High Plains (United States)

Last updated

High Plains
Johnson 1920 HighPlains.jpg
A buffalo wallow on the High Plains. [1]
Contiguous US physiographic divisions.png
Physiographic regions of the United States. The High Plains region is the center yellow area designated 13d. [2]
Floor elevation1,800–7,000 ft (550–2,130 m) [3]
Length800 mi (1,300 km)
Width400 mi (640 km)
Area174,000 sq mi (450,000 km2) [3]
Geography
CountryUnited States
The High Plains ecology region is designated by 25 on this map. Level III ecoregions, United States.png
The High Plains ecology region is designated by 25 on this map.
Childress County, Texas, June 1938. Power farming displaces tenants, Childress County, Texas ppmsc00232u.jpg
Childress County, Texas, June 1938.

The High Plains are a subregion of the Great Plains, mainly in the Western United States, but also partly in the Midwest states of Nebraska, Kansas, and South Dakota, generally encompassing the western part of the Great Plains before the region reaches the Rocky Mountains. The High Plains are located in eastern Montana, southeastern Wyoming, southwestern South Dakota, western Nebraska, eastern Colorado, western Kansas, eastern New Mexico, the Oklahoma Panhandle, and the Texas Panhandle. [4] The southern region of the Western High Plains ecology region contains the geological formation known as Llano Estacado which can be seen from a short distance or on satellite maps. [5] From east to west, the High Plains rise in elevation from around 1,800 to 7,000 ft (550 to 2,130 m). [3]

Contents

Name

The term "Great Plains", for the region west of about the 96th or 98th meridian and east of the Rocky Mountains, was not generally used before the early 20th century. Nevin Fenneman's 1916 study, Physiographic Subdivision of the United States, [6] brought the term Great Plains into more widespread usage. Prior to 1916, the region was almost invariably called the High Plains, in contrast to the lower Prairie Plains of the Midwestern states. [7] Today the term "High Plains" is usually used for a subregion instead of the whole of the Great Plains.

Geography and climate

The High Plains has a "cold semi-arid" climateKöppen BSk—receiving between 10–20 in (250–510 mm) of precipitation annually.

Due to low moisture and high elevation, the High Plains commonly experiences wide ranges and extremes in temperature. The temperature range from day to night is usually 30 °F (~16.5 °C), and 24-hour temperature shifts of 100 °F (~55.5 °C) are possible, as evidenced by a weather event that occurred in Browning, Montana, from January 23–24, 1916, when the temperature fell from 44 to −56 °F (7 to −49 °C). This is the world record for the greatest temperature change in 24 hours. [8] The region is known for the steady, and sometimes intense, winds that prevail from the west. The winds add a considerable wind chill factor in the winter. The development of wind farms in the High Plains is one of the newest areas of economic development.

The High Plains are anomalously high in elevation. An explanation has recently been proposed to explain this high elevation. As the Farallon plate was subducted into the mantle beneath the region, water trapped in hydrous minerals in the descending slab was forced up into the lower crust above. Within the crust this water caused the hydration of dense garnet and other phases into lower density amphibole and mica minerals. The resulting increase in crustal volume raised the elevation about one mile. [9] [10]

Flora

Typical plant communities of the region are shortgrass prairie, prickly pear cacti and scrub. Sagebrush steppe is also present, particularly in high and dry areas closer to the Rocky Mountains.

Economy

Agriculture in the forms of cattle ranching and the growing of wheat, corn, and sunflowers is the primary economic activity in the region. The aridity of the region necessitates either dryland farming methods or irrigation; much water for irrigation is drawn from the underlying Ogallala Aquifer, which makes it possible to grow water-intensive crops such as corn, which the region's aridity would otherwise not support. [11] Some areas of the High Plains have significant petroleum and natural gas deposits.

The combination of oil, natural gas, and wind energy along with plentiful underground water, has allowed some areas (such as West Texas) to sustain a range of economic activity, including occasional industry. For example, the ASARCO refinery in Amarillo, Texas has been in operation since 1924 due to the plentiful and inexpensive natural gas and water that are needed in metal ore refining.[ citation needed ]

Demographics

The High Plains has one of the lowest population densities of any region in the continental United States; Wyoming, for example, has the second lowest population density in the country after Alaska. In contrast to the stagnant population growth in the northern and western High Plains, cities in west Texas have shown sustained growth; Amarillo and Lubbock both have populations near or above 200,000 and continue to grow.[ citation needed ] Smaller towns, on the other hand, often struggle to sustain their population.

