The wood is hard and brittle. A cubic foot weighs 51.43 pounds when

thoroughly dry. The wood of mature trees is reddish-brown; but young and

middle aged trunks are all sapwood, and are white from bark to center.

When sapwood is exposed to the air a considerable time it changes color

and becomes very dark brown. The medullary rays of this oak are broad,

fairly numerous, and are darker than the surrounding wood. When the log

is quarter-sawed, the exposed flecks of bright surface are the darkest

parts. To that extent, it resembles quarter-sawed sycamore, but the

woods do not look alike in any other particular. This oak is very

porous, and the pores--as is usual with live oaks--are arranged in rows

running from bark to center rather than parallel with the annual rings.

No clear line is distinguishable between spring and summerwood.

Cordwood constitutes the most important use for California live oak. It

rates high in fuel value, and the many large and crooked limbs make the

tree an ideal one, from the cordwood cutter’s viewpoint. By carefully

ricking the wood, with the crooks and elbows in every possible

direction--at which some cordwood cutters are very proficient--a cord of

wood may be constructed in the forest, which, when sold and delivered in

the buyer’s shed, contracts like an accordion.

CANYON LIVE OAK (_Quercus chrysolepis_). This splendid California

oak bears many names. It is an evergreen, and therefore is called

live oak. It is hard when thoroughly seasoned, and this has won for

it the name iron oak. Wagon makers often so designate it. It is

called Valparaiso oak, but for what reason is not apparent. Black

live oak doubtless refers to the dark color of the foliage. The most

shapely trees grow in the bottoms of canyons, and the name, canyon

live oak, refers to that circumstance. Hickory oak is not an

appropriate name, though it doubtless implies that the wood

possesses the toughness of hickory. It is about as tough as white

oak. The name golden cup oak is a translation of its botanical name

which, in Greek, means “golden scale,” a reference to a yellow

tomentum or wool which covers the cups of the acorns. The wood’s

hardness qualifies it to serve as mauls, hence the name maul oak.

The northern limit of its growth is in southern Oregon. It goes

south from there on the coast ranges of California and the western

slopes of the Sierra Nevadas to the highlands of southern

California. Its growth on the mountains of southern Arizona and New

Mexico is always shrubby. The lowest limit of its range is about

1,000 feet above sea level, the best specimens occurring at low

altitudes in the sheltered canyons of the coast ranges of

California. Gradually diminishing in size, it grows to the very tops

of many of the high mountains, sometimes reaching 9,000 feet, being

not more than a foot high at the upper limits of its range. In

appearance this tree resembles the eastern live oak (_Quercus

virginiana_), having the same majestic wide-spreading crown, except

in the high altitudes where it forms dense thickets covering large

areas.

When in its favorite habitat, the massive proportions and majestic

appearance of this tree are imposing, the crown sometimes being 150

feet across, the bole short and thick, and the great branches long

and horizontal. It is not clothed in the somber Spanish moss that is

often present on the great live oaks of the southeastern states, but

there is a similarity of appearance in the drooping slender twigs.

One hundred and fifty feet across is cited as an unusual width of

crown, one hundred feet being a good average size, and forty or

fifty feet the usual height, although it sometimes reaches 100. The

bole is vested in a gray-brown, reddish-tinged bark, about an inch

thick, and broken into numerous scales which in old age become flaky

and pliable and fall off.

The bark is light colored, and has the stringy character of white

oak. The tree would readily pass for a white oak were it not for its

two-year acorns which class it in the black oak group. The wood

resembles white oak, and weighs 52.93 pounds per cubic foot.

Few oaks, if any, retain their leaves a longer time than this. They

remain on the branches three or four years. Most evergreen oaks shed

theirs at the beginning of the second year. The leaves of this tree

are peculiar in another way. They assume various forms. That in

itself is not unusual and occurs with many species; but the canyon

live oak has one pattern of leaf for the young tree, another for the

old. One form has a margin with sharp, hooked teeth; another has

smooth-margined leaves, and there are various intermediate forms.

