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Artesonraju [3] [4] [5] [2] is a pyramidal mountain peak located near the city of Caraz in the Cordillera Blanca mountain range in the Peruvian Andes.It is located at the Peruvian province of Huaylas and its slopes are within two cities: Santa Cruz and Caraz.
The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about half a kilometer (0.3 miles). [6] The mountains are on the border between Pitkin County and Gunnison County, Colorado, United States, about 19 kilometres (12 mi) southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 4,317 metres ...
Mount Sneffels is the highest summit of the Sneffels Range in the Rocky Mountains of North America.The 14,153-foot (4313.93 m) fourteener is located in the Mount Sneffels Wilderness of Uncompahgre National Forest, 6.7 miles (10.8 km) west by south (bearing 256°) of the City of Ouray in Ouray County, Colorado, United States.
The line of mountains continues east of the plateau as the Qinling, which separates the Ordos Plateau from Sichuan. North of the mountains runs the Gansu or Hexi Corridor which was the main silk-road route from China proper to the West. The plateau is a high-altitude arid steppe interspersed with mountain ranges and large brackish lakes.
Images of the numbered Flatirons on Green Mountain are ubiquitous symbols of the city of Boulder. The area abounds with Flatirons photographs, drawings, paintings, and sculptures. The city government, the University of Colorado, and many businesses make use of this symbol in their logos, advertisements, and marketing materials.
The mountains are just northeast of Yellowstone National Park [1] and are part of the Greater Yellowstone Ecosystem. The mountains are traversed by road via the Beartooth Highway (U.S. 212) with the highest elevation at Beartooth Pass 10,947 ft (3,337 m)). The name of the mountain range has been attributed by the U.S. Forest Service to a rugged ...
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 .