Major cities and towns

See also

Related Research Articles

<span class="mw-page-title-main">Great Plains</span> Flat expanse in western North America

The Great Plains, sometimes simply "the Plains", is a broad expanse of flatland in North America. It is located just to the east of the Rocky Mountains, much of it covered in prairie, steppe, and grassland. It is the western part of the Interior Plains, which also include the mixed grass prairie, the tallgrass prairie between the Great Lakes and Appalachian Plateau, and the Taiga Plains and Boreal Plains ecozones in Northern Canada. Great Plains or Western Plains is also used to describe the ecoregion of the Great Plains, or alternatively the western portion of the Great Plains.

<span class="mw-page-title-main">Center-pivot irrigation</span> Method of crop irrigation

Center-pivot irrigation, also called water-wheel and circle irrigation, is a method of crop irrigation in which equipment rotates around a pivot and crops are watered with sprinklers. A circular area centered on the pivot is irrigated, often creating a circular pattern in crops when viewed from above. Most center pivots were initially water-powered, however today most are propelled by electric motors.

<span class="mw-page-title-main">Ogallala Aquifer</span> Water table aquifer beneath the Great Plains in the United States

The Ogallala Aquifer is a shallow water table aquifer surrounded by sand, silt, clay, and gravel located beneath the Great Plains in the United States. As one of the world's largest aquifers, it underlies an area of approximately 174,000 sq mi (450,000 km2) in portions of eight states. It was named in 1898 by geologist N. H. Darton from its type locality near the town of Ogallala, Nebraska. The aquifer is part of the High Plains Aquifer System, and resides in the Ogallala Formation, which is the principal geologic unit underlying 80% of the High Plains.

<span class="mw-page-title-main">Palo Duro Canyon</span> Texas panhandle escarpment

Palo Duro Canyon is a canyon system of the Caprock Escarpment located in the Texas Panhandle near the cities of Amarillo and Canyon. As the second-largest canyon in the United States, it is roughly 120 mi (190 km) long and has an average width of 6 mi (9.7 km), but reaches a width of 20 mi (32 km) at places. Its depth is around 800 ft (240 m), but in some locations, it increases to 1,000 ft (300 m). Palo Duro Canyon has been named "The Grand Canyon of Texas" both for its size and for its dramatic geological features, including the multicolored layers of rock and steep mesa walls, which are similar to those in the Grand Canyon. It is part of Palo Duro Canyon State Park. The State Park had 442,242 visitors in 2022.

<span class="mw-page-title-main">Texas Panhandle</span> Region in Texas, United States

The Texas Panhandle is a region of the U.S. state of Texas consisting of the northernmost 26 counties in the state. The panhandle is a square-shaped area bordered by New Mexico to the west and Oklahoma to the north and east. It is adjacent to the Oklahoma Panhandle, land which Texas previously claimed as its own before slavery was outlawed above the current border's latitude line. The Handbook of Texas defines the southern border of Swisher County as the southern boundary of the Texas Panhandle region.

<span class="mw-page-title-main">Interior Plains</span> Physiographic and geologic region of the United States and Canada

The Interior Plains is a vast physiographic region that spreads across the Laurentian craton of central North America, extending along the east flank of the Rocky Mountains from the Gulf Coast region to the Arctic Beaufort Sea. In Canada, it encompasses the Canadian Prairies separating the Canadian Rockies from the Canadian Shield, as well as the Boreal Plains and Taiga Plains east of the Mackenzie and Richardson Mountains; while in the United States, it includes the Great Plains of the West/Midwest and the tallgrass prairie region to the south of the Great Lakes extending east to the Appalachian Plateau region.

<span class="mw-page-title-main">Great American Desert</span> Historical term for the High Plains region of North America

The term Great American Desert was used in the 19th century to describe the part of North America east of the Rocky Mountains to approxomiately the 100th meridian. It can be traced to Stephen H. Long's 1820 scientific expedition which put the Great American Desert on the map.