Sizes vary no less than shapes of both acorns and leaves. Some

acorns are half an inch in length, others two inches.

The canyon live oak is believed to be long-lived, but further

information is desirable. The massive trunks represent centuries.

They usually occur in sheltered places which are measurably secure

from the ordinary perils which beset trees, notably the woodsman’s

ax and the periodic forest fire. The bottoms of canyons where this

oak makes choice of situation do not usually burn fiercely, and

trees sheltered there escape. Cordwood cutters are the most constant

peril to good fuel trees in California; but many a canyon is safe

from their invasions, because of lack of roads. There the most

magnificent oaks rear their crowns in security, while trees of

inferior size and character, which grow on exposed slopes and flats,

fall before the cordwood cutter, and go to the ricks in village

woodyards.

The wood of canyon live oak is superior to that of any other oak in

its range. It is of light brown color, and is tough, strong, stiff,

and heavy. The trunks are generally unsuitable for sawlogs, being

too short, but when a chance tree is found that may be cut into

lumber, it is considered a prize. Trunks are seldom good for more

than one sawlog. In that respect this oak may be compared with the

southern live oak. The scarcity of good hardwoods on the Pacific

coast adds to the value of what may be found there. If the canyon

live oak grew in the East, and developed a trunk of the same size

and shape as it has in its present home, it would attract no more

attention from the users of hardwoods than the live oak in the South

attracts now. But place makes great difference.

Factories in California do not report the use of much of this oak,

yet considerable quantities of it are in service. The most important

place found for it is in country and village blacksmith shops, where

wagons are repaired. Nearly every piece of wood which goes into a

wagon, except the bed, may be this oak. Many persons consider it the

best wagon timber on the Pacific coast, and it is particularly

valued for tongues, not only for wagons, but for heavy log trucks

which are operated by several yoke of oxen. The wood is likewise

made into singletrees. It has always been in use in California for

pack saddles. That article is small, but many saddles were formerly

made, and the pack saddle is still an important article in the

mountains. Trains of mules, horses, and burros thread the narrow

paths, where wheeled vehicles cannot go, and deliver supplies to

camps and mines in remote districts. The pack saddle’s strength is

frequently all that intervenes between the load and destruction; for

the snapping of a piece of wood may let the pack go over a precipice

beyond recovery. The pack trains are slowly passing out of use in

the West, as they long ago disappeared from the “bridle paths” of

eastern mountains and forests; but they are still to be seen among

the fastnesses of the Sierra Nevadas, as in the days when a western

poet burst into inspired song of the long pack trains going

“Up and down o’er the mountain trail

With one horse tied to another’s tail.”

HUCKLEBERRY OAK (_Quercus chrysolepis vaccinifolia_) is a variety of

canyon live oak, and is never large enough to supply wood for any

purpose, but is valuable as a covering to the ground on exposed

mountains. It is usually a shrub, and specimens no more than a foot

high are mature and bear acorns enormously out of proportion to the

size of the tree. If the canyon live oak of largest size in the low

hills bore acorns proportionately as large, they would be the size

of barrels. The huckleberry oak’s acorns are set in their golden

cups. The name huckleberry is applied because of a fancied

resemblance of the leaves to those of huckleberries. They are

generally less than one inch in length, sometimes not half an inch.

This unique variety of oak ranges on elevated slopes and ridges of

the Sierra Nevada mountains, and the traveler in climbing to the

peaks is often grateful for the privilege of pulling himself up the

steep slopes by grasping in his hands the tops of full grown trees.

PALMER OAK (_Quercus chrysolepis palmeri_) is considered a variety

of canyon live oak by some, but Sudworth believes it is a distinct

species, and draws his conclusion from forms of leaves, flowers, and

fruit. It forms large thickets on foothills and plateaus near the

southern boundary of California, eighty miles or more east of San

Diego. The trees do not attain sufficient size to give them

commercial importance.

