De I. VNER VEW D Forest Trees of the Pacific Slope
De I. VNER VEW D Forest Trees of the Pacific Slope
De I. VNER VEW D Forest Trees of the Pacific Slope
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FOREST TREES OF THE PACIFIC SLOPE.<br />
thread-like stem, and are about one-fourth to seven-eighths <strong>of</strong> an inch long.<br />
The leaf-bearing branchlets, especially those <strong>of</strong> <strong>the</strong> season's growth, are more<br />
or less minutely hairy. The small, few-scaled cones nod from <strong>the</strong> tips <strong>of</strong><br />
brauchlets, matnuing from <strong>the</strong> middle to <strong>the</strong> end <strong>of</strong> August. They open rapidly<br />
afterwards and usually shed <strong>the</strong>ir small, winged seeds during September.<br />
By spring most <strong>of</strong> <strong>the</strong> cones have fallen from <strong>the</strong> trees. The cones are from<br />
about three-fourths inch to sometimes nearly 1 s Inches long, and when open are<br />
reddish ecay-brown (fig. 34). Cone-scales, peculiar in being sharply narrowed<br />
from about <strong>the</strong>ir middle, are faintly downy on <strong>the</strong>ir outer surfaces. The seeds<br />
(fig. 34, a) are light brown. Their comparatively large wings enable <strong>the</strong> wind to<br />
carry <strong>the</strong>m to a considerable distance from <strong>the</strong> parent tree. Seed-leaves 5,<br />
pointed, and about one-fourth inch long. By <strong>the</strong> third year seedlings produce<br />
foliage like that <strong>of</strong> <strong>the</strong> adult tree. In <strong>the</strong> dense, moist forests in which this<br />
tree grows best its numerous seedlhigs grown on moss-covered stumps and<br />
logs-<strong>of</strong>ten high in <strong>the</strong> air, and even in <strong>the</strong> moss on living trunks-are a<br />
familiar sight. Not infrequently seedlings extend <strong>the</strong>ir roots through or over<br />
<strong>the</strong>ir host stumps and decaying logs into <strong>the</strong> soil and become firmly rooted;<br />
many o<strong>the</strong>rs, unable to do this, die. The ability <strong>of</strong> this tree to grow throughout<br />
its life in <strong>the</strong> densest shade explains <strong>the</strong> <strong>of</strong>ten almost pure stands which have<br />
followed removal <strong>of</strong> <strong>the</strong> older forest in which hemlock was widely but only<br />
sparingly represented. The hemlocks had covered <strong>the</strong> shaded ground with<br />
seedlings which later excluded o<strong>the</strong>r species trying to come in after <strong>the</strong> old trees<br />
were removed.<br />
Wood, fine-grained, pale yellowish brown, with <strong>the</strong> slightest tinge <strong>of</strong> red. It<br />
is ra<strong>the</strong>r light, s<strong>of</strong>t (works like s<strong>of</strong>t pine), and very unlike <strong>the</strong> slivery wood <strong>of</strong><br />
its eastern relative, which it o<strong>the</strong>rwise resembles. The unfounded prejudice<br />
against western hemlock wood is exceedingly unfortunate, for in its best grades<br />
it is useful for nmany <strong>of</strong> <strong>the</strong> better commercial purposes, while its bark yields<br />
a much higher percentage <strong>of</strong> tannin than does that <strong>of</strong> <strong>the</strong> eastern hemlock<br />
(Tseiga canadensis), so extensively used for tanning.<br />
LONGEVITY.-Very long-lived, growing slowly in height and diameter. <strong>Trees</strong><br />
16 or 17 inches in diameter are 195 or 200 years old. Large trees are from 300<br />
to 500 years old, and it is believed that very much older trees will be noted.<br />
RANGE.<br />
<strong>Pacific</strong> coast region from Alaska southward to nor<strong>the</strong>rn California; inland to sou<strong>the</strong>rn<br />
British Columbia, nor<strong>the</strong>rn Idaho, and Montana, and into <strong>the</strong> Cascades in Oregon and<br />
Washington.<br />
ALAsKA.-Islands and seaward slope <strong>of</strong> coast ranges westward to Cape Puget on west<br />
side <strong>of</strong> Prince William Sound; generally from sea level to timber line (3,000 feet on<br />
sou<strong>the</strong>astern coast to 1.600 feet on Prince William Sound). Lynn Canal region, from<br />
elevations <strong>of</strong> 130 to 2,600 feet. South slope <strong>of</strong> St. Elias Range to 1,625 and 2,700 feet;<br />
Yakutat Bay, up to 2,200 feet on Mount Tebenk<strong>of</strong> (east end <strong>of</strong> bay), gradually dropping<br />
to sea level at Disenchantment Bay (head <strong>of</strong> Yakutat Bay). Coast from Dry Bay<br />
to Prince William Sound, up to 400 feet, and to 1,600 feet; on coastal plain, hillsides<br />
facing open water and valleys <strong>of</strong> streams, sometimes extending inland 3 to 5 miles,<br />
as at head <strong>of</strong> Cordova, Gravina, ard Fidalgo bays.<br />
BRITISH COLUIMBIA.-Islands, Coast Range, and inland up river valleys to limit <strong>of</strong><br />
abundant rainfall, from sea level to 2,000 or 3,000 feet elevation. Reappears eastward<br />
in Gold and Selkirk mountains, reaching 3,500 to 5,000 feet. Up <strong>De</strong>an Inlet and Salmon<br />
River to point 18 miles from sea and to elevation <strong>of</strong> 600 feet; appears still far<strong>the</strong>r inland,<br />
in Coast Range, sparingly on lower part <strong>of</strong> Iltasyouco River (tributary Salmon<br />
River). Inland 53 miles on Homathco River (flows into Bute Inlet) to an elevation <strong>of</strong><br />
2,320 feet. In lower Fraser River Valley eastern limits are Uztlihoos River (nor<strong>the</strong>astern<br />
branch <strong>of</strong> Anderson River), at point 6 to 10 miles east <strong>of</strong> Fraser River, and summit<br />
between Coquihalla River (eastern tributary Fraser Rivern and Coldwater River.<br />
Abundant on southwest coast <strong>of</strong> Vancouver Island, reaching elevation <strong>of</strong> 975 feet about<br />
Port Renfrew. Extends into Gold Range (from eastern Washington) and into Selkirk<br />
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