<span class="mw-page-title-main">Llano Estacado</span> Southwestern United States in New Mexico and Texas

The Llano Estacado, sometimes translated into English as the Staked Plains, is a region in the Southwestern United States that encompasses parts of eastern New Mexico and northwestern Texas. One of the largest mesas or tablelands on the North American continent, the elevation rises from 3,000 feet (900 m) in the southeast to over 5,000 feet (1,500 m) in the northwest, sloping almost uniformly at about 10 feet per mile (2 m/km).

<span class="mw-page-title-main">West Texas</span> Region in Texas, United States

West Texas is a loosely defined region in the U.S. state of Texas, generally encompassing the arid and semiarid lands west of a line drawn between the cities of Wichita Falls, Abilene, and Del Rio.

<span class="mw-page-title-main">Arikaree River</span> River in the central United States

The Arikaree River is a 156-mile-long (251 km) river in the central Great Plains of North America. It lies mostly in the American state of Colorado, draining land between the North and South Forks of the Republican River, and it flows into the North Fork in Nebraska after flowing a short distance through Kansas. It is a designated area within the Colorado Natural Areas Program to protect native and uncommon species that may be endangered or threatened.

<span class="mw-page-title-main">Eastern New Mexico</span> Region in New Mexico, United States

Eastern New Mexico is a physiographic subregion within the U.S. state of New Mexico. The region is sometimes called the "High Plains," or "Eastern Plains ," and was historically referred to as part of the "Great American Desert". The region is largely coterminous with the portion of the Llano Estacado in New Mexico. Portions of Eastern New Mexico's elevation extends to over 4,000 ft (1,200 m). The region is characterized by flat, largely-featureless terrain with the exception of the Pecos River valley and the abrupt breaks along the Mescalero Ridge and northern caprock escarpments of the Llano Estacado. The region typically lacks the high relief of central and northern New Mexico, such as that in the Sangre de Cristo and Sandia mountain ranges. The climate is semi-arid with hot summers and is characterized by significant wind and dust storms in the springtime.

<span class="mw-page-title-main">Geography of Texas</span> Geographical features of Texas

The geography of Texas is diverse and large. Occupying about 7% of the total water and land area of the U.S., it is the second largest state after Alaska, and is the southernmost part of the Great Plains, which end in the south against the folded Sierra Madre Oriental of Mexico. Texas is in the South Central United States of America, and is considered to form part of the U.S. South and also part of the U.S. Southwest.

<span class="mw-page-title-main">Texas wine</span> Wine made from grapes grown in Texas, United States

Texas has a long history of wine production. The sunny and dry climate of the major winemaking regions in the state have drawn comparison to Portuguese wines, in addition to other regions in Europe like Spain, France, and Italy. Some of the earliest recorded Texas wines were produced by Spanish missionaries in the 1650s near El Paso. Texas ranked as the fifth largest wine producing state by 2019.

<span class="mw-page-title-main">Shortgrass prairie</span> Ecosystem located on the North American Great Plains

The shortgrass prairie is an ecosystem located in the Great Plains of North America. The two most dominant grasses in the shortgrass prairie are blue grama and buffalograss, the two less dominant grasses in the prairie are greasegrass and sideoats grama. The prairie was formerly maintained by grazing pressure of American bison, which is the keystone species. Due to its semiarid climate, the shortgrass prairie receives on average less precipitation than that of the tall and mixed grass prairies to the east.

<span class="mw-page-title-main">White River (Texas)</span> River in Texas, United States

The White River is an intermittent stream in the South Plains of Texas and a tributary of the Brazos River of the United States. It rises 8 miles (13 km) west of Floydada in southwestern Floyd County at the confluence of Callahan and Runningwater Draws. From there, it runs southeast for 62 miles (100 km) to its mouth on the Salt Fork of the Brazos River in northwestern Kent County. Besides these two headwaters, which rise near Hale Center and in Curry County, New Mexico, respectively, other tributaries include Pete, Crawfish, and Davidson Creeks. The White River drains an area of 1,690 sq mi (4,377 km2).

<span class="mw-page-title-main">Tierra Blanca Creek</span> River in the United States

Tierra Blanca Creek is an ephemeral stream about 75 mi (121 km) long, heading in Curry County, New Mexico, flowing east-northeast across northern portions of the Llano Estacado to join Palo Duro Creek to form the Prairie Dog Town Fork Red River southeast of Amarillo, Texas. Overall, Tierra Blanca Creek descends 1,050 ft (320 m) from its headwaters in Eastern New Mexico to its confluence with Palo Duro Creek at the head of Palo Duro Canyon.

