The tamarack’s geographical range is remarkable. It is said to be best

developed in the region east of Manitoba, but it extends southward into

West Virginia and northward to the land of the midnight sun. It

maintains its place almost to the arctic snows, and the willow is about

the only tree that pushes farther north. It is found from Newfoundland

and Labrador far down toward the mouth of the Mackenzie river, north of

the arctic circle. It grows on dry land as well as wet, but is oftenest

found in cold swamps, particularly in the southern part of its range.

Silted-up lakes are favorite situations, and on the made-land above old

beaver dams.

Tamarack forests frequently stand on ground so soft that a pole may be

thrust ten feet deep in the mud. The moist, monotonous sphagnum moss

generally furnishes ground cover in such places. A tamarack swamp in

summer is cool and pleasant--provided there is not too much water on the

ground--but in winter a more desolate picture can scarcely be imagined.

The leafless trees appear to be dead, and covered with lifeless cones;

but the first warm days bring it to life.

The average height of tamarack trees is from forty to sixty feet,

diameter twenty inches or less. Leaves are one-half or one and a half

inches long; cones one-half or three-quarter inches, and bright chestnut

brown at maturity. They fall when two years old. The winged seeds are

very small. The tree is neither a frequent nor abundant seeder. The

foliage is thin, and is not sufficient to shut much sunlight from the

ground.

The wood is heavy, hard, very strong, and is durable in contact with the

soil. The growth is slow, annual rings narrow, summerwood occupies

nearly half the ring, and is dark-colored, resinous, and conspicuous;

resin passages few and obscure; medullary rays numerous and obscure;

color of wood light brown, the sapwood nearly white.

The uses of tamarack go back to prehistoric times. The Indians of Canada

and northeastern United States drew supplies from four forest trees when

they made their bark canoes. The bark for the shell came from paper

birch, threads for sewing the strips of bark together were tamarack

roots, resin for stopping leaks was a product of balsam fir, and the

light framework of wood was northern white cedar.

The roots which best suited the Indian’s purpose came from trees which

grew in soft, deep mud, where lakes and beaver ponds had silted up. Such

roots are long, slender, and very tough and pliant, and may be gathered

in large numbers, particularly where running streams have partly

undermined standing trees.

White men likewise made use of tamarack roots in boat building, but the

roots were different from what the Indians used. “Instep” crooks were

hewed for ship knees. These were large roots, the larger the better.

Trees which produced them did not grow in deep mud, for there the roots

did not develop crooks. The ship knee operator hunted for tamarack

forests growing on a soft surface soil two or three feet deep, underlaid

by stiff clay or rock which roots could not penetrate. In situations

like that the roots go straight down until they reach the hard stratum,

and then turn at right angles and grow in a horizontal direction. The

turning point in the root develops the crook of which the ship knee is

made.

Tamarack is seldom of sufficient size for the largest ship knees. Such

were formerly supplied by southern live oak; and in that case crooks

formed by the union of trunk and large branches were as good as those

produced by the union of trunk and large roots.

Tamarack is still employed in the manufacture of boat knees, but not as

much as formerly. Steel frames have largely taken the place of wood in

the construction of ship skeletons. Boat builders use tamarack now for

floors, keels, stringers, and knees.

Tamarack has come into much use in recent years. Sawmills cut from it

more than 125,000,000 feet of lumber a year. Fourteen states contribute,

but most of the lumber is produced in Minnesota, Michigan, and

Wisconsin. Railroads in the United States buy 5,000,000 or more

tamarack ties a year, which reduced to board measure amount to over

150,000,000 feet. Fence posts and telegraph poles come in large numbers

from tamarack forests.

The wood is stiff and strong, its stiffness being eighty-four per cent

of that of long leaf pine, and its strength about eighty per cent.

Unusual variations in both strength and stiffness are found. One stick

of tamarack may rate twice as high as another.

The wood-using factories of Michigan consume nearly 20,000,000 feet of

this wood yearly. It is made into boxes, excelsior, pails, tanks, tubs,

house finish, refrigerators, windmills, and wooden pipes for waterworks

and for draining mines.

