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Nevada–California–Baja California side
Nevada–California–Baja California side
*[[Eldorado Valley]]-([[endorheic]]
*[[Eldorado Valley]]-([[endorheic]])
*[[Piute Valley]]
*[[Piute Valley]]
*[[Laughlin, Nevada|Laughlin]]–[[Bullhead City, Arizona|Bullhead City]]
*[[Laughlin, Nevada|Laughlin]]–[[Bullhead City, Arizona|Bullhead City]]

Revision as of 23:36, 21 June 2020

A section of the LCRV showing the Colorado Desert-(yellow highlight) in west, the Salton Sea, and the three US bordering states on the Colorado River. Portions of the Mexican states of Baja California and Sonora also shown. Proximity to San Diego and the rain shadow of coastal mountains, also shown.
The Colorado River watershed; the LCRV arbitrarily starts south of Lake Mead, at Hoover Dam in Nevada.

The Lower Colorado River Valley (LCRV) is the river region of the lower Colorado River of the southwestern United States in North America that rises in the Rocky Mountains and has its outlet at the Colorado River Delta in the northern Gulf of California in northwestern Mexico, between the states of Baja California and Sonora. This north–south stretch of the Colorado River forms the border between the U.S. states of California/Arizona and Nevada/Arizona,[1] and between the Mexican states of Baja California/Sonora.

It is commonly defined as the region from below Hoover Dam and Lake Mead to its outlet at the northern Gulf of California (Sea of Cortez); it includes the Colorado River proper, canyons, the valley, mountain ranges with wilderness areas, and the floodplain and associated riparian environments. It is home to recreation activities from the river, the lakes created by dams, agriculture, and the home of various cities, communities, and towns along the river, or associated with the valley region. Five Indian reservations are located in the LCRV: the Chemehuevi, Fort Mojave and Colorado River Indian Reservations; at Yuma are the Quechan and Cocopah reservations.

Ecology

Trigo Mountains Wilderness, a ridgeline wilderness area on the eastern border of the river proper, 30 miles north of Yuma-Winterhaven. A buckhorn cholla cactus is in foreground; creosote bush scrubland on hillsides.

Some of the highest absolute air temperatures (of North America) are recorded in the LCRV, rivaling Death Valley; specifically Bullhead City, Lake Havasu City, Laughlin, Needles, Yuma, or the southeastern deserts of California, west of the Colorado River where extreme heat is the main summertime weather feature. Worldwide, only some deserts found in Africa and in the Middle East stand up with an even hotter summer climate on average. The LCRV is defined by three deserts. The Mojave Desert is in southeast California, southern Nevada, and northwest Arizona. South of the Mojave the Sonoran Desert spans both sides of the Colorado River. The Lower Colorado River Valley is in the western part of the Sonoran Desert, which is called the Colorado Desert. the Sonoran Desert region proper extends from areas west of the river, and then southeastwards to southeast Arizona, south along the eastern side of the Baja Peninsula cordillera to Baja California Sur, and southeast Sonora state, Mexico to the northern border of neighboring Sinaloa.

The LCRV extends about 350 miles (563 km) from Hoover Dam to the Colorado River Delta. The Sonoran Desert itself is more than twice as extensive north-to-south, and about 450 miles (724 km) in width. Two species, Desert Ironwood-(Olneya tesota)[2] and the Lesser Long-nosed Bat, have geographic ranges identical to the Sonoran Desert, and are indicator species of the Sonoran Desert region. The spring flowering of ironwood, and the bat species migration arrivals also become indicators of annual or multi-year climate trends for regions of the Sonoran Desert.

Flora

The Lower Colorado River Valley has unique plant communities because it is it is the most arid part of the desert and it has the highest temperatures, in excess of 120 °F (49 °C) during the summer. The low humidity means that most plants must have mechanisms that deal with severe water loss through evaporation. The soils tend to be typical desert soils, coarse and without well-developed organic horizons, and plants can only obtain soil water during and very soon after the infrequent rains.[3]

Dominant plants in the valleys are low shrubs such as Ambrosia dumosa (white bursage) and Larrea tridentata (creosote bush). Over half of the floral diversity comprises annual species, with even higher percentages in drier habitats.[3] Vulnerable species and plant communities include saltbush/wolfberry flats, saguaro, nightblooming cereus cacti, tamarisks, barrel cactus, Sonoran panicgrass, and Acuna cactus.[4]

Threats

The Lower Colorado River Valley subregion of the Sonoran Desert bioregion has multiple threats. Some major threats include urbanization, clearing of land for agriculture, human occupancy – especially as a result of imported external resources, and camping and camptrailers on BLM land. Other threats include harvesting for fuelwood, campfires, etc. of desert ironwood, Olneya tesota, destruction of land by offroad vehicles, especially in sand dunes, and harvesting and manipulation of groundwater.[4]

List of major cities and communities

Complete list of towns, areas, etc, north to south

Feeder-valleys, or included small valleys

References

Wikimedia Commons has media related to Lower Colorado River Valley.
  1. ^ "Lower Colorado River Valley" section, Center for Sonoran Desert Studies; [1]
  2. ^ Atlas of United States Trees, Volume 3, Minor Western Hardwoods, Map 103-Olneya tesota
  3. ^ a b "Sonoran Desertscrub - Lower Colorado River Valley by Mark A. Dimmitt :: ASDM Sonoran Desert Digital Library". Desertmuseumdigitallibrary.org. Retrieved 15 September 2018.
  4. ^ a b Ecological threats, Lower Colorado River Valley
  • Little. Atlas of United States Trees, Volume 3, Minor Western Hardwoods, Little, Elbert L, 1976, US Government Printing Office. Library of Congress No. 79-653298. Map 103, Olneya tesota.
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