitened spectral monuments of a former forest +which was swept by a severe forest fire in 1885. Taken along the road to +Camp of the Clouds at an altitude of 5,500 feet. + +Photograph by A.H. Barnes.] + + +Notwithstanding the shortness of the summer season at high altitudes, +the subalpine forests in some parts of the park have suffered severely +from fire (fig. 1). The bare white trunks of fire-killed amabilis and +alpine firs bear witness to numerous fires which occurred from time to +time before the regulations governing the park went into effect. The +little resin pockets in the bark of these trees blaze fiercely for a +short time and the heat separates the bark from the trunk. In this way +the tree is killed, although the naked trunk is left untouched by fire. +The destruction of the alpine forest in this way is often erroneously +attributed to disease or to the depredations of insects. + +There has been little apparent change in the alpine burns within the +last 30 years. Reforestation at high altitudes is extremely slow. The +seed production is rather scanty and the ground conditions are not +favorable for its reproduction. It will take more than one century for +nature to replace the beautiful groves which have been destroyed by the +carelessness of the first visitors to the mountain. + +At low elevations the forest recovers more rapidly from the effects of +fire. Between the subalpine areas and the river valleys there are +several large ancient burns which are partly reforested. The most +extensive of these tracts is the Muddy Fork burn. It is crossed by the +Stevens Canyon Trail from Reflection Lakes through the Ohanopecosh Hot +Springs. This burn includes an area of 20 square miles in the park and +extends north nearly to the glaciers and south for several miles beyond +the park boundary nearly to the main Cowlitz River. The open sunlit +spaces and wide outlooks afforded by reforested tracts of this character +present a strong contrast to the deep shades and dim vistas of the +primitive forest. On the whole they have a cheerful and pleasing +appearance, very different from the sad, desolate aspect of the alpine +burns which less kindly conditions of climate and exposure have kept +from reforestation. + +The original forest was fire killed many years before the coming of the +white man. A few naked and weather beaten stubs are still standing. Only +the larger of the fallen trunks remain, and these are rotten except for +a few seasoned and weatherworn shells. The second growth is of all ages, +from seedlings to trees 12 to 14 inches in diameter. Vine maple, willow, +and mountain ash have sprung up along the streams and the hillsides are +covered with huckleberry bushes and a variety of grasses and flowering +plants. + +Similar old burns are found on the ridge between Huckleberry Creek and +White River, in the northeastern part of the park, and on the ridge +between Tahoma Creek and Kautz Creek below Henrys Hunting Ground. + +The old burns in the middle altitudes of the park occupy regions once +frequented by the Klickitat Indians. Every summer parties of hunters and +berry pickers from the sagebrush plains crossed the Cascades with their +horses. They followed the high divides and open summits of the secondary +ridges until they came around to the open parks about Mount Rainier +where they turned their horses out to graze and made their summer camp. +The woman picked huckleberries and the men hunted deer and goats. They +made great fires to dry their berries and kindled smudges to protect +their horses from flies. It was also their custom to systematically set +out fires as they returned. Burning made the country better for the +Indians. The fires kept down the brush and made it more accessible. Deer +could be more easily seen and tracked and the huckleberry patches spread +more widely over the hills. + +No considerable part of the lower forests of the park has been burned. +The principal danger is from lightning. However, few of the trees struck +are ignited and these fires are usually extinguished by the rain. On +account of the coolness of the air and its greater humidity the fire +danger in the forests on the lower slopes of Mount Rainier seems much +less than it is in corresponding situations in the main range of the +Cascades. + + + + +AGE AND DIMENSIONS OF TREES. + + +Trees grow more rapidly at low altitudes than at higher and cooler +elevations. Under similar conditions some species increase in size +faster than others, but the rate of growth depends principally upon +environment. The average increase at the stump in valley land is about 1 +inch in 6 years. A Douglas fir growing along the stage road between the +park boundary and Longmire's, at the age of 90 to 120 years may have a +breast diameter of 20 inches and yield 700 feet of saw timber. But many +of the trees of this size may be much older on account of having grown +in the shade or under other adverse conditions. The trees between 200 +and 300 years of age are often 40 to 50 inches in diameter and may yield +an average of from 2,700 to 5,500 board feet. The largest Douglas firs +are sometimes over 400 years old and 60 to 70 inches in diameter. Such +trees when sound will produce over 8,000 feet of lumber. + +The western red cedar has a shorter and more tapering trunk and its +volume in board feet is proportionally smaller. A tree 50 inches in +diameter and 175 feet high contains about 3,400 board feet. + +The size of the trees decreases rapidly at higher elevations. In the +subalpine forest the annual growth is very small. At elevations of 6,000 +feet the white-bark pine requires 200 years to attain a diameter of 10 +or 12 inches. The annual rings are so close together that they can not +be distinguished without a magnifying glass. + + + + +DESCRIPTIONS OF SPECIES. + + +DOUGLAS FIR (PSEUDOTSUGA TAXIFOLIA). + +The Douglas fir (figs. 2, 3, 4, and 5) is the best known and the most +important timber tree of western North America. It is found from +British Columbia southward to northern Mexico. The finest forests occur +in Oregon and Washington at low elevations. The Douglas fir is common in +the park up to 3,500 feet, sometimes in nearly pure stands, but more +often mixed with other species. It grows in all situations. In the +higher mountains it prefers warm southern exposures and is seldom found +on wind-swept ridges. It seeds annually, but most profusely at intervals +three or four years apart. The red squirrels gather and store large +quantities of the cones in order to provide a supply of the seeds for +their winter rations. The growth of the young tree is very rapid. As the +tree becomes older the rate of growth varies with the situation and the +character of the soil so that the size does not closely determine the +age of the tree. + +[Illustration: FIG. 2.--Douglas fir (_Pseudotsuga taxifolia_).] + +The Douglas fir is a long-lived tree, and specimens are occasionally +found 250 to 270 feet high and over 8 feet in diameter and between 400 +and 500 years in age. It reaches its greatest height and most perfect +proportions in mature even-age stands growing on fairly moist +well-drained bench lands. Under these conditions it is a very tall and +beautiful tree. The trunk is straight, round, and free from branches for +two-thirds of its height and tapers gently to the crown. The dark-brown +deep-furrowed bark is 5 to 10 inches thick at the base of the tree. + +The Douglas fir ranks first among the trees of the Pacific slope in +importance for the production of lumber. It is often sold under the name +of Oregon pine. Lumber dealers class the coarse-grained reddish wood +produced by the young growth in open forests as "red fir." The older +growth produced when the forest is more dense is a finer grained and +more valuable wood, sold under the name of "yellow fir." + +[Illustration: FIG. 3.--Douglas fir (_Pseudotsuga taxifolia_).] + +The Douglas fir is used for nearly all purposes where durability, +strength, and hardness are desirable. It is made into dimension timbers, +lumber, flooring, and is particularly adapted for masts and spars. The +lumber is shipped by rail to the Middle Western States. The foreign +cargo shipments are made to all parts of the world. The greatest amount +goes to Australia, the west and east coasts of South America, China, the +United Kingdom, and Europe, Japan, and the South Sea Islands. Coastwise +shipments are made to California, Alaska, and Panama. Large quantities +of the seed of this tree are sent to Europe, where the Douglas fir is +grown for timber and for ornament. + + +WESTERN RED CEDAR (THUJA PLICATA.)[1] + +[Illustration: FIG. 4.--Douglas fir (_Pseudotsuga taxifolia_).] + +The western red cedar (title page and fig. 5) ranges from south-eastern +Alaska to northern California. It is a common tree in the park. It +occurs in patches along the river bottoms where the flat scalelike +foliage is conspicuous among the needle-shaped leaves of the hemlock and +fir. The bark is fibrous in appearance and may be readily separated into +long strips. The trunks of the older trees are swelled and irregularly +fluted at the base. The leaves are fragrant and the wood has a pleasing +aromatic odor. Nearly all the large trees are hollow at the butt. The +roots spread laterally to a great distance, but extend only for a short +distance below the surface of the ground. The tree is easily overthrown +by the wind and usually grows in sheltered localities. On account of the +thinness of the bark it is easily killed by fire. + +[Illustration: FIG. 5.--Two big Douglas firs and a western red cedar (on +the left) along the road up the Nisqually Valley, Mount Rainier National +Park. + +Photograph by A.H. Denman.] + +The red cedar flourishes on fertile and well-watered soils near sea +level, where it grows to an enormous size. In the park it is a smaller +tree, 150 to 170 feet high and rarely more than 4 or 5 feet through +above the swollen butt. It grows occasionally up to an altitude of 4,000 +feet, but is a small and insignificant tree in the high mountains. + +In the sapling stage the red cedar grows rapidly. The mature tree +increases very slowly in size. It exceeds all other trees in the +Cascades in longevity. Individuals more than 500 years old are not +uncommon and there is a well-authenticated instance where the annual +rings indicated a growth of more than 1,100 years. + +While the red cedar forms no great proportion of the forest of the +Pacific Northwest, it is peculiarly valuable to the pioneer on account +of the durability of the wood and the ease with which it can be split +into boards, shakes, and planking. The early settlers used cedar split +by hand as a substitute for sawn lumber in flooring and finishing their +cabins and for the tables and shelves with which they were furnished. +The Indians hollowed the great trunks with fire and made them into +canoes, some of which were large and seaworthy enough to be used on the +Sound and in making voyages along the coast. They wove the fibrous roots +into baskets that carried water and plaited the bark into matting. The +wood of the red cedar is reddish brown in color. It is soft, light, and +very brittle, but very durable. It is extensively used for shingles, the +manufacture of which forms one of the important industries of the State. +The clear logs are sawed into lumber used for siding, interior and +exterior finish, moldings, tank stock, and similar purposes. Common logs +are utilized for shingles. In many localities the entire tree is cut +into 52-inch bolts, which are hauled to the mills or floated to them +down the streams. + +The western red cedar makes excellent posts and rails for farm fences. +The young trees are used for telegraph and telephone poles. + + +WESTERN HEMLOCK (TSUGA HETEROPHYLLA). + +Next to the Douglas fir the western hemlock is the most abundant tree in +the forests of Oregon and Washington. It occurs from Alaska southward to +northern California. About Mount Rainier it is found up to an altitude +of 5,000 feet. In the river valleys in moist situations it is a large +tree, sometimes reaching a height of 250 feet and a diameter of 5 feet. +On the high ridges it is stunted. It grows best on moist deep soils in +dense forests, but thrives under almost all conditions of soil and +exposure if provided with plenty of moisture. + +Western hemlock (figs. 6 and 7) is usually associated with Douglas fir +and red cedar, but sometimes forms a forest of nearly pure growth. The +hemlock produces abundant seed each year, although it is more prolific +at irregular intervals. The seeds germinate readily on decayed moss and +rotten wood as well as upon the mineral soil. Seedlings frequently grow +on fallen logs and extend their vigorous roots around the side until +they reach the ground and become firmly anchored in it. Young hemlocks +thrive in the shade. On logged-off areas which have not been burned over +and which are partially shaded by uncut trees, the reproduction of +hemlock springs up, to the exclusion of the more valuable Douglas fir. + +[Illustration: FIG. 6.--The lower slope forest, near Longmire Springs, +altitude 3,000 feet, here composed largely of western hemlock (_Tsuga +heterophylla_); the tree on the extreme left is a Douglas fir +(_Pseudotsuga taxifolia_). + +Photograph by A.H. Barnes.] + +The hemlock is long lived and grows slowly. The largest trees are from +200 to 500 years old and are usually hollow-hearted. The bark is thin +and the tree very easily killed by ground fire. The wood of the hemlock +is tough, light, and straight grained. It is not as durable as the +Douglas fir and decays rapidly when exposed to the weather. The clear +lumber is suitable for interior finish. The wood is also used for +flooring, joists, lath, and paper pulp. The common and rough lumber does +not find a ready market, except for the limited amount used in temporary +construction. The western hemlock is, however, superior to the eastern +hemlock, and its value will probably be recognized as its usefulness for +many purposes becomes better known. + + +WESTERN WHITE PINE (PINUS MONTICOLA). + +[Illustration: FIG. 7.--A forest of Douglas fir, with an understory of +western hemlock, on the lower slopes of the hills, Mount Rainier +National Park. + +Photograph by A.H. Denman.] + +The western white pine (fig. 8) is found from southern Alaska to +northern California. In the park it occurs occasionally up to 4,000 +feet. It usually grows on level benches and gentle slopes associated +with Douglas fir, western hemlock, and noble and amabilis fir. It +reaches its best development at elevations of from 3,000 to 3,500 feet, +where it attains a height of 150 feet and a diameter of 40 inches. The +shaft is straight, cylindrical, and clear of limbs. It bears a small, +narrow crown of drooping branches. In open areas, where it is exposed to +sunlight, its mode of growth is wholly different. The trunk is short, +rapidly tapering, and bears wide-spreading branches nearly to the +ground. At high elevations the western white pine is very short and +stunted. + +[Illustration: FIG. 8.--Western white pine (_Pinus monticola_). + +Diameter 24 inches, height 50 feet.] + +Although the western white pine is not a common tree in the park, it is +often noticed on account of its abundance of slender, pendant cones, 6 +to 10 inches long. They mature every two years and shed their seed early +in September. The seed are provided with long wings and are often +carried by the wind for a great distance from the parent tree. + +The wood is light, soft, free from pitch, and the most valuable of any +of the pines of the Cascades. It is used for interior finish, pattern +making, and other purposes. The supply of this tree is so limited that +it is not of great commercial importance in the Mount Rainier region. + + +AMABILIS FIR (ABIES AMABILIS).[2] + +Amabilis fir (figs. 9 and 10) ranges from southern Alaska to Oregon. It +is abundant in the park at elevations from 2,500 to 5,000 feet on level +bench lands, and gentle slopes with a northern exposure. It is rarely +found in unmixed stands, but is usually associated with western hemlock, +Douglas fir, and noble fir. The largest trees are 150 to 180 feet high +and 3 to 5 feet in diameter. In dense forests the stem is free from +branches for 50 to 100 feet. + +[Illustration: FIG. 9.--Amabilis fir (_Abies amabilis_).] + +At altitudes over 4,000 feet, small amabilis firs often occur in +clusters and open groves. The trunk is covered with branches which grow +to the ground, turning downward and outward in long graceful curves, +admirably adapted to withstand the pressure of the frozen snow. The +foliage is a deep and brilliant green, forming a strong contrast to the +dark-purple cones. The seeds ripen each year early in October. Like the +seed of the other alpine species of trees that grow in the cold and +humid climate of the high Cascades, they soon lose their vitality when +stored in dry places. The amabilis fir is grown in Europe as an +ornamental tree. Under cultivation it loses much of the natural grace +and beauty which it acquired in adapting itself to the deep snows and +long winters of its native environment. + +[Illustration: FIG. 10.--The forests of western hemlock, amabilis fir, +and other species, on the middle slopes of the mountains, along the +Crater Lake trail, Mount Rainier National Park. + +Photograph by Geo. O. Ceasar.] + +The bark is thin and the tree is easily killed by fire. The wood is +straw colored, compact, and straight grained. It is not strong and +splits easily. It is sold to some extent under the name of larch or +mixed with inferior grades of fir and hemlock. The lumber is of little +value commercially. + + +NOBLE FIR (ABIES NOBILIS). + +The noble fir (figs. 11 and 12) is a common mountain tree in the western +parts of Washington and Oregon. Like amabilis fir, it is usually called +larch by lumbermen. About Mount Rainier it grows at elevations of from +3,500 to 5,000 feet in dense stands associated with amabilis fir, +western hemlock, and Douglas fir. The noble fir avoids steep side hills +and exposed situations. In moist soils on flats and gentle slopes it +often reaches a height of from 150 to 200 feet. The tall and upright +trunk supports a rounded crown of bluish green foliage, which is very +noticeable among the purer green leaves of its associates. The branches +are short, thick, and crowded with stiff, flattened leaves, which turn +upward and outward. The light-green bract-covered cones are sometimes 6 +inches long and nearly 3 inches thick. They ripen early in September. +Seed is borne every year, although in some seasons it is much more +abundant than in others. + +[Illustration: FIG. 11.