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Wildlife Specialist report

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AFFECTED ENVIRONMENT<br />

The Gila National Forest is located in southwest New Mexico. The Forest is divided<br />

into six Ranger Districts that have the responsibility of managing a land mass of 3.3<br />

million acres within Catron, Grant, Sierra, and Hidalgo Counties. Within this acreage<br />

there are 792,000 acres of designated Wilderness, and 2,300 acres of designated and<br />

proposed Research Natural Area. The Forest is currently open to motorized cross country<br />

use except in wilderness, designated and proposed Research Natural Areas, and restricted<br />

off-road vehicle areas or areas specifically signed or closed by Forest Order.<br />

The Forest landscape includes a wide variety of mountainous terrain. The Mogollon,<br />

Pinos Altos, Black Range, and Tularosa are the larger mountain ranges on the forest.<br />

Elevation ranges from 4,200 feet in the semi-desert lowlands to almost 11,000 feet in the<br />

rugged Mogollon Mountains. Lower elevations are characterized by rolling hills<br />

dissected by moderately steep canyons and sand washes. Higher elevations are<br />

characterized by rugged mountains, deep headwater canyons, elevated mesas, and rock<br />

walled cliffs. Rocky outcrops are prevalent, with some of the most rugged and remote<br />

areas in the southwest found along the west face of the Mogollon Mountains and the east<br />

face of the Black Range Mountains.<br />

Major drainages on the Forest include the main-stem and headwaters of the Gila, San<br />

Francisco, and Mimbres rivers. The Forest also has drainages that flow into the Rio<br />

Grande from the Black Range Mountains. Drainages that flow out of the Black Range<br />

that support perennial flow include Animas, Seco, Palomas, Cloride, and Percha creeks.<br />

The southwest side of the Black Range is drained by the headwaters and main-stem of the<br />

Mimbres River. Major tributaries to this river include McKnight Creek, and Iron Creek.<br />

Major tributaries within the Gila and San Francisco watersheds include the West, Middle,<br />

and East forks of the Gila River; Beaver, Taylor, Diamond, South Diamond, Black<br />

Canyon, Little, Sapillo, Turkey, Mogollon, Bear, Sycamores, Willow, Negrito, Tularosa,<br />

Centerfire creeks and Dry Blue River. Major variables that relate directly to the spatial<br />

distribution of riparian vegetation along these drainages are flooding, groundwater<br />

conditions, and various soil properties (particularly soil moisture). The flow regimes of<br />

the Gila, San Francisco, and Mimbres Rivers are primarily unrestricted by major<br />

impoundments or diversions; therefore, channel configurations are widely variable and<br />

the vegetation communities are represented by a diverse mosaic of many communities.<br />

Within these drainages there are tributaries and associated springs and seeps that support<br />

perennial and intermittent waters sources with associated riparian vegetation. Lakes on<br />

the Forest include Lake Roberts, Snow Lake, and Quemado Lake.<br />

Vegetation on the forest is diverse and complex. Tree, shrub, grass and forb species from<br />

the Rocky Mountains and Mogollon Plateau are integrated with species from the<br />

Chihuahuan Desert. The highest zone encompasses Engelmann and corkbark fir<br />

communities, followed by the Engelmann spruce and Douglas-fir community. Douglasfir,<br />

ponderosa pine, white fir, and southwestern white pine are dominant members of the<br />

next lower community. Aspen is commonly intermixed in portions of these higher<br />

elevations. Ponderosa pine is typically intermixed with either Gambel oak or alligator<br />

7

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