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Pueblo Peak is part of the Taos Mountains which are a subset of the Sangre de Cristo Mountains, and it ranks as the 27th-highest summit in New Mexico. [1] The mountain is located nine miles (14 km) northeast of the city of Taos and six miles southwest of Wheeler Peak, the highest point in the state.
A key trail into Taos was "The Old Taos Trail", which began at the Bent's Fort on the Arkansas River in Colorado, west of the Spanish Peaks, through Sangre de Cristo Pass (west of Walsenburg, Colorado), Old La Veta Pass and into Questa area (NM 522/NM38 area). [8] [9] It came into Taos at either Taos Pueblo road or half a mile west on Couse Hill.
Vallecito Mountain is part of the Taos Mountains which are a subset of the Sangre de Cristo Mountains and it ranks as the 14th-highest summit in New Mexico. [1] [4] The mountain is located 12 miles northeast of the town of Taos and three miles west-southwest of Wheeler Peak, the highest point in the state.
Ute Mountain (10, 093 ft) and the upper Rio Grande gorge. The Rio Grande del Norte National Monument is an approximately 242,555-acre (98,159 ha) area of public lands in Taos County, New Mexico, United States, proclaimed as a national monument on March 25, 2013, by President Barack Obama under the provisions of the Antiquities Act.
[1] [3] The mountain is located within the Carson National Forest, 18.5 miles north-northeast of the town of Taos and 6.5 miles north-northwest of Wheeler Peak, the highest point in the state. Precipitation runoff from the mountain drains to Red River and Rio Hondo which are tributaries the Rio Grande.
Venado Peak is one of the major peaks of the Taos Mountains group of the Sangre de Cristo Mountains, a subrange of the Rocky Mountains. It is located in Taos County, New Mexico, about 8 miles (13 km) northeast of the town of Questa. Its summit is the highest point in the Latir Peak Wilderness, part of Carson National Forest. [1]
A historical marker memorializing the trail, located on County Road 520 in Huerfano County, Colorado. The Taos Mountain Trail was the historic pathway for trade and business exchanges between agrarian Taos and the Great Plains from pre-history (1100 A.D.) through the Spanish Colonial period and into the time of the European and American presence.
Ute Mountain is a free-standing, dacitic, extinct Pliocene volcanic cone set within the Taos Plateau volcanic field. [8] Ute Mountain has a base diameter of five miles and topographic relief is significant as the summit rises 2,500 feet (760 meters) above the surrounding sagebrush-covered basalt plains. [ 2 ]