--Noble fir (_Abies nobilis_).] + +[Illustration: FIG. 12.--Noble fir (_Abies nobilis_), 6 feet in +diameter.] + +The wood is strong, close grained, and elastic. It is used for lumber +and particularly for inside finishing. The noble fir is a slow-growing +and long-lived tree. Old trees in mixed forests are easily distinguished +from the associated species by the ashy-brown outer bark broken into +large irregular plates. + + +ALPINE FIR (ABIES LASIOCARPA).[3] + +[Illustration: FIG. 13.--A cluster of Alpine firs (_Abies lasiocarpa_), +whose spire-shaped crowns are characteristic, at 5,500 feet altitude, in +Cowlitz Park, Mount Rainier National Park. + +Photograph by A.H. Barnes.] + +The alpine fir (fig. 13) ranges from Alaska to New Mexico. It is a +common tree in the park at elevations above 4,500 feet. It is a tree of +the high mountains and with the white bark pine and the mountain +hemlock, is found up to the limit of arborescent life. It demands +moisture and is generally restricted to regions of deep snowfall. + +The alpine fir occurs in unmixed stands, but is often associated with +the mountain hemlock. At the lower levels of its range it is a +fair-sized tree 50 or 60 feet high. The crown of deep-green foliage is +broad at the base and tapers to the top, where it terminates in a +slender, pointed tip. At its upper limit it becomes a stunted shrub, +with wide extended branches resting on the ground. + +The alpine fir bears upright clusters of deep-purple cones. It seeds +sparingly each year. The seasons of heavy seed production occur at +intervals of three or four years. The wood is soft and splits easily. It +is of no commercial value. The tree is easily killed by fire, which +blisters the thin bark and frequently springs into the drooping lower +branches. + + +GRAND FIR (ABIES GRANDIS.)[4] + +The grand fir (fig. 14), like several other species, is generally given +the name of white fir on account of its smooth, light-colored bark. It +is a common tree in the river bottoms from British Columbia south to +northern California. In the Mount Rainier National Park it occurs up to +4,000 feet. The grand fir is a moisture-loving tree and is usually found +firmly rooted in deep alluvial bottom lands along the banks of streams. +With the Douglas fir, hemlock, and red cedar it forms the dense forest +characteristic of the lower mountain valleys. + +In favorable conditions the grand fir grows to a height of from 100 to +200 feet and is a noble and stately tree. The trunk tapers rapidly and +bears a rounded pyramidal crown. In dense forests the trunk is clear for +half its height, but where the trees stand in the open it carries its +branches nearly to the ground. The leaves are a bright and shining +green. The large light-green cones mature early in the fall. The wood is +soft and very heavy before it is seasoned. It rots in a very short time +when laid on the ground. When dry it is white, coarse-grained, light, +and odorous. It is used for interior finish and for crates and packing +boxes, but is of little value commercially. + + +ENGELMANN SPRUCE (PICEA ENGELMANNI). + +The Engelmann spruce (fig. 15) is a mountain tree ranging from British +Columbia to Arizona and New Mexico. It is common along the summit and on +the east side of the Cascade Range and occurs on the northeastern and +eastern slopes of Mount Rainier at elevations of from 3,500 to 6,000 +feet. + +This tree requires a moist soil and prefers cool northern exposures. Up +to 5,000 feet it commonly grows in sheltered basins at the head of +canyons and in stream valleys. At its upper limits it is common on flats +and depressions and about lakes on level summits. It avoids steep +mountain sides and exposed situations. + +[Illustration: FIG. 14.--Grand fir (_Abies grandis_).] + +The Engelmann spruce is easily distinguished from its associates by its +stiff, bluish-green pointed leaves, which prick the hand when they are +grasped. In the mountain parks it is a handsome tree 50 to 60 feet high. +When it stands apart from other trees the lower branches are thick and +long and extend to the ground. The crown is very broad at the base, but +narrow and spirelike at the top. The Engelmann spruce reaches its best +development at low elevations, where it often grows in dense, pure +stands. Under these conditions it reaches a height of 100 feet. The bole +is straight and free from limbs and the top is short and compact. + +[Illustration: FIG. 15.--Engelmann spruce (_Picea engelmanni_).] + +The young cones are massed in upright green and purple clusters at the +tips of the upper branches. They are notable for the purity and +brilliance of their coloring. As they mature they become pendant and +fade to a light brown. The seed is produced in abundance nearly every +year, although small and seedling trees are not usually numerous. + +The wood is soft, white, compact, and even grained. It is free from +pitch and odor. It is valuable for boxing, cooperage, and certain kinds +of finish. It is also an excellent material for the tops of violins and +other stringed instruments. The Engelmann spruce is, however, of little +importance as a timber tree on account of its scarcity and the scattered +stands in which it grows. It is a long-lived tree unless attacked by +fire, to which it is very vulnerable. + +[Illustration: FIG. 16.--A group of yellow cypresses (_Chamaecyparis +nootkatensis_) on the high slopes of Mount Rainier National Park, +altitude about 6,000 feet. + +Photograph by A.H. Barnes.] + + +YELLOW CYPRESS (CHAMAECYPARIS NOOTKATENSIS). + +Yellow cypress (fig. 16) ranges from the seacoast of southern Alaska +south to the mountains of Washington and Oregon. It occurs in the park +up to the elevation of 7,000 feet. It is common on northern exposures, +along streams, and in basins at the head of canyons. It also grows on +crests and ridges, where the frequent showers and fogs supply the +moisture which it demands. In sheltered localities it grows to a height +of 75 or 80 feet, but it is commonly a small tree with, a bent and +twisted stem, which, with its pendulous branches, presents a somewhat +scrubby appearance. The foliage is green, sometimes with a bluish tinge. +It resembles that of the common western red cedar, but the leaves are +sharper, more pointed, and rougher to handle. The small, rounded, +inconspicuous cones are produced somewhat sparingly. The bark of the +young tree is red. On the mature tree it becomes gray and fibrous. The +wood is yellow, close grained, and aromatic. Unlike that of the western +red cedar, the trunk is usually sound to the center. The wood is used +for boat building and cabinetwork. It is very durable. + +The yellow cypress grows very slowly, particularly at high elevations. +The number of annual rings on trees 15 to 20 inches in diameter indicate +that they are over 200 years old. + + +LODGEPOLE PINE (PINUS CONTORTA). + +Lodgepole pine (fig. 17) is widely distributed from Alaska to Lower +California and eastward through the Rockies to Dakota and Colorado. It +occurs sparingly in the park up to 5,000 feet above sea level. It adapts +itself easily to the different conditions of soil, moisture, and +exposure. + +[Illustration: FIG. 17.--Lodgepole pine (_Pinus contorta_), 60 inches in +diameter.] + +This tree varies greatly in the different regions where it is found. +About Mount Rainier it does not often exceed 20 to 40 feet in height +and is often a much smaller tree. It produces cones at the age of 5 to 7 +years. The foliage is a yellowish green. At high elevations the leaves +have a peculiar whorled appearance which gives it a different aspect +from that of the other pines. The short, heavily limbed trunk bears no +resemblance to the tall and slender shaft of the lodgepole pine of the +Rocky Mountains. The root system is shallow and the tree is easily fire +killed. The wood of the variety which grows in the park is of no +commercial value. + +[Illustration: FIG. 18.--The feathery foliage of mountain hemlock +(_Tsuga mertensiana_), Grand Park, Mount Rainier National Park. + +Photograph by A.H. Denman.] + + +MOUNTAIN HEMLOCK (TSUGA MERTENSIANA). + +The mountain hemlock (figs. 18, 19, and 20) is found on the Pacific +coast from the Sierras of California to the northern part of Alaska +where it grows at sea level. On Mount Rainier it occurs at altitudes of +from 3,500 to 7,500 feet. It forms dense forests under 4,500 feet, where +it is often a fair-sized tree 50 to 90 feet high. With the ascent of the +mountain it diminishes in height and the branches become gnarled and +twisted. Near timber line the trunk is dwarfed and bent at the base and +the crown becomes a flattened mass of branches lying close to the ground +(fig. 20). + +[Illustration: FIG. 19.--Two solitary mountain hemlocks (_Tsuga +mertensiana_), Spray Park, Mount Rainier National Park. + +Photograph by Geo. O. Ceasar.] + +The mountain hemlock is abundant on high, rocky ridges, but the best +stands are on cool, moist soil at the heads of ravines, on flats, and on +gentle slopes with a northern exposure. + +This tree seeds every year. In good seed years the upper branches are +laden with a profusion of beautiful, deep-purple cones, often in such +abundance as to bend down the branchlets with their weight. The +reproduction is slow. In the high mountains the trees are buried in snow +from October to late in June, and the growing season is very short. + + +WHITE-BARK PINE (PINUS ALBICAULIS). + +[Illustration: FIG. 20.--A gnarled, wind-swept mountain hemlock (_Tsuga +mertensiana_), near the upper limits of tree growth, Spray Park, Mount +Rainier National Park. + +Photograph by A.H. Denman.] + +The white-bark pine (fig. 21) grows close to timber line in the +mountains of the Pacific coast from British Columbia to southern +California. In the Canadian Rockies it extends north to the fifty-third +parallel. It is the most alpine of all the pines. Its lower limit on +Mount Rainier is about 5,000 feet above sea level. In sheltered places +where the soil is deep the trees are sometimes 30 to 40 feet high and 20 +inches in diameter. The trunks are free from limbs for 8 or 10 feet. The +outer bark, from which the tree derives its name, consists of thin, +light-gray scales. + +As the white-bark pine advances up the mountain its habit changes +rapidly. The stem shortens and becomes gnarled and twisted. The tough, +flexible branches reach the ground and spread over it to a great +distance from the tree. On rocky summits and the bleak crests of +wind-swept ridges the twisted trunk and branches are quite prostrate and +the crown is a dense flattened mass of foliage. + +The roots of the tree are deep, long, and tenacious. They spread wide +and deep and cling so firmly to the rocks that the tree is rarely +overthrown by the violent winds that sweep over the mountain. + +[Illustration: FIG. 21.--A white-bark pine (_Pinus albicaulis_) in its +characteristic mountain habitat, Mount Rainier National Park. + +Photograph by A.H. Denman.] + +The thick, purple cones require two years to mature. They ripen early in +September and produce chocolate-brown seeds a little larger than a grain +of corn. They are much relished by the Klickitat Indians, who go to +considerable pains to secure them. The wood is close grained and +resinous. It makes excellent fuel for the camp fires of sheep herders +and mountain travelers. + + +WESTERN YEW (TAXUS BREVIFOLIA).[5] + +The western yew is found from southern Alaska to northern California. It +occurs in the park up to 4,000 feet, growing in rich, gravelly soil on +moist flats and benches and in deep ravines. It is a small branching +tree, rarely over 20 feet high. The bark is purple or reddish brown. The +branches extend almost to the ground. It bears a small, bright, +amber-red berry. + +The dark-brown or red heartwood is very tough, hard and heavy. It takes +a fine polish and is used for fancy cabinetwork. The Indians use it for +spear handles, bows, and fishhooks. + +[Illustration: FIG. 22.--Broadleaf maple (_Acer macrophyllum_).] + + +DECIDUOUS TREES. + +The silva of the Western Cascades is rich in evergreens remarkable for +their size and beauty. The deciduous trees are few and insignificant. +The forests of the park are almost wholly coniferous. Vine maple and +willow are found as undergrowth. On the margins of rivers there are +occasional groves of alders and cottonwoods. The lighter hues of the +branching trunks and the changing tints of the foliage in these patches +of broad-leaved woodland present a pleasing diversity to the evergreen +forest. + +Broadleaf maple (_Acer macrophyllum_) (fig. 22), the largest of the +Pacific coast maples, ranges from Alaska to southern California. Near +sea level it often attains a height of 50 or 60 feet. In the park it is +a short-stemmed, branching tree, occasionally found on the borders of +streams. It grows at elevations under 3,000 feet. + +[Illustration: FIG. 23.--Vine maple (_Acer circinatum_).] + +Vine maple (_Acer circinatum_) (fig. 23) is abundant from British +Columbia to northern California. On rich river bottoms it is sometimes +15 to 20 feet high and 6 inches in diameter. In the park it is usually a +bush or low shrub with a bent and curiously crooked stem, growing along +streams and as undergrowth in the forest. It is very common up to 3,000 +feet. In autumn the leaves are a bright scarlet. The wood is tough and +elastic and makes a hot and lasting fire. + +[Illustration: FIG. 24.--Red alder (_Alnus oregona_).] + +[Illustration: FIG. 25.--Black cottonwood (_Populus trichocarpa_).] + +Red alder (_Alnus oregona_) (fig. 24) occurs from Alaska to southern +California. It is common about Mount Rainier, in river bottoms, on the +banks of large streams, and in swampy places. It usually grows to a +height of 30 or 40 feet. The bark varies from nearly white to light +gray. It is the most abundant of all the deciduous trees in the park. + +Black cottonwood (_Populus trichocarpa_) (fig. 25) is common from Alaska +to southern California. It is occasionally found in the park up to 4,000 +feet. It grows along streams and on sandy river bottoms often associated +with the alder. The leaves are almost always in motion, very gentle +winds being sufficient to make them twinkle and turn. + +The wood is soft, but tough and compact. It is used for staves, +woodenware, wood pulp, trunks, barrels, and for drawer bottoms. + + +FOOTNOTES + +[1] This species is known as arbor vitæ in Glacier Park. + +[2] This species is known as silver fir in Crater Lake Park. + +[3] This species is known as balsam in Glacier and Yellowstone Parks. + +[4] This species is known as silver fir in Yellowstone and Glacier +Parks. + +[5] This species is known as Oregon yew in Crater Lake National Park and +as yew in Yellowstone and Glacier Parks. + + + + +INDEX TO SPECIES DESCRIBED. + +[Roman numerals indicate pages containing descriptions; italic numerals +indicate pages containing illustrations.] + + + _Abies amabilis_ 15-16, _15_, _16_ + _grandis_ 20, _21_ + _lasiocarpa_ 19-20, _19_ + _nobilis_ 17-19, _17_, _18_ + + _Acer circinatum_ 30, _30_ + _macrophyllum_ 29, _29_ + + Alder, red (_Alnus oregona_) 30, _31_ + + _Alnus oregona_ 30, _31_ + + Alpine fir (_Abies lasiocarpa_) 19-20, _19_ + + Amabilis fir (_Abies amabilis_) 15-16, _15_, _16_ + + Arbor vitæ. _See_ Western red cedar. + + + Balsam. _See_ Alpine fir. + + Black cottonwood (_Populus trichocarpa_) 30-32, _31_ + + Broadleaf maple (_Acer macrophyllum_) 29, _29_ + + + Cedar, western red (_Thuja plicata_) 9-11, _10_ + + _Chamaecyparis nootkatensis_ 23-24, _23_ + + Cottonwood, black (_Populus trichocarpa_) 30-32, _31_ + + Cypress, yellow (_Chamaecyparis nootkatensis_) 23-24, _23_ + + + Douglas fir (_Pseudotsuga taxifolia_) 6-8, _7_, _8_, _9_, _10_, + _12_, _13_ + + + Engelmann spruce (_Picea engelmanni_) 20-23, _22_ + + + Fir, alpine (_Abies lasiocarpa_) 19-20, _19_ + amabilis (_Abies amabilis_) 15-16, _15_, _16_ + Douglas (_Pseudotsuga taxifolia_) 6-8, _7_, _8_, _9_, _10_, + _12_, _13_ + grand (_Abies grandis_) 20, _21_ + noble (_Abies nobilis_) 17-19, _17_, _18_ + silver. _See_ Fir, amabilis; Fir, grand. + + + Grand fir (_Abies grandis_) 20, _21_ + + + Hemlock, mountain (_Tsuga mertensiana_) 25-27, _25_, _26_, _27_ + western (_Tsuga heterophylla_) 11-13, _12_, _13_, _16_ + + + Larch. _See_ Noble fir; Amabilis fir. + + Lodgepole pine (_Pinus contorta_) 24-25, _24_ + + + Maple, broadleaf (_Acer macrophyllum_) 29, _29_ + vine (_Acer circinatum_) 30, _30_ + + Mountain hemlock (_Tsuga mertensiana_) 25-27, _25_, _26_, _27_ + + + Noble fir (_Abies nobilis_) 17-19, _17_, _18_ + + + Oregon yew. _See_ Western yew. + + + _Picea engelmanni_ 20-23, _22_ + + Pine, lodgepole (_Pinus contorta_) 24-25, _24_ + western white (_Pinus monticola_) 13-15, _14_ + white-bark (_Pinus albicaulis_) 27-28, _28_ + + _Pinus albicaulis_ 27-28, _28_ + _contorta_ 24-25, _24_ + _monticola_ 13-15, _14_ + + _Populus trichocarpa_ 30-32, _31_ + + _Pseudotsuga taxifolia_ 6-8, _7_, _8_, _9_, _10_, _12_, _13_ + + + Red alder (_Alnus oregona_) 30, _31_ + cedar, western (_Thuja plicata_) 9-11, _10_ + + + Silver fir. _See_ Amabilis fir; Grand fir. + + Spruce, Engelmann (_Picea engelmanni_) 20-23, _22_ + + + _Taxus brevifolia_ 28-29 + + _Thuja plicata_ 9-11, _10_ + + _Tsuga heterophylla_ 11-13, _12_, _13_, _16_ + _mertensiana_ 25-27, _25_, _26_, _27_ + + + Vine maple (_Acer circinatum_) 30, _30_ + + + Western hemlock (_Tsuga heterophylla_) 11-13, _12_, _13_, _16_ + red cedar (_Thuja plicata_) 9-11, _10_ + white pine (_Pinus monticola_) 13-15, _14_ + yew (_Taxus brevifolia_) 28-29 + + White-bark pine (_Pinus albicaulis_) 27-28, _28_ + + White pine, western (_Pinus monticola_) 13-15, _14_ + + + Yellow cypress (_Chamaecyparis nootkatensis_) 23-24, _23_ + + Yew, Oregon. _See_ Yew, western. + western (_Taxus brevifolia_) 28-29 + + + + + +End of the Project Gutenberg EBook of The Forests of Mount Rainier National +Park, by Grenville F. 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Allen. + </title> + <style type="text/css"> +<!