[Illustration]

CALIFORNIA TANBARK OAK

[Illustration: CALIFORNIA TANBARK OAK]

CALIFORNIA TANBARK OAK

(_Quercus Densiflora_)

Botanists dispute the right of this tree to the name of oak, and some of

them refuse to call it an oak. It is admitted that it possesses

characters not found in any other oak, but these are important to the

botanist only, while laymen have never considered the tree anything but

an oak. It has been variously called tanbark oak, chestnut oak,

California chestnut oak, live oak, and peach oak. The trunk, branches,

and foliage look much like chestnut. The leaf is like the chestnut’s,

but it is evergreen. There are three or four crops on the tree at one

time, and none fall until they are three or four years old. Young leaves

are remarkably woolly, but late in their first summer they get rid of

most of the fuzz, and become thick in texture.

Tanbark oaks are of all sizes, from mere shrubs on high mountains in the

northern Sierra Nevadas to fine and symmetrical timber in the damp

climate of the fog belt between San Francisco and the Oregon line. The

average height of mature trees is from seventy to 100 feet, with

diameters up to six feet in rare cases, though more trunks are under

than over two feet in diameter.

The range of this oak reaches southern Oregon on the north, and runs

southward three or four hundred miles along the Sierra Nevada mountains,

to Mariposa county, and six hundred miles through the Coast range to

Santa Barbara county. The tree is affected by climatic conditions, and

where surroundings do not suit, it is small and shrubby, often less than

ten feet high. It does best in the redwood belt where fogs from the

Pacific ocean keep the air moist and the ground damp. It sometimes

associates with Douglas fir, and at other times with California live

oak. If it grows in dense side shade it loses its lower branches and

develops a long, clean trunk; but in open ground it keeps its limbs

until late in life.

This is the most important source of tanbark on the Pacific coast, and

up to the present it has been procurable in large quantities. The annual

output is nearly 40,000 tons, and it commands a higher price than the

bark of any other oak or of hemlock. The absence of other adequate

tanning materials on the Pacific coast gives this tree much importance.

Its range covers several thousand square miles, and the stand is fairly

good on much of it. But on the other hand, the destruction of timber to

secure the bark has been excessive. What occurred with chestnut oak and

hemlock in the East, is occurring with tanbark oak in the West. Trees

are cut and peeled, and are left by thousands to rot in the woods, or

to feed fires and make them more destructive. The bark peelers do their

principal work in the California redwood region, because there the oak

is at its best. Economic conditions make the salvage of the trunks

impossible. The bark can be hauled to market, but the wood is unsalable

at living prices, after the long haul. It has, therefore, been usually

abandoned, and becomes a total loss. It cannot even be sold for fuel,

because the country within reach of it is thinly settled, and wood is

plentiful on every side.

Large oaks are felled, because the bark can not be stripped from the

trunks in any other way, and small trees are not spared. The peelers

often do not take the trouble to cut them down, but strip off the bark

as high as a man can reach, and leave them standing. A future tree is

thus destroyed for the sake of a strip of bark a few feet long. Such

trees live a year or two, sometimes several years, before yielding to

the inevitable. Usually, as a last expiring effort, they bear an

abnormally large crop of acorns. That performance, in the language of

the bark peelers, is “the last kick.” A tanbark slashing, when the

peelers are ready to abandon it, is a sorry spectacle. The barkless and

sun-cracked trunks strew the ground, the tops and limbs are piled in

windrows, the small peeled trees stand dying, and the last ricks of bark

have been sledded down the tote roads, marking the close of operations

in that district. A few months later, when fire runs through, the end of

the tanbark oak on that tract is accomplished.

Within recent years commendable efforts have been made to use the wood

as well as the bark. One of the first steps in that direction was to

overcome the prejudice against the wood. It was long considered to be

valueless. That belief was founded on the single fact that this oak is

difficult to season. Few woods in this country check as badly as this,

when it is left exposed to sun and wind after the bark has been removed.

It checks both radially and along the annual rings. The medullary rays

are broad and extend much of the distance from the center to the

outside. These are natural lines of cleavage when the log begins to

season and the internal stresses develop. It must be admitted that the

prospect of making anything out of timber of that character is

discouraging; but it has been accomplished, and tanbark oak is now a

material of considerable value.

