American Big Game in Its Haunts Part 24

THE BLACK MESA FOREST RESERVE OF ARIZONA AND ITS AVAILABILITY AS A GAME PRESERVE.

The Black Mesa Forest Reserve lies in central-eastern Arizona, and contains 1,658,880 acres, is about 180 miles long in a northwesterly and southeasterly direction and a direct continuation southeasterly from the San Francisco Mountain Forest Reserve. On the north it contains a part of the Mogollon Mesa, which is covered with a magnificent open forest of Arizona yellow pine (_Pinus ponderosa_) in which there is an abundance of bunch gra.s.s and here and there are beautiful gra.s.sy parks. To the southeast the reserve covers a large part of the White Mountains, one of the largest areas of generally high elevation in Arizona. The yellow pine forest, similar in character to that on the Mogollon Mesa, is found over a large part of the reserve between 7,000 and 8,500 feet alt.i.tude, and its general character is shown in the accompanying view.

The Black Mesa Reserve is irregular in outline. The large compact areas at each end are joined by a long, narrow strip, very irregular in outline and less than a towns.h.i.+p broad at various points. It lies along the southern border of the Great Colorado Plateau, and covers the southern and western borders of the basin of the Little Colorado River. Taken as a whole, this reserve includes some of the wildest and most attractive mountain scenery in the West.

Owing to the wide separation of the two main areas of the reserve, and certain differences in physical character, they will be described separately, beginning with the northwestern and middle areas, which are similar in character.

THE NORTHWESTERN SECTION OP THE BLACK MESA RESERVE.

With the exception of an area in the extreme western part, which drains into the Rio Verde, practically all of this portion of the reserve lies along the upper border of the basin of the Little Colorado. It is a continuation of the general easy slope which begins about 5,000 feet on the river and extends back so gradually at first that it is frequently almost imperceptible, but by degrees becomes more rolling and steeper until the summit is reached at an alt.i.tude of from 6,000 to 9,000 feet. The reserve occupies the upper portion of this slope, which has more the form of a mountainous plateau country, scored by deep and rugged canyons, than of a typical mountain range. From the summit of this elevated divide, with the exception of the district draining into the Rio Verde, the southern and western slope drops away abruptly several thousand feet into Tonto Creek Basin. The top of the huge escarpment thus formed faces south and west, and is known as the rim of Tonto Basin, or, locally, "The Rim." From the summit of this gigantic rocky declivity is obtained an inspiring view of the south, where range after range of mountains lie spread out to the distant horizon.

The rolling plateau country sloping toward the Little Colorado is heavily scored with deep box canyons often hundreds of feet deep and frequently inaccessible for long distances. Most of the permanent surface water is found in these canyons, and the general drainage is through them down to the lower plains bordering the river. The greater part of this portion of the reserve is covered with yellow pine forests, below which is a belt, varying greatly in width, of pinons, cedars and junipers, interspersed with a more or less abundant growth of gramma gra.s.s. This belt of scrubby conifers contains many open gra.s.sy areas, and nearer the river gives way to continuous broad gra.s.sy plains. Nowhere in this district, either among the yellow pines or in the lower country, is there much surface water, and a large share of the best watering places are occupied by sheep owners.

The wild and rugged slopes of Tonto Basin, with their southerly exposure, have a more arid character than the area just described. On these slopes yellow pines soon give way to pinons, cedars and junipers, and many scrubby oaks and various species of hardy bushes. The watering places are scarce until the bottom of the basin is approached. Tonto Basin and its slopes are also occupied by numerous sheep herds, especially in winter.

There are several small settlements of farmers, sheep and cattle growers within the limits of the narrow strip connecting the larger parts of the reserve, notably Show Low, Pinetop and Linden. The wagon road from Holbrook, on the Santa Fe Pacific Railroad, to the military post at Camp Apache, on the White Mountain Indian Reservation, pa.s.ses through this strip by way of Show Low. The old trails through Sunset Pa.s.s to Camp Verde and across "The Rim" into Tonto Basin traverse the northern part of the reserve, and are used by stockmen and others at short intervals, except in midwinter.