-- + p { + margin-top : 0.75em; + text-align : justify; + margin-bottom : 0.75em; + text-indent : 1.25em; + line-height : 130%; + } + + h1 { + text-align : center; + clear : both; + font-size : 2.1em; + font-weight : normal; + } + + h2 { + text-align : center; + clear : both; + font-size : 1.4em; + font-weight : normal; + } + + h3 { + text-align : center; + clear : both; + font-size : 1.2em; + font-weight : normal; + } + + h4 { + text-align : center; + clear : both; + font-size : 0.9em; + font-weight : normal; + } + + hr { + width : 50%; + margin-top : 2em; + margin-bottom : 2em; + margin-left : auto; + margin-right : auto; + clear : both; + } + + body { + margin-left : 10%; + margin-right : 10%; + } + +.pagenum { + display : inline; + font-size : 0.8em; + text-align : right; + position : absolute; + right : 2%; + text-indent : 0; + padding : 1px 1px; + font-style : normal; + font-family : garamond, serif; + font-variant : normal; + font-weight : normal; + text-decoration : none; + color : #000; + background-color : #ccff66; + } + + .center { + text-align : center; + text-indent : 0; + } + + .smcap { + font-variant : small-caps; + } + + .noin { + text-indent : 0; + } + + .hang { + text-indent : -1.5em; + margin-left : 2em; + } + + .hang2 { + text-indent : -1.5em; + margin-left : 2em; + font-size : 90%; + } + + .blockquot { + margin-left : 5%; + margin-right : 10%; + font-size : 90%; + } + + .caption { + font-weight : normal; + font-size : 0.95em; + text-align: center; + + } + + .figcenter { + margin : auto; + text-align : left; + } + + .index { + margin-left: 5%; + margin-right: 10%; + } + + .footnotes {border: dashed 1px;} + .footnote {margin-left: 10%; margin-right: 10%; font-size: 0.9em;} + .footnote .label {position: absolute; right: 84%; text-align: right;} + .fnanchor {font-size: .8em; text-decoration: none;} + .tn {background-color: #EEE; padding: 0.5em 1em 0.5em 1em;} + +--> + </style> + </head> +<body> + + +<pre> + +The Project Gutenberg EBook of The Forests of Mount Rainier National Park, by +Grenville F. Allen + +This eBook is for the use of anyone anywhere at no cost and with +almost no restrictions whatsoever. You may copy it, give it away or +re-use it under the terms of the Project Gutenberg License included +with this eBook or online at www.gutenberg.org + + +Title: The Forests of Mount Rainier National Park + +Author: Grenville F. Allen + +Release Date: April 15, 2010 [EBook #31994] + +Language: English + +Character set encoding: ISO-8859-1 + +*** START OF THIS PROJECT GUTENBERG EBOOK FORESTS OF MT RAINIER NAT. PARK *** + + + + +Produced by Greg Bergquist and the Online Distributed +Proofreading Team at https://www.pgdp.net (This file was +produced from images generously made available by The +Internet Archive/American Libraries.) + + + + + + +</pre> + + +<div class="tn"> +<p class="center"><big><b>Transcriber’s Note</b></big></p> +<p class="center">The punctuation and spelling from the original text have been faithfully preserved.</p> +</div> + +<hr /> +<h1> +FORESTS OF MOUNT RAINIER<br /> +NATIONAL PARK</h1> + +<div class="figcenter" style="width: 500px;"><a name="title_page" id="title_page"></a> +<img src="images/i002.jpg" width="500" height="619" alt="title page" title="" /> +</div> + +<p class="center">DEPARTMENT OF THE INTERIOR<br /> +OFFICE OF THE SECRETARY<br /> +1916</p> + +<p class="center"><small>For sale by the Superintendent of Documents, Government Printing Office, Washington, D.C. Price, 20 cents.</small></p> + + + +<hr /> +<h3>PUBLICATIONS ON MOUNT RAINIER NATIONAL PARK SOLD BY<br /> +THE SUPERINTENDENT OF DOCUMENTS.</h3> + + +<p>Remittances for these publications should be by money order, payable to the +Superintendent of Documents, Government Printing Office, Washington, D.C., or +in cash. Checks and postage stamps can not be accepted.</p> + +<p class="hang">Features of the Flora of Mount Rainier National Park, by J.B. Flett. 1916. 48 +pages, including 40 illustrations. 25 cents.</p> + +<div class="blockquot"><p>Contains descriptions of the flowering trees and shrubs in the park.</p></div> + +<p class="hang">Mount Rainier and Its Glaciers, by F.E. Matthes. 1914. 48 pages, including 26 +illustrations. 15 cents.</p> + +<div class="blockquot"><p>Contains a general account of the glaciers of Mount Rainier and of the development of the valleys +and basins surrounding the peak.</p></div> + +<p class="hang">Panoramic view of Mount Rainier National Park, 20 by 19 inches, scale 1 mile to +the inch. 25 cents.</p> + + + +<hr /><p><span class='pagenum'><a name="Page_1" id="Page_1">[Pg 1]</a></span></p> +<h2>THE FORESTS OF MOUNT RAINIER NATIONAL PARK.</h2> + +<p class="center">By <span class="smcap">G.F. Allen</span>, <i>United States Forest Service</i>.</p> + + + + +<h3>GENERAL STATEMENT.</h3> + + +<p>The remarkable development of the forests about the base of +Mount Rainier results from climatic conditions peculiarly favorable +to tree growth. The winters are mild and short. The ocean winds +that pass through the gaps of the Coast Range are laden with +moisture which falls in the form of rain or snow on the west slope +of the Cascades. The trees are nourished by this moisture through +a long season of annual growth, and form an evergreen forest which +is, in some respects, the most remarkable in the world. This forest, +distinguished by the extraordinary size and beauty of the trees and +by the density of the stand, extends into the deep valleys of the rivers +which have their sources in the glaciers. On the dividing ridges and +in the upper stream basins the composition and character of the +forest change with the increasing severity of the climate.</p> + +<p>The distribution of the different species of trees according to the +intervals of altitude at which they occur separate the forests of the +Mount Rainier National Park into different types. The lines of separation +are to some extent also determined by complex conditions of +slope, exposure, and moisture. The successive forest belts are uniform +in the composition of their central areas, but blend and overlap +where they come together.</p> + +<p>The low valleys of the main and west forks of White River, of +the Carbon, the Mowich, the Nisqually, and the Ohanopecosh are +covered with a dense and somber forest of fir, hemlock, and cedar. +The trees, pushing upward for light, are very tall and free from +limbs for more than half their height. Their tops form a continuous +cover which the sunshine rarely penetrates, and on which +the light snows of early winter fall and melt, without reaching the +ground. Even in midsummer the light is soft and shaded, and the +air cool and humid. In the wintertime the young growth is sheltered +from wind and the severity of the cold is tempered by the protecting +mountain ranges. Saved from fire by the uniform dampness of the +air the trees grow until they decay and fall from old age. They are<span class='pagenum'><a name="Page_2" id="Page_2">[Pg 2]</a></span> +succeeded by the suppressed younger trees. The forest remains +mature, not uniformly sound and vigorous, yet not decreasing as a +whole in size and volume. Individuals perish, but the character of +the forest is constant. The deep alluvial soil covered with moss and +decayed vegetation nourishes a luxuriant tangled undergrowth of +vine maple, willow, and devil's-club. The forest floor is covered with +a deep layer of decayed vegetation and is encumbered with fallen +and mossy logs and upturned stumps. The explorer who leaves the +trails must be a strong and active man if he can carry his pack +6 or 8 miles in a long summer day.</p> + +<p>Ascending from the river bottoms to the lower slopes of the dividing +ridges the forest becomes more open and the trees are smaller. +Salal, Oregon grape, and huckleberry bushes take the place of the +taller undergrowth of the valleys. Up to 3,000 feet the Douglas fir +and the hemlock still are the dominant species. Above this altitude +new species are found intermingled with the trees typical of the lowland, +but forming a distinct forest type. The noble and amabilis +fir appear, sometimes growing in pure stands, but more often +associated with the Douglas fir and western hemlock at the lower +limits of the type, and with alpine fir and mountain hemlock at the +upper limit.</p> + +<p>Nearly all the trees of this type have deep and wide-spreading +roots which serve to hold in place the surface deposit of volcanic +pumice which covers the slopes of the mountain. Evidence afforded +by the after effects of forest fires in other parts of the Cascades +indicates that the destruction of the forest on the mountain sides is +followed by erosion. Heavy rains and the melting of the upper +snow banks by warm Chinook winds combine to produce a surface +run-off that denudes the steeper declivities down to the underlying +bedrock.</p> + +<p>At elevations above 4,500 feet the lowland trees have disappeared +entirely. Subalpine species adapted to withstand the burden of deep +snow take their place. Mountain hemlock, alpine fir, and Engelmann +spruce grow singly and in scattered groups or form open +groves alternating with grassy parks and rocky ridges. The symmetrical +outline of the slender pyramidal crowns and rapidly tapering +trunks of the spruce and alpine fir trees that stand singly on the +greensward of the open parks bring to mind the closely trimmed +cultivated evergreens that adorn city parks and lawns. Their lower +branches reach the ground and the tops terminate in slender upright +spires.</p> + +<p>As timber line is approached tree growth is confined to dwarfed +and flattened mountain hemlocks, alpine firs, and the white-bark +pines firmly rooted among the crevices of the rocks.</p> + +<p><span class='pagenum'><a name="Page_3" id="Page_3">[Pg 3]</a></span></p><p>The extreme limit of tree growth on Mount Rainier is 7,600 feet +above sea level. There is no well-defined timber line. Scattered +clumps of low stunted trees occur up to 7,000 feet. A few very small +and flattened mountain hemlocks grow above this elevation. A very +large part of the area above 4,500 feet consists of glaciers, talus +slopes, barren rocky peaks, and open parks. Basins at the heads of +canyons in the high mountains are usually treeless, on account of +the great depth of snow which accumulates in them during the +winter. On the steep, smooth upper inclines the snow banks frequently +slip and form slides which acquire momentum as they rush +down the mountain side and break and carry away large trees. Repeated +snowslides in the same place keep the slopes nonforested, and +their track is marked by light green strips of brush and herbage.</p> + +<p>The transition of the forest from its lowland to its extreme alpine +type is one of the most interesting features of a visit to the mountain. +Entering the park at the western boundary close to the Nisqually +River the road skirts the base of the lightly timbered spurs and +passes into a forest of large and old Douglas fir and western hemlock. +Red cedars grow along the streams that cross the road. Little yew +trees and vine maples mingle with the young conifers that form the +undergrowth; the gloom of the forest is occasionally relieved by the +white bark of alders and the smooth gray stems of the cottonwoods +that grow on the sandy bank of the Nisqually. After the road +crosses the Rainier Fork, noble fir and amabilis fir appear, but the +Douglas fir and western hemlock are still the prevailing species.</p> + +<p>Above Longmire Springs the noble and amabilis fir, mixed with +western hemlock, become the dominant type. The trees are shorter +and the branches heavier. Mountain ash and yellow cypress grow +on the margin of the mountain streams. Huckleberry bushes take +the place of the taller undergrowth of the valley.</p> + +<p>Above Narada Falls the forest is more open, and the trees are still +smaller. Mountain hemlock and alpine fir succeed the trees of the +lower slope. Little glades and mountain meadows are seen. They +become larger and more numerous and the traveler soon enters the +open park of Paradise Valley, in which are but scattered groves of +trees. The same successive altitudinal types are met in ascending to +Moraine and Grand Parks by way of the Carbon Valley, and in following +the Mowich watershed, Crater Lake, and Spray Park routes.</p> + +<p>Approaching the park from the east the routes pass through open +western yellow pine forests and western larch stands. Since Mount +Rainier is west of and apart from the summit line, these species +which are peculiar to the eastern slope are not found within the +limits of the park.</p> + + + +<hr /><p><span class='pagenum'><a name="Page_4" id="Page_4">[Pg 4]</a></span></p> +<h3>EFFECTS OF FIRE.</h3> + +<div class="figcenter" style="width: 500px;"><a name="Fig_1" id="Fig_1"></a> +<img src="images/i007.jpg" width="500" height="706" alt="Fig. 1." title="" /> +<div class="hang2"><span class="smcap">Fig. 1.</span>—Whitened spectral monuments of a former forest which was swept by +a severe forest fire in 1885. Taken along the road to Camp of the Clouds at +an altitude of 5,500 feet.<br /></div> + +<p class="center"><small>Photograph by A.H. Barnes.</small></p> +</div> + + +<p>Notwithstanding the shortness of the summer season at high altitudes, +the subalpine forests in some parts of the park have suffered +severely from fire (<a href="#Fig_1">fig. 1</a>). The bare white trunks of fire-killed +amabilis and alpine firs bear witness to numerous fires which occurred<span class='pagenum'><a name="Page_5" id="Page_5">[Pg 5]</a></span> +from time to time before the regulations governing the park +went into effect. The little resin pockets in the bark of these trees +blaze fiercely for a short time and the heat separates the bark from +the trunk. In this way the tree is killed, although the naked trunk +is left untouched by fire. The destruction of the alpine forest in +this way is often erroneously attributed to disease or to the depredations +of insects.</p> + +<p>There has been little apparent change in the alpine burns within +the last 30 years. Reforestation at high altitudes is extremely slow. +The seed production is rather scanty and the ground conditions are +not favorable for its reproduction. It will take more than one century +for nature to replace the beautiful groves which have been destroyed +by the carelessness of the first visitors to the mountain.</p> + +<p>At low elevations the forest recovers more rapidly from the effects +of fire. Between the subalpine areas and the river valleys there are +several large ancient burns which are partly reforested. The most +extensive of these tracts is the Muddy Fork burn. It is crossed by the +Stevens Canyon Trail from Reflection Lakes through the Ohanopecosh +Hot Springs. This burn includes an area of 20 square miles in +the park and extends north nearly to the glaciers and south for several +miles beyond the park boundary nearly to the main Cowlitz +River. The open sunlit spaces and wide outlooks afforded by reforested +tracts of this character present a strong contrast to the deep +shades and dim vistas of the primitive forest. On the whole they +have a cheerful and pleasing appearance, very different from the +sad, desolate aspect of the alpine burns which less kindly conditions +of climate and exposure have kept from reforestation.</p> + +<p>The original forest was fire killed many years before the coming +of the white man. A few naked and weather beaten stubs are still +standing. Only the larger of the fallen trunks remain, and these +are rotten except for a few seasoned and weatherworn shells. The +second growth is of all ages, from seedlings to trees 12 to 14 inches +in diameter. Vine maple, willow, and mountain ash have sprung up +along the streams and the hillsides are covered with huckleberry +bushes and a variety of grasses and flowering plants.</p> + +<p>Similar old burns are found on the ridge between Huckleberry +Creek and White River, in the northeastern part of the park, and +on the ridge between Tahoma Creek and Kautz Creek below Henrys +Hunting Ground.</p> + +<p>The old burns in the middle altitudes of the park occupy regions +once frequented by the Klickitat Indians. Every summer parties +of hunters and berry pickers from the sagebrush plains crossed the +Cascades with their horses. They followed the high divides and open +summits of the secondary ridges until they came around to the +open parks about Mount Rainier where they turned their horses out<span class='pagenum'><a name="Page_6" id="Page_6">[Pg 6]</a></span> +to graze and made their summer camp. The woman picked huckleberries +and the men hunted deer and goats. They made great fires +to dry their berries and kindled smudges to protect their horses from +flies. It was also their custom to systematically set out fires as they +returned. Burning made the country better for the Indians. The +fires kept down the brush and made it more accessible. Deer could +be more easily seen and tracked and the huckleberry patches spread +more widely over the hills.</p> + +<p>No considerable part of the lower forests of the park has been +burned. The principal danger is from lightning. However, few of +the trees struck are ignited and these fires are usually extinguished +by the rain. On account of the coolness of the air and its greater +humidity the fire danger in the forests on the lower slopes of Mount +Rainier seems much less than it is in corresponding situations in the +main range of the Cascades.</p> + + + +<hr /> +<h3>AGE AND DIMENSIONS OF TREES.</h3> + + +<p>Trees grow more rapidly at low altitudes than at higher and +cooler elevations. Under similar conditions some species increase in +size faster than others, but the rate of growth depends principally +upon environment. The average increase at the stump in valley land +is about 1 inch in 6 years. A Douglas fir growing along the stage +road between the park boundary and Longmire's, at the age of 90 to +120 years may have a breast diameter of 20 inches and yield 700 feet +of saw timber. But many of the trees of this size may be much +older on account of having grown in the shade or under other +adverse conditions. The trees between 200 and 300 years of age are +often 40 to 50 inches in diameter and may yield an average of from +2,700 to 5,500 board feet. The largest Douglas firs are sometimes +over 400 years old and 60 to 70 inches in diameter. Such trees when +sound will produce over 8,000 feet of lumber.</p> + +<p>The western red cedar has a shorter and more tapering trunk and +its volume in board feet is proportionally smaller. A tree 50 inches +in diameter and 175 feet high contains about 3,400 board feet.