
McCullough Mountain (view northeast from Highway 164 near the
California State line).
|
Overview
South McCullough is a fairly large (44,252 acres)
wilderness
area that includes most of the southern part of the north-south
trending McCullough Range and the large bajada to the southwest. The
Southern McCullough Mountains are formed of 1.7-billion-year-old
metamorphic rock, with a bit of more recent volcanic rock in the
northern part of the wilderness area. The peaks and ridges look softer
and more rounded than many peaks in southern Nevada, but they are still
quite rocky, rugged, and exceed 7,000 feet in height. The base of the
mountains are at about 3,300 feet on the west side and 4,500 feet on
the east side. Springs in the wilderness area provide water for
wildlife and early human inhabitants.
Despite the proximity to Las Vegas, the South
McCullough
Wilderness Area is a wild and rugged place with few signs of human use
except for cattle that still roam the area. The difficulty of getting
to the wilderness area adds to the feeling of isolation, providing a
true wilderness experience for hikers. Even visiting the edge of the
wilderness area (e.g., Pipe Spring) provides a great introduction to
this wonderful and wild place. A hike up McCullough
Mountain (7,026 ft), into the heart of the wilderness area,
provides a great introduction to the area.
|

McCullough Mountain (view northwest from Wee Thump Wilderness Area). |
Although the northern and southern ends of the
McCullough
Range are named as a single mountain range, the two ends differ and are
not one geologic feature. The northern end of the McCullough
Range (North
McCullough Wilderness Area)
was formed from recent volcanic activity, while the southern end (South
McCullough Wilderness Area) is a ridge of ancient metamorphic rock.
Link to map
of the wilderness area.
Location
The wilderness area is located approximately 45
air-miles
south of Las Vegas, between Interstate-15 and Highway 95, and north of
Highway 164. It is about 15 miles northwest of Searchlight.
|

Sandy wash. |
Boundaries
The boundaries of this wilderness area are
complex, but
essentially they include all of the high elevation land surrounding
South McCullough Mountain. The northern boundary is marked by a
powerline road that runs over McCullough Pass. The southern boundary is
not marked, but it follows canyons on the east and west sides of the
range (the canyons just south of Pine Spring Canyon). The western
boundary extends out from the base of the mountains to follow a wash in
the valley between the McCullough Range and the Lucy Gray Range. The
eastern boundary basically follows the contour of the mountains at the
top of the bajada.
Access
Access is from dirt roads on the southeast, west,
and
northern sides of the wilderness area. The southeast side of
the wilderness area can be accessed from
Searchlight via Pipe Spring Road. The road is marginally accessible in
a 2-wheel-drive, high-clearance vehicle when the road is dry. For
details of the road, see the McCullough
Mountain hike.
|

Singleleaf Pinyons, Utah Junipers, and Joshua Trees on rounded ridges.
|
Terrain
The Southern McCullough Range is a north-south
orientated,
ridge of rugged old metamorphic rock deeply cut by canyons on the east
and west sides. North of McCullough Mountain (7,026 ft),
fault-influenced valleys run north-south, parallel to the crest of the
range, creating a jumble of peaks and valleys. The wilderness area
includes a wide bajada on the west side of the mountains.
While the overall structure of the mountain range
is a
north-south ridge with canyons cutting east and west from the crest,
the detail of the terrain is quite complex. Ridges and canyons run in
all directions; for example, one canyon on the west side of the range
begins by running east, then curves to the south before turning and
running west and out onto the bajada. The rounded ridgetops and winding
canyons make this a challenging area for route finding.
|

Nature art.
|
Habitat Types
The lower elevations are dominated by Mojave Desert
Scrub
(Upper Sonoran Life Zone), where Creosote
Bush, Mojave
Yucca, Banana
Yucca, Buckhorn
Cholla, and low-growing shrubs are common. Scattered
Honey
Mesquite
occur in washes, as do more common Catclaw
Acacia and Apache
Plume.
The middle elevations are
also Mojave
Desert Scrub (Upper Sonoran Life Zone), but the vegetation is
dominated by Blackbrush,
Joshua
Trees, Buckhorn
Cholla, Mojave Yucca,
and Banana
Yucca.
The higher elevations are dominated by a Pinyon-Juniper
Woodland
(Upper Sonoran Life Zone), where Singleleaf
Pinyon Pine, Utah
Juniper, various Cholla, Pricklypear,
and Hedgehog
cactus, Banana
Yucca,
and a variety of knee-high shrubs are common. On the peaks, California
Juniper replace Utah
Juniper.
|

Sunset from atop McCullough Mountain. |
Wildlife
Mammals include desert
bighorn sheep, mule deer, black-tailed
jackrabbits, desert
cottontail rabbit, White-tailed Antelope Squirrel, woodrats,
and cows. Reptiles include desert
tortoise at the lower elevations, Western
Fence Lizards, Side-blotched
Lizards,
and a variety of other lizards and snakes. Birds include Gambel's
quail, Chukar, Juniper Titmouse, Spotted Towhee, Bushtits, Red-tailed
Hawks, Common Raven, Golden Eagle, Northern Flicker, Black-throated
Sparrows, Chipping Sparrow, White-crowned Sparrow, Crissal Thrasher,
and other songbirds.
Archaeology
No specific information, but locals report
petroglyphs
near Pipe Spring. I looked, but not see any rock art.
|

Banded metamorphic rock. |
Geology
The South McCullough Mountains are formed
primarily of
1.7-billion-year-old foliated metamorphic rocks, the second oldest
rocks in Nevada. Most of the ridges have weathered to a gently rounded
tops with steep sides, but rocky outcrops of layered metamorphic rock
and quartzite are common. Near the crest of the range, the ridges
themselves are steep, even though they retain broad, gently rounded
crests. The wilderness area has been influenced by volcanic activity to
the north. Faults north of McCullough Mountain (7,026 ft) run
north-south and parallel to the crest of the range, creating deep
canyons that run north-south before turning and flowing out onto the
bajada. The bajada on the west side of the range is formed on old
alluvial deposits, which is in contrast to the Quaternary alluvial
deposits found in most of southern Nevada. The ridges are steep and
rocky, but rounded, and the washes are deep, sandy, and run at more
gentle grades than are found in the limestone mountains around southern
Nevada.
|

Ancient juniper trees. |
Threats
As of 2007, cattle still roam these mountains, including the
highest
ridges and peaks, and their grazing and bedding activities disturb
large areas of soil on many of the ridges. Cattle trails can be found
on many ridges, some sidehills, and in washes.
Off-road vehicles penetrate far up the sandy
washes on
the east and west sides of the range.
|
|