The climate of this section of the reserve is rather arid in summer, the rainfall being much more uncertain than in the more elevated areas about the San Francisco Mountains to the northwest and the White Mountains to the southeast. The summers are usually hot and dry, the temperature being modified, however, by the alt.i.tude. Rains sometimes occur during July and August, but are more common in the autumn, when they are often followed by abundant snowfall. During some seasons snow falls to a depth of three or more feet on a level in the yellow pine forests, and remains until spring. During other seasons, however, the snowfall is insignificant, and much of the ground remains bare during the winter, especially on southern exposures. As a matter of course, the lower slope of the pinon belt and the gra.s.sy plains of the Little Colorado, both of which lie outside of the reserve, have less and less snow, according to the alt.i.tude, and it never remains for any very considerable time. On the southern exposure, facing Tonto Basin, the snow is still less permanent. The winter in the yellow pine belt extends from November to April.

LARGE GAME IN THE NORTHERN PART OF THE BLACK MESA RESERVE.

Black-tailed deer, antelope, black and silver tipped bears and mountain lions are the larger game animals which frequent the yellow pine forests in summer. Wild turkeys are also common.

The black-tailed deer are still common and generally distributed. In winter the heavy snow drives them to a lower range in the pinon belt toward the Little Colorado and also down the slope of Tonto Basin, both of these areas lying outside the reserve. The Arizona white-tailed deer is resident throughout the year in comparatively small numbers on the brushy slopes of Tonto Basin, and sometimes strays up in summer into the border of the pine forest. Antelope were once plentiful on the plains of the Little Colorado, and in summer ranged through the open yellow pine forest now included in the reserve. They still occur, in very limited numbers, in this forest during the summer, and at the first snowfall descend to the lower border of the pinon belt and adjacent gra.s.sy plains. Both species of bears occur throughout the pine forests in summer, often following sheep herds. As winter approaches and the sheep are moved out of the higher ranges, many of the bears go over "The Rim" to the slopes of Tonto Basin, where they find acorns, juniper berries and other food, until cold weather causes them to hibernate.

The mountain lions are always most numerous on the rugged slopes of Tonto Basin, especially during winter, when sheep and game have left the elevated forest.

From the foregoing notes it is apparent that the northwestern and middle portions of the Black Mesa Reserve are without proper winter range for game within its limits, and that the conditions are otherwise unfavorable for their use as game preserves.

THE SOUTHEASTERN SECTION OF THE BLACK MESA RESERVE.

The southeastern portion of the reserve remains to be considered. The map shows this to be a rectangular area, about thirty by fifty miles in extent, lying between the White Mountain Indian Reservation and the western border of New Mexico, and covering the adjacent parts of Apache and Graham counties. It includes the eastern part of the White Mountains, which culminate in Ord and Thomas peaks, rising respectively to 10,266 feet and to 11,496 feet, on the White Mountain Indian Reservation, just off the western border of the Forest Reserve. This section of the reserve is strikingly more varied in physical conditions than the northern portion, as will be shown by the following description:

The northwestern part of this section, next to the peaks just mentioned, is an elevated mountainous plateau country forming the watershed between the extreme headwaters of the Little Colorado on the north and the Black and San Francisco rivers, tributaries of the Gila, on the south. The divide between the heads of these streams is so low that in the midst of the undulating country, where they rise, it is often difficult to determine at first sight to which drainage some of the small tributaries belong. This district is largely of volcanic formation, and beds of lava cover large tracts, usually overlaid with soil, on which the forest flourishes.

The entire northern side of this section is bordered by the sloping gra.s.sy plains of the Little Colorado, which at their upper border have an elevation of 6,500 to 7,500 feet, and are covered here and there with pinons, cedars and junipers, especially along the sides of the canyons and similar slopes. At the upper border of this belt the general slope becomes abruptly mountainous, and rises to 8,000 or 8,500 feet to a broad bench-like summit, from which extends back the elevated plateau country already mentioned. This outer slope of the plateau is covered with a fine belt of yellow pine forests, similar in character to that found in the northern part of the reserve. Owing to the more abrupt character of the northerly slope of this belt, and its greater humidity, the forest is more varied by firs and aspens, especially along the canyons, than is the case further north. Here and there along the upper tributaries of the Little Colorado, small valleys open out, which are frequently wooded and contain beautiful mountain parks.

The summit of the elevated plateau country about the headwaters of the Little Colorado and Black rivers (which is known locally as the "Big Mesa"), is an extended area of rolling gra.s.sy plain, entirely surrounded by forests and varied irregularly by wooded ridges and points of timber. This open plain extends in a long sweep from a point a few miles south of Springerville westward for about fifteen miles along the top of the divide to the bases of Ord and Thomas peaks. These elevated plains are separated from those of the Little Colorado to the north by the belt of forests already described as covering the abrupt northern wall of the plateau. On the other sides of the "Big Mesa" an unbroken forest extends away over the undulating mountainous country as far as the eye can reach. The northerly slopes of the higher elevations in this section are covered with spruce forest.