</p> + +<p>The size of the trees decreases rapidly at higher elevations. In the +subalpine forest the annual growth is very small. At elevations of +6,000 feet the white-bark pine requires 200 years to attain a diameter +of 10 or 12 inches. The annual rings are so close together that they +can not be distinguished without a magnifying glass.</p> + + + +<hr /> +<h3>DESCRIPTIONS OF SPECIES.</h3> + + +<h4>DOUGLAS FIR (PSEUDOTSUGA TAXIFOLIA).</h4> + +<p>The Douglas fir (<a href="#Fig_2">figs. 2</a>, <a href="#Fig_3">3</a>, <a href="#Fig_4">4</a>, and <a href="#Fig_5">5</a>) is the best known and the +most important timber tree of western North America. It is found<span class='pagenum'><a name="Page_7" id="Page_7">[Pg 7]</a></span> +from British Columbia southward to northern Mexico. The finest +forests occur in Oregon and Washington at low elevations. The +Douglas fir is common in the park up to 3,500 feet, sometimes in +nearly pure stands, but more often mixed with other species. It +grows in all situations. In the higher mountains it prefers warm +southern exposures and is seldom found on wind-swept ridges. It +seeds annually, but most profusely at intervals three or four years +apart. The red squirrels gather and store large quantities of the +cones in order to provide a supply of the seeds for their winter rations. +The growth of the young tree is very rapid. As the tree becomes +older the rate of growth varies with the situation and the +character of the soil so that the size does not closely determine the +age of the tree.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_2" id="Fig_2"></a> +<img src="images/i010.jpg" width="500" height="425" alt="Fig. 2." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 2.</span>—Douglas fir (<i>Pseudotsuga taxifolia</i>).</span></p> +</div> + +<p>The Douglas fir is a long-lived tree, and specimens are occasionally +found 250 to 270 feet high and over 8 feet in diameter and between +400 and 500 years in age. It reaches its greatest height and +most perfect proportions in mature even-age stands growing on fairly +moist well-drained bench lands. Under these conditions it is a very +tall and beautiful tree. The trunk is straight, round, and free from +branches for two-thirds of its height and tapers gently to the crown. +The dark-brown deep-furrowed bark is 5 to 10 inches thick at the +base of the tree.</p> + +<p><span class='pagenum'><a name="Page_8" id="Page_8">[Pg 8]</a></span></p><p>The Douglas fir ranks first among the trees of the Pacific slope in +importance for the production of lumber. It is often sold under +the name of Oregon pine. Lumber dealers class the coarse-grained +reddish wood produced by the young growth in open forests as "red +fir." The older growth produced when the forest is more dense +is a finer grained and more valuable wood, sold under the name of +"yellow fir."</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_3" id="Fig_3"></a> +<img src="images/i011.jpg" width="500" height="404" alt="Fig. 3." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 3.</span>—Douglas fir (<i>Pseudotsuga taxifolia</i>).</span></p> +</div> + +<p>The Douglas fir is used for nearly all purposes where durability, +strength, and hardness are desirable. It is made into dimension +timbers, lumber, flooring, and is particularly adapted for masts and +spars. The lumber is shipped by rail to the Middle Western States. +The foreign cargo shipments are made to all parts of the world. +The greatest amount goes to Australia, the west and east coasts of +South America, China, the United Kingdom, and Europe, Japan, +and the South Sea Islands. Coastwise shipments are made to California, +Alaska, and Panama. Large quantities of the seed of this +tree are sent to Europe, where the Douglas fir is grown for timber +and for ornament.</p> + + +<p><span class='pagenum'><a name="Page_9" id="Page_9">[Pg 9]</a></span></p> +<h4>WESTERN RED CEDAR (THUJA PLICATA.)<a name="FNanchor_1_1" id="FNanchor_1_1"></a><a href="#Footnote_1_1" class="fnanchor">[1]</a></h4> + +<div class="figcenter" style="width: 500px;"><a name="Fig_4" id="Fig_4"></a> +<img src="images/i012.jpg" width="500" height="633" alt="Fig. 4." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 4.</span>—Douglas fir (<i>Pseudotsuga taxifolia</i>).</span></p> +</div> + +<p>The western red cedar (<a href="#title_page">title page</a> and <a href="#Fig_5">fig. 5</a>) ranges from south-eastern +Alaska to northern California. It is a common tree in the +park. It occurs in patches along the river bottoms where the flat +scalelike foliage is conspicuous among the needle-shaped leaves of +the hemlock and fir. The bark is fibrous in appearance and may be +readily separated into long strips. The trunks of the older trees are +swelled and irregularly fluted at the base. The leaves are fragrant<span class='pagenum'><a name="Page_10" id="Page_10">[Pg 10]</a></span> +and the wood has a pleasing aromatic odor. Nearly all the large +trees are hollow at the butt. The roots spread laterally to a great +distance, but extend only for a short distance below the surface of the +ground. The tree is easily overthrown by the wind and usually +grows in sheltered localities. On account of the thinness of the bark +it is easily killed by fire.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_5" id="Fig_5"></a> +<img src="images/i013.jpg" width="500" height="401" alt="Fig. 5." title="" /> +<div class="hang2"><span class="smcap">Fig. 5.</span>—Two big Douglas firs and a western red cedar (on the left) along the +road up the Nisqually Valley, Mount Rainier National Park.<br /></div> + +<p class="center"><small>Photograph by A.H. Denman.</small></p> +</div> + +<p>The red cedar flourishes on fertile and well-watered soils near sea +level, where it grows to an enormous size. In the park it is a smaller +tree, 150 to 170 feet high and rarely more than 4 or 5 feet through +above the swollen butt. It grows occasionally up to an altitude of +4,000 feet, but is a small and insignificant tree in the high mountains.</p> + +<p>In the sapling stage the red cedar grows rapidly. The mature +tree increases very slowly in size. It exceeds all other trees in the +Cascades in longevity. Individuals more than 500 years old are not +uncommon and there is a well-authenticated instance where the annual +rings indicated a growth of more than 1,100 years.</p> + +<p>While the red cedar forms no great proportion of the forest of the +Pacific Northwest, it is peculiarly valuable to the pioneer on account +of the durability of the wood and the ease with which it can be split<span class='pagenum'><a name="Page_11" id="Page_11">[Pg 11]</a></span> +into boards, shakes, and planking. The early settlers used cedar +split by hand as a substitute for sawn lumber in flooring and finishing +their cabins and for the tables and shelves with which they were +furnished. The Indians hollowed the great trunks with fire and +made them into canoes, some of which were large and seaworthy +enough to be used on the Sound and in making voyages along the +coast. They wove the fibrous roots into baskets that carried water +and plaited the bark into matting. The wood of the red cedar is +reddish brown in color. It is soft, light, and very brittle, but very +durable. It is extensively used for shingles, the manufacture of +which forms one of the important industries of the State. The clear +logs are sawed into lumber used for siding, interior and exterior +finish, moldings, tank stock, and similar purposes. Common logs +are utilized for shingles. In many localities the entire tree is cut +into 52–inch bolts, which are hauled to the mills or floated to them +down the streams.</p> + +<p>The western red cedar makes excellent posts and rails for farm +fences. The young trees are used for telegraph and telephone poles.</p> + + +<h4>WESTERN HEMLOCK (TSUGA HETEROPHYLLA).</h4> + +<p>Next to the Douglas fir the western hemlock is the most abundant +tree in the forests of Oregon and Washington. It occurs from +Alaska southward to northern California. About Mount Rainier it +is found up to an altitude of 5,000 feet. In the river valleys in moist +situations it is a large tree, sometimes reaching a height of 250 feet +and a diameter of 5 feet. On the high ridges it is stunted. It grows +best on moist deep soils in dense forests, but thrives under almost all +conditions of soil and exposure if provided with plenty of moisture.</p> + +<p>Western hemlock (<a href="#Fig_6">figs. 6</a> and <a href="#Fig_7">7</a>) is usually associated with Douglas +fir and red cedar, but sometimes forms a forest of nearly pure growth. +The hemlock produces abundant seed each year, although it is more +prolific at irregular intervals. The seeds germinate readily on decayed +moss and rotten wood as well as upon the mineral soil. Seedlings +frequently grow on fallen logs and extend their vigorous roots +around the side until they reach the ground and become firmly anchored +in it. Young hemlocks thrive in the shade. On logged-off +areas which have not been burned over and which are partially +shaded by uncut trees, the reproduction of hemlock springs up, to the +exclusion of the more valuable Douglas fir.</p> + +<p><span class='pagenum'><a name="Page_12" id="Page_12">[Pg 12]</a></span></p> +<div class="figcenter" style="width: 500px;"><a name="Fig_6" id="Fig_6"></a> +<img src="images/i015.jpg" width="500" height="717" alt="Fig. 6." title="" /> +<div class="hang2"><span class="smcap">Fig. 6.</span>—The lower slope forest, near Longmire Springs, altitude 3,000 feet, +here composed largely of western hemlock (Tsuga heterophylla); the tree +on the extreme left is a Douglas fir (<i>Pseudotsuga taxifolia</i>).</div> + +<p class="center"><small>Photograph by A.H. Barnes.</small></p> +</div> + + +<p>The hemlock is long lived and grows slowly. The largest trees +are from 200 to 500 years old and are usually hollow-hearted. The +bark is thin and the tree very easily killed by ground fire. The wood +of the hemlock is tough, light, and straight grained. It is not as +durable as the Douglas fir and decays rapidly when exposed to the +weather. The clear lumber is suitable for interior finish. The wood +is also used for flooring, joists, lath, and paper pulp. The common +and rough lumber does not find a ready market, except for the +limited amount used in temporary construction. The western hemlock<span class='pagenum'><a name="Page_13" id="Page_13">[Pg 13]</a></span> +is, however, superior to the eastern hemlock, and its value will +probably be recognized as its usefulness for many purposes becomes +better known.</p> + + +<h4>WESTERN WHITE PINE (PINUS MONTICOLA).</h4> + +<div class="figcenter" style="width: 500px;"><a name="Fig_7" id="Fig_7"></a> +<img src="images/i016.jpg" width="500" height="617" alt="Fig. 7." title="" /> +<div class="hang2"><span class="smcap">Fig. 7.</span>—A forest of Douglas fir, with an understory of western hemlock, on the +lower slopes of the hills, Mount Rainier National Park.</div> + +<p class="center"><small>Photograph by A.H. Denman.</small></p> +</div> + +<p>The western white pine (<a href="#Fig_8">fig. 8</a>) is found from southern Alaska to +northern California. In the park it occurs occasionally up to 4,000 +feet. It usually grows on level benches and gentle slopes associated +with Douglas fir, western hemlock, and noble and amabilis fir. It +reaches its best development at elevations of from 3,000 to 3,500 +feet, where it attains a height of 150 feet and a diameter of 40 inches. +The shaft is straight, cylindrical, and clear of limbs. It bears a small, +narrow crown of drooping branches. In open areas, where it is +exposed to sunlight, its mode of growth is wholly different. The<span class='pagenum'><a name="Page_14" id="Page_14">[Pg 14]</a></span> +trunk is short, rapidly tapering, and bears wide-spreading branches +nearly to the ground. At high elevations the western white pine is +very short and stunted.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_8" id="Fig_8"></a> +<img src="images/i017.jpg" width="500" height="492" alt="Fig. 8." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 8.</span>—Western white pine (<i>Pinus monticola</i>).</span><br /> + +<small>Diameter 24 inches, height 50 feet.</small></p> +</div> + +<p>Although the western white pine is not a common tree in the park, +it is often noticed on account of its abundance of slender, pendant +cones, 6 to 10 inches long. They mature every two years and shed +their seed early in September. The seed are provided with long +wings and are often carried by the wind for a great distance from the +parent tree.</p> + +<p>The wood is light, soft, free from pitch, and the most valuable of +any of the pines of the Cascades. It is used for interior finish, pattern +making, and other purposes. The supply of this tree is so limited +that it is not of great commercial importance in the Mount +Rainier region.</p> + + +<p><span class='pagenum'><a name="Page_15" id="Page_15">[Pg 15]</a></span></p> +<h4>AMABILIS FIR (ABIES AMABILIS).<a name="FNanchor_2_2" id="FNanchor_2_2"></a><a href="#Footnote_2_2" class="fnanchor">[2]</a></h4> + +<p>Amabilis fir (<a href="#Fig_9">figs. 9</a> and <a href="#Fig_10">10</a>) ranges from southern Alaska to Oregon. +It is abundant in the park at elevations from 2,500 to 5,000 feet +on level bench lands, and gentle slopes with a northern exposure. It +is rarely found in unmixed stands, but is usually associated with +western hemlock, Douglas fir, and noble fir. The largest trees are +150 to 180 feet high and 3 to 5 feet in diameter. In dense forests the +stem is free from branches for 50 to 100 feet.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_9" id="Fig_9"></a> +<img src="images/i018.jpg" width="500" height="550" alt="Fig. 9." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 9.</span>—Amabilis fir (<i>Abies amabilis</i>).</span></p> +</div> + +<p>At altitudes over 4,000 feet, small amabilis firs often occur in +clusters and open groves. The trunk is covered with branches which +grow to the ground, turning downward and outward in long graceful +curves, admirably adapted to withstand the pressure of the +frozen snow. The foliage is a deep and brilliant green, forming +a strong contrast to the dark-purple cones. The seeds ripen each year<span class='pagenum'><a name="Page_16" id="Page_16">[Pg 16]</a></span> +early in October. Like the seed of the other alpine species of trees +that grow in the cold and humid climate of the high Cascades, they +soon lose their vitality when stored in dry places. The amabilis fir +is grown in Europe as an ornamental tree. Under cultivation it loses +much of the natural grace and beauty which it acquired in adapting +itself to the deep snows and long winters of its native environment.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_10" id="Fig_10"></a> +<img src="images/i019.jpg" width="500" height="406" alt="Fig. 10." title="" /> +<div class="hang2"><span class="smcap">Fig. 10.</span>—The forests of western hemlock, amabilis fir, and other species, on the +middle slopes of the mountains, along the Crater Lake trail, Mount Rainier +National Park.<br /></div> + +<p class="center"><small>Photograph by Geo. O. Ceasar.</small></p> +</div> + +<p>The bark is thin and the tree is easily killed by fire. The wood is +straw colored, compact, and straight grained. It is not strong and +splits easily. It is sold to some extent under the name of larch or +mixed with inferior grades of fir and hemlock. The lumber is of little +value commercially.</p> + + +<h4>NOBLE FIR (ABIES NOBILIS).</h4> + +<p>The noble fir (<a href="#Fig_11">figs. 11</a> and <a href="#Fig_12">12</a>) is a common mountain tree in the +western parts of Washington and Oregon. Like amabilis fir, it is +usually called larch by lumbermen. About Mount Rainier it grows +at elevations of from 3,500 to 5,000 feet in dense stands associated<span class='pagenum'><a name="Page_17" id="Page_17">[Pg 17]</a></span> +with amabilis fir, western hemlock, and Douglas fir. The noble fir +avoids steep side hills and exposed situations. In moist soils on flats +and gentle slopes it often reaches a height of from 150 to 200 feet. +The tall and upright trunk supports a rounded crown of bluish +green foliage, which is very noticeable among the purer green leaves +of its associates. The branches are short, thick, and crowded with +stiff, flattened leaves, which turn upward and outward. The light-green +bract-covered cones are sometimes 6 inches long and nearly +3 inches thick. They ripen early in September. Seed is borne +every year, although in some seasons it is much more abundant than +in others.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_11" id="Fig_11"></a> +<img src="images/i020.jpg" width="500" height="613" alt="Fig. 11." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 11.</span>—Noble fir (<i>Abies nobilis</i>).</span></p> +</div> + +<p><span class='pagenum'><a name="Page_18" id="Page_18">[Pg 18]</a></span></p> +<div class="figcenter" style="width: 500px;"><a name="Fig_12" id="Fig_12"></a> +<img src="images/i021.jpg" width="500" height="693" alt="Fig. 12." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 12.</span>—Noble fir (<i>Abies nobilis</i>), 6 feet in diameter.</span> +</p></div> + +<p>The wood is strong, close grained, and elastic. It is used for +lumber and particularly for inside finishing. The noble fir is a +slow-growing and long-lived tree. Old trees in mixed forests are +easily distinguished from the associated species by the ashy-brown +outer bark broken into large irregular plates.</p> + + +<p><span class='pagenum'><a name="Page_19" id="Page_19">[Pg 19]</a></span></p> +<h4>ALPINE FIR (ABIES LASIOCARPA).<a name="FNanchor_3_3" id="FNanchor_3_3"></a><a href="#Footnote_3_3" class="fnanchor">[3]</a></h4> + +<div class="figcenter" style="width: 500px;"><a name="Fig_13" id="Fig_13"></a> +<img src="images/i022.jpg" width="500" height="663" alt="Fig. 13." title="" /> +<div class="hang2"><span class="smcap">Fig. 13.</span>—A cluster of Alpine firs (<i>Abies lasiocarpa</i>), whose spire-shaped crowns +are characteristic, at 5,500 feet altitude, in Cowlitz Park, Mount Rainier +National Park.<br /></div> + +<p class="center"><small>Photograph by A.H. Barnes.</small></p> +</div> + +<p>The alpine fir (<a href="#Fig_13">fig. 13</a>) ranges from Alaska to New Mexico. It +is a common tree in the park at elevations above 4,500 feet. It is a +tree of the high mountains and with the white bark pine and the +mountain hemlock, is found up to the limit of arborescent life. It<span class='pagenum'><a name="Page_20" id="Page_20">[Pg 20]</a></span> +demands moisture and is generally restricted to regions of deep +snowfall.