Description | Kilbourne Hole is a maar volcanic crater, located 30 miles west of the Franklin mountains of El Paso, Texas, in the Potrillo Volcanic Field of Doña Ana County, New Mexico. The hole is a rare example of volcanic action without a mountainous rim. The theory of formation is that a volcanic eruption occurs in the presence of ground waters, beneath the surface of the earth. As the hot lava and magma encounter the waters, a huge bubble of steam is produced, which blows out a large crater; thus, it is not necessary for the lava and magma to build up a mountainous deposit. The crater is thought to be 80,000 years old. It is a very well known geologic site, especially because there are many mantle and crustal xenoliths sitting in loose sediment on the surface. This view shows the west rim of the hole. |