Tippett Canyon, is a valley whose creek drains the northwest watershed of the South Mountains in White Pine County, Nevada. Its mouth is at an elevation of 6,450 feet (1,970 meters). Its source is at the head of the canyon near Cedar Pass, at an elevation of 6,649 feet (2,027 meters) at 39°46′04″N114°10′02″W / 39.76778°N 114.16722°W . [1] [2]
The Feather River is the principal tributary of the Sacramento River, in the Sacramento Valley of Northern California. The river's main stem is about 73 miles (117 km) long. Its length to its most distant headwater tributary is just over 210 miles (340 km). The main stem Feather River begins in Lake Oroville, where its four long tributary forks join—the South Fork, Middle Fork, North Fork, and West Branch Feather Rivers. These and other tributaries drain part of the northern Sierra Nevada, and the extreme southern Cascades, as well as a small portion of the Sacramento Valley. The total drainage basin is about 6,200 square miles (16,000 km2), with approximately 3,604 square miles (9,330 km2) above Lake Oroville.
Temescal Creek is an approximately 29-mile-long (47 km) watercourse in Riverside County, in the U.S. state of California. Flowing primarily in a northwestern direction, it connects Lake Elsinore with the Santa Ana River. It drains the eastern slopes of the Santa Ana Mountains on its left and on its right the western slopes of the Temescal Mountains along its length. With a drainage basin of about 1,000 square miles (2,600 km2), it is the largest tributary of the Santa Ana River, hydrologically connecting the 720-square-mile (1,900 km2) San Jacinto River and Lake Elsinore watersheds to the rest of the Santa Ana watershed. However, flowing through an arid rain shadow zone of the Santa Ana Mountains, and with diversion of ground water for human use, the creek today is ephemeral for most of its length, except for runoff from housing developments and agricultural return flows.
Temescal Mountains, also known as the Sierra Temescal, are one of the northernmost mountain ranges of the Peninsular Ranges in western Riverside County, in Southern California in the United States. They extend for approximately 25 mi (40 km) southeast of the Santa Ana River east of the Elsinore Fault Zone to the Temecula Basin and form the western edge of the Perris Block.
Callville Wash is an ephemeral stream or wash in Clark County, Nevada. It was named for Callville the riverport settlement founded in 1866, at its mouth where it had its original confluence with the Colorado River.
Chaco River is a river tributary to the San Juan River in San Juan County, New Mexico. Its mouth lies at an elevation of 4,918 feet. Its source is located at an elevation of 6,050 feet at 36°05′10″N108°00′30″W, its confluence with Chaco Wash and Escavado Wash just northwest of the mouth of Chaco Canyon.
Elephant Butte Canyon or Lawhorn Canyon is a canyon in the Animas Mountains of Hidalgo County, New Mexico. Its stream is a tributary of Walnut Creek. Its mouth is located at elevation 5,535 feet / 1,687 feet at its confluence with Walnut Creek, just below Lawhorn Tank. Its source is located at 3.5 miles north northeast of its mouth 31°36′25″N108°39′20″W at an elevation of 6,050 feet on the southwest slope of Elephant Butte.
Currant Creek is a stream in eastern Juab County and southern Utah County in northern Utah, United States.
Coal Creek is a stream in eastern Iron County, Utah, United States.
Ingram Canyon is a valley or canyon where the upper reach of Ingram Creek runs in Stanislaus County, California.
Tippett is a populated place in White Pine County, Nevada. It lies at an elevation of 5,692 feet in Antelope Valley, south of the Goshute Indian Reservation.
South Mountains are a range of mountains primarily in White Pine County, Nevada and partially to the east in Juab County, Utah. The range is sometimes referred to as the Deep Creek Mountains, or the Ibenpah Mountains. The South Mountains are divided from the Kern Mountains to the south by Tippett Canyon on the west and Pleasant Valley to the east. They are divided from the Deep Creek Range to the east in Utah by Johnson Canyon, on the north, and by Water Canyon on the south. The range is bounded on the north by Spring Creek Flat and on the west by Antelope Valley.
Spring Valley is a long north south trending basin, largely in White Pine County, Nevada and a small portion in the extreme south in Lincoln County, Nevada. It extends from 39°59′00″N114°29′33″W in White Pine County to the north to 38°33′57″N114°21′05″W in the south in Lincoln County. The bottom of the basin is at Yelland Dry Lake at an elevation of 5,551 feet. Bahsahwahbee, a grove of Rocky Mountain juniper trees, locally called swamp cedars, where multiple massacres of Western Shoshone people occurred in the 19th century, lies in Spring Valley. The Spring Valley Wind Farm is to its south.
Cedar Pass is a gap between Tippett Canyon and Pleasant Valley in White Pine County, Nevada. These valleys divide the South Mountains from the Kern Mountains. It is lies at an altitude of 7,264 feet.
Regan is a ghost town, a historical mining town, and a former populated place in White Pine County, Nevada. It had its own Regan post office from August 1906 to November 1907. Its site lies at an elevation of 6,863 feet in Tippett Canyon in the South Mountains.
Johnson Canyon is a valley or canyon in Juab County, Utah. Its creek drains the eastern watershed of the South Mountains and divides those mountains from the Deep Creek Range to the east. The mouth of the canyon is at an elevation of 6,686 feet. Its source is at the head of the canyon at an elevation of 2,530 feet at 39°45′22″N114°01′48″W.
39°47′48″N114°12′10″W / 39.79667°N 114.20278°W