
South Loop trail heading towards the summit of Mt. Charleston (view
northwest).
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Overview
Mt. Charleston is a large
(56,600 acres) wilderness area that includes the highest peak in
southern Nevada, Mt. Charleston (11,918 feet), and all of the higher
elevations in the Spring Mountains. Much of the land over about 7,000
feet is included in the wilderness area. These mountains are rugged,
with towering carbonate cliffs, steep hillsides, and deep narrow
canyons. The highest, wind-swept summit ridges are barren, but the
lower ridges and slopes are cloaked in a forest of ancient bristlecone
pine. Lower down, extensive forests of ponderosa pine and white fir
provide habitat for the Palmer's chipmunk, a species that only occurs
in the Spring Mountains. Below those forests, a pinyon-juniper woodland
dominates the landscape. The only herd of Rocky Mountain elk in Clark
County can be found near Cold Creek. Snowmelt and a few springs provide
water for wildlife.
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Trail art (view north).
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In 1989, about 43,000
acres of the Mt. Charleston National Recreation Areas was designated as
the Mt. Charleston Wilderness Area. In 2002, another 13,600 acres were
added, for a total of about 56,600 acres in the Mt. Charleston
Wilderness Area. This wilderness area is adjacent to the La Madre
Wilderness Area, which is adjacent to the Rainbow Mountain Wilderness
Area. In total, these three areas combine to form about 129,000 acres
of designated wilderness.
Link to a map
of the
wilderness
area.
Link to hikes
in the wilderness area.
Location
The Mt. Charleston
Wilderness Area is located about 20 air-miles northwest of downtown Las
Vegas.
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Rocks and bristlecone pine on the summit of Bonanza Peak (view south
towards Mt. Charleston).
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Boundaries
The boundary of this
wilderness area is complex, largely following contour lines and
ridgelines. Essentially, the wilderness area includes all of the high
elevation land surrounding Charleston Peak. This creates a hub at Mt.
Charleston with six large lobes that extend out in all directions. The
wilderness extends south to the USFS boundary (boundary of the La Madre
Mountain Wilderness Area) and north to Willow Peak near the town of
Cold Creek. The wilderness area extends east to encompass Mummy
Mountain and southwest to include the ridge between Carpenter and Trout
canyons. The developed areas in Kyle and Lee canyons are almost
entirely surrounded by wilderness.
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Fall colors on a sunny hillside below Griffith Peak (view west).
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Access
Access easiest access if
from the paved roads into Kyle and Lee canyons. Access is also provided
by several dirt roads, including the Harris Canyon Road, the road above
Cold Creek, and several roads on the west side of the mountains.
Terrain
Mt. Charleston Wilderness
area includes much of the Spring Mountains, which is a high and rugged
carbonate ridge that generally runs north-south. There are towering
crags, deep and wide canyons, narrow slot canyon, and steep hillsides.
Elevations range from about 6,500 feet on the lowest slopes in the
southwest part of the wilderness area, to nearly 12,000 feet at the
summit of Mt. Charleston. Most of the land is steep. There are many
deep canyons, but little flowing water after the snow melts.
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Limestone canyon below McFarland Peak (view northwest).
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Habitat Type
The Spring Mountains have
about a 10,000-foot elevation gradient (from desert floor to Mt.
Charleston summit). As one goes up, the climate gets cooler, producing
climate zones, and the climate zones produce life zones where different
species of plants and animals can exist. There are six climate zones in
the Spring Mountains, a change in habitat that would be similar to
traveling from the Desert Southwest to the Canadian Arctic. From bottom
to top, the life zones are Lower Sonoran, Upper Sonoran, Transition,
Canadian (montane), Hudsonian (subalpine) and Arctic.
The Lower Sonoran and
Upper Sonoran both provide conditions suitable for creosote bush and
Joshua trees, but the Lower Sonoran is drier and hotter than the Upper
Sonoran. The lower Transition Zone provides conditions suitable for
pinyon-juniper forests and sagebrush, while the upper Transition Zone
provides conditions suitable for ponderosa pine, manzanita, and scrub
oak. The Canadian (montane) Zone provides conditions suitable for
Douglas fir, spruce trees, and aspen. The Hudsonian (subalpine) Zone
provides conditions suitable for bristlecone pine and few other
species. The Arctic Zone provides conditions that are unsuitable for
trees; this is above treeline where only low shrubs, grasses, and forbs
can exist.
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Old ponderosa pine and fir trees along the North Loop trail (view
south).
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The wilderness area
contains 18,000 acres of Bristlecone pine, the most extensive stand of
these ancient trees in the intermountain region. These trees are among
the oldest living organisms in the world.
Wildlife
The same elevation zones
that provide conditions suitable for different species of vegetation
also provide conditions that area suitable for different species of
animals. At low elevation, species typical of the desert (for example,
white-tailed antelope squirrel, jackrabbit, kit fox) are common. At
middle elevations, other species exist (for example, Palmer's chipmunk,
mule deer). At higher elevations, others occur (for example, golden
mantle ground squirrel). Conditions are too harsh at the highest
elevations from most species, but Rock Wrens, and Ravens can be found
there.
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Above treeline southeast of Mt. Charleston (view north).
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The diversity of
elevations and vegetation types provides habitat for numerous species
of mammals, including bighorn sheep, deer, mountain lion, bob cats,
foxes, and a plethora of bat and rodent species. Reptiles and birds are
equally diverse. The higher elevations provide nesting habitat for
neotropical migrants. Water is available in sandstone potholes and
springs.
Archaeology
No specific information, but the mountain is important to local tribes.
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Grand views from the summit of Mt. Charleston, even if that is Las
Vegas in the background (view southeast).
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Geology
The Spring Mountains are
formed from tilted and uplifted carbonate rocks that date from the
Cambrian through the Pennsylvanian, with a bit of Permian rock mixed
in. Fossils generally are uncommon, but crinoid stems and shells are
abundant in some places (for example, the summit of Griffith Peak).
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