<span class="mw-page-title-main">Yellow House Draw</span> River in the United States of America

Yellow House Draw is an ephemeral watercourse about 236 km (147 mi) long, heading about 20 km (12 mi) southwest of Melrose, New Mexico, and tending generally east-southeastward across the Llano Estacado to the city of Lubbock, where it joins Blackwater Draw to form Yellow House Canyon at the head of the North Fork Double Mountain Fork Brazos River. It stretches across Roosevelt, Curry, Bailey, Cochran, Hockley, and Lubbock Counties of eastern New Mexico and West Texas, and drains an area of 9,790 km2 (3,780 sq mi).

<span class="mw-page-title-main">Plant X</span> Power plant in Texas

Plant X is a steam-electric power plant located in the partially vegetated sandhills south of the West Texas town of Earth in Lamb County, Texas. It is owned and operated by Southwestern Public Service Company, a subsidiary of Xcel Energy.

<span class="mw-page-title-main">Ogallala Formation</span> Geologic formation in the western United States

The Ogallala Formation is a Miocene to early Pliocene geologic formation in the central High Plains of the western United States and the location of the Ogallala Aquifer. In Nebraska and South Dakota it is also classified as the Ogallala Group. Notably, it records the North American Land Mammal Ages (NALMAs) Hemphillian, Clarendonian, and Barstovian. It also includes an excellent record of grass seeds and other plant seeds, which can be used for biostratigraphic dating within the formation. The Ogallala Formation outcrops of Lake Meredith National Recreation Area preserve fish fossils. Similar specimens from the same unit are found at Alibates Flint Quarries National Monument in Texas.

The ecology of the Great Plains is diverse, largely owing to their great size. Differences in rainfall, elevation, and latitude create a variety of habitats including short grass, mixed grass, and tall-grass prairies, and riparian ecosystems.

References

  1. Darton, Nelson Horatio (1920). Syracuse-Lakin folio, Kansas. Folios of the Geologic Atlas, No. 212: United States Department of the Interior, U.S. Geological Survey. p. 17 (plate 2). Archived from the original on October 4, 2011. Retrieved October 6, 2010.{{cite book}}: CS1 maint: location (link)
  2. "Physiographic Regions". U.S. Department of the Interior. U.S. Geological Survey. Archived from the original on May 15, 2006. Retrieved October 6, 2010.
  3. 1 2 3 "USGS High Plains Aquifer WLMS". U.S. Department of the Interior. U.S. Geological Survey. Archived from the original on May 27, 2010. Retrieved October 6, 2010.
  4. File:Level III ecoregions, United States.png
  5. "Shaded relief image of the Llano Estacado". Handbook of Texas: Llano Estacado. June 15, 2010. Archived from the original on August 1, 2013. Retrieved August 6, 2013.
  6. Fenneman, Nevin M. (January 1917). "Physiographic Subdivision of the United States". Proceedings of the National Academy of Sciences of the United States of America . 3 (1): 17–22. Bibcode:1917PNAS....3...17F. doi: 10.1073/pnas.3.1.17 . OCLC   43473694. PMC   1091163 . PMID   16586678.
  7. Brown, Ralph Hall (1948). Historical Geography of the United States . New York: Harcourt, Brace & Co. pp.  373–374. OCLC   186331193.
  8. "Top Ten Montana Weather Events of the 20th Century". National Weather Service Unveils Montana's Top Ten Weather/Water/Climate Events of the 20th Century. National Weather Service. Archived from the original on March 13, 2013. Retrieved June 1, 2015.
  9. "Why Are the High Plains So High?". THECHERRYCREEKNEwsxWS.COM. March 15, 2005. Archived from the original on March 19, 2015. Retrieved March 15, 2015.
  10. Jones, Craig H.; Mahan, Kevin H.; Butcher, Lesley A.; Levandowski, William B.; Farmer, G. Lang (2015). "Continental uplift through crustal hydration". Geology . 43 (4): 355–358. Bibcode:2015Geo....43..355J. doi:10.1130/G36509.1.
  11. Scott, Michon. "National Climate Assessment: Great Plains' Ogallala Aquifer drying out". climate.gov. NOAA. Archived from the original on September 27, 2019. Retrieved September 27, 2019.