</p> + +<p>The alpine fir occurs in unmixed stands, but is often associated +with the mountain hemlock. At the lower levels of its range it is +a fair-sized tree 50 or 60 feet high. The crown of deep-green foliage +is broad at the base and tapers to the top, where it terminates in a +slender, pointed tip. At its upper limit it becomes a stunted shrub, +with wide extended branches resting on the ground.</p> + +<p>The alpine fir bears upright clusters of deep-purple cones. It +seeds sparingly each year. The seasons of heavy seed production +occur at intervals of three or four years. The wood is soft and splits +easily. It is of no commercial value. The tree is easily killed by +fire, which blisters the thin bark and frequently springs into the +drooping lower branches.</p> + + +<h4>GRAND FIR (ABIES GRANDIS.)<a name="FNanchor_4_4" id="FNanchor_4_4"></a><a href="#Footnote_4_4" class="fnanchor">[4]</a></h4> + +<p>The grand fir (<a href="#Fig_14">fig. 14</a>), like several other species, is generally +given the name of white fir on account of its smooth, light-colored +bark. It is a common tree in the river bottoms from British Columbia +south to northern California. In the Mount Rainier National +Park it occurs up to 4,000 feet. The grand fir is a moisture-loving +tree and is usually found firmly rooted in deep alluvial bottom +lands along the banks of streams. With the Douglas fir, hemlock, +and red cedar it forms the dense forest characteristic of the lower +mountain valleys.</p> + +<p>In favorable conditions the grand fir grows to a height of from +100 to 200 feet and is a noble and stately tree. The trunk tapers +rapidly and bears a rounded pyramidal crown. In dense forests the +trunk is clear for half its height, but where the trees stand in the +open it carries its branches nearly to the ground. The leaves are a +bright and shining green. The large light-green cones mature early +in the fall. The wood is soft and very heavy before it is seasoned. +It rots in a very short time when laid on the ground. When dry it is +white, coarse-grained, light, and odorous. It is used for interior +finish and for crates and packing boxes, but is of little value commercially.</p> + + +<h4>ENGELMANN SPRUCE (PICEA ENGELMANNI).</h4> + +<p>The Engelmann spruce (<a href="#Fig_15">fig. 15</a>) is a mountain tree ranging from +British Columbia to Arizona and New Mexico. It is common along +the summit and on the east side of the Cascade Range and occurs +on the northeastern and eastern slopes of Mount Rainier at elevations +of from 3,500 to 6,000 feet.</p> + +<p>This tree requires a moist soil and prefers cool northern exposures. +Up to 5,000 feet it commonly grows in sheltered basins at the head<span class='pagenum'><a name="Page_21" id="Page_21">[Pg 21]</a></span> +of canyons and in stream valleys. At its upper limits it is common +on flats and depressions and about lakes on level summits. It avoids +steep mountain sides and exposed situations.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_14" id="Fig_14"></a> +<img src="images/i024.jpg" width="500" height="724" alt="Fig. 14." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 14.</span>—Grand fir (<i>Abies grandis</i>).</span></p> +</div> + +<p>The Engelmann spruce is easily distinguished from its associates +by its stiff, bluish-green pointed leaves, which prick the hand when<span class='pagenum'><a name="Page_22" id="Page_22">[Pg 22]</a></span> +they are grasped. In the mountain parks it is a handsome tree 50 to +60 feet high. When it stands apart from other trees the lower +branches are thick and long and extend to the ground. The crown +is very broad at the base, but narrow and spirelike at the top. The +Engelmann spruce reaches its best development at low elevations, +where it often grows in dense, pure stands. Under these conditions +it reaches a height of 100 feet. The bole is straight and free from +limbs and the top is short and compact.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_15" id="Fig_15"></a> +<img src="images/i025.jpg" width="500" height="626" alt="Fig. 15." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 15.</span>—Engelmann spruce (<i>Picea engelmanni</i>).</span></p> +</div> + +<p>The young cones are massed in upright green and purple clusters +at the tips of the upper branches. They are notable for the purity +and brilliance of their coloring. As they mature they become pendant +and fade to a light brown. The seed is produced in abundance +nearly every year, although small and seedling trees are not usually +numerous.</p> + +<p>The wood is soft, white, compact, and even grained. It is free +from pitch and odor. It is valuable for boxing, cooperage, and certain<span class='pagenum'><a name="Page_23" id="Page_23">[Pg 23]</a></span> +kinds of finish. It is also an excellent material for the tops of +violins and other stringed instruments. The Engelmann spruce is, +however, of little importance as a timber tree on account of its +scarcity and the scattered stands in which it grows. It is a long-lived +tree unless attacked by fire, to which it is very vulnerable.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_16" id="Fig_16"></a> +<img src="images/i026.jpg" width="500" height="654" alt="Fig. 16." title="" /> +<div class="hang2"><span class="smcap">Fig. 16.</span>—A group of yellow cypresses (<i>Chamaecyparis nootkatensis</i>) on the +high slopes of Mount Rainier National Park, altitude about 6,000 feet.<br /></div> + +<p class="center"><small>Photograph by A.H. Barnes.</small></p> +</div> + + +<h4>YELLOW CYPRESS (CHAMAECYPARIS NOOTKATENSIS).</h4> + +<p>Yellow cypress (<a href="#Fig_16">fig. 16</a>) ranges from the seacoast of southern +Alaska south to the mountains of Washington and Oregon. It occurs<span class='pagenum'><a name="Page_24" id="Page_24">[Pg 24]</a></span> +in the park up to the elevation of 7,000 feet. It is common on northern +exposures, along streams, and in basins at the head of canyons. +It also grows on crests and ridges, where the frequent showers and +fogs supply the moisture which it demands. In sheltered localities it +grows to a height of 75 or 80 feet, but it is commonly a small tree +with, a bent and twisted stem, +which, with its pendulous +branches, presents a somewhat +scrubby appearance. The foliage +is green, sometimes with a +bluish tinge. It resembles that +of the common western red cedar, +but the leaves are sharper, +more pointed, and rougher to +handle. The small, rounded, +inconspicuous cones are produced +somewhat sparingly. +The bark of the young tree is +red. On the mature tree it becomes +gray and fibrous. The +wood is yellow, close grained, +and aromatic. Unlike that of +the western red cedar, the trunk +is usually sound to the center. +The wood is used for boat +building and cabinetwork. It +is very durable.</p> + +<p>The yellow cypress grows +very slowly, particularly at +high elevations. The number +of annual rings on trees 15 to 20 +inches in diameter indicate that +they are over 200 years old.</p> + + +<h4>LODGEPOLE PINE (PINUS +CONTORTA).</h4> + +<p>Lodgepole pine (<a href="#Fig_17">fig. 17</a>) is +widely distributed from Alaska +to Lower California and eastward +through the Rockies to Dakota and Colorado. It occurs +sparingly in the park up to 5,000 feet above sea level. It adapts +itself easily to the different conditions of soil, moisture, and exposure.</p> + +<div class="figcenter" style="width: 300px;"><a name="Fig_17" id="Fig_17"></a> +<img src="images/i027.jpg" width="300" height="694" alt="Fig. 17." title="" /> +<div class="hang2"><span class="smcap">Fig. 17.</span>—Lodgepole pine (<i>Pinus contorta</i>), +60 inches in diameter.</div> +</div> + +<p>This tree varies greatly in the different regions where it is found. +About Mount Rainier it does not often exceed 20 to 40 feet in height<span class='pagenum'><a name="Page_25" id="Page_25">[Pg 25]</a></span> +and is often a much smaller tree. It produces cones at the age of 5 +to 7 years. The foliage is a yellowish green. At high elevations the +leaves have a peculiar whorled appearance which gives it a different +aspect from that of the other pines. The short, heavily limbed trunk +bears no resemblance to the tall and slender shaft of the lodgepole +pine of the Rocky Mountains. The root system is shallow and the +tree is easily fire killed. The wood of the variety which grows in +the park is of no commercial value.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_18" id="Fig_18"></a> +<img src="images/i028.jpg" width="500" height="615" alt="Fig. 18." title="" /> +<div class="hang2"><span class="smcap">Fig. 18.</span>—The feathery foliage of mountain hemlock (<i>Tsuga mertensiana</i>), +Grand Park, Mount Rainier National Park.<br /></div> + +<p class="center"><small>Photograph by A.H. Denman.</small></p> +</div> + + +<h4>MOUNTAIN HEMLOCK (TSUGA MERTENSIANA).</h4> + +<p>The mountain hemlock (<a href="#Fig_18">figs. 18</a>, <a href="#Fig_19">19</a>, and <a href="#Fig_20">20</a>) is found on the Pacific +coast from the Sierras of California to the northern part of Alaska<span class='pagenum'><a name="Page_26" id="Page_26">[Pg 26]</a></span> +where it grows at sea level. On Mount Rainier it occurs at altitudes +of from 3,500 to 7,500 feet. It forms dense forests under 4,500 feet, +where it is often a fair-sized tree 50 to 90 feet high. With the ascent +of the mountain it diminishes in height and the branches become +gnarled and twisted. Near timber line the trunk is dwarfed and +bent at the base and the crown becomes a flattened mass of branches +lying close to the ground (<a href="#Fig_20">fig. 20</a>).</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_19" id="Fig_19"></a> +<img src="images/i029.jpg" width="500" height="868" alt="Fig. 19." title="" /> +<div class="hang2"><span class="smcap">Fig. 19.</span>—Two solitary mountain hemlocks (<i>Tsuga mertensiana</i>), Spray Park, +Mount Rainier National Park.<br /></div> + +<p class="center"><small>Photograph by Geo. O. Ceasar.</small></p> +</div> + +<p>The mountain hemlock is abundant on high, rocky ridges, but the +best stands are on cool, moist soil at the heads of ravines, on flats, and +on gentle slopes with a northern exposure.</p> + +<p><span class='pagenum'><a name="Page_27" id="Page_27">[Pg 27]</a></span></p><p>This tree seeds every year. In good seed years the upper branches +are laden with a profusion of beautiful, deep-purple cones, often +in such abundance as to bend down the branchlets with their weight. +The reproduction is slow. In the high mountains the trees are +buried in snow from October to late in June, and the growing season +is very short.</p> + + +<h4>WHITE-BARK PINE (PINUS ALBICAULIS).</h4> + +<div class="figcenter" style="width: 500px;"><a name="Fig_20" id="Fig_20"></a> +<img src="images/i030.jpg" width="500" height="403" alt="Fig. 20." title="" /> +<div class="hang2"><span class="smcap">Fig. 20.</span>—A gnarled, wind-swept mountain hemlock (<i>Tsuga mertensiana</i>), near +the upper limits of tree growth, Spray Park, Mount Rainier National Park.<br /></div> + +<p class="center"><small>Photograph by A.H. Denman.</small></p> +</div> + +<p>The white-bark pine (<a href="#Fig_21">fig. 21</a>) grows close to timber line in the +mountains of the Pacific coast from British Columbia to southern +California. In the Canadian Rockies it extends north to the +fifty-third parallel. It is the most alpine of all the pines. Its lower limit +on Mount Rainier is about 5,000 feet above sea level. In sheltered +places where the soil is deep the trees are sometimes 30 to 40 feet +high and 20 inches in diameter. The trunks are free from limbs for +8 or 10 feet. The outer bark, from which the tree derives its name, +consists of thin, light-gray scales.</p> + +<p>As the white-bark pine advances up the mountain its habit changes +rapidly. The stem shortens and becomes gnarled and twisted. The +tough, flexible branches reach the ground and spread over it to a<span class='pagenum'><a name="Page_28" id="Page_28">[Pg 28]</a></span> +great distance from the tree. On rocky summits and the bleak crests +of wind-swept ridges the twisted trunk and branches are quite prostrate +and the crown is a dense flattened mass of foliage.</p> + +<p>The roots of the tree are deep, long, and tenacious. They spread +wide and deep and cling so firmly to the rocks that the tree is rarely +overthrown by the violent winds that sweep over the mountain.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_21" id="Fig_21"></a> +<img src="images/i031.jpg" width="500" height="599" alt="Fig. 21." title="" /> +<div class="hang2"><span class="smcap">Fig. 21.</span>—A white-bark pine (<i>Pinus albicaulis</i>) in its characteristic mountain +habitat, Mount Rainier National Park.<br /></div> + +<p class="center"><small>Photograph by A.H. Denman.</small></p> +</div> + +<p>The thick, purple cones require two years to mature. They ripen +early in September and produce chocolate-brown seeds a little larger +than a grain of corn. They are much relished by the Klickitat Indians, +who go to considerable pains to secure them. The wood is +close grained and resinous. It makes excellent fuel for the camp fires +of sheep herders and mountain travelers.</p> + + +<p><span class='pagenum'><a name="Page_29" id="Page_29">[Pg 29]</a></span></p> +<h4>WESTERN YEW (TAXUS BREVIFOLIA).<a name="FNanchor_5_5" id="FNanchor_5_5"></a><a href="#Footnote_5_5" class="fnanchor">[5]</a></h4> + +<p>The western yew is found from southern Alaska to northern California. +It occurs in the park up to 4,000 feet, growing in rich, +gravelly soil on moist flats and benches and in deep ravines. It is +a small branching tree, rarely over 20 feet high. The bark is purple +or reddish brown. The branches extend almost to the ground. It +bears a small, bright, amber-red berry.</p> + +<p>The dark-brown or red heartwood is very tough, hard and heavy. +It takes a fine polish and is used for fancy cabinetwork. The Indians +use it for spear handles, bows, and fishhooks.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_22" id="Fig_22"></a> +<img src="images/i032.jpg" width="500" height="418" alt="Fig. 22." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 22.</span>—Broadleaf maple (<i>Acer macrophyllum</i>).</span></p> +</div> + + +<h4>DECIDUOUS TREES.</h4> + +<p>The silva of the Western Cascades is rich in evergreens remarkable +for their size and beauty. The deciduous trees are few and insignificant. +The forests of the park are almost wholly coniferous. Vine +maple and willow are found as undergrowth. On the margins of +rivers there are occasional groves of alders and cottonwoods. The +lighter hues of the branching trunks and the changing tints of the<span class='pagenum'><a name="Page_30" id="Page_30">[Pg 30]</a></span> +foliage in these patches of broad-leaved woodland present a pleasing +diversity to the evergreen forest.</p> + +<p>Broadleaf maple (<i>Acer macrophyllum</i>) (<a href="#Fig_22">fig. 22</a>), the largest of +the Pacific coast maples, ranges from Alaska to southern California. +Near sea level it often attains a height of 50 or 60 feet. In +the park it is a short-stemmed, branching tree, occasionally found +on the borders of streams. It grows at elevations under 3,000 feet.</p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_23" id="Fig_23"></a> +<img src="images/i033.jpg" width="500" height="567" alt="Fig. 23." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 23.</span>—Vine maple (<i>Acer circinatum</i>).</span></p> +</div> + +<p>Vine maple (<i>Acer circinatum</i>) (<a href="#Fig_23">fig. 23</a>) is abundant from British +Columbia to northern California. On rich river bottoms it is +sometimes 15 to 20 feet high and 6 inches in diameter. In the park +it is usually a bush or low shrub with a bent and curiously crooked +stem, growing along streams and as undergrowth in the forest. It is +very common up to 3,000 feet. In autumn the leaves are a bright scarlet. +The wood is tough and elastic and makes a hot and lasting fire.</p> + +<p><span class='pagenum'><a name="Page_31" id="Page_31">[Pg 31]</a></span></p> + +<div class="figcenter" style="width: 500px;"><a name="Fig_24" id="Fig_24"></a> +<img src="images/i034.jpg" width="500" height="372" alt="Fig. 24." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 24.</span>—Red alder (<i>Alnus oregona</i>).</span></p> +<br /></div> + +<div class="figcenter" style="width: 500px;"><a name="Fig_25" id="Fig_25"></a> +<img src="images/i034a.jpg" width="500" height="342" alt="Fig. 25." title="" /> +<p class="center"><span class="caption"><span class="smcap">Fig. 25.</span>—Black cottonwood (<i>Populus trichocarpa</i>).</span></p> +</div> + +<p><span class='pagenum'><a name="Page_32" id="Page_32">[Pg 32]</a></span></p><p>Red alder (<i>Alnus oregona</i>) (<a href="#Fig_24">fig. 24</a>) occurs from Alaska to southern +California. It is common about Mount Rainier, in river bottoms, +on the banks of large streams, and in swampy places. It +usually grows to a height of 30 or 40 feet. The bark varies from +nearly white to light gray. It is the most abundant of all the +deciduous trees in the park.</p> + +<p>Black cottonwood (<i>Populus trichocarpa</i>) (<a href="#Fig_25">fig. 25</a>) is common from +Alaska to southern California. It is occasionally found in the park +up to 4,000 feet. It grows along streams and on sandy river bottoms +often associated with the alder. The leaves are almost always in +motion, very gentle winds being sufficient to make them twinkle and +turn.</p> + +<p>The wood is soft, but tough and compact. It is used for staves, +woodenware, wood pulp, trunks, barrels, and for drawer bottoms.</p> + + +<h3>FOOTNOTES</h3> + +<div class="footnote"><p><a name="Footnote_1_1" id="Footnote_1_1"></a><a href="#FNanchor_1_1"><span class="label">[1]</span></a> This species is known as arbor vitæ in Glacier Park.</p></div> + +<div class="footnote"><p><a name="Footnote_2_2" id="Footnote_2_2"></a><a href="#FNanchor_2_2"><span class="label">[2]</span></a> This species is known as silver fir in Crater Lake Park.</p></div> + +<div class="footnote"><p><a name="Footnote_3_3" id="Footnote_3_3"></a><a href="#FNanchor_3_3"><span class="label">[3]</span></a> This species is known as balsam in Glacier and Yellowstone Parks.</p></div> + +<div class="footnote"><p><a name="Footnote_4_4" id="Footnote_4_4"></a><a href="#FNanchor_4_4"><span class="label">[4]</span></a> This species is known as silver fir in Yellowstone and Glacier Parks.