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. 205<br />
rowed to about three-fourths <strong>of</strong> an inch, gradually increasing in width, toward<br />
and above <strong>the</strong> middle, to about 1 or 1 inches; <strong>the</strong>n tapering to a stiff sharp<br />
point (fig. 81, b). The blade is thin and <strong>the</strong> edges are strongly curled or rolled<br />
from above <strong>the</strong> middle to <strong>the</strong> point. The edges are, moreover, conspicuously<br />
marked with thread-like fibers, which are frayed from <strong>the</strong> borders as <strong>the</strong> leaf<br />
grows older. A single branched cluster (about 14 to 16 inches long) <strong>of</strong> flowers<br />
is borne from among <strong>the</strong> uppermost green leaves. The pulpy, sweetish fruit<br />
(fig. 81, c), ripened late in August or early in September, is on a slender drooping<br />
stem. It is 3i or 4 inches long, blunt at <strong>the</strong> ends, <strong>the</strong> top end having a short<br />
thick point. The fiat seeds, packed in 6 chambers <strong>of</strong> <strong>the</strong> fruit, are black (fig.<br />
81, d). Wood: Nothing can now be said <strong>of</strong> <strong>the</strong> wood <strong>of</strong> this yucca, except that<br />
it is lighter and somewhat s<strong>of</strong>ter than that <strong>of</strong> <strong>the</strong> Joshua tree.<br />
LONGEVITY-No definite statement can be made concerning <strong>the</strong> age limit <strong>of</strong><br />
this yucca, which, however, can hardly be less long-lived than <strong>the</strong> Joshua tree.<br />
Messrs. C. R. Orcutt and S. B. Parish, who know <strong>the</strong> tree yuccas from long<br />
observation, both inform <strong>the</strong> writer that <strong>the</strong> Mohave yucca is an exceedingly<br />
persistent but very slow grower in its native habitat, scarcely any change having<br />
been perceived in trees under observation for <strong>the</strong> last twenty-five years.<br />
RAAGE.<br />
From nor<strong>the</strong>astern Arizona and sou<strong>the</strong>rn Nevada across <strong>the</strong> Mohave <strong>De</strong>sert into California,<br />
and from <strong>the</strong> sou<strong>the</strong>rn base <strong>of</strong> <strong>the</strong> San Bernardino Mountains to <strong>the</strong> coast and<br />
northward to Monterey, sometimes ascending mountain slopes to 4,000 feet,<br />
Similar to Joshua Iree.<br />
OCC URRENCE.<br />
SimOcca tTYohuc<br />
DICOTYL ED ONE S.<br />
The trees <strong>of</strong> <strong>the</strong> great dicotyledonous class are so called because <strong>the</strong> germinating<br />
seeds produce two seed-leaves, or cotyledons. They have broad leaves,<br />
with a central vein and a network <strong>of</strong> smaller connected veins. They are fur<strong>the</strong>r<br />
characterized by having <strong>the</strong> non-resinous wood <strong>of</strong> <strong>the</strong>ir trunks in annual layers,<br />
which appear as concentric rings on a cross-section <strong>of</strong> <strong>the</strong> trunk. Each layer is<br />
formed just beneath <strong>the</strong> living bark and over <strong>the</strong> layer produced <strong>the</strong> previous<br />
year. This mode <strong>of</strong> diameter growth gave rise in earlier days to <strong>the</strong> class name<br />
" exogens," or outside growers, in contradistinction to " endogens," or inside<br />
growers, a class name <strong>the</strong>n given to <strong>the</strong> trees we now more generally call " monocotyledones."<br />
The two terms, " endogens " and " exogens," originated when<br />
knowledge <strong>of</strong> how members <strong>of</strong> <strong>the</strong> two classes grow was incomplete. Later<br />
studies show that <strong>the</strong> term " exogens " is still correctly applicable to all dicotyledonous<br />
trees, but that <strong>the</strong> term " endogens " does not express <strong>the</strong> manner in<br />
which monocotyledones actually make <strong>the</strong>ir diameter growth. Monocotyledones<br />
were once thought to increase in diameter by <strong>the</strong> addition, each year, <strong>of</strong><br />
scattered woody fibers at <strong>the</strong> center or pith <strong>of</strong> <strong>the</strong> tree, thus gradually crowding<br />
<strong>the</strong> woody tissue previously formed to <strong>the</strong> outside <strong>of</strong> <strong>the</strong> trunk. In o<strong>the</strong>r words,<br />
<strong>the</strong> outside <strong>of</strong> <strong>the</strong> trunk was believed to have once occupied <strong>the</strong> center <strong>of</strong> <strong>the</strong><br />
stem. We now know, however, that <strong>the</strong>se trees grow in diameter by laying on<br />
tissue outside <strong>of</strong> that formed <strong>the</strong> previous year, but not in a distinguishable<br />
layer as in dicotyledonous trees. Diameter growth <strong>of</strong> <strong>the</strong> gymnosperms (pines,<br />
spruces, firs, etc.) is produced in exactly <strong>the</strong> same way as in dicotyledonous<br />
trees, but <strong>the</strong> oleo-resinous woods <strong>of</strong> <strong>the</strong> former distinguish <strong>the</strong>m from <strong>the</strong> latter<br />
class. It is true, -indeed, that <strong>the</strong> wood <strong>of</strong> some <strong>of</strong> our broadleaf trees contains<br />
r6sinous matter, but it is not in any high degree oleo-resinous, as in gymno-<br />
15188-OS 14