Some regions in Texas are more associated with the American Southeast (primarily East Texas, Central Texas, and North Texas). The Panhandle is part of the Great Plains and is considered by many to have more in common with parts of the Midwest than either the South or Southwest. Geographically and culturally, El Paso is closer to New Mexico or Arizona than it is to Austin or to East Texas. The size of Texas prohibits easy categorization of the entire state wholly in any recognized region of the United States, and even cultural diversity among regions of the state makes it difficult to treat Texas as a region in its own right.
Physical geography
Texas covers a total area of 268,581 square miles (695,622 km2). The longest straight-line distance is from the northwest corner of the panhandle to the Rio Grande river just below Brownsville, 801 miles (1,289 km).[1] The greatest east–west distance is 773 miles (1,244 km) from the extreme eastward bend in the Sabine River in Newton County to the extreme western bulge of the Rio Grande just above El Paso.[4] The largest continental state is so expansive that El Paso, in the western corner of the state, is closer to San Diego, California, than to the Houston/Beaumont area, near the Louisiana state line; while Orange, on the border with Louisiana, is closer to Jacksonville, Florida, than it is to El Paso. Texarkana, in the northeastern corner of the state, is about the same distance from Chicago, Illinois, as it is from El Paso, and Dalhart, in the northwestern corner of the state, is closer to the state capitals of Kansas, Nebraska, Colorado, New Mexico, Oklahoma and Wyoming than it is to Austin, its own state capital.[5]
The geographic center of Texas is about 15 miles (24 km) northeast of Brady in northern McCulloch County. Guadalupe Peak, at 8,749 feet (2,666.7 m) above sea level, is the highest point in Texas, the lowest being sea level where Texas meets the Gulf of Mexico.[6] Texas has five state forests and 120 state parks totalling over 605,000 acres (2,450 km2).[7] There are 3,700 named streams and 15 major river systems flowing through 191,000 miles (307,000 km) of Texas, supporting over 212 reservoirs.[8]
With 10 climatic regions, 14 soil regions, and 11 distinct ecological regions, regional classification becomes problematic with differences in soils, topography, geology, rainfall, and plant and animal communities.[9]
Coast and estuaries
Much of the 367-mile (591 km) Gulf coastline of Texas is paralleled by the Texas barrier islands, many of which enclose a series of estuaries where the state's rivers mix with water from the Gulf of Mexico. These water bodies include some of the largest and most ecologically productive coastal estuaries in the United States and contribute significantly to the ecological and economic resources of Texas.[10]
The North Central Plains are bounded by the Caprock Escarpment to the west, the Edwards Plateau to the south, and the Eastern Cross Timbers to the east. This area includes the North Central Plains around the cities of Abilene and Wichita Falls, the Western Cross Timbers to the west of Fort Worth, the Grand Prairie, and the Eastern Cross Timbers to the east of Dallas. With about 35 to 50 inches (890 to 1,270 mm) annual rainfall, gently rolling to hilly forested land is part of a larger pine-hardwood forest of oaks, hickories, elm and gum trees.[11] Soils vary from coarse sands to tight clays or shet rock clays and shales.[13]
Texas's blackland prairies were some of the first areas farmed in Texas. Highly expansive clays with characteristic dark coloration, called the Houston Black series, occur on about 1.5 million acres (6,000 km2) extending from north of Dallas south to San Antonio. The Professional Soil Scientists Association of Texas has recommended to the State Legislature that the Houston Black series be designated the State soil. The series was established in 1902.[14] National Parks in this area are the Lyndon B. Johnson National Historical Park and the San Antonio Missions National Historical Park.[12]
Mountains and basins
The Trans-Pecos Natural Region has less than 12 inches (300 mm) annual rainfall. The most complex Natural Region, it includes Sand Hills, the Stockton Plateau, desert valleys, wooded mountain slopes and desert grasslands. The Basin and Range Province is in West Texas, west of the Pecos River, beginning with the Davis Mountains on the east and the Rio Grande to its west and south. The Trans-Pecos region is the only part of Texas regarded as mountainous and includes seven named peaks in elevation greater than 8,000 feet (2,400 m). This region includes sand hills, desert valleys, wooded mountain slopes and desert grasslands.[11]
Continental, Mountain, and Modified Marine are the three major climatic types of Texas, with no distinguishable boundaries. Modified Marine, or subtropical, dominates the majority of the state.[16] Texas has an annual precipitation range from 60.57 inches (1,538 mm) in Jasper County, East Texas, to 9.43 inches (240 mm) in El Paso. The record high of 120 °F (49 °C) was reached at Seymour on 12 August 1936, and Monahans on 28 June 1994. The low also ties at −23 °F (−31 °C) in Tulia on 12 February 1899, and Seminole on 8 February 1933.[17]
With a large supply of natural resources, Texas is a major agricultural and industrial state, producing oil, cattle, sheep, and cotton. The state also produces poultry, eggs, dairy products, greenhouse and nursery products, wheat, hay, rice, sugar cane, and peanuts, and a range of fruits and vegetables.[18]
Cement is produced in Bexar, Comal, Dallas, Ector, Ellis, El Paso, Harris, Hays, McLennan, Nolan, Nueces, Potter, and Tarrant counties. Historically, Texas' Portland cement output accounts for about 10% of the annual United States production.[citation needed]
With an abundance of various types of clays, Texas is one of the leading producers of clays.
Bituminous coal occurs primarily in Coleman, Eastland, Erath, Jack, McCulloch, Montague, Palo Pinto, Parker, Throckmorton, Wise, and Young counties of Texas. Lignite, or brown coal, occurs in deposits in the Texas Coastal Plain.
Fluorspar or fluorite is an important industrial mineral used in the manufacture of steel, aluminum, glass, and fluorocarbons. It occurs at several localities in the Trans-Pecos and Llano regions of Texas.
Deposits of graphite occur in the Llano region and was previously produced in Burnet County.
Bat guano occurs in numerous caverns in the Edwards Plateau and in the Trans-Pecos region and to a more limited extent in Central Texas.
Gypsum is extensively developed in Texas where the main occurrences are in the Permian Basin, the Cretaceous Edwards Formation in Gillespie and Menard counties, and the Gulf Coast salt domes of Harris County and previously Brooks County.
Texas is the leading producer of helium solely from the Cliffside gas field near Amarillo.
Deposits of iron ore are present in northeastern Texas as well as several in Central Texas.
Elements of the Lanthanide series are commonly termed rare-earth elements. Several of the rare earths have anomalous concentrations in the rhyolitic and related igneous rocks in the Trans-Pecos area of Texas. A deposit containing several rare-earth minerals was exposed at Barringer Hill in Llano County before it was covered by the waters of Lake Buchanan.
Limestones, abundant in many parts of Texas, are used in the manufacture of lime. Plants for the production of lime are operating in Bexar, Bosque, Burnet, Comal, Deaf Smith, Hill, Johnson, Nueces, and Travis counties.
Salts occurs in large quantities in salt domes in the Texas Coastal Plain and with other evaporites in the Permian Basin of West Texas, as well as near Grand Saline, Texas.
Sands used for industrial purposes commonly have been found in the Texas Coastal Plains, East Texas, north central Texas, and Central Texas; and sand mines have opened in the Shinnery (dunes) ecosystem of northern West Texas and the eastern part of the West Wingtip.
The discovery of silver in Texas has been credited by some to Franciscans who discovered and operated mines near El Paso about 1680. Documented silver production started in the late 1880s at the Presidio Mine, in Presidio County. Texas produced 32,663,405 troy ounces of silver between 1885 and 1955.
Sulfur occurs in the caprocks of salt domes in the Gulf Coastal Plain, in Permian-age bedded deposits in Trans-Pecos Texas.
In the past, uranium was produced from surface mines in Atascosa, Gonzales, Karnes, and Live Oak counties. All uranium mines are closed and Texas is no longer a producer.[19]
The Barnett Shale, located in the Fort Worth basin, has gained attention in recent years as a source of natural gas. Controversy regarding drilling and exploration rights is an issue.
Regions
There are several different methods used to describe the geographic and geological differences within the state, and there are often subdivisions within a region which more accurately describe both the terrain and the culture.[20] Because there is no single standard for subdividing the regions of Texas, many accepted areas either overlap or seem to contradict others. All are included for completeness.
Gulf Coast, also known as Texas Gulf Coast, which can refer to either an economic region defined by the Texas Comptroller or a geographical region encompassing all of Texas's coastline on the Gulf of Mexico.
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