</p></div> + +<div class="footnote"><p><a name="Footnote_5_5" id="Footnote_5_5"></a><a href="#FNanchor_5_5"><span class="label">[5]</span></a> This species is known as Oregon yew in Crater Lake National Park and as yew in +Yellowstone and Glacier Parks.</p></div> + + + +<hr /> +<h2>INDEX TO SPECIES DESCRIBED.</h2> + +<p class="center">[Roman numerals indicate pages containing descriptions; italic numerals indicate pages containing +illustrations.]</p> + + +<p class="index"><br /> +<i>Abies amabilis</i> <a href="#Page_15">15–16</a>, <a href="#Page_15"><i>15</i></a>, <a href="#Page_16"><i>16</i></a><br /> +<span style="margin-left: 1em;"><i>grandis</i> <a href="#Page_20">20</a>, <a href="#Page_21"><i>21</i></a></span><br /> +<span style="margin-left: 1em;"><i>lasiocarpa</i> <a href="#Page_19">19–20</a>, <a href="#Page_19"><i>19</i></a></span><br /> +<span style="margin-left: 1em;"><i>nobilis</i> <a href="#Page_17">17–19</a>, <a href="#Page_17"><i>17</i></a>, <a href="#Page_18"><i>18</i></a></span><br /> +<br /> +<i>Acer circinatum</i> <a href="#Page_30">30</a>, <i><a href="#Page_30">30</a></i><br /> +<span style="margin-left: 1em;"><i>macrophyllum</i> <a href="#Page_29">29</a>, <i><a href="#Page_29">29</a></i></span><br /> +<br /> +Alder, red (<i>Alnus oregona</i>) <a href="#Page_30">30</a>, <i><a href="#Page_31">31</a></i><br /> +<br /> +<i>Alnus oregona</i> <a href="#Page_30">30</a>, <i><a href="#Page_31">31</a></i><br /> +<br /> +Alpine fir (<i>Abies lasiocarpa</i>) <a href="#Page_19">19–20</a>, <a href="#Page_19"><i>19</i></a><br /> +<br /> +Amabilis fir (<i>Abies amabilis</i>) <a href="#Page_15">15–16</a>, <a href="#Page_15"><i>15</i></a>,<a href="#Page_16"> <i>16</i></a><br /> +<br /> +Arbor vitæ. <i>See</i> Western red cedar.<br /> +<br /> +<br /> +Balsam. <i>See</i> Alpine fir.<br /> +<br /> +Black cottonwood (<i>Populus trichocarpa</i>) <a href="#Page_30">30–32</a>, <a href="#Page_31"><i>31</i></a><br /> +<br /> +Broadleaf maple (<i>Acer macrophyllum</i>) <a href="#Page_29">29</a>, <a href="#Page_29"><i>29</i></a><br /> +<br /> +<br /> +Cedar, western red (<i>Thuja plicata</i>) <a href="#Page_9">9–11</a>, <a href="#Page_10"><i>10</i></a><br /> +<br /> +<i>Chamaecyparis nootkatensis</i> <a href="#Page_23">23–24</a>, <a href="#Page_23"><i>23</i></a><br /> +<br /> +Cottonwood, black (<i>Populus trichocarpa</i>) <a href="#Page_30">30–32</a>, <a href="#Page_31"><i>31</i></a><br /> +<br /> +Cypress, yellow (<i>Chamaecyparis nootkatensis</i>) <a href="#Page_23">23–24</a>, <a href="#Page_23"><i>23</i></a><br /> +<br /> +<br /> +Douglas fir (<i>Pseudotsuga taxifolia</i>) <a href="#Page_6">6–8</a>, <a href="#Page_7"><i>7</i></a>, <a href="#Page_8"><i>8</i></a>, <a href="#Page_9"><i>9</i></a>, <a href="#Page_10"><i>10</i></a>, <a href="#Page_12"><i>12</i></a>, <a href="#Page_13"><i>13</i></a><br /> +<br /> +<br /> +Engelmann spruce (<i>Picea engelmanni</i>) <a href="#Page_20">20–23</a>, <a href="#Page_22"><i>22</i></a><br /> +<br /> +<br /> +Fir, alpine (<i>Abies lasiocarpa</i>) <a href="#Page_19">19–20</a>, <a href="#Page_19"><i>19</i></a><br /> +<span style="margin-left: 1em;">amabilis (<i>Abies amabilis</i>) <a href="#Page_15">15–16</a>, <a href="#Page_15"><i>15</i></a>, <a href="#Page_16"><i>16</i></a></span><br /> +<span style="margin-left: 1em;">Douglas (<i>Pseudotsuga taxifolia</i>) <a href="#Page_6">6–8</a>, <a href="#Page_7"><i>7</i></a>, <a href="#Page_8"><i>8</i></a>, <a href="#Page_9"><i>9</i></a>, <a href="#Page_10"><i>10</i></a>, <a href="#Page_12"><i>12</i></a>, <a href="#Page_13"><i>13</i></a></span><br /> +<span style="margin-left: 1em;">grand (<i>Abies grandis</i>) <a href="#Page_20">20</a>, <a href="#Page_21"><i>21</i></a></span><br /> +<span style="margin-left: 1em;">noble (<i>Abies nobilis</i>) <a href="#Page_17">17–19</a>, <a href="#Page_17"><i>17</i></a>, <a href="#Page_18"><i>18</i></a></span><br /> +<span style="margin-left: 1em;">silver. <i>See</i> Fir, amabilis; Fir, grand.</span><br /> +<br /> +<br /> +Grand fir (<i>Abies grandis</i>) <a href="#Page_20">20</a>, <a href="#Page_21"><i>21</i></a><br /> +<br /> +<br /> +Hemlock, mountain (<i>Tsuga mertensiana</i>) <a href="#Page_25">25–27</a>, <a href="#Page_25"><i>25</i></a>, <a href="#Page_26"><i>26</i></a>, <a href="#Page_27"><i>27</i></a><br /> +<span style="margin-left: 1em;">western (<i>Tsuga heterophylla</i>) <a href="#Page_11">11–13</a>, <a href="#Page_12"><i>12</i></a>, <a href="#Page_13"><i>13</i></a>, <a href="#Page_16"><i>16</i></a></span><br /> +<br /> +<br /> +Larch. <i>See</i> Noble fir; Amabilis fir.<br /> +<br /> +Lodgepole pine (<i>Pinus contorta</i>) <a href="#Page_24">24–25</a>, <a href="#Page_24"><i>24</i></a><br /> +<br /> +<br /> +Maple, broadleaf (<i>Acer macrophyllum</i>) <a href="#Page_29">29</a>, <a href="#Page_29"><i>29</i></a><br /> +<span style="margin-left: 1em;">vine (<i>Acer circinatum</i>) <a href="#Page_30">30</a>, <a href="#Page_30"><i>30</i></a></span><br /> +<br /> +Mountain hemlock (<i>Tsuga mertensiana</i>) <a href="#Page_25">25–27</a>, <a href="#Page_25"><i>25</i></a>, <a href="#Page_26"><i>26</i></a>, <a href="#Page_27"><i>27</i></a><br /> +<br /> +<br /> +Noble fir (<i>Abies nobilis</i>) <a href="#Page_17">17–19</a>, <a href="#Page_17"><i>17</i></a>, <a href="#Page_18"><i>18</i></a><br /> +<br /> +<br /> +Oregon yew. <i>See</i> Western yew.<br /> +<br /> +<br /> +<i>Picea engelmanni</i> <a href="#Page_20">20–23</a>, <a href="#Page_22"><i>22</i></a><br /> +<br /> +Pine, lodgepole (<i>Pinus contorta</i>) <a href="#Page_24">24–25</a>, <a href="#Page_24"><i>24</i></a><br /> +<span style="margin-left: 1em;">western white (<i>Pinus monticola</i>) <a href="#Page_13">13–15</a>, <a href="#Page_14"><i>14</i></a></span><br /> +<span style="margin-left: 1em;">white-bark (<i>Pinus albicaulis</i>) <a href="#Page_27">27–28</a>, <a href="#Page_28"><i>28</i></a></span><br /> +<br /> +<i>Pinus albicaulis</i> <a href="#Page_27">27–28</a>, <a href="#Page_28"><i>28</i></a><br /> +<span style="margin-left: 1em;"><i>contorta</i> <a href="#Page_24">24–25</a>, <a href="#Fig_24"><i>24</i></a></span><br /> +<span style="margin-left: 1em;"><i>monticola</i> <a href="#Page_13">13–15</a>, <a href="#Page_14"><i>14</i></a></span><br /> +<br /> +<i>Populus trichocarpa</i> <a href="#Page_30">30–32</a>, <a href="#Page_31"><i>31</i></a><br /> +<br /> +<i>Pseudotsuga taxifolia</i> <a href="#Page_6">6–8</a>, <a href="#Page_7"><i>7</i></a>, <a href="#Page_8"><i>8</i></a>, <a href="#Page_9"><i>9</i></a>, <a href="#Page_10"><i>10</i></a>, <a href="#Page_12"><i>12</i></a>, <a href="#Page_13"><i>13</i></a><br /> +<br /> +<br /> +Red alder (<i>Alnus oregona</i>) <a href="#Page_30">30</a>, <a href="#Page_31"><i>31</i></a><br /> +<span style="margin-left: 1em;">cedar, western (<i>Thuja plicata</i>) <a href="#Page_9">9–11</a>, <a href="#Page_10"><i>10</i></a></span><br /> +<br /> +<br /> +Silver fir. <i>See</i> Amabilis fir; Grand fir.<br /> +<br /> +Spruce, Engelmann (<i>Picea engelmanni</i>) <a href="#Page_20">20–23</a>, <a href="#Page_22"><i>22</i></a><br /> +<br /> +<br /> +<i>Taxus brevifolia</i> <a href="#Page_28">28–29</a><br /> +<br /> +<i>Thuja plicata</i> <a href="#Page_9">9–11</a>, <a href="#Page_10"><i>10</i></a><br /> +<br /> +<i>Tsuga heterophylla</i> <a href="#Page_11">11–13</a>, <a href="#Page_12"><i>12</i></a>, <a href="#Page_13"><i>13</i></a>, <a href="#Page_16"><i>16</i></a><br /> +<span style="margin-left: 1em;"><i>mertensiana</i> <a href="#Page_25">25–27</a>, <a href="#Page_25"><i>25</i></a>, <a href="#Page_26"><i>26</i></a>, <a href="#Page_27"><i>27</i></a></span><br /> +<br /> +<br /> +Vine maple (<i>Acer circinatum</i>) <a href="#Page_30">30</a>, <a href="#Page_30"><i>30</i></a><br /> +<br /> +<br /> +Western hemlock (<i>Tsuga heterophylla</i>) <a href="#Page_11">11–13</a>, <a href="#Page_12"><i>12</i></a>, <a href="#Page_13"><i>13</i></a>, <a href="#Page_16"><i>16</i></a><br /> +<span style="margin-left: 1em;">red cedar (<i>Thuja plicata</i>) <a href="#Page_9">9–11</a>, <a href="#Page_10"><i>10</i></a></span><br /> +<span style="margin-left: 1em;">white pine (<i>Pinus monticola</i>) <a href="#Page_13">13–15</a>, <a href="#Page_14"><i>14</i></a></span><br /> +<span style="margin-left: 1em;">yew (<i>Taxus brevifolia</i>) <a href="#Page_28">28–29</a></span><br /> +<br /> +White-bark pine (<i>Pinus albicaulis</i>) <a href="#Page_27">27–28</a>, <a href="#Page_28"><i>28</i></a><br /> +<br /> +White pine, western (<i>Pinus monticola</i>) <a href="#Page_13">13–15</a>, <a href="#Page_14"><i>14</i></a><br /> +<br /> +<br /> +Yellow cypress (<i>Chamaecyparis nootkatensis</i>) <a href="#Page_23">23–24</a>, <a href="#Page_23"><i>23</i></a><br /> +<br /> +Yew, Oregon. <i>See</i> Yew, western.<br /> +<span style="margin-left: 1em;">western (<i>Taxus brevifolia</i>) <a href="#Page_28">28–29</a></span><br /> +</p> + + + + + + + +<pre> + + + + + +End of the Project Gutenberg EBook of The Forests of Mount Rainier National +Park, by Grenville F. 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file mode 100644 index 0000000..2aa8a1b --- /dev/null +++ b/31994.txt @@ -0,0 +1,1390 @@ +The Project Gutenberg EBook of The Forests of Mount Rainier National Park, by +Grenville F. Allen + +This eBook is for the use of anyone anywhere at no cost and with +almost no restrictions whatsoever. You may copy it, give it away or +re-use it under the terms of the Project Gutenberg License included +with this eBook or online at www.gutenberg.org + + +Title: The Forests of Mount Rainier National Park + +Author: Grenville F. Allen + +Release Date: April 15, 2010 [EBook #31994] + +Language: English + +Character set encoding: ASCII + +*** START OF THIS PROJECT GUTENBERG EBOOK FORESTS OF MT RAINIER NAT. PARK *** + + + + +Produced by Greg Bergquist and the Online Distributed +Proofreading Team at https://www.pgdp.net (This file was +produced from images generously made available by The +Internet Archive/American Libraries.) + + + + + + + +Transcriber's Note + +The punctuation and spelling from the original text have been faithfully +preserved. + + + FORESTS OF MOUNT RAINIER + NATIONAL PARK + + [Illustration] + + DEPARTMENT OF THE INTERIOR + OFFICE OF THE SECRETARY + 1916 + +For sale by the Superintendent of Documents, Government Printing Office, +Washington, D.C. Price, 20 cents. + + + + +PUBLICATIONS ON MOUNT RAINIER NATIONAL PARK SOLD BY THE SUPERINTENDENT +OF DOCUMENTS. + + +Remittances for these publications should be by money order, payable to +the Superintendent of Documents, Government Printing Office, Washington, +D.C., or in cash. Checks and postage stamps can not be accepted. + +Features of the Flora of Mount Rainier National Park, by J.B. Flett. +1916. 48 pages, including 40 illustrations. 25 cents. + + Contains descriptions of the flowering trees and shrubs in the + park. + +Mount Rainier and Its Glaciers, by F.E. Matthes. 1914. 48 pages, +including 26 illustrations. 15 cents. + + Contains a general account of the glaciers of Mount Rainier and of + the development of the valleys and basins surrounding the peak. + +Panoramic view of Mount Rainier National Park, 20 by 19 inches, scale 1 +mile to the inch. 25 cents. + + + + +THE FORESTS OF MOUNT RAINIER NATIONAL PARK. + +By G.F. ALLEN, _United States Forest Service_. + + + + +GENERAL STATEMENT. + + +The remarkable development of the forests about the base of Mount +Rainier results from climatic conditions peculiarly favorable to tree +growth. The winters are mild and short. The ocean winds that pass +through the gaps of the Coast Range are laden with moisture which falls +in the form of rain or snow on the west slope of the Cascades. The trees +are nourished by this moisture through a long season of annual growth, +and form an evergreen forest which is, in some respects, the most +remarkable in the world. This forest, distinguished by the extraordinary +size and beauty of the trees and by the density of the stand, extends +into the deep valleys of the rivers which have their sources in the +glaciers. On the dividing ridges and in the upper stream basins the +composition and character of the forest change with the increasing +severity of the climate. + +The distribution of the different species of trees according to the +intervals of altitude at which they occur separate the forests of the +Mount Rainier National Park into different types. The lines of +separation are to some extent also determined by complex conditions of +slope, exposure, and moisture. The successive forest belts are uniform +in the composition of their central areas, but blend and overlap where +they come together. + +The low valleys of the main and west forks of White River, of the +Carbon, the Mowich, the Nisqually, and the Ohanopecosh are covered with +a dense and somber forest of fir, hemlock, and cedar. The trees, pushing +upward for light, are very tall and free from limbs for more than half +their height. Their tops form a continuous cover which the sunshine +rarely penetrates, and on which the light snows of early winter fall and +melt, without reaching the ground. Even in midsummer the light is soft +and shaded, and the air cool and humid. In the wintertime the young +growth is sheltered from wind and the severity of the cold is tempered +by the protecting mountain ranges. Saved from fire by the uniform +dampness of the air the trees grow until they decay and fall from old +age. They are succeeded by the suppressed younger trees. The forest +remains mature, not uniformly sound and vigorous, yet not decreasing as +a whole in size and volume. Individuals perish, but the character of the +forest is constant. The deep alluvial soil covered with moss and decayed +vegetation nourishes a luxuriant tangled undergrowth of vine maple, +willow, and devil's-club. The forest floor is covered with a deep layer +of decayed vegetation and is encumbered with fallen and mossy logs and +upturned stumps. The explorer who leaves the trails must be a strong and +active man if he can carry his pack 6 or 8 miles in a long summer day. + +Ascending from the river bottoms to the lower slopes of the dividing +ridges the forest becomes more open and the trees are smaller. Salal, +Oregon grape, and huckleberry bushes take the place of the taller +undergrowth of the valleys. Up to 3,000 feet the Douglas fir and the +hemlock still are the dominant species. Above this altitude new species +are found intermingled with the trees typical of the lowland, but +forming a distinct forest type. The noble and amabilis fir appear, +sometimes growing in pure stands, but more often associated with the +Douglas fir and western hemlock at the lower limits of the type, and +with alpine fir and mountain hemlock at the upper limit. + +Nearly all the trees of this type have deep and wide-spreading roots +which serve to hold in place the surface deposit of volcanic pumice +which covers the slopes of the mountain. Evidence afforded by the after +effects of forest fires in other parts of the Cascades indicates that +the destruction of the forest on the mountain sides is followed by +erosion. Heavy rains and the melting of the upper snow banks by warm +Chinook winds combine to produce a surface run-off that denudes the +steeper declivities down to the underlying bedrock. + +At elevations above 4,500 feet the lowland trees have disappeared +entirely. Subalpine species adapted to withstand the burden of deep snow +take their place. Mountain hemlock, alpine fir, and Engelmann spruce +grow singly and in scattered groups or form open groves alternating with +grassy parks and rocky ridges. The symmetrical outline of the slender +pyramidal crowns and rapidly tapering trunks of the spruce and alpine +fir trees that stand singly on the greensward of the open parks bring to +mind the closely trimmed cultivated evergreens that adorn city parks and +lawns. Their lower branches reach the ground and the tops terminate in +slender upright spires. + +As timber line is approached tree growth is confined to dwarfed and +flattened mountain hemlocks, alpine firs, and the white-bark pines +firmly rooted among the crevices of the rocks. + +The extreme limit of tree growth on Mount Rainier is 7,600 feet above +sea level. There is no well-defined timber line. Scattered clumps of low +stunted trees occur up to 7,000 feet. A few very small and flattened +mountain hemlocks grow above this elevation. A very large part of the +area above 4,500 feet consists of glaciers, talus slopes, barren rocky +peaks, and open parks. Basins at the heads of canyons in the high +mountains are usually treeless, on account of the great depth of snow +which accumulates in them during the winter. On the steep, smooth upper +inclines the snow banks frequently slip and form slides which acquire +momentum as they rush down the mountain side and break and carry away +large trees. Repeated snowslides in the same place keep the slopes +nonforested, and their track is marked by light green strips of brush +and herbage. + +The transition of the forest from its lowland to its extreme alpine type +is one of the most interesting features of a visit to the mountain. +Entering the park at the western boundary close to the Nisqually River +the road skirts the base of the lightly timbered spurs and passes into a +forest of large and old Douglas fir and western hemlock. Red cedars grow +along the streams that cross the road. Little yew trees and vine maples +mingle with the young conifers that form the undergrowth; the gloom of +the forest is occasionally relieved by the white bark of alders and the +smooth gray stems of the cottonwoods that grow on the sandy bank of the +Nisqually. After the road crosses the Rainier Fork, noble fir and +amabilis fir appear, but the Douglas fir and western hemlock are still +the prevailing species. + +Above Longmire Springs the noble and amabilis fir, mixed with western +hemlock, become the dominant type. The trees are shorter and the +branches heavier. Mountain ash and yellow cypress grow on the margin of +the mountain streams. Huckleberry bushes take the place of the taller +undergrowth of the valley. + +Above Narada Falls the forest is more open, and the trees are still +smaller. Mountain hemlock and alpine fir succeed the trees of the lower +slope. Little glades and mountain meadows are seen. They become larger +and more numerous and the traveler soon enters the open park of Paradise +Valley, in which are but scattered groves of trees. The same successive +altitudinal types are met in ascending to Moraine and Grand Parks by way +of the Carbon Valley, and in following the Mowich watershed, Crater +Lake, and Spray Park routes. + +Approaching the park from the east the routes pass through open western +yellow pine forests and western larch stands. Since Mount Rainier is +west of and apart from the summit line, these species which are peculiar +to the eastern slope are not found within the limits of the park. + + + + +EFFECTS OF FIRE. + +[Illustration: FIG. 1.