The most varied and beautiful part of the entire Black Mesa Reserve lies in the country extending southeasterly from Ord and Thomas peaks and immediately south of the "Big Mesa." This is the extreme upper part of the basin of Black River, which is formed by numerous little streams rising from springs and wet meadows at an elevation of from 8,500 to 9,500 feet. The little meadows form attractive gra.s.sy openings in the forest, covered in summer with a mult.i.tude of wild flowers and surrounded by the varied foliage of different trees and shrubs. The little streams flow down gently sloping courses, which gradually deepen to form shallow side canyons leading into the main river. Black River is a clear, sparkling trout stream at the bottom of a deep, rugged box canyon, cut through a lava bed and forming a series of wildly picturesque views. The sides of Black River Canyon and its small tributaries are well forested. On the cool northerly slope the forest is made up of a heavy growth of pines, firs, aspens and alder bushes, which give way on the southerly slope, where the full force of the sun is felt, to a thin growth of pines, gra.s.s and a little underbrush.

At the head of Black River, between 8,000 and 9,000 feet, there are many nearly level or gently sloping areas, sometimes of considerable extent.

These are covered with open yellow pine forests, with many white-barked aspens scattered here and there, and an abundance of gra.s.ses and low bushes. This was once a favorite summer country for elk, and I have seen there many bushes and small saplings which had been twisted and barked by bull elk while rubbing the velvet from their horns.

Immediately south and east of Black River lies the Prieto Plateau, a well wooded mountain ma.s.s rising steeply from Black River Canyon to a broad summit about 9,000 feet in alt.i.tude. The northerly slopes of this plateau, facing the river, are heavily forested with pines, firs, aspens and brushy undergrowth, and are good elk country. The summit is cold and damp, with areas of spruce thickets and attractive wet meadows scattered here and there. Beyond the summit of the plateau, to the south and east, the country descends abruptly several thousand feet, in a series of rocky declivities and sharp spur-like ridges, to the canyon of Blue River, a tributary of the San Francisco River. This slope, near the summit, is overgrown with firs, aspens and pines, which give way as the descent is made, to pinons, cedar and scrubby oak trees and a more or less abundant growth of chaparral. Small streams and springs are found in the larger canyons on this slope, while far below, at an alt.i.tude of about 5,000 feet, lies Blue River.

The country at the extreme head of Blue River forms a great mountain amphitheater, with one side so near the upper course of Black River that one can traverse the distance between the basins of the two streams in a short ride. The descent into the drainage of Blue River is very abrupt, and is known locally as the "breaks" of Blue River. The scenery of these breaks nearly, if not quite, equals that on "The Rim" of Tonto Basin in its wild magnificence. The vegetation on the breaks shows at a glance the milder character of the climate, as compared with that of the more elevated area about the head of Black River. In the midst of the shrubbery growth on the breaks there is a fine growth of nutritious gra.s.ses, which forms excellent winter forage.

The entire southern part of the reserve lying beyond the Prieto Plateau is an excessively broken mountainous country, with abrupt changes in alt.i.tude from the hot canyons, where cottonwoods flourish, to the high ridges, where pines and firs abound.

The northeastern part of the section of the reserve under consideration is cut off from the rest by the valley of Nutrioso Creek, a tributary of the Little Colorado, and by the headwaters of the San Francisco River. It is a limited district, mainly occupied by Escudilla Mountain, rising to 10,691 feet, and its foothills. Escudilla Mountain slopes abruptly to a long truncated summit, and is heavily forested from base to summit by pines, aspens and spruces. On the south the foothills merge into the generally mountainous area. On the north, at an alt.i.tude of about 8,000 feet, they merge into the plains of the Little Colorado, varied by gra.s.sy prairies and irregular belts of pinon timber.

The upper parts of the Little Colorado and Black Rivers, above 7,500 feet, are clear and cold, and well stocked with a native species of small brook trout.

