The Raton Basin is a geologic structural basin in southern Colorado and northern New Mexico. It takes its name from Raton Pass and the town of Raton, New Mexico. In extent, the basin is approximately 50 miles east-west, and 90 miles north-south, in Huerfano and Las Animas Counties, Colorado, and Colfax County, New Mexico.

Topography

Although structurally a basin, the Raton Basin forms a topographic high dissected by eastward-flowing streams such as the Purgatoire River. The basin forms the foothills of the Rocky Mountains, immediately east of the Sangre de Cristo Range.

Geology

The sedimentary beds that form the basin are of Paleozoic, Mesozoic and Tertiary age. In the eastern part of the basin, the sedimentary section is capped by flows of basalt of Miocene age. The basin is highly asymmetrical, the beds dipping more steeply on the west side than the east.

The sedimentary rocks of the basin are extensively intruded by igneous plugs, dikes and sills of Eocene to Oligocene age. Two large granitic intrusives near the center of the basin form East Spanish Peak and West Spanish Peak. Dikes of felsic to intermediate composition radiate outward from East and West Spanish Peaks. Dikes of mafic and ultramafic composition trend east-northeast to west-southwest across the basin. Basaltic sills tend to intrude along the coal beds.

The site of the Raton Basin was a coastal plain at the end of Cretaceous and beginning of Tertiary time, and has a well-preserved sequence of rocks spanning the Cretaceous-Tertiary boundary. For this reason, the Raton Basin had been studied for evidence of the iridium anomaly thought to be evidence for a large meteor impact at the end of the Cretaceous that is in turn thought to have caused the Cretaceous–Tertiary extinction event. The boundary is represented in the basin by a 1-cm thick tonstein clay layer which has been found to contain anomalously high concentrations of iridium. The boundary clay layer is accessible to the public at Trinidad Lake State Park, among other places in the basin.

Natural Resources

Coal

Bituminous coal mines opened in the Raton Basin in 1873. Walsenburg, Colorado, Trinidad, Colorado and Raton, New Mexico became coal-mining towns. The coal deposits are in the Vermejo Formation (Cretaceous) and overlying Raton Formation (Cretaceous and Paleocene). Most of the mines were underground room-and-pillar, although in later years some mines in New Mexico used longwall mining. Some strip mining was done in New Mexico.

Much of the mining on the Colorado side of the basin supplied the steel mills at Pueblo, Colorado. Production through 1975 was 326 million short tons (295 million tonnes). There are currently no active coal mines in the basin, although the New Elk coal mine is being permitted to reopen.

Oil and gas

A number of wells have been drilled over the years seeking conventional oil and natural gas, but none has been produced in economic quantities in the basin. In April 2008, Pioneer Natural Resources announced that they were developing natural gas reserves in the Cretaceous Pierre Shale on their leasehold in the Raton Basin.

Coalbed methane

Coals in the Raton Basin were long known to be "gassy." During development of the Morely mine in the early part of the 20th century, two gas relief wells were drilled into the coal, as a safety measure to drain off gas ahead of mining.

The first wells seeking to produce coalbed methane were drilled in the Raton Basin in 1982. Thousands of wells have successfully extracted coalbed methane from the Vermejo Formation and Raton Formation coals. The productive coalbed methane area now covers the central part of the basin, and straddles the Colorado-New Mexico state line. The two major producing companies are Pioneer Natural Resources (on the Colorado side) and El Paso Corporation (on the New Mexico side).

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