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Exposed and buried parts of Capitan Reef. Blue area shows area once flooded by the Delaware Sea. The Delaware Basin is a geologic depositional and structural basin in West Texas and southern New Mexico, famous for holding large oil fields and for a fossilized reef exposed at the surface.
The map of North America with the Western Interior Seaway during the Campanian. The Western Interior Seaway (also called the Cretaceous Seaway, the Niobraran Sea, the North American Inland Sea, the Western Interior Sea and sometimes nicknamed "Hell's Aquarium") was a large inland sea that split the continent of North America into two landmasses for 34 million years.
The city's geographic center is at an elevation of 4,281 feet (1,305 m) above sea level. [15] U.S. Routes 60, 70, and 84 pass through the city. US 60 and 84 lead west 60 miles (97 km) to Fort Sumner, while US 70 leads southwest 19 miles (31 km) to Portales and 110 miles (180 km) to Roswell.
New Braunfels (/ ˈ b r ɔː n f ə l z / ⓘ BRAWN-fəlz) is a city in Comal and Guadalupe counties in the U.S. state of Texas. It is the seat of Comal County. The city covers 44.9 square miles (116 km 2 ) and had a population of 90,403 as of the 2020 Census . [ 7 ]
Canyon Lake (Texas) 1 Shore length is not a well-defined measure. Canyon Lake is a reservoir on the Guadalupe River in the Texas Hill Country in the United States. Canyon Lake is a U.S. Army Corps of Engineers reservoir formed on the Guadalupe River in Comal County by Canyon Dam, which is located about sixteen miles northwest of New Braunfels.
Geography of New Mexico. With a total area of 121,590 square miles (314,900 km 2), [1] New Mexico is the fifth-largest state, after Alaska, Texas, California, and Montana. Its eastern border lies along 103°W longitude with the state of Oklahoma, and 2.2 miles (3.5 kilometres) west of 103°W longitude with Texas (due to a 19th-century surveying ...
The geologic history of the state began with its assembly during the Yavapai and Mazatzal orogenies 1750 to 1650 million years ago (Mya). This was followed by 200 million years of tectonic quiescence that ended in the Picuris orogeny. This event transformed the New Mexico crust into mature continental crust.
El Malpais National Monument and National Conservation Area. El Malpais National Monument is a National Monument located in western New Mexico, in the Southwestern United States. [3] The name El Malpais is from the Spanish term Malpaís, meaning badlands, due to the extremely barren and dramatic volcanic field that covers much of the park's area.