Owing to the generally elevated character of the southeastern section of the Black Mesa Reserve, containing three mountain peaks rising above 10,000 feet, the annual precipitation is decidedly greater than elsewhere on the reserve. The summer rains are irregular in character, being abundant in some seasons and very scanty in others; but there is always enough rainfall about the extreme head of Black River to make gra.s.s, although there is always much hot, dry weather between May and October. The fall and winter storms are more certain than those of summer, and the parts of the reserve lying above 8,000 feet are usually buried in snow before spring--frequently with several feet of snow on a level. The amount of snow increases steadily with increase of alt.i.tude. Some of the winter storms are severe, and on one occasion, while living at an alt.i.tude of 7,500 feet, I witnessed a storm during which snow fell continuously for nearly two days. The weather was perfectly calm at the time, and after the first day the pine trees became so loaded that an almost continual succession of reports were heard from the breaking of large branches. At the close of the storm there was a measured depth of 26 inches of snow on a level at an alt.i.tude of 7,500 feet. A thousand feet lower, on the plains of the Little Colorado, a few miles to the north, only a foot of snow fell, while at higher alt.i.tudes the amount was much greater than that measured.

The summer temperatures are never excessive in this section, and the winters are mild, although at times reaching from 15 to 20 degrees below zero. Above 7,500 feet, except on sheltered south slopes, snow ordinarily remains on the ground from four to five months in sufficient quant.i.ty to practically close this area from winter grazing. Cattle, and the antelope which once frequented the "Big Mesa" in considerable numbers, appeared to have premonitions of the coming of the first snow in fall. On one occasion, while stopping at a ranch on the plains of the Little Colorado, just below the border of the Big Mesa country, in November, I was surprised to see hundreds of cattle in an almost endless line coming down from the Mesa, intermingled with occasional bands of antelope. They were following one of the main trails leading from the mountain out on the plains of the Little Colorado. Although the sun was s.h.i.+ning at the time, there was a slight haziness in the atmosphere, and the ranchmen a.s.sured me that this movement of the stock always foretold the approach of a snowstorm. The following morning the plains around the ranch where I was stopping were covered with six inches of snow, while over a foot of snow covered the mountains. Bands of half-wild horses ranging on the Big Mesa show more indifference to snow, as they can dig down to the gra.s.s; but the depth of snow sometimes increases so rapidly that the horses become "yarded," and their owners have much difficulty in extricating them.

The southerly slopes leading down from the divide to the lower alt.i.tudes along the Black River and the breaks of the Blue, are sheltered from the cold northerly winds of the Little Colorado Valley, while the greater natural warmth of the situation aids in preventing any serious acc.u.mulation of snow. As a result, this entire portion of the reserve forms an ideal winter game range, with an abundance of gra.s.s and edible bushes. The varied character of the country about the head of Black River makes it an equally favorable summer range for game, and that this conjunction of summer and winter ranges is appreciated by the game animals is shown by the fact that this district is probably the best game country in all Arizona.

LARGE GAME IN THE SOUTHEASTERN PART OF TUB BLACK MESA RESERVE.

The large game found in this section of the reserve includes the elk, black-tailed deer, Arizona white-tailed deer, black and silver-tipped bears, mountain lions and wildcats, timber wolves and coyotes.

Elk were formerly found over most of the pine and fir forested parts of this section of the reserve, but were already becoming rather scarce in 1885, and, although they were still found there in 1897, it is now a question whether any survive or not. If they still survive, they are restricted to a limited area about the head of Black River from Ord Peak to the Prieto Plateau. Black-tailed deer are still common, and their summer range extends more or less generally over all of the forested part of this section above 7,500 feet. In winter only a few stray individuals remain within the reserve on the Little Colorado side, but a number range out into the pinon country on the plains of the Little Colorado. The country about the head of Black River is a favorite summer range of this deer, but in winter they gradually retreat before the heavy snowfalls to the sheltered canyons along Black River and the breaks of the Blue. In September and October the old males keep by themselves in parties of from four to ten and range through the glades of the yellow pine forest.

The Arizona white-tailed deer is not found on the part of the reserve drained by the Little Colorado River, but is abundant in the basin of Blue River, and ranges in summer up into the lower part of the yellow pine forest along Black River. They retreat before the early snows to the breaks of the Blue, where they are very numerous. During hunting trips into their haunts in October and November, I have several times seen herds of these deer numbering from thirty to forty, both before and after the first snowfall. Antelope formerly ranged up in summer from the plains of the Little Colorado over the gra.s.sy Big Mesa country and through the surrounding open pine forest, retreating to the plains in the autumn, but they are now nearly or quite exterminated in that section. Bears of both species wander irregularly over most of the reserve in summer, but are most numerous on the breaks of the Blue and about the head of Black River. In autumn, previous to their hibernation, they descend along the canyon of the Black River and among the breaks of the Blue, where acorns and other food is abundant.

