Bibliography: p. 60-65.
|Statement||by W. E. King [and others]|
|Series||WRRI report ;, no. 6|
|LC Classifications||GB705.N6 N64 no. 6, GB1025.N6 N64 no. 6|
|The Physical Object|
|Pagination||v, 141 p.|
|Number of Pages||141|
|LC Control Number||79635967|
Get this from a library! Hydrogeology of the Rio Grande Valley and adjacent intermontane areas of southern New Mexico,. [William Edward King;]. known facts about the hydrogeology of the Rio Grande valley and adjacent intermontane basins of Doña Ana County in southern New Mexico. Although the area is one of great importance to the present economy and growth potential of New Mexico, its hydro-geology has received but little attention during the last fifteen years. Southern Rio Grande Rift. The Southern segment – from Socorro, New Mexico to El Paso, Texas has undergone the most extension. This is suggested by the widening of the rift near Socorro into a north-trending series of parallel basins and ranges with a total width around times that of the single, large basins to the north. Their work led to “Hydrogeology of the Rio Grande Valley and adjacent intermontane areas in southern New Mexico” by William E. King, Hawley, and graduate students Andrew Taylor and Richard Wilson, published as WRRI Miscellaneous Report No. 6 in
Rio Grande gold gravels: Report on the newly discovered auriferous gravels of the Upper Rio Grande del Norte in the counties of Taos and Rio Arriba, New Mexico. Omaha, Nebraska: Henry Gibson. The binational western Hueco Bolson-Paso del Norte area of the southern Rio Grande rift (RGr) tectonic province occupies parts of Trans-Pecos Texas and south-central New Mexico, USA, and north-central Chihuahua, MX. It includes a long reach of the Rio Grande Valley, adjacent parts of the southern Mesilla and Tularosa Basins, and the El. The Rio Grande aquifer system is the principal aquifer in a 70,square-mile area of southern Colorado, central New Mexico, and western Texas (fig. 52). The aquifer system consists of a network of hydraulically interconnected aquifers in basin-fill deposits located along . valley fills, geomorphic history of the Rio Grande Valley and adjacent basins, ancient cienega deposits and Pleisto-cene vetebrate faunas in the Santa Fe Group, and Ouater-nary basalts of the La Mesa area. In addition to the above, a number of other studies in the border region should be mentioned. Investigations of three.
Buy Hydrogeology of the Rio Grande Valley and adjacent intermontane areas of southern New Mexico, (WRRI report) by William Edward King (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : William Edward King. The Rio Grande Valley is a transborder socio-cultural region located in a floodplain draining into the Rio Grande river near its mouth. The region includes the southernmost tip of South Texas and a portion of northern Tamaulipas, consists of the Brownsville, Harlingen, Weslaco, Pharr, McAllen, Edinburg, Mission, San Juan, and Rio Grande City metropolitan areas in the United States. Hydrogeology of the Rio Grande Valley and Adjacent Intermontane Areas of Southern New Mexico. New Mexico State University,June [Hydrogeology and Texas Geology] (21 . The Rio Grande is among the longest twenty-five rivers in the world and the fourth or fifth longest in North America. It starts near the Continental Divide in the San Juan Mountains, runs miles through New Mexico to the border of Texas and the Mexican province of Chihuahua, and empties into the Gulf of Mexico.