Search results
Results From The WOW.Com Content Network
Roughly along U.S. Route 85 between its junction with New Mexico State Road 90 and the El Paso city limits 32°12′58″N 106°57′31″W / 32.216111°N 106.958611°W / 32.216111; -106.958611 ( Elephant Butte Irrigation
The Enchantments is a region within the Alpine Lakes Wilderness area of Washington state's Cascade Mountain Range. [2] At an elevation of 4,500 feet (1,372 m), it is home to over 700 alpine lakes and ponds surrounded by the vast peaks of Cashmere Crags, which rate among the best rock-climbing sites in the western United States. [3]
The high point of the Rampart Range is Devils Head at an elevation of 9,748 feet (2,971 m). Several other peaks in the range are over 9,000 feet (2,743 m), but these elevations stand in contrast to the higher peaks of the Front Range to the north ( Mount Blue Sky ) and south ( Pikes Peak ).
After meeting the El Paso Ysleta Port of Entry, the highway curves northwest, following the Mexican border along the Rio Grande. Heading into downtown, the highway intersects US 54 at an interchange, passing unter the El Paso BOTA Port of Entry. The highway continues west into downtown, ending at US 62/US 85 Paisano Drive in downtown.
For premium support please call: 800-290-4726 more ways to reach us
Dating "Classic" Coso Style Sheep Petroglyphs in the Coso Range and El Paso Mountains: Implications for Regional Prehistory, v.2/15/04; C.Michael Hogan. 2008. Morro Creek, ed. by A. Burnham ; Allan, Stuart (2005). California Road and Recreation Atlas. Benchmark Maps. p. 94. ISBN 0-929591-80-1.
North Franklin is located entirely within the city of El Paso, approximately 10 miles (16 km) east of the Texas–New Mexico border and 15 miles (24 km) north of the U.S.–Mexico border. The mountain is the highest of the Franklins, clipping nearby Anthony's Nose by just over 200 feet (61 m) and neighboring South Franklin by nearly 300 feet ...
The Franklin Mountains of Texas (Spanish: Sierras de los Mansos [1]) are a small range 23 miles (37 km) long, 3 miles (5 km) wide that extend from El Paso, Texas, north into New Mexico. [2] The Franklins were formed due to crustal extension related to the Cenozoic Rio Grande rift .