--Whitened spectral monuments of a former forest +which was swept by a severe forest fire in 1885. Taken along the road to +Camp of the Clouds at an altitude of 5,500 feet. + +Photograph by A.H. Barnes.] + + +Notwithstanding the shortness of the summer season at high altitudes, +the subalpine forests in some parts of the park have suffered severely +from fire (fig. 1). The bare white trunks of fire-killed amabilis and +alpine firs bear witness to numerous fires which occurred from time to +time before the regulations governing the park went into effect. The +little resin pockets in the bark of these trees blaze fiercely for a +short time and the heat separates the bark from the trunk. In this way +the tree is killed, although the naked trunk is left untouched by fire. +The destruction of the alpine forest in this way is often erroneously +attributed to disease or to the depredations of insects. + +There has been little apparent change in the alpine burns within the +last 30 years. Reforestation at high altitudes is extremely slow. The +seed production is rather scanty and the ground conditions are not +favorable for its reproduction. It will take more than one century for +nature to replace the beautiful groves which have been destroyed by the +carelessness of the first visitors to the mountain. + +At low elevations the forest recovers more rapidly from the effects of +fire. Between the subalpine areas and the river valleys there are +several large ancient burns which are partly reforested. The most +extensive of these tracts is the Muddy Fork burn. It is crossed by the +Stevens Canyon Trail from Reflection Lakes through the Ohanopecosh Hot +Springs. This burn includes an area of 20 square miles in the park and +extends north nearly to the glaciers and south for several miles beyond +the park boundary nearly to the main Cowlitz River. The open sunlit +spaces and wide outlooks afforded by reforested tracts of this character +present a strong contrast to the deep shades and dim vistas of the +primitive forest. On the whole they have a cheerful and pleasing +appearance, very different from the sad, desolate aspect of the alpine +burns which less kindly conditions of climate and exposure have kept +from reforestation. + +The original forest was fire killed many years before the coming of the +white man. A few naked and weather beaten stubs are still standing. Only +the larger of the fallen trunks remain, and these are rotten except for +a few seasoned and weatherworn shells. The second growth is of all ages, +from seedlings to trees 12 to 14 inches in diameter. Vine maple, willow, +and mountain ash have sprung up along the streams and the hillsides are +covered with huckleberry bushes and a variety of grasses and flowering +plants. + +Similar old burns are found on the ridge between Huckleberry Creek and +White River, in the northeastern part of the park, and on the ridge +between Tahoma Creek and Kautz Creek below Henrys Hunting Ground. + +The old burns in the middle altitudes of the park occupy regions once +frequented by the Klickitat Indians. Every summer parties of hunters and +berry pickers from the sagebrush plains crossed the Cascades with their +horses. They followed the high divides and open summits of the secondary +ridges until they came around to the open parks about Mount Rainier +where they turned their horses out to graze and made their summer camp. +The woman picked huckleberries and the men hunted deer and goats. They +made great fires to dry their berries and kindled smudges to protect +their horses from flies. It was also their custom to systematically set +out fires as they returned. Burning made the country better for the +Indians. The fires kept down the brush and made it more accessible. Deer +could be more easily seen and tracked and the huckleberry patches spread +more widely over the hills. + +No considerable part of the lower forests of the park has been burned. +The principal danger is from lightning. However, few of the trees struck +are ignited and these fires are usually extinguished by the rain. On +account of the coolness of the air and its greater humidity the fire +danger in the forests on the lower slopes of Mount Rainier seems much +less than it is in corresponding situations in the main range of the +Cascades. + + + + +AGE AND DIMENSIONS OF TREES. + + +Trees grow more rapidly at low altitudes than at higher and cooler +elevations. Under similar conditions some species increase in size +faster than others, but the rate of growth depends principally upon +environment. The average increase at the stump in valley land is about 1 +inch in 6 years. A Douglas fir growing along the stage road between the +park boundary and Longmire's, at the age of 90 to 120 years may have a +breast diameter of 20 inches and yield 700 feet of saw timber. But many +of the trees of this size may be much older on account of having grown +in the shade or under other adverse conditions. The trees between 200 +and 300 years of age are often 40 to 50 inches in diameter and may yield +an average of from 2,700 to 5,500 board feet. The largest Douglas firs +are sometimes over 400 years old and 60 to 70 inches in diameter. Such +trees when sound will produce over 8,000 feet of lumber. + +The western red cedar has a shorter and more tapering trunk and its +volume in board feet is proportionally smaller. A tree 50 inches in +diameter and 175 feet high contains about 3,400 board feet. + +The size of the trees decreases rapidly at higher elevations. In the +subalpine forest the annual growth is very small. At elevations of 6,000 +feet the white-bark pine requires 200 years to attain a diameter of 10 +or 12 inches. The annual rings are so close together that they can not +be distinguished without a magnifying glass. + + + + +DESCRIPTIONS OF SPECIES. + + +DOUGLAS FIR (PSEUDOTSUGA TAXIFOLIA). + +The Douglas fir (figs. 2, 3, 4, and 5) is the best known and the most +important timber tree of western North America. It is found from +British Columbia southward to northern Mexico. The finest forests occur +in Oregon and Washington at low elevations. The Douglas fir is common in +the park up to 3,500 feet, sometimes in nearly pure stands, but more +often mixed with other species. It grows in all situations. In the +higher mountains it prefers warm southern exposures and is seldom found +on wind-swept ridges. It seeds annually, but most profusely at intervals +three or four years apart. The red squirrels gather and store large +quantities of the cones in order to provide a supply of the seeds for +their winter rations. The growth of the young tree is very rapid. As the +tree becomes older the rate of growth varies with the situation and the +character of the soil so that the size does not closely determine the +age of the tree. + +[Illustration: FIG. 2.--Douglas fir (_Pseudotsuga taxifolia_).] + +The Douglas fir is a long-lived tree, and specimens are occasionally +found 250 to 270 feet high and over 8 feet in diameter and between 400 +and 500 years in age. It reaches its greatest height and most perfect +proportions in mature even-age stands growing on fairly moist +well-drained bench lands. Under these conditions it is a very tall and +beautiful tree. The trunk is straight, round, and free from branches for +two-thirds of its height and tapers gently to the crown. The dark-brown +deep-furrowed bark is 5 to 10 inches thick at the base of the tree. + +The Douglas fir ranks first among the trees of the Pacific slope in +importance for the production of lumber. It is often sold under the name +of Oregon pine. Lumber dealers class the coarse-grained reddish wood +produced by the young growth in open forests as "red fir." The older +growth produced when the forest is more dense is a finer grained and +more valuable wood, sold under the name of "yellow fir." + +[Illustration: FIG. 3.--Douglas fir (_Pseudotsuga taxifolia_).] + +The Douglas fir is used for nearly all purposes where durability, +strength, and hardness are desirable. It is made into dimension timbers, +lumber, flooring, and is particularly adapted for masts and spars. The +lumber is shipped by rail to the Middle Western States. The foreign +cargo shipments are made to all parts of the world. The greatest amount +goes to Australia, the west and east coasts of South America, China, the +United Kingdom, and Europe, Japan, and the South Sea Islands. Coastwise +shipments are made to California, Alaska, and Panama. Large quantities +of the seed of this tree are sent to Europe, where the Douglas fir is +grown for timber and for ornament. + + +WESTERN RED CEDAR (THUJA PLICATA.)[1] + +[Illustration: FIG. 4.--Douglas fir (_Pseudotsuga taxifolia_).] + +The western red cedar (title page and fig. 5) ranges from south-eastern +Alaska to northern California. It is a common tree in the park. It +occurs in patches along the river bottoms where the flat scalelike +foliage is conspicuous among the needle-shaped leaves of the hemlock and +fir. The bark is fibrous in appearance and may be readily separated into +long strips. The trunks of the older trees are swelled and irregularly +fluted at the base. The leaves are fragrant and the wood has a pleasing +aromatic odor. Nearly all the large trees are hollow at the butt. The +roots spread laterally to a great distance, but extend only for a short +distance below the surface of the ground. The tree is easily overthrown +by the wind and usually grows in sheltered localities. On account of the +thinness of the bark it is easily killed by fire. + +[Illustration: FIG. 5.--Two big Douglas firs and a western red cedar (on +the left) along the road up the Nisqually Valley, Mount Rainier National +Park. + +Photograph by A.H. Denman.] + +The red cedar flourishes on fertile and well-watered soils near sea +level, where it grows to an enormous size. In the park it is a smaller +tree, 150 to 170 feet high and rarely more than 4 or 5 feet through +above the swollen butt. It grows occasionally up to an altitude of 4,000 +feet, but is a small and insignificant tree in the high mountains. + +In the sapling stage the red cedar grows rapidly. The mature tree +increases very slowly in size. It exceeds all other trees in the +Cascades in longevity. Individuals more than 500 years old are not +uncommon and there is a well-authenticated instance where the annual +rings indicated a growth of more than 1,100 years. + +While the red cedar forms no great proportion of the forest of the +Pacific Northwest, it is peculiarly valuable to the pioneer on account +of the durability of the wood and the ease with which it can be split +into boards, shakes, and planking. The early settlers used cedar split +by hand as a substitute for sawn lumber in flooring and finishing their +cabins and for the tables and shelves with which they were furnished. +The Indians hollowed the great trunks with fire and made them into +canoes, some of which were large and seaworthy enough to be used on the +Sound and in making voyages along the coast. They wove the fibrous roots +into baskets that carried water and plaited the bark into matting. The +wood of the red cedar is reddish brown in color. It is soft, light, and +very brittle, but very durable. It is extensively used for shingles, the +manufacture of which forms one of the important industries of the State. +The clear logs are sawed into lumber used for siding, interior and +exterior finish, moldings, tank stock, and similar purposes. Common logs +are utilized for shingles. In many localities the entire tree is cut +into 52-inch bolts, which are hauled to the mills or floated to them +down the streams. + +The western red cedar makes excellent posts and rails for farm fences. +The young trees are used for telegraph and telephone poles. + + +WESTERN HEMLOCK (TSUGA HETEROPHYLLA). + +Next to the Douglas fir the western hemlock is the most abundant tree in +the forests of Oregon and Washington. It occurs from Alaska southward to +northern California. About Mount Rainier it is found up to an altitude +of 5,000 feet. In the river valleys in moist situations it is a large +tree, sometimes reaching a height of 250 feet and a diameter of 5 feet. +On the high ridges it is stunted. It grows best on moist deep soils in +dense forests, but thrives under almost all conditions of soil and +exposure if provided with plenty of moisture. + +Western hemlock (figs. 6 and 7) is usually associated with Douglas fir +and red cedar, but sometimes forms a forest of nearly pure growth. The +hemlock produces abundant seed each year, although it is more prolific +at irregular intervals. The seeds germinate readily on decayed moss and +rotten wood as well as upon the mineral soil. Seedlings frequently grow +on fallen logs and extend their vigorous roots around the side until +they reach the ground and become firmly anchored in it. Young hemlocks +thrive in the shade. On logged-off areas which have not been burned over +and which are partially shaded by uncut trees, the reproduction of +hemlock springs up, to the exclusion of the more valuable Douglas fir. + +[Illustration: FIG. 6.--The lower slope forest, near Longmire Springs, +altitude 3,000 feet, here composed largely of western hemlock (_Tsuga +heterophylla_); the tree on the extreme left is a Douglas fir +(_Pseudotsuga taxifolia_). + +Photograph by A.H. Barnes.] + +The hemlock is long lived and grows slowly. The largest trees are from +200 to 500 years old and are usually hollow-hearted. The bark is thin +and the tree very easily killed by ground fire. The wood of the hemlock +is tough, light, and straight grained. It is not as durable as the +Douglas fir and decays rapidly when exposed to the weather. The clear +lumber is suitable for interior finish. The wood is also used for +flooring, joists, lath, and paper pulp. The common and rough lumber does +not find a ready market, except for the limited amount used in temporary +construction. The western hemlock is, however, superior to the eastern +hemlock, and its value will probably be recognized as its usefulness for +many purposes becomes better known. + + +WESTERN WHITE PINE (PINUS MONTICOLA). + +[Illustration: FIG. 7.--A forest of Douglas fir, with an understory of +western hemlock, on the lower slopes of the hills, Mount Rainier +National Park. + +Photograph by A.H. Denman.] + +The western white pine (fig. 8) is found from southern Alaska to +northern California. In the park it occurs occasionally up to 4,000 +feet. It usually grows on level benches and gentle slopes associated +with Douglas fir, western hemlock, and noble and amabilis fir. It +reaches its best development at elevations of from 3,000 to 3,500 feet, +where it attains a height of 150 feet and a diameter of 40 inches. The +shaft is straight, cylindrical, and clear of limbs. It bears a small, +narrow crown of drooping branches. In open areas, where it is exposed to +sunlight, its mode of growth is wholly different. The trunk is short, +rapidly tapering, and bears wide-spreading branches nearly to the +ground. At high elevations the western white pine is very short and +stunted. + +[Illustration: FIG. 8.--Western white pine (_Pinus monticola_). + +Diameter 24 inches, height 50 feet.] + +Although the western white pine is not a common tree in the park, it is +often noticed on account of its abundance of slender, pendant cones, 6 +to 10 inches long. They mature every two years and shed their seed early +in September. The seed are provided with long wings and are often +carried by the wind for a great distance from the parent tree. + +The wood is light, soft, free from pitch, and the most valuable of any +of the pines of the Cascades. It is used for interior finish, pattern +making, and other purposes. The supply of this tree is so limited that +it is not of great commercial importance in the Mount Rainier region. + + +AMABILIS FIR (ABIES AMABILIS).[2] + +Amabilis fir (figs. 9 and 10) ranges from southern Alaska to Oregon. It +is abundant in the park at elevations from 2,500 to 5,000 feet on level +bench lands, and gentle slopes with a northern exposure. It is rarely +found in unmixed stands, but is usually associated with western hemlock, +Douglas fir, and noble fir. The largest trees are 150 to 180 feet high +and 3 to 5 feet in diameter. In dense forests the stem is free from +branches for 50 to 100 feet. + +[Illustration: FIG. 9.--Amabilis fir (_Abies amabilis_).] + +At altitudes over 4,000 feet, small amabilis firs often occur in +clusters and open groves. The trunk is covered with branches which grow +to the ground, turning downward and outward in long graceful curves, +admirably adapted to withstand the pressure of the frozen snow. The +foliage is a deep and brilliant green, forming a strong contrast to the +dark-purple cones. The seeds ripen each year early in October. Like the +seed of the other alpine species of trees that grow in the cold and +humid climate of the high Cascades, they soon lose their vitality when +stored in dry places. The amabilis fir is grown in Europe as an +ornamental tree. Under cultivation it loses much of the natural grace +and beauty which it acquired in adapting itself to the deep snows and +long winters of its native environment. + +[Illustration: FIG. 10.--The forests of western hemlock, amabilis fir, +and other species, on the middle slopes of the mountains, along the +Crater Lake trail, Mount Rainier National Park. + +Photograph by Geo. O. Ceasar.] + +The bark is thin and the tree is easily killed by fire. The wood is +straw colored, compact, and straight grained. It is not strong and +splits easily. It is sold to some extent under the name of larch or +mixed with inferior grades of fir and hemlock. The lumber is of little +value commercially. + + +NOBLE FIR (ABIES NOBILIS). + +The noble fir (figs. 11 and 12) is a common mountain tree in the western +parts of Washington and Oregon. Like amabilis fir, it is usually called +larch by lumbermen. About Mount Rainier it grows at elevations of from +3,500 to 5,000 feet in dense stands associated with amabilis fir, +western hemlock, and Douglas fir. The noble fir avoids steep side hills +and exposed situations. In moist soils on flats and gentle slopes it +often reaches a height of from 150 to 200 feet. The tall and upright +trunk supports a rounded crown of bluish green foliage, which is very +noticeable among the purer green leaves of its associates. The branches +are short, thick, and crowded with stiff, flattened leaves, which turn +upward and outward. The light-green bract-covered cones are sometimes 6 +inches long and nearly 3 inches thick. They ripen early in September. +Seed is borne every year, although in some seasons it is much more +abundant than in others. + +[Illustration: FIG. 11.