HOME

TheInfoList



OR:

North Franklin Mountain (or North Franklin Peak) is a mountain in the Franklin Mountains of
El Paso, Texas El Paso (; "the pass") is a city in and the county seat, seat of El Paso County, Texas, El Paso County in the western corner of the U.S. state of Texas. The 2020 population of the city from the United States Census Bureau, U.S. Census Bureau w ...
, located in the Southwestern United States. North Franklin, at , is the highest point in El Paso, and the 27th-highest mountain in the state of Texas.Texas Highest Named Summits
/ref> Surrounded by a state park and with a maintained trail leading to its summit, the mountain is a popular hiking destination. North Franklin is located entirely within the city of El Paso, approximately east of the Texas–New Mexico border and north of the U.S.–Mexico border. The mountain is the highest of the Franklins, clipping nearby Anthony's Nose by just over and neighboring South Franklin by nearly . North Franklin rises above both its western base in the
Mesilla Valley The Mesilla Valley is a geographic feature of Southern New Mexico and far West Texas. It was formed by repeated heavy spring floods of the Rio Grande. Background The fertile Mesilla Valley extends from Radium Springs, New Mexico, to the west s ...
and its eastern base in the Hueco Bolson. In spite of its name, North Franklin is actually in the ''central'' Franklins, being the northernmost of the range's two key peaks (South Franklin, of course, is the other). To the south of these, the South Franklins include the peaks Mount Franklin and Ranger Peak (all of the television broadcast towers for El Paso are in the Southern Franklins). Like most of the Franklins, North Franklin Mountain is visible from many miles away. When observed from the east or west, North Franklin is shaped like a scalene triangle, with its long side facing its dome-shaped sister peak South Franklin Mountain. This quality makes it a valuable navigation point when traversing the desert areas around El Paso.


Geology

The Franklin Mountains are tilted-block fault mountains composed of sedimentary rocks, some of which date back to Precambrian times and are among the oldest in Texas. The mountains are the southernmost extent of the
Laramide orogeny The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 70 to 80 million years ago, and ended 35 to 55 million years ago. The exact duration and ages of beginning and end of the ...
, which occurred 60-70 million years ago. The Precambrian rocks atop North Franklin Mountain represent "the highest geological structure in the state of Texas." North Franklin gets its reddish color from the unusually high levels of oxidized iron in the volcanic rocks coating its summit and higher slopes.


History

For centuries, Native Americans and other travellers have used the vegetation and wildlife in the Franklins when crossing the Paso del Norte—the gap between the Franklin Mountains and the Juarez Mountains that is now the site of Ciudad Juárez and El Paso. Pictographs and mortar pits attest to a human presence in the mountains dating back more than 12,000 years. The Franklin Mountains are probably named after Benjamin Franklin Coons, who in 1849 purchased a ranch in what is now the El Paso area. Initially known as Coons Ranch, by 1851 the settlement had apparently taken Coons' middle name and was called "Franklin". Despite the town being officially named El Paso in 1852, the locals continued to call it Franklin throughout the 1850s. The El Paso Tin Mining and Smelting Company operated a tin mine on the northeast slope of North Franklin from 1909–1915. While the mine had the distinction of being the only tin mine ever located in the U.S., the venture was an economic failure. Today, a trail leading to the ruins of the mine forks off the North Franklin Peak Trail, just east of Mundy's Gap.Robert Miles,
Franklin Mountains
" ''The Handbook of Texas Online''. Retrieved: 1 April 2007.


Access

The trailhead is in the Tom Mays Unit (not the park headquarters in
McKelligon Canyon McKelligon Canyon is the location of a 1,503-seat amphitheater located in El Paso, Texas, United States, where the play '' Viva El Paso!'' is presented. The amphitheater is also used for concerts, graduation ceremonies, and other special events. Ad ...
) of the Franklin Mountains State Park near the summit of
Texas State Highway Loop 375 Loop 375 is a beltway that partially encircles the city of El Paso, Texas. The beltway is mostly a freeway, except for its northern section, which includes at-grade intersections. The highway passes through various areas of El Paso, funneling tr ...
. The Mundy's Gap Trail rises out of the Tom Mays section and winds to Mundy's Gap, on the north slope of North Franklin Mountain. From Mundy's Gap, the North Franklin Peak Trail follows the mountain's eastern slope for approximately three miles to the summit. Various spur trails branch off the main trail along the way. The summit of North Franklin has been flattened out, with an area equal to the size of a small parking lot. The only man-made structure at the summit is a
ham radio Amateur radio, also known as ham radio, is the use of the radio frequency spectrum for purposes of non-commercial exchange of messages, wireless experimentation, self-training, private recreation, radiosport, contesting, and emergency communica ...
repeater and ELT receiver maintained by the West Texas Repeater Association. On a typical day, the
Organ Mountains The Organ Mountains (also known as La Sierra de los Órganos) are a rugged mountain range in southern New Mexico in the Southwestern United States. Organ Mountains–Desert Peaks National Monument was declared a national monument on May 21, 2 ...
of New Mexico can be seen along the horizon to the north. To the east, the
Guadalupe Mountains The Guadalupe Mountains ( es, Sierra de Guadalupe) are a mountain range located in West Texas and southeastern New Mexico. The range includes the highest summit in Texas, Guadalupe Peak, , and the "signature peak" of West Texas, El Capitan, both ...
rise some in the distance. Most of the
Mesilla Valley The Mesilla Valley is a geographic feature of Southern New Mexico and far West Texas. It was formed by repeated heavy spring floods of the Rio Grande. Background The fertile Mesilla Valley extends from Radium Springs, New Mexico, to the west s ...
is visible to the west, including parts of El Paso and Ciudad Juárez, and most of the town of
Anthony Anthony or Antony is a masculine given name, derived from the '' Antonii'', a ''gens'' ( Roman family name) to which Mark Antony (''Marcus Antonius'') belonged. According to Plutarch, the Antonii gens were Heracleidae, being descendants of Anton, ...
. South Franklin Mountain and the Juarez Mountains are to the south. Anthony's Nose, the second highest peak, can be accessed from Tom Mays Unit by an unofficial trail originating from the C5 campsite (parking is at the same place as for the Aztec Cave trail). From the C5 campsite, the trail gradually winds uphill to the left, then goes directly up to the ridgeline across a narrow rocky pass. The trail then follows the ridgeline northward about 2 miles directly to Anthony's Nose. Although no technical gear is needed, there are a couple of difficult climbing areas along the way and the entire round trip takes about 10 hours. Once again, it is not an official trail, so it is not as well-maintained as other trails in the park.


References


External links


Franklin Mountains State Park, Tom Mays Unit, trail map


– Hosted by the University of Texas-El Paso
West Texas Repeater Association
– The WTRA maintains the repeater atop North Franklin {{Mountains of Texas Geography of El Paso, Texas Mountains of Texas Landforms of El Paso County, Texas