Callville Wash

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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. [1]

Its mouth is at its confluence with Callville Bay, at an elevation of 1,234 feet / 376 meters when Lake Mead is at its full level. Currently as the reservoir is at a much lower level its mouth is found at approximately 36°08′3″N114°42′38″W / 36.13417°N 114.71056°W / 36.13417; -114.71056 . [2] Its source is located at an elevation of 3,510 feet / 1,070 meters at 36°16′35″N114°41′00″W / 36.27639°N 114.68333°W / 36.27639; -114.68333 on the southern slope of Muddy Peak (5387 ft / 1642 m) in the Muddy Mountains. [1]

Callville Wash originally had a tributary, originally known as West Fork Callville Wash, whose confluence with Callville Wash is now under Callville Bay. Following the creation of Lake Mead it now flows into Callville Bay, at 36°08′24″N114°42′57″W / 36.14000°N 114.71583°W / 36.14000; -114.71583 and is known as West End Wash. [3]

History

Callville Wash was part of the original 1829 Armijo Route of the Old Spanish Trail along the Colorado River, between the mouth of the Virgin River and mouth of Las Vegas Wash. That trail route bypassed the deep narrow gorge of Boulder Canyon through the Black Mountains by way of Boulder Wash, Pinto Valley and Cottonwood Spring to upper Callville Wash which it then followed down to the river. [4] Later the road between St. Thomas and Callville passed along this wash then northeasterly toward St. Thomas.

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West End Wash is an ephemeral stream or wash in Clark County, Nevada. Its mouth is at its confluence with the Callville Wash of Lake Mead at an elevation 1,250 feet / 381 meters at when Lake Mead is at its full level. Currently as the reservoir is at a much lower level its mouth is found at approximately 36°08′24″N114°42′57″W. Its source is at 36°15′55″N114°43′58″W at 3,083 feet / 940 meters in the Gale Hills.

Gale Hills, formerly considered part of the Muddy Range (1879), and later the South Muddy Mountains (1980s), are a range of hills southwest of the Muddy Mountains and about three miles north of the Boulder Basin of Lake Mead, in Clark County, Nevada. It is bounded on the east by Callville Wash; on the south by the Black Mesa lava flows; on the northwest by the valley of Gypsum Wash. Its highpoint is at 36°15′32″N114°43′12″W which lies at 3,756 feet / 1,145 meters.

Gypsum Wash is an ephemeral stream or wash in Clark County, Nevada. Gypsum Wash was originally a tributary of Las Vegas Wash before the formation of Lake Mead which submerged their confluence under Las Vegas Bay. Due to the lowering of the reservoir over recent years Gypsum Wash is once again a tributary of Las Vegas Wash, now exposed at 36°07′04″N114°50′54″W at an elevation of 1085 feet. When Las Vegas Bay is at its full level, Gypsum Wash flows into Lower Gypsum Wash Cove at 36°07′43″N114°51′26″W at an elevation of 1,204 feet / 367 meters.

Boulder Wash Cove is a cove in Lake Mead, in Clark County, Nevada. Boulder Wash for which the cove is named has its mouth in the cove at an elevation of 1,204 / 367 meters when the reservoir is at its full level.

Boulder Basin is the westernmost of the three basins occupied by the Lake Mead reservoir and lies within the boundaries of Clark County, Nevada and Mohave County, Arizona. It includes the area between Hoover Dam and the mouth of Boulder Canyon at Auxiliary Point. When the reservoir is full it reaches an elevation of 1,204 feet / 367 meters. It includes Las Vegas Bay, Swallow Bay, Callville Bay and Hamblin Bay.

References

Coordinates: 36°10′07″N114°33′07″W / 36.16861°N 114.55194°W / 36.16861; -114.55194