Mountain lions also wander over all parts of the reserve, but are common only in the rough country along the Blue. Wildcats are rather common and widely distributed, but are far more numerous on the Black and the Blue rivers. Timber wolves were once rather common, but are now nearly extinct, owing to their persecution by owners of sheep and cattle. Coyotes occur in this district occasionally in summer. Wild turkeys are found more or less generally throughout this section of the reserve, retreating in winter to the warmer country along the breaks of the Blue and the canyon of Black River, where they sometimes gather in very large flocks.

NOTES ON SETTLEMENTS, ROADS AND OTHER MATTERS.

The greater part of this section of the Black Mesa Reserve is unsettled, but the northeastern corner, along Nutrioso Creek and the head of San Francisco River, is traversed by a wagon road leading to Springerville. Within the limits of the reservation on this road are two small farming villages of Nutriose and Alpine. The owners of the small farms along the valleys of these streams also raise a limited number of cattle and horses on the surrounding hills. A few claims are also held at scattered points along the extreme northern edge of the reserve between Springerville and Nutrioso. Between 1883 and 1895 several herds of cattle were grazed on the head of Black River, and ranged in winter down on the breaks of the Blue and the canyons of Black River; but I understand that these ranges have since been abandoned by the cattle men. For some years the sheep men have grazed their flocks in summer over the Big Mesa country and through the surrounding open forest. In addition to the damage done by the grazing of the sheep, the carelessness of the herders in starting forest fires has resulted in some destruction to the timber. Fortunately, the permanent settlers on this section of the reserve are located in the northeastern corner, which is the least suitable portion of the tract for game. In addition to the wagon road from Springerville to Nutrioso another road has been made from Springerville south across the Big Mesa to the head of Black River. Trails run from Nutrioso and Springerville to the head of Blue River and down it to the copper mining town of Clifton, but are little used. At various times scattered settlers have located along the Blue, and cultivated small garden patches. The first of these settlers were killed by the Apaches, and I am unable to say whether these farms are now occupied or not. In any case, the conditions along the tipper Blue are entirely unsuited for successful farming.

Perhaps the most serious menace to the successful preservation of game on this tract is its proximity to the White Mountain Indian Reservation. This reservation not only takes in some of the finest game country immediately bordering the timber reserve, including Ord and Thomas peaks, but is often visited by hunting parties of Indians.

During spring and early summer, all of the yellow pine and fir country in this section is subjected to a plague of tabano flies, which are about the size of large horse-flies. These flies swarm in great numbers and attack stock and game so viciously that, as a consequence, the animals are frequently much reduced in flesh. The Apaches take advantage of this plague to set fire to the forest and lie in wait for the game, which has taken shelter in the smoke to rid itself from the flies. In this way the Indians kill large numbers of breeding deer, and at the same time destroy considerable areas of forest. While on a visit to this district in the summer of 1899 Mr. Pinchot saw the smoke of five forest fires at different places in the mountains, which had been set by hunting parties of Indians for the purpose. The only method by which not only the game but the forest along the western side of this reserve can be successfully protected will be to have the western border of the forest reserve extended to take in a belt eight to twelve miles wide of the Indian reservation. This would include Ord and Thomas peaks, and would serve efficiently to protect the country about the headwaters of the rivers from these destructive inroads.

The northern border of this section of the reserve is about one hundred miles by wagon road from the nearest point on the Santa Fe Pacific Railroad. Seven miles from its northern border is the town of Springerville, with a few hundred inhabitants in its vicinity engaged in farming, cattle and sheep growing. From Springerville north extends the plains of the Little Colorado to St. Johns, the county seat of Apache county, containing a few hundred people. To the south and east of the reserve there are no towns for some distance, except a few small settlements along the course of the San Francisco River in New Mexico, which are far removed from the part of the reserve which is most suitable for game. The fact that deer continue abundant in the district about the head of Black River, although hunted at all seasons for many years, and the continuance there of elk for so long, under the same conditions, is good evidence of the favorable conditions existing in that section for game.

_E.W. Nelson_.

Const.i.tution of the Boone and Crockett Club

FOUNDED DECEMBER 1887.