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Modoc National Forest |
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Forest Plan Roadless AreasNational Roadless Policy web page.
Within its boundaries, the Modoc National Forest has 19 inventoried roadless areas totaling 201,600 Acres.
The information about the
Roadless Areas is summarized from Appendix E of the Modoc National Forest
Land and Resources Management Plan Environmental Impact Statement prepared
in 1991. The Damon Area description
has information pertaining to recent management activities. After the 1978 Roadless
Area Review and Evaluation, the Forest Service recommended adding
1,940 acres to the South Warner Wilderness.
On September 28, 1984, The California Wilderness Act (Public Law
98-425) amended the boundary of the South Warner Wilderness to include
those recommendations and released the remiaining inventoried roadless
areas from wilderness consideration for this planning period. Bear
Camp Flat – 2,300 acres
Bear Camp Flat adjoins the
South Warner Wilderness. The terrain is gently sloping until it approaches
the Wilderness where it steepens sharply to the ridge tops that form the
boundary on the west, north, and east sides of Bear Camp Flat. Lodgepole
pine, mahogany, and meadows dominate the landscape.
Big
Canyon – 6,400 Acres
Big Canyon
is located in the central portion of the Forest and is bisected by the
Pit River. The terrain is mountainous and extremely steep along the sides
of the river. Elevations range from 4,320 feet to 5,730 feet at the summit
of Noble Bluff to the west. The boundary is irregular and ill‑defined.
Roads surround the area. Big Canyon to the west is a long, arrow, moderately sloped canyon, with scattered ponderosa pine with dense pockets of timber at the head of the canyon. Pit River Canyon is extremely steep, dominated by large rocky outcrops. A major feature is Hanging Rock. The east side of the canyon contains numerous steep sided draws which contain scattered dense pockets of ponderosa pine. The canyon walls are vegetated with sagebrush and grass. Current uses include cattle grazing, hunting, and fishing.
Burnt
Lava Flow – 8,800 Acres
Burnt
Lava Flow is located on the western portion of the Forest and extends
onto the Shasta-Trinity National Forest.
The configuration is generally oval with the boundary following
the lava flow. The Flow
consists of a recent flow of jumbled, black lava surrounding three large
islands of timber on old cinder cones that protrude above the flow as
well as several small islands of timber in depressions caused by lava
dividing and flowing around them.
The prominent feature is High Hole Crater at the north, a semi-barren
cinder cone rising 386 feet above the flow, with a crater approximately
150 deep. Several ice caves
are located at the northern edge of the flow and others probably exist
in the largely unexplored interior region. There is no water source. Well-traveled
roads are visible from most points within the area. The Burnt
Lava Flow was withdrawn from mineral entry in 1967, following its original
classification as a Virgin Area in 1957.
On May 21, 1982, the area was classified as a Geological Area by
the Pacific Southwest Regional Forester.
This classification requires that the area remain in as near natural
condition as possible. Callahan
Flow – 8,000 Acres
The Callahan
Flow is located in the northwestern portion of the Forest and rests against
the south and west boundaries of the Lava Beds National Monument.
The configuration is long and narrow.
The north, west, and south boundaries meander along the Callahan
Lava Flow. The topography
is formed by two major lava flows and is characterized by broken rough
lava, gently flowing into two wavy fan shapes.
The oldest flow to the north is extensively covered by native bunchgrass,
while the southern area is rugged and difficult to travel. No water exists. Current
uses are principally cattle grazing, occasional sightseeing, hunting,
and educational and scientific study. Historic logging railroad grade parallels the southern boundary. Crane
Mountain – 2,400 Acres
Crane
Mountain is located in the north Warner Mountain range extending into
Oregon on the Fremont National Forest. This discussion is confined to
the 10% portion in California. The south boundary parallels the road north
of Cave Lake and Lily Lake campgrounds. The
topography is steep and mountainous, ranging from 5,000 feet along the
west boundary to 7,000 feet at the summit of an unnamed peak near the
Oregon border. Mixed conifer, white fir, juniper, lodgepole pine, and mountain mahogany dominate the area. Primary uses include a little cattle grazing and sightseeing. Non‑conforming uses include 2 miles of primitive roads providing access into private property, and remnants of past gold mining activity. Damon
Butte - 24,700 Acres
Damon Butte is located in the western portion of the Forest. The area
nestles between the Burlington Northern Railroad to the west and State
Highway 139 to the cast. Beyond the boundary to the north and south projects
Timber Mountain and Damon Butte .The
terrain is defined by vast expansions of relatively wary rough lava. Large
areas of juniper and sagebrush to the north and established timber stands
to the south provide some variety. Current uses include sheep grazing,
hunting, and wood gathering. Nearly
10,000 Acres of the area was burned in the 1996 Damon-Long Fire.
Over 65 miles of dozer lines were established during this 23,373
acre fire, many in the Damon Butte area.
