Lower Colorado River Basin
An overview of the Lower Colorado River Basin, including its geographical location, impacts, and human involvement.
Map of the Lower Colorado
Ryan Connick: GEOG 110 - Lower Colorado
Follow a Raindrop
Below, you can follow a raindrop through the Colorado River, including the Lower Colorado River Basin, on its way from White Hills, Arizona to the Golfo de California (the Gulf of California).
River Runner Global
Guided Tour
The Little Colorado River - A Tributary
The Little Colorado River is a tributary to the Lower Colorado River Basin and serves as an important connection to this larger body of water. As stated in the name, it is much smaller than its sibling river, the Colorado River, in length, flow, and drainage area. The waters are a turquoise color, which directly contrasts the appearance of the larger Colorado River.
4 things to know about the little colorado river. Grand Canyon Trust. (2023, September 13). https://www.grandcanyontrust.org/blog/4-things-know-about-little-colorado-river
Little colorado river. Nature Culture and History at the Grand Canyon. (n.d.). https://grcahistory.org/sites/colorado-river-corridor/little-colorado-river/
Rocky Mountain National Park
The Rocky Mountain National Park is located in Colorado and covers 265,807 acres. It is home to some of the highest mountains in the continental United States, which is up to 14,000 feet above sea level. This national park is home to a variety of wildlife and different habitats spanning from meadows to mountains.
U.S. Department of the Interior. (n.d.-b). Rocky Mountain National Park (U.S. National Park Service). National Parks Service.
Confluence of the Colorado River and the Little Colorado River
The confluence, the area where the Colorado River and Little Colorado River meet, is located at the eastern edge of the Grand Canyon. The intersection of these two rivers is a picturesque scene with the meeting of the light blue waters of the Little Colorado River and the blue-green waters of the Colorado River.
Yellowhair, V. (2023, April 23). Save the colorado river. Save the Confluence. https://savetheconfluence.com/environment/water/save-the-colorado-river/
Lake Havasu City
Lake Havasu City is a town on the edge of the Lower Colorado River Basin in western Arizona and was founded in 1964. More specifically, the city is located along Lake Havasu, and it is impounded by the Parker Dam, which is a major tourism spot.
Encyclopædia Britannica, inc. (2023, November 28). Lake Havasu City. Encyclopædia Britannica. https://www.britannica.com/place/Lake-Havasu-City
Hoover Dam
The Hoover Dam, which rests at 660 feet thick and nearly 726 feet high, stores part of the Colorado River which irrigates two million acres and generates enough hydroelectric power to serve 1.3 million people a year. The Hoover Dam is a huge tourism spot in itself, while influencing much of the surrounding population.
U.S. Department of the Interior. (n.d.). Nevada and Arizona: Hoover dam (U.S. National Park Service). National Parks Service. https://www.nps.gov/articles/nevada-and-arizona-hoover-dam.htm
Lee's Ferry
Lee's Ferry in Arizona serves as both an important political and historical landmark. It is the political boundary between the Upper Basin and the Lower Basin of the Colorado River. Historically, Lee's Ferry was the sight of the Mountain Meadows Massacre: a massacre of a group known as the Fancher Party. When negotiations were made for this location to be a safe crossing passage for this group, they were then massacred by the Mormon Militia disguised as Native Americans. The site is named after John D. Lee who orchestrated the attack and was later executed for his involvement. 120 people died during the attack in September 1857.
Wadzinski, G. (2023, October 11). Story of Lee’s ferry and the Mountain Meadows Masacre. Grand Canyon National Park Trips. https://www.mygrandcanyonpark.com/park/history/john-d-lee/#:~:text=After%20an%20initial%20siege%2C%20Lee,under%208%20years%20of%20age.
Climate Zone
Subtropical Desert - Bwh
The Lower Colorado River Basin's climate is classified as a Subtropical Desert, coded as "Bwh."
Characterized By:
- Referred to as a "hot desert," compared to the midlatitude deserts, which are referred to as "cold deserts."
- Tend to be centered around 25°-30° N and S latitude, especially along the west coast of continents, extending inward.
- Precipitation is scarce, unreliable, and intense
- Annual precipitation is usually between 2-8 inches.
- Summers are extremely hot (average is high 90s℉) and winters are mild (average is mid-60s℉)
- Increased insolation
- Spring and Fall as transition seasons
- Up to a 50℉ daily temperature range
Hess, D. (2017). McKnight's Physical Geography: A Landscape Appreciation (12th ed.). Pearson.
30-Year Normal Climograph
- A visual of the precipitation and temperature averages over 30 years (from 1991-2020), generated by PRISM.
- Precipitation
- Heavier precipitation during the winter months, with little to no precipitation during the summer months
- Temperature
- Temperature range of 67.2℉ between the maximum and minimum temperatures recorded
- Maximum temperature is on the lower end compared to some subtropical desert climate areas, but the minimum temperature is typical for this climate zone.
Oregon State University. (2024). Prism Climate Group: Northwest Alliance for Computational Science & Engineering. https://prism.oregonstate.edu/
30-Year Normal Data
A compilation of the average data points for the precipitation, minimum temperature, maximum temperature, and mean temperature for each month over 30 years.
Oregon State University. (2024). Prism Climate Group: Northwest Alliance for Computational Science & Engineering. https://prism.oregonstate.edu/
2021-2022 Climograph
- 2021
- Most precipitation occurred during the summer months, which is the opposite of the 30-year normal
- Generally a warmer year overall compared to the 30-year normal, with a maximum temperature of 108.5℉
- 2022
- Follows a similar pattern to 2021, both precipitation and temperature wise
- Most precipitation occurred in the summer and fall months, which varies from the 30-year normal.