--Noble fir (_Abies nobilis_).] + +[Illustration: FIG. 12.--Noble fir (_Abies nobilis_), 6 feet in +diameter.] + +The wood is strong, close grained, and elastic. It is used for lumber +and particularly for inside finishing. The noble fir is a slow-growing +and long-lived tree. Old trees in mixed forests are easily distinguished +from the associated species by the ashy-brown outer bark broken into +large irregular plates. + + +ALPINE FIR (ABIES LASIOCARPA).[3] + +[Illustration: FIG. 13.--A cluster of Alpine firs (_Abies lasiocarpa_), +whose spire-shaped crowns are characteristic, at 5,500 feet altitude, in +Cowlitz Park, Mount Rainier National Park. + +Photograph by A.H. Barnes.] + +The alpine fir (fig. 13) ranges from Alaska to New Mexico. It is a +common tree in the park at elevations above 4,500 feet. It is a tree of +the high mountains and with the white bark pine and the mountain +hemlock, is found up to the limit of arborescent life. It demands +moisture and is generally restricted to regions of deep snowfall. + +The alpine fir occurs in unmixed stands, but is often associated with +the mountain hemlock. At the lower levels of its range it is a +fair-sized tree 50 or 60 feet high. The crown of deep-green foliage is +broad at the base and tapers to the top, where it terminates in a +slender, pointed tip. At its upper limit it becomes a stunted shrub, +with wide extended branches resting on the ground. + +The alpine fir bears upright clusters of deep-purple cones. It seeds +sparingly each year. The seasons of heavy seed production occur at +intervals of three or four years. The wood is soft and splits easily. It +is of no commercial value. The tree is easily killed by fire, which +blisters the thin bark and frequently springs into the drooping lower +branches. + + +GRAND FIR (ABIES GRANDIS.)[4] + +The grand fir (fig. 14), like several other species, is generally given +the name of white fir on account of its smooth, light-colored bark. It +is a common tree in the river bottoms from British Columbia south to +northern California. In the Mount Rainier National Park it occurs up to +4,000 feet. The grand fir is a moisture-loving tree and is usually found +firmly rooted in deep alluvial bottom lands along the banks of streams. +With the Douglas fir, hemlock, and red cedar it forms the dense forest +characteristic of the lower mountain valleys. + +In favorable conditions the grand fir grows to a height of from 100 to +200 feet and is a noble and stately tree. The trunk tapers rapidly and +bears a rounded pyramidal crown. In dense forests the trunk is clear for +half its height, but where the trees stand in the open it carries its +branches nearly to the ground. The leaves are a bright and shining +green. The large light-green cones mature early in the fall. The wood is +soft and very heavy before it is seasoned. It rots in a very short time +when laid on the ground. When dry it is white, coarse-grained, light, +and odorous. It is used for interior finish and for crates and packing +boxes, but is of little value commercially. + + +ENGELMANN SPRUCE (PICEA ENGELMANNI). + +The Engelmann spruce (fig. 15) is a mountain tree ranging from British +Columbia to Arizona and New Mexico. It is common along the summit and on +the east side of the Cascade Range and occurs on the northeastern and +eastern slopes of Mount Rainier at elevations of from 3,500 to 6,000 +feet. + +This tree requires a moist soil and prefers cool northern exposures. Up +to 5,000 feet it commonly grows in sheltered basins at the head of +canyons and in stream valleys. At its upper limits it is common on flats +and depressions and about lakes on level summits. It avoids steep +mountain sides and exposed situations. + +[Illustration: FIG. 14.--Grand fir (_Abies grandis_).] + +The Engelmann spruce is easily distinguished from its associates by its +stiff, bluish-green pointed leaves, which prick the hand when they are +grasped. In the mountain parks it is a handsome tree 50 to 60 feet high. +When it stands apart from other trees the lower branches are thick and +long and extend to the ground. The crown is very broad at the base, but +narrow and spirelike at the top. The Engelmann spruce reaches its best +development at low elevations, where it often grows in dense, pure +stands. Under these conditions it reaches a height of 100 feet. The bole +is straight and free from limbs and the top is short and compact. + +[Illustration: FIG. 15.--Engelmann spruce (_Picea engelmanni_).] + +The young cones are massed in upright green and purple clusters at the +tips of the upper branches. They are notable for the purity and +brilliance of their coloring. As they mature they become pendant and +fade to a light brown. The seed is produced in abundance nearly every +year, although small and seedling trees are not usually numerous. + +The wood is soft, white, compact, and even grained. It is free from +pitch and odor. It is valuable for boxing, cooperage, and certain kinds +of finish. It is also an excellent material for the tops of violins and +other stringed instruments. The Engelmann spruce is, however, of little +importance as a timber tree on account of its scarcity and the scattered +stands in which it grows. It is a long-lived tree unless attacked by +fire, to which it is very vulnerable. + +[Illustration: FIG. 16.--A group of yellow cypresses (_Chamaecyparis +nootkatensis_) on the high slopes of Mount Rainier National Park, +altitude about 6,000 feet. + +Photograph by A.H. Barnes.] + + +YELLOW CYPRESS (CHAMAECYPARIS NOOTKATENSIS). + +Yellow cypress (fig. 16) ranges from the seacoast of southern Alaska +south to the mountains of Washington and Oregon. It occurs in the park +up to the elevation of 7,000 feet. It is common on northern exposures, +along streams, and in basins at the head of canyons. It also grows on +crests and ridges, where the frequent showers and fogs supply the +moisture which it demands. In sheltered localities it grows to a height +of 75 or 80 feet, but it is commonly a small tree with, a bent and +twisted stem, which, with its pendulous branches, presents a somewhat +scrubby appearance. The foliage is green, sometimes with a bluish tinge. +It resembles that of the common western red cedar, but the leaves are +sharper, more pointed, and rougher to handle. The small, rounded, +inconspicuous cones are produced somewhat sparingly. The bark of the +young tree is red. On the mature tree it becomes gray and fibrous. The +wood is yellow, close grained, and aromatic. Unlike that of the western +red cedar, the trunk is usually sound to the center. The wood is used +for boat building and cabinetwork. It is very durable. + +The yellow cypress grows very slowly, particularly at high elevations. +The number of annual rings on trees 15 to 20 inches in diameter indicate +that they are over 200 years old. + + +LODGEPOLE PINE (PINUS CONTORTA). + +Lodgepole pine (fig. 17) is widely distributed from Alaska to Lower +California and eastward through the Rockies to Dakota and Colorado. It +occurs sparingly in the park up to 5,000 feet above sea level. It adapts +itself easily to the different conditions of soil, moisture, and +exposure. + +[Illustration: FIG. 17.--Lodgepole pine (_Pinus contorta_), 60 inches in +diameter.] + +This tree varies greatly in the different regions where it is found. +About Mount Rainier it does not often exceed 20 to 40 feet in height +and is often a much smaller tree. It produces cones at the age of 5 to 7 +years. The foliage is a yellowish green. At high elevations the leaves +have a peculiar whorled appearance which gives it a different aspect +from that of the other pines. The short, heavily limbed trunk bears no +resemblance to the tall and slender shaft of the lodgepole pine of the +Rocky Mountains. The root system is shallow and the tree is easily fire +killed. The wood of the variety which grows in the park is of no +commercial value. + +[Illustration: FIG. 18.--The feathery foliage of mountain hemlock +(_Tsuga mertensiana_), Grand Park, Mount Rainier National Park. + +Photograph by A.H. Denman.] + + +MOUNTAIN HEMLOCK (TSUGA MERTENSIANA). + +The mountain hemlock (figs. 18, 19, and 20) is found on the Pacific +coast from the Sierras of California to the northern part of Alaska +where it grows at sea level. On Mount Rainier it occurs at altitudes of +from 3,500 to 7,500 feet. It forms dense forests under 4,500 feet, where +it is often a fair-sized tree 50 to 90 feet high. With the ascent of the +mountain it diminishes in height and the branches become gnarled and +twisted. Near timber line the trunk is dwarfed and bent at the base and +the crown becomes a flattened mass of branches lying close to the ground +(fig. 20). + +[Illustration: FIG. 19.--Two solitary mountain hemlocks (_Tsuga +mertensiana_), Spray Park, Mount Rainier National Park. + +Photograph by Geo. O. Ceasar.] + +The mountain hemlock is abundant on high, rocky ridges, but the best +stands are on cool, moist soil at the heads of ravines, on flats, and on +gentle slopes with a northern exposure. + +This tree seeds every year. In good seed years the upper branches are +laden with a profusion of beautiful, deep-purple cones, often in such +abundance as to bend down the branchlets with their weight. The +reproduction is slow. In the high mountains the trees are buried in snow +from October to late in June, and the growing season is very short. + + +WHITE-BARK PINE (PINUS ALBICAULIS). + +[Illustration: FIG. 20.--A gnarled, wind-swept mountain hemlock (_Tsuga +mertensiana_), near the upper limits of tree growth, Spray Park, Mount +Rainier National Park. + +Photograph by A.H. Denman.] + +The white-bark pine (fig. 21) grows close to timber line in the +mountains of the Pacific coast from British Columbia to southern +California. In the Canadian Rockies it extends north to the fifty-third +parallel. It is the most alpine of all the pines. Its lower limit on +Mount Rainier is about 5,000 feet above sea level. In sheltered places +where the soil is deep the trees are sometimes 30 to 40 feet high and 20 +inches in diameter. The trunks are free from limbs for 8 or 10 feet. The +outer bark, from which the tree derives its name, consists of thin, +light-gray scales. + +As the white-bark pine advances up the mountain its habit changes +rapidly. The stem shortens and becomes gnarled and twisted. The tough, +flexible branches reach the ground and spread over it to a great +distance from the tree. On rocky summits and the bleak crests of +wind-swept ridges the twisted trunk and branches are quite prostrate and +the crown is a dense flattened mass of foliage. + +The roots of the tree are deep, long, and tenacious. They spread wide +and deep and cling so firmly to the rocks that the tree is rarely +overthrown by the violent winds that sweep over the mountain. + +[Illustration: FIG. 21.--A white-bark pine (_Pinus albicaulis_) in its +characteristic mountain habitat, Mount Rainier National Park. + +Photograph by A.H. Denman.] + +The thick, purple cones require two years to mature. They ripen early in +September and produce chocolate-brown seeds a little larger than a grain +of corn. They are much relished by the Klickitat Indians, who go to +considerable pains to secure them. The wood is close grained and +resinous. It makes excellent fuel for the camp fires of sheep herders +and mountain travelers. + + +WESTERN YEW (TAXUS BREVIFOLIA).[5] + +The western yew is found from southern Alaska to northern California. It +occurs in the park up to 4,000 feet, growing in rich, gravelly soil on +moist flats and benches and in deep ravines. It is a small branching +tree, rarely over 20 feet high. The bark is purple or reddish brown. The +branches extend almost to the ground. It bears a small, bright, +amber-red berry. + +The dark-brown or red heartwood is very tough, hard and heavy. It takes +a fine polish and is used for fancy cabinetwork. The Indians use it for +spear handles, bows, and fishhooks. + +[Illustration: FIG. 22.--Broadleaf maple (_Acer macrophyllum_).] + + +DECIDUOUS TREES. + +The silva of the Western Cascades is rich in evergreens remarkable for +their size and beauty. The deciduous trees are few and insignificant. +The forests of the park are almost wholly coniferous. Vine maple and +willow are found as undergrowth. On the margins of rivers there are +occasional groves of alders and cottonwoods. The lighter hues of the +branching trunks and the changing tints of the foliage in these patches +of broad-leaved woodland present a pleasing diversity to the evergreen +forest. + +Broadleaf maple (_Acer macrophyllum_) (fig. 22), the largest of the +Pacific coast maples, ranges from Alaska to southern California. Near +sea level it often attains a height of 50 or 60 feet. In the park it is +a short-stemmed, branching tree, occasionally found on the borders of +streams. It grows at elevations under 3,000 feet. + +[Illustration: FIG. 23.--Vine maple (_Acer circinatum_).] + +Vine maple (_Acer circinatum_) (fig. 23) is abundant from British +Columbia to northern California. On rich river bottoms it is sometimes +15 to 20 feet high and 6 inches in diameter. In the park it is usually a +bush or low shrub with a bent and curiously crooked stem, growing along +streams and as undergrowth in the forest. It is very common up to 3,000 +feet. In autumn the leaves are a bright scarlet. The wood is tough and +elastic and makes a hot and lasting fire. + +[Illustration: FIG. 24.--Red alder (_Alnus oregona_).] + +[Illustration: FIG. 25.--Black cottonwood (_Populus trichocarpa_).] + +Red alder (_Alnus oregona_) (fig. 24) occurs from Alaska to southern +California. It is common about Mount Rainier, in river bottoms, on the +banks of large streams, and in swampy places. It usually grows to a +height of 30 or 40 feet. The bark varies from nearly white to light +gray. It is the most abundant of all the deciduous trees in the park. + +Black cottonwood (_Populus trichocarpa_) (fig. 25) is common from Alaska +to southern California. It is occasionally found in the park up to 4,000 +feet. It grows along streams and on sandy river bottoms often associated +with the alder. The leaves are almost always in motion, very gentle +winds being sufficient to make them twinkle and turn. + +The wood is soft, but tough and compact. It is used for staves, +woodenware, wood pulp, trunks, barrels, and for drawer bottoms. + + +FOOTNOTES + +[1] This species is known as arbor vitae in Glacier Park. + +[2] This species is known as silver fir in Crater Lake Park. + +[3] This species is known as balsam in Glacier and Yellowstone Parks. + +[4] This species is known as silver fir in Yellowstone and Glacier +Parks. + +[5] This species is known as Oregon yew in Crater Lake National Park and +as yew in Yellowstone and Glacier Parks. + + + + +INDEX TO SPECIES DESCRIBED. + +[Roman numerals indicate pages containing descriptions; italic numerals +indicate pages containing illustrations.] + + + _Abies amabilis_ 15-16, _15_, _16_ + _grandis_ 20, _21_ + _lasiocarpa_ 19-20, _19_ + _nobilis_ 17-19, _17_, _18_ + + _Acer circinatum_ 30, _30_ + _macrophyllum_ 29, _29_ + + Alder, red (_Alnus oregona_) 30, _31_ + + _Alnus oregona_ 30, _31_ + + Alpine fir (_Abies lasiocarpa_) 19-20, _19_ + + Amabilis fir (_Abies amabilis_) 15-16, _15_, _16_ + + Arbor vitae. _See_ Western red cedar. + + + Balsam. _See_ Alpine fir. + + Black cottonwood (_Populus trichocarpa_) 30-32, _31_ + + Broadleaf maple (_Acer macrophyllum_) 29, _29_ + + + Cedar, western red (_Thuja plicata_) 9-11, _10_ + + _Chamaecyparis nootkatensis_ 23-24, _23_ + + Cottonwood, black (_Populus trichocarpa_) 30-32, _31_ + + Cypress, yellow (_Chamaecyparis nootkatensis_) 23-24, _23_ + + + Douglas fir (_Pseudotsuga taxifolia_) 6-8, _7_, _8_, _9_, _10_, + _12_, _13_ + + + Engelmann spruce (_Picea engelmanni_) 20-23, _22_ + + + Fir, alpine (_Abies lasiocarpa_) 19-20, _19_ + amabilis (_Abies amabilis_) 15-16, _15_, _16_ + Douglas (_Pseudotsuga taxifolia_) 6-8, _7_, _8_, _9_, _10_, + _12_, _13_ + grand (_Abies grandis_) 20, _21_ + noble (_Abies nobilis_) 17-19, _17_, _18_ + silver. _See_ Fir, amabilis; Fir, grand. + + + Grand fir (_Abies grandis_) 20, _21_ + + + Hemlock, mountain (_Tsuga mertensiana_) 25-27, _25_, _26_, _27_ + western (_Tsuga heterophylla_) 11-13, _12_, _13_, _16_ + + + Larch. _See_ Noble fir; Amabilis fir. + + Lodgepole pine (_Pinus contorta_) 24-25, _24_ + + + Maple, broadleaf (_Acer macrophyllum_) 29, _29_ + vine (_Acer circinatum_) 30, _30_ + + Mountain hemlock (_Tsuga mertensiana_) 25-27, _25_, _26_, _27_ + + + Noble fir (_Abies nobilis_) 17-19, _17_, _18_ + + + Oregon yew. _See_ Western yew. + + + _Picea engelmanni_ 20-23, _22_ + + Pine, lodgepole (_Pinus contorta_) 24-25, _24_ + western white (_Pinus monticola_) 13-15, _14_ + white-bark (_Pinus albicaulis_) 27-28, _28_ + + _Pinus albicaulis_ 27-28, _28_ + _contorta_ 24-25, _24_ + _monticola_ 13-15, _14_ + + _Populus trichocarpa_ 30-32, _31_ + + _Pseudotsuga taxifolia_ 6-8, _7_, _8_, _9_, _10_, _12_, _13_ + + + Red alder (_Alnus oregona_) 30, _31_ + cedar, western (_Thuja plicata_) 9-11, _10_ + + + Silver fir. _See_ Amabilis fir; Grand fir. + + Spruce, Engelmann (_Picea engelmanni_) 20-23, _22_ + + + _Taxus brevifolia_ 28-29 + + _Thuja plicata_ 9-11, _10_ + + _Tsuga heterophylla_ 11-13, _12_, _13_, _16_ + _mertensiana_ 25-27, _25_, _26_, _27_ + + + Vine maple (_Acer circinatum_) 30, _30_ + + + Western hemlock (_Tsuga heterophylla_) 11-13, _12_, _13_, _16_ + red cedar (_Thuja plicata_) 9-11, _10_ + white pine (_Pinus monticola_) 13-15, _14_ + yew (_Taxus brevifolia_) 28-29 + + White-bark pine (_Pinus albicaulis_) 27-28, _28_ + + White pine, western (_Pinus monticola_) 13-15, _14_ + + + Yellow cypress (_Chamaecyparis nootkatensis_) 23-24, _23_ + + Yew, Oregon. _See_ Yew, western. + western (_Taxus brevifolia_) 28-29 + + + + + +End of the Project Gutenberg EBook of The Forests of Mount Rainier National +Park, by Grenville F. 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