Timber salvage occurred on the scattered timber stands over 2,600
acres. Much of the area is
in plantations and managed for timber production.
Over 48 miles of roads are contained in the area. Dobie Flat – 12,900 Acres
Dobie
Flat is located in the western portion of the Forest. The boundary runs
parallel to the Southern Pacific Railroad and a 500‑KV power line
on the east, and the Burlington Northern Railroad (BNR) on the west. The
Lavas roadless area lies across the tracks to the west of the BNR. The
terrain consists of expansive areas of flat, broken, rough lava. Grasses
interrupted by extensive stands of sagebrush and juniper dominate the
landscape. The predominant feature of the area is Casuse Mountain, a barren
hill. The climate is generally windy year‑round. The topography
provides little available refuge. Wild fires are common.
Dry
– 7,100 Acres
Dry is located in the central portion of the Warner Mountain range, adjacent to the Forest boundary, and north of the Parker Creek Road. Terrain is mountainous and steep, ranging from 5,200 feet to 6,840 feet at the summit of an unnamed peak east of Dry Creek Basin. Vegetation consists of heavy timber in the canyons with juniper on the ridges. Primary
uses include hunting and cattle grazing. Nonconforming uses include livestock
ponds, scattered throughout the area, and a fence which borders the private
land to the north. The
area contains habitat for mule deer winter and summer range, and fawning
areas, as well as prairie falcon nest sites. Hat
Mountain – 9,900 Acres
Hat
Mountain is located at the extreme southern end of the Warner Mountains
adjacent to the Forest boundary. The terrain is generally mountainous,
ranging from 7,000 feet to 8,700 feet at the summit of Hat Mountain. Lodgepole
pine and mixed conifers, mountain mahogany, and grasses dominate the
landscape. Hunting
and livestock grazing are primary uses. Nonconforming uses including
livestock watering ponds, approximately 27 miles of primitive road and
2.5 miles of road providing logging truck access to a 730‑acre commercial
firewood cutting area. Wildlife
habitat consists of mule deer summer range and fawning areas; existing
and potential goshawk; potential for pileated woodpecker, osprey, and
prairie falcon; and nesting and brood rearing sites for waterfowl. Knox Mountain – 5,900 Acres Knox
Mountain is located at the southern edge of the Forest and straddles the
Modoc‑Lassen County line. Sears Flat roadless area is located to
the east. The west boundary follows a ridge but the northwest and eastern
boundaries lack definition. Knox Mountain, the prominent feature runs
north and south through the central part. The eastern slopes of Knox Mountain
are dominated with open stands of ponderosa pine. Wild fires are typical.
The western slopes of Knox Mountain are dominated with sagebrush and
scattered young juniper with large stands of mountain mahogany.
Primary uses of the area include hunting and cattle grazing. Suitable
wildlife habitat consists of summer range for pronghorn, and winter and
summer range for mule deer with localized areas used for fawning.
Lavas
– 25,400 Acres
Lavas
is located in the western portion of the Forest. The boundary runs parallel
to the Lava Beds National Monument on the west, and the BNR on the east.
Dobie Flat roadless area lies across the tracks to the east of the BNR.
The terrain consists of expansive areas of flat, broken, rough lava.
Grasses interrupted by extensive stands of sagebrush and juniper
dominate the landscape. The climate is generally windy year‑round.
The topography provides little available refuge. Wild fires are common.
Primary uses of the area are sheep grazing and big game hunting. The area
provides key winter range for deer and pronghorn.
Mount Bidwell – 11,600 AcresMount
Bidwell is located north of the Warner Mountain range extending into
Oregon on the Fremont National Forest. This discussion is confined to
the 72% portion in California. This roadless area is bordered on the east
by the Forest boundary, and the road from Fort Bidwell to New Pine Creek
forms most of the western boundary. About 620 acres of private land are
located within the area. Topography
is generally mountainous and extremely steep, ranging from 5,400 feet
to 8,290 feet high at the summit of Mount Bidwell, the dominant feature.
Vegetation consists of lodgepole pine and mixed conifer at higher elevations,
giving way to mountain mahogany, aspen and willows and grasses at the
lower elevations. Primary
uses include hunting and livestock grazing. Non‑conforming uses
include fences and primitive roads. Old mining cabins, related facilities,
and mine tailings are visible along the northwestern boundary. Mount Hoffman – 10,800 Acres Mount
Hoffman is located in the western portion of the Forest to the north and
northeast of Medicine Lake recreational complex. The area consists of
two distinct contrasting features ‑ forested slopes of Mount Hoffman
to the west and Glass Mountain volcanic glass flow to the east. The configuration
is wide and narrow and generally surrounded by primitive logging and mining
roads. The western portion extends into the Klamath National Forest.