- The mean temperature varied more compared to 2021 but was still similar to the 30-year normal.
Oregon State University. (2024). Prism Climate Group: Northwest Alliance for Computational Science & Engineering. https://prism.oregonstate.edu/
2021-2022 Climograph Data
A compilation of the data points for the precipitation, minimum temperature, maximum temperature, and mean temperature for each month over 2021 and 2022.
Oregon State University. (2024). Prism Climate Group: Northwest Alliance for Computational Science & Engineering. https://prism.oregonstate.edu/
Ecoregions
Level I Ecoregions are the 15 broad ecological classifications across North America (US EPA, 2015). These broad classifications allow for determining the intercontinental ecological patterns and are labeled as: Arctic Cordillera, Tundra, Taiga, Hudson Plains, Northern Forests, Northwestern Forested Mountains, Marine West Coast Forests, Eastern Temperate Forests, Great Plains, North American Deserts, Mediterranean California, Southern Semi-Arid Highlands, Temperate Sierras, Tropical Dry Forests and Tropical Wet Forests (US EPA, 2015). The Level I Ecoregions are easily distinguished from each other yet contain a high level of variability within them (Omernik & Griffith, 2014).
US EPA, O. (2015). Ecoregions of North America. https://www.epa.gov/eco-research/ecoregions-north-america Omernik, J. M. & Griffith, G. E. (2014). Ecoregions of the Conterminous United States: Evolution of a Hierarchical Spatial Framework. Environmental Management. DOI: 10.1007/s00267-014-0364-1
Ecoregions Level 1
An image of the Colorado River, the main river of the Lower Colorado River Basin.
- The Lower Colorado River Basin lies in the North American Desert classification of the Level I Ecoregions, which is characterized by its unique aridity, low-lying shrub, grass and cactus vegetation, lack of trees, and generally lower elevation compared to the surrounding ecoregions (Commission for Environmental Cooperation, 1997).
- According to the Commission for Environmental Cooperation (1997), North American Deserts' general physical characterizations are plains with hills, plains with mountains, and tablelands of high relief; the southern mountain ranges are smaller than the northern ones; wind and water erosion of sedimentary rock has left behind vast canyons, cliffs, buttes, and mesas; the soil is dry and lacks in organic matter and distinct soil profiles, and sand dunes are common (Commission for Environmental Cooperation, 1997).
- Concerning the climate zone of the Lower Colorado River Basin, which is a subtropical desert, the Level I Ecoregion designation closely resembles the climate zone with 130mm - 380mm (5.1in - 15in) of precipitation with extreme temperatures (Commission for Environmental Cooperation, 1997). This is in the character of the subtropical desert climates, which experience very high temperatures in the summer months with only 2-8 inches of precipitation annually.
- As for the biological factors of the area, most of the northern low-lying vegetation has been converted into agricultural areas, with a low presence of large mammals (the large mammals in the area include mule deer, pronghorn antelope, coyotes, bobcats, and badgers) (Commission for Environmental Cooperation, 1997).
Commission for Environmental Cooperation. (1997). Ecological Regions of North America Toward a Common Perspective. Communications and Public Outreach Department. http://www.cec.org/files/documents/publications/1701-ecological-regions-north-america-toward-common-perspective-en.pdf
Anthromes
Anthromes
An anthropogenic biome, or anthromes (also known as human biomes), as described by NASA's Socioeconomic Data and Applications Center (n.d.), are the terrestrial ecological regions in their human-altered form and are defined by consistent human interaction. There are 21 specific anthromes which are differentiated by population density, land use, and vegetation and are grouped into distinct six categories, which are dense settlements, villages, croplands, rangeland, forested, and wildlands (Socioeconomic Data and Applications Center, n.d.).
Socioeconomic Data and Applications Center. (n.d.). Anthropogenic Biomes. NASA. https://sedac.ciesin.columbia.edu/data/collection/anthromes
An image of an Arizona rangeland.
- Within the Lower Colorado River Basin, there are nine distinct anthromes, which, in order of most present to least, are:
- Remote Rangeland: Areas with livestock grazing, minimal crops and forests, and inconsequential human populations (Ellis and Ramankutty, 2008).
- Populated Rangeland: Areas with livestock grazing, minimal crops and forests, and minor human populations (Ellis and Ramankutty, 2008).
- Residential Rangeland: Areas with livestock grazing, minimal crops and forests, and substantial human populations (Ellis and Ramankutty, 2008).
- Populated Irrigated Cropland: Areas with annual crops mixed with other land uses and land covers that are irrigated with minor human populations (Ellis and Ramankutty, 2008).
- Residential Irrigated Cropland: Areas with annual crops mixed with other land uses and land covers that are irrigated with substantial human populations (Ellis and Ramankutty, 2008).
- Cropped and Pastoral Villages: Dense agricultural settlements with a mix of crops and pasture (Ellis and Ramankutty, 2008).
- Remote Cropland: Areas with annual crops mixed with other land uses and land covers with inconsequential human populations (Ellis and Ramankutty, 2008).
- Barren: Land without human populations or agriculture with no tree cover and are mostly deserts and frozen land (Ellis and Ramankutty, 2008).
- Urban: Dense settlements with a substantial urban area and densely built environments with very high human populations (Ellis and Ramankutty, 2008).
Erle C Ellis and Navin Ramankutty. (2008). Putting people in the map: anthropogenic biomes of the world. The Ecological Society of America. 10.1890/070062