There is little likelihood that the supply of tamarack will run short in

the near future. While it is not in the first rank of the important

trees in this country, it is useful, and it is fortunate that it

promises to hold its ground against fires which do grave injury to

northern forests. In the swamps where the most of it is found the ground

litter is too damp to burn. The tree does not grow rapidly, but it

usually occupies lands which cannot be profitably devoted to

agriculture, and it will, therefore, be let alone until it reaches

maturity.

Tamarack is a familiar tree in parks, and it grows farther south than

its natural range extends. It is not as desirable a park tree as

hemlock, spruce, fir, the cedars, and some of the pines, because its

foliage is thin in summer and wanting in winter. It is in a class with

cypress. In the early spring, however, while its soft green needles are

beginning to show themselves in clusters along the twigs, its delicate

and unusual appearance attracts more attention than its companion trees

which are always in full leaf and for that reason are somewhat

monotonous.

[Illustration]

WESTERN LARCH

[Illustration: WESTERN LARCH]

WESTERN LARCH

(_Larix Occidentalis_)

This is a magnificent tree of the Northwest, and its range lies

principally on the upper tributaries of the Columbia river, in Idaho,

Montana, and British Columbia, but it occurs also among the Blue

Mountains of Washington and Oregon. It is the largest member of the

larch genus, either in the old world or the new. The finest trees are

250 feet high with diameters of six or eight feet, but sizes half of

that are nearer the average. The trunk is of splendid form. In early

life it is limby, but later it prunes itself, and a long, tapering bole

is developed with a very small crown of thin foliage. No other tree of

its size, with the possible exception of old sequoias, has so little

foliage in proportion to the trunk.

The result is apparent in the rate of growth after the larch has passed

its youth. Sometimes such a tree does not increase its trunk diameter as

much in seventy-five years as a vigorous loblolly pine or willow oak

will in one year. The trunk of a tree, as is well known, grows by means

of food manufactured by the leaves and sent down to be transformed into

wood. With so few leaves and a trunk so large, the slowness of growth is

a natural consequence. Though the annual rings are usually quite narrow,

the bands of summerwood are relatively broad. That accounts for the

density of larchwood and its great weight. It is six per cent heavier

than longleaf pine, and is not much inferior in strength and elasticity.

The leaves are from one to one and three-quarter inches long, the cones

from one to one and a half inches, and the seeds nearly one-quarter inch

in length. They are equipped with wings of sufficient power to carry

them a short distance from the parent tree.

The bark on young larches is thin, but on large trunks, and near the

ground, it may be five or six inches thick. When a notch is cut in the

trunk it collects a resin of sweetish taste which the Indians use as an

article of food.

The western larch reaches its best development in northern Idaho and

Montana on streams which flow into Flathead lake. The tree prefers moist

bottom lands, but grows well in other situations, at altitudes of from

2,000 to 7,000 feet. The figures given above on the wood’s weight,

strength, and stiffness show its value for manufacturing purposes. Its

remoteness from markets has stood in the way of large use, but it has

been tried for many purposes and with highly satisfactory results. In

1910 sawmills in the four western states where it grows cut 255,186,000

feet. Most of this is used as rough lumber, but some is made into

furniture, finish, boxes, and boats. The wood has several names, though

larch is the most common. It is otherwise known as tamarack and

hackmatack, which names are oftener applied to the eastern tree; red

American larch, western tamarack, and great western larch.

Some of the annual cut of lumber credited to western larch does not

belong to it. Lumbermen have confused names and mixed figures by

applying this tree’s name to noble fir, which is a different tree. If

the fir lumber listed as larch were given its proper name, it would

result in lowering the output of larch as shown in statistical figures.

In spite of this, however, larch lumber fills an important place in the

trade of the northern Rocky Mountain region.

There is little doubt that it will fill a much more important place in

the future, for a beginning has scarcely been made in marketing this

timber. The available supply is large, but exact figures are not

available. Some stands are dense and extensive, and the trees are of

large size and fine form. It is not supposed, however, that there will

be much after the present stand has been cut, because a second crop from

trees of so slow growth will be far in the future. Sudworth says that

larch trees eighteen or twenty inches in diameter are from 250 to 300

years old, and that the ordinary age of these trees in the forests of

the Northwest is from 300 to 500 years; while larger trees are 600 or

700. Much remains to be learned concerning the ages of these trees in

different situations and in different parts of its range. It is

apparent, however, that when a period covering two or three centuries is

required to produce a sawlog of only moderate size, timber owners will

not look forward with much eagerness to a second growth forest of

western larch.

The value of the wood of western larch has been the subject of much

controversy. In the tables compiled for the federal census of 1880,

under direction of Charles S. Sargent, its strength and elasticity were

shown to be remarkably high. The figures indicate that it is about

thirty-nine per cent stronger than white oak and fifty-one per cent

stiffer. This places it a little above longleaf pine in strength and

nearly equal to it in stiffness or elasticity. Engineers have expressed

doubts as to the correctness of Sargent’s figures. They believe them too

high. The samples tested by Sargent were six in number, four of them

collected in Washington and two in Montana.

The wood of western larch is heavier than longleaf pine, and

approximately of the same weight as white oak. It is among the heaviest,

if not actually the heaviest, of softwoods of the United States. Sargent

thus described the physical properties of the wood: “Heavy, exceedingly

hard and strong, rather coarse grained, compact, satiny, susceptible of

a fine polish, very durable in contact with the soil; bands of small

summer cells broad, occupying fully half the width of the annual growth,

very resinous, dark-colored, conspicuous resin passages few, obscure;

medullary rays few, thin; color, light bright red, the thin sapwood

nearly white.” The wood is described by Sudworth: “Clear, reddish brown,

heavy, and fine grained; commercially valuable; very durable in an

unprotected state, differing greatly in this respect from the wood of

the eastern larch.”

The seasoning of western larch has given lumbermen much trouble. It

checks badly and splinters rise from the surface of boards. It is

generally admitted that this is the most serious obstacle in the way of

securing wide utilization for the wood. The structure of the annual ring

is reason for believing that there is slight adhesion between the

springwood and that of the late season. Checks are very numerous

parallel with the growth rings, and splinters part from the board along

the same lines. Standing timber is frequently windshaken, and the cracks

follow the rings.

All of this is presumptive evidence that the principle defect of larch

is a lack of adhesion between the early and the late wood. If that is

correct, it is a fundamental defect in the growing tree, and is inherent

in the wood. No artificial treatment can wholly remove it. It should not

be considered impossible, however, to devise methods of seasoning which

would not accentuate the weaknesses natural to the wood.

The form of the larch’s trunk is perfect, from the lumberman’s

viewpoint, and its size is all that could be desired. It is amply able

to perpetuate its species, though it consumes a great deal of time in

the process. Abundant crops of seeds are borne, but only once in several

years. It rarely bears seeds as early as its twenty-fifth year, and

generally not until it passes forty; but its fruitful period is long,

extending over several centuries. The seeds retain their vitality

moderately well, which is an important consideration in view of the

tree’s habit of opening and closing its cones alternately as the weather

happens to be damp or dry. The dispersion of seeds extends over a

considerable part of the season, and the changing winds scatter them in

all directions. Many seeds fall on the snow in winter to be let down on

the damp ground ready to germinate during the early spring. The best

germination occurs on mineral soil, and this is often found in areas

recently bared by fire. Lodgepole pine contends also for this ground;

but the race between the two species is not swift after the process of

scattering seeds has been completed; for both are of growth so

exceedingly slow that a hundred years will scarcely tell which is

gaining. In the long run, however, the larch outstrips the pine and

becomes a larger tree. If both start at the same time, and there is not

room for both, the pine will kill the larch by shading it. The latter’s

thin foliage renders it incapable of casting a shadow dense enough to

hurt the pine. The best areas for larch are those so thoroughly burned

as to preclude the immediate heavy reproduction of lodgepole pine.

Much of the natural ranges of larch and lodgepole pine lie in the

national forests owned by the government, and careful studies have been

made in recent years to determine the requirements, and the actual and

comparative values of the two species. It has been shown that larch is

one of the most intolerant of the western forest trees. It cannot endure

shade. Its own thin foliage, where it occurs in pure stands, is

sufficient to shade off the lower limbs of boles, and produce tall,

clean trunks; but if a larch happens to stand in the open, where light

is abundant, it retains its branches almost to the ground. It is more

intolerant, even, than western yellow pine, which so often grows in

open, parklike stands.

ALPINE LARCH (_Larix lyallii_) never grows naturally below an altitude

of 4,000 feet, and near the southern border of its range it climbs to

8,000, where it stands on the brink of precipices, faces of cliffs, and

on windswept summits. It is too much exposed to storms, and has its

roots in soil too sterile to develop symmetrical forms. It is found in

Montana, Idaho, Washington, and Oregon. The finest trees are sometimes

seventy-five feet high and three or four in diameter, but the average

height ranges from forty to fifty, with diameters of twenty inches or

less. Its leaves are one and a half inches or less in length; cones one

and a half inches long, and bristling with hair; seeds one-eighth of an

inch long with wings one-fourth inch; wood heavy, hard, and of a light,

reddish brown color. It is seldom used except about mountain camps where

it is sometimes burned for fuel or is employed in constructing corrals

for sheep and cattle. It is impossible for lumbermen ever to make much

use of it, because it is scarce and hard to get at.

[Illustration]

RED CEDAR

[Illustration: RED CEDAR]

RED CEDAR

(_Juniperus Virginiana_)

This widely distributed tree is called red cedar in New Hampshire,

Vermont, Massachusetts, Rhode Island, New York, New Jersey,

Pennsylvania, Delaware, West Virginia, North Carolina, South Carolina,

Georgia, Florida, Alabama, Mississippi, Louisiana, Kentucky, Missouri,

Illinois, Indiana, Wisconsin, Iowa, Michigan, Minnesota, Ohio, and

Ontario; cedar in Connecticut, Pennsylvania, New Jersey, South Carolina,

Kentucky, Illinois, Iowa, and Ohio; savin in Massachusetts, Rhode

Island, New York, Pennsylvania and Minnesota; juniper in New York and

Pennsylvania; juniper bush in Minnesota; cedre in Louisiana.

The names as given above indicate the tree’s commercial range. It

appears as scattered growth and in doubtful forms outside of that range,

particularly in the West where several cedars closely resemble the red

cedar, yet differ sufficiently from it to give them places as separate

species in the lists of some botanists. They are so listed by the United

States Forest Service; and the following names are given: Western

Juniper, Rocky Mountain Juniper, One Seed Juniper, Mountain Juniper,

California Juniper, Utah Juniper, Drooping Juniper, Dwarf Juniper, and

Alligator Juniper. These species are not of much importance from the

lumberman’s viewpoint, yet they are highly interesting trees, and in

this book will be treated individually.

The red cedar grows slowly, and thrives in almost any soil and situation

except deep swamps. It is often classed as a poor-land species, yet it

does not naturally seek poor land. That it is often found in such

situations is because it has been crowded from better places by stronger

trees, and has retreated to rocky ridges, dry slopes, and thin soils

where competitors are unable to follow. The trees often stand wide apart

or solitary, yet they can grow in thickets almost impenetrable, as they

do in Texas and other southern states. It is an old-field tree in much

of its range. Birds plant the seeds, particularly along fence rows. That

is why long lines of cedars may often be seen extending across old

fields or deserted plantations.

The extreme size attained by this cedar is four feet in diameter, and

one hundred in height, but that size was never common, and at present

the half of it is above the average. That which reaches market is more

often under than over eighteen inches in diameter. The reddish-brown and

fibrous bark may be peeled in long strips. Stringiness of bark is

characteristic of all the cedars, and typical of red cedar.

The wood is medium light and is strong, considering that it is very

brittle. Tests show it to be eighty per cent as strong as white oak. The

grain is very fine, even, and homogeneous, except as interfered with

by knots. The annual rings are narrow, the summerwood narrow and

indistinct; medullary rays numerous but very obscure. The color

is red, the thin sapwood nearly white. The heart and sap are

sometimes intermingled, and this characteristic is prominent in the

closely-related western species of red cedar. The wood is easily worked,

gives little trouble because of warping and shrinking, and the heart is

considered as durable as any other American wood. It has a delicate,

agreeable fragrance, which is especially marked. This odor is

disagreeable to insects, and for that reason chests and closets of cedar

are highly appreciated as storage places for garments subject to the

ravages of the moth and buffalo bug. An extract from the fruit and

leaves is used in medicine, while oil of red cedar, distilled from the

wood, is used in making perfume. Cedar has a sweet taste. It burns

badly, scarcely being able to support a flame; it is exceedingly

aromatic and noisy when burning and the embers glow long in still air.

Some of the bungalow owners in Florida buy cedar fuel in preference to

all others for burning in open fireplaces.

Its representative uses are for posts, railway ties, pails, sills, cigar

boxes, interior finish and cabinet making, but its most general use is

in the manufacture of lead pencils, for which its fine, straight grain

and soft texture are peculiarly adapted. The farther south cedar is

found, the softer and clearer it is. In the North, in ornamental trees,

it is very hard, slow-growing, and knotty. It shows but a small

percentage of clear lumber. In eastern Tennessee there were considerable

quantities of red cedar brake that were for years considered of little

value. About the only way the wood was employed a few years ago was in

fence rails and posts, fuel, and charcoal. Of late people in localities

where cedar grows in any abundance have awakened to its value, and cedar

fences are rapidly disappearing, owing to the high prices now paid for

the wood, and the excellent demand. On no other southern wood has such

depredation been practiced. Because of its lightness and the ease with

which it can be worked, it has been used for purposes for which other

and less valuable woods were well adapted. On account of its slow

growth, its complete exhaustion has often been predicted, but a second

growth has appeared which, though much inferior to the virgin timber,

can be used in many ways to excellent advantage. Instead of the huge

piles of cedar flooring, chest boards, and smooth railings of the old

days, one now sees at points of distribution great piles of knotty,

rough poles, ten to forty feet long, which years ago would have been

discarded. Today they represent bridge piling, the better and smoother

among them being used for telephone and telegraph poles.

Middle Tennessee has produced more red cedar than any other part of the

United States, but the bulk of production has been confined to a few

counties, which produce a higher class and more aromatic variety of wood

than that found elsewhere. A century ago these counties abounded in

splendid forests of cedar. The early settlers built their cabins of

cedar logs, sills, studding, and rafters; their smoke houses were built

of them; their barns; even the roofs were shingled with cedar and the

rooms and porches floored with the sweet-scented wood. Not many years

ago trees three feet or more in diameter were often found, but the days

are past when timber like that can be had anywhere.

Although the most general use at the present time is for lead pencils,

few people who sharpen one and smell the fragrant wood, stop to wonder

where it came from. One would smile were it suggested to him that

perhaps his pencil was formerly part of some Tennessee farmer’s worm

fence. The best timber obtained now is hewn into export logs and shipped

to Europe, particularly Germany, where a great quantity is converted

into pencils. The red wood is made into the higher grades and the sap or

streaked wood is used for the cheaper varieties and for pen holders. The

smaller and inferior logs are cut into slats, while odds and ends,

cutoffs, etc., are collected and sold by the hundred pounds to pencil

factories. There are many such factories in the United States now, as

well as in Europe, and pencil men are scouring the cedar sections to buy

all they can. The farmer who has a red cedar picket or worm fence can

sell it to these companies at a round price. Pencil men are even going

back over tracts from which the timber was cut twenty-five years ago,

buying up the stumps. When the wood was plentiful lumbermen were not

frugal, and usually cut down a tree about two feet above the ground,

allowing the best part of it to be wasted.

American Forest Trees · 第 6 / 52 段