The gentle slopes of Mount Hoffman sweep upward rising to a peak of 7,913
feet where the surrounding area, including Mount Shasta and Lassen Peak,
can be viewed. Over 5,000 acres of fir, lodgepole pine, and mixed conifer
cover the landscape in an unbroken pattern. To
the east, in stark contrast, is Glass Mountain which is devoid of vegetation.
Formed through the accumulation of three independent lava flows, the
area displays a great mass of volcanic extrusion and a wide variety of
obsidian, pumice and minerals. Glass Mountain is a monolith reaching to
7,622 feet, the highest elevation of any lava flow in the Medicine Lake
Highlands. Visitation to the area is generally confined to the exterior
because of the rough, rugged lava terrain. There is no water.
Mount
Vida – 9,100 Acres
Mount
Vida is located on both sides of the main crest in the north Warner Mountains.
It is bordered on the west by the Forest boundary and meanders in a southeasterly
direction. Its configuration is long and narrow, and its boundary difficult
to locate on the ground. The topography is mountainous with steep canyons.
Elevations range from 5,200 feet along the western boundary to 8,200 feet
at the summit of Mount Vida, the dominant feature. Mount Vida provides
an excellent vista of California, Nevada, and Oregon. Vegetation
consists of scattered mixed conifer stands at the higher elevations giving
way to sage and grasses at the lower elevations. Primary uses are cattle
grazing and hiking. Non‑conforming uses include livestock water
developments and fences associated with grazing. The Highgrade National
Recreation Trail bisects the area in a southwest to northeast direction,
passing immediately west of the Mount Vida summit. Suitable
habitat for bald eagles has been identified in the area. Other habitat
includes mule deer. summer and winter range, existing and potential habitat
for goshawk, and potential nesting sites for prairie falcon and peregrine
falcon. Parsnip
– 8,200 Acres
Parsnip
is located in the southwest corner of the Warner Mountain range adjacent
to the Forest boundary. Blue Lake is located just east of the area, with
West Valley Reservoir to the west, outside the Forest boundary. Terrain
is gently sloping in the western portion, becoming gradually steeper
in the eastern portion with elevations ranging from 5,000 feet to 7,000
feet. Vegetation consists of mixed conifer at the higher elevations,
giving way to juniper and mahogany at the lower elevations. Primary
uses include hunting and cattle grazing. Nonconforming uses include livestock
ponds, trails, fences, a water diversion ditch not currently in use, and
four miles of primitive roads. Portions
of three cattle allotments, and one special use pasture, exist within
the area, producing approximately 650 AUMs annually.
Powley
– 6,200 Acres
Situated
on the eastern facing escarpment of the Warner Mountains, Powley is mountainous
and extremely steep. Elevations range from 5,000 feet to 7,600 feet at
the crest of the Warners. Vegetation in the area consists of lodgepole pine, mixed conifer, white fir, and ponderosa pine at the higher elevations, giving way to bitterbrush, mahogany, sage, and grasses at the lower elevations. Primary
use is limited by the steep terrain and consists of hunting and cattle
grazing. There are no physical improvements within the area.
Sears
Flat – 12,500 Acres
The
topography is characterized by moderate terrain dominated by sage, juniper
and mountain mahogany. Several small pockets of ponderosa pine are located
in the western portion. Primary
use of the area is cattle grazing and big game hunting. Wildlife habitat consist of pronghorn summer range and kidding grounds, and mule deer intermediate and summer range.
Soldier
– 9, 400 Acres
Soldier
is located in the central portion of the Warner Mountain range between
Lake City Canyon on the north and Highway 299 on the south. The area is
contiguous to the eastern boundary of the Forest. The communities of Lake
City and Cedarville are immediately east in Surprise Valley. The Lake
City Canyon road separates this area from Powley roadless area to the
north. Situated
on the eastern facing escarpment of the Warner Mountains, Soldier is mountainous
and extremely steep. Elevations range from 5,000 feet to 8,270 feet at
the summit of Bald Mountain. Vegetation
consists of lodgepole pine, mixed conifer, white fir, and ponderosa pine
at the higher elevations, giving way to mountain mahogany, sage, and grasses
at the lower elevations. Primary
use is limited by the steep terrain and consists of hunting and cattle
grazing. There is evidence of past logging on some of the lower slopes
(abandoned road, mill site, old stumps) but the area has almost returned
to a natural state. There are no other improvements existing in the area.
Steele
Swamp – 20,000 Acres
Steel
Swamp is located cast of Clear Lake Reservoir approximately three miles
south of the Oregon border. It is a remote area, and seldom visited except
for occasional recreational hunting and livestock operations. Most
of the land is open; topography is flat. Regular patterns of juniper and
grass dominate the landscape. The boundary is not well defined by topographic
or readily identifiable land features. Wet
meadows exist on about 30% of the area. Current uses in the area include livestock watering tanks, fences, an old telephone line right-of-way, and approximately 15 miles of primitive road. The historic Applegate Trail crosses the southwest portion. |
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USDA Forest Service - Modoc National Forest |