Mapa topográfico Red Canyon

Younger igneous rocks form spectacular topographic features. The Henry Mountains, La Sal Range, and Abajo Mountains, ranges that dominate many views in southeastern Utah, are formed about igneous rocks that were intruded in the interval from 20 to 31 million years: some igneous intrusions in these mountains…

Altitud media: 1.512 m

Altitud media: 1.406 m

Altitud media: 1.851 m

Located within the Colorado Plateau, the monument has three distinct bridges in White and Armstrong Canyons. These canyons were formed when the Colorado River eroded the Permian Cedar Mesa Sandstone. The Sipapu, Kachina, and Owachoma bridges were formed through rock decay, weathering and erosion, as water cut…

Altitud media: 1.916 m

Altitud media: 1.424 m

Younger igneous rocks form spectacular topographic features. The Henry Mountains, La Sal