The wood has about the strength and stiffness of white oak, while it is

four pounds lighter per cubic foot. The structure is similar to that of

California live oak, but the pores of tanbark oak are smaller. They run

in rows from center to circumference. The medullary rays are broad

enough to show well in quarter-sawing, but the wood’s appearance when so

worked is not wholly satisfactory. The exposed flat surfaces of the

rays show a faint purplish or violet tinge which is considered

objectionable. But when the wood is worked plain it is dependable and

substantial. It makes good flooring, fairly good furniture, finish,

vehicles, and agricultural implements. It is perishable when placed in

damp situations, and this detracts somewhat from its value as railway

ties; but the wood’s porous nature indicates that it will readily yield

to preservative treatment.

Since the value of the wood is coming to be understood it is to be

expected that less of it will be destroyed than formerly, and that

second growth will be given opportunity to hold the ground when old

stands are cut. The tree is a prolific seeder, but not every year, and

seedlings come up abundantly in sheltered places. Sprouts rise from

stumps and grow to vigorous trees. It would seem, therefore, that the

tanbark oak will hold at least part of the ground where nature planted

it.

TOUMEY OAK (_Quercus toumeyi_). No oak in this country has smaller

leaves than this. They are usually less than three-fourths of an inch

long and half an inch wide, and they hang on petioles one-sixteenth inch

long. The leaves have no lobes or notches. They remain all winter and

fall in the spring in time to make room for the new crop. The acorns are

nearly as long as the leaves and ripen in June of the first year. Few

persons ever see this oak, for its known range is restricted to Mule

mountain, in Cochise county, southeastern Arizona. It attains a height

of twenty-five or thirty feet, and a diameter of six or eight inches.

The trunk is not only small, but is of form so poor that it can never be

of value for anything but fuel. It divides near the ground into crooked

branches. The heart of the tree is light brown, the thick sapwood is

lighter.

WOOLLY OAK (_Quercus tomentella_) has apparently been crowded off

the American continent and has taken refuge on islands off the

southern California coast. As far as known, not a single tree stands

on the mainland, but several groves, with a few isolated specimens,

are found on Santa Cruz, Santa Rosa, and Catalina islands, where

they are huddled together in the bottoms of sheltered canyons. The

leaves are thick, leathery, and are toothed like holly. The trees

are evergreen. The acorns do not mature until the second season.

They are generally more than an inch long. The scarcity of this oak

relegates it to an unimportant place among commercial woods. This

seems unfortunate, for the appearance of the wood indicates that it

possesses excellent properties. No other oak looks like this wood.

It is decidedly yellow, and is dense and firm. The medullary rays

are different from those of any other oak. When seen in cross

section they are arranged in short, wavy lines, broadest in the

middle and tapering toward both ends. The pores are arranged between

the rays, and follow wavy lines also. Trees grow with fair rapidity,

and the largest on the islands are seventy-five feet high and two in

diameter.

BARREN OAK (_Quercus pumila_) is called dwarf black oak, or simply

scrub oak. Its habit of growing on barren land is responsible for

its common name which some people shorten to “bear” oak. It is one

of the poorest oaks of the East, and it seldom grows more than

twenty-five feet high and a few inches in diameter. Its range

follows the Atlantic coast southward from Mount Desert Island,

Maine, to North Carolina. It is probably more abundant on the pine

barrens of New Jersey than elsewhere. The trunks are too small to be

of use for anything but fuel.

PRICE OAK (_Quercus pricei_) is a California tree, supposed to be

very local in its range, since it has not been found outside the

drainage basin of a small stream in Monterey county. That locality

on the coast of California appears to be the starting place or

principal abiding place of several tree species, among which are

Monterey cypress and Monterey pine. The Price oak attains a height

of twenty-five or thirty feet, and a diameter of twelve inches or

less; consequently it is too small to be of value to lumbermen, even

if it were abundant. The leaves resemble those of California live

oak, and are believed to remain two summers on the tree. The acorns

mature the second season.

[Illustration]

SHINGLE OAK

[Illustration: SHINGLE OAK]

SHINGLE OAK

(_Quercus Imbricaria_)

The origin of this tree’s name has been the subject of considerable

controversy. According to one account the name was first used by the

French colonists at Kaskaskia, Illinois, nearly 150 years ago. They

found that the wood rived well and it was abundant in the vicinity of

their settlement. They split it for shingles and covered their cabins.

It was the best wood obtainable for the purpose in that region, and they

designated the tree shingle oak, a name translated into Latin by the

botanist Michaux and still retained as the tree’s botanical name. The

story of the name appears to be well authenticated, but the fact cannot

be denied that as much reason exists for another theory. A person who

sees a shingle oak tree in full leaf, particularly if it stands in open

ground where its foliage has had opportunity to develop along natural

lines, will at once notice the peculiar and characteristic overlapping

of the leaves. They suggest the courses of shingles nailed on a roof. No

other oak has that arrangement. The similitude is so striking that it

would be surprising if the name shingle oak were not applied.

It is not a one-name tree, but following the fashion, it carries several

names. It is called laurel oak in some regions. The form and appearance

of the leaf give the name. The oak looks like a mammoth laurel tree more

than like its own species. The shingle oak is known as jack oak in some

parts of Illinois. That is a name liable to be applied to any tree when

its real name is not known. In North Carolina they call the tree water

oak, which name, like jack oak, is often used to conceal ignorance of

the true name. Another southern species (_Quercus nigra_) is properly

named water oak.

Shingle oak requires good soil for growth but is not partial either to

uplands or bottoms. It is found at its best in the lower Ohio river

basin and in Missouri, but is comparatively rare in the East. From

middle Pennsylvania its range extends southward along the Alleghanies to

northern Georgia, Alabama, Tennessee, and west Arkansas. It is found in

Michigan, Wisconsin, and westward to Kansas.

It manifests a strong tendency to hybridize with other oaks, and it

readily crosses with black jack oak, pin oak, and yellow oak. It is

believed that a cross between yellow oak and shingle oak produced the

species known as lea oak.

A mature tree may be one hundred feet high and three or four feet in

diameter. It has a round or pyramidal attractive crown composed of many

slender branches and twigs. The foliage is distinctively grouped at the

ends of the twigs in star-like clusters. The leaves are four or six

inches long, with wedge-shaped or rounded bases, and are deep green and

shiny on the upper side, but lighter below. The acorns are short,

stubby, and rounded, covered one-third of the way with thin shallow

cups.

Shingle oak grows rapidly, and it is often sold by nurseries which deal

in ornamental forest trees. It is hardy as far north as Massachusetts.

Although it bears great abundance of leaves, they are so arranged that

the crown seems open. One may see through the branches of a large

shingle oak, and it suggests an airiness not common with oaks.

Differences of opinion exist concerning the value of shingle oak for

commercial purposes. It belongs in the black oak group, and its wood

goes to market as red oak, and apparently is never listed as anything

else. It is never named in market reports; shops and factories never

report it, and it has been pronounced inferior to red oak in strength

and seasoning properties. Tests have been made of some of its physical

properties, and the results do not indicate that the wood belongs with

inferior timbers. Its breaking strength is given at 39 per cent greater

than white oak, and its stiffness at 28 per cent greater. However, these

values, which are calculated from Sargent’s tables, are based on tests

of only a few specimens of the wood, and fuller investigation might make

revision necessary.

The wood is heavy, hard, and is said to check badly in drying. The pores

are large and are arranged in rows; medullary rays are broad and

conspicuous. The wood is light brown, tinged with red, the sapwood much

lighter. The broad medullary rays, running radially, give the wood its

good splitting qualities.

The tree is fairly abundant in different parts of its range, and is cut

and manufactured with other oaks and hardwoods. Slack coopers use it for

barrels; box makers employ it for crates; chair mills saw dimension

stock and ship it to factories to be finished; some goes to furniture

factories; some is turned for spindles for grills, and for balusters for

stairs; other fills various places as interior finish and molding. But

it all goes to market and passes through factories under names other

than its own.

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