DELAWARE MOUNTAINS. The Delaware Mountains begin just south of Guadalupe Pass in northwestern Culberson County and stretch thirty-eight miles southeast (their center point is at 31°47' N, 104°47' W). The highest elevation in the Delawares is 5,632 feet above sea level. The mountains are characterized by long horizontal layers of sandstone, limestone, and shale, which were deposited in the sea at the edge of the Delaware Basin in Permian times, 250 million years ago. They and the Apache Mountains, to the south, are the uplifted eastern border of the salt flats in western Culberson County. The area's steep and rocky terrain is surfaced by shallow, stony soils that support live oak, piñon, juniper, and grasses. The mountains are named for the Delaware Indians.
Image Use Disclaimer
All copyrighted materials included within the Handbook of Texas Online are in accordance with Title 17 U.S.C. Section 107 related to Copyright and “Fair Use” for Non-Profit educational institutions, which permits the Texas State Historical Association (TSHA), to utilize copyrighted materials to further scholarship, education, and inform the public. The TSHA makes every effort to conform to the principles of fair use and to comply with copyright law.
For more information go to: http://www.law.cornell.edu/uscode/17/107.shtml
If you wish to use copyrighted material from this site for purposes of your own that go beyond fair use, you must obtain permission from the copyright owner.
The following, adapted from the Chicago Manual of Style, 15th edition, is the preferred citation for this article.Handbook of Texas Online, "Delaware Mountains," accessed July 25, 2016, http://www.tshaonline.org/handbook/online/articles/rjd08.
Uploaded on June 12, 2010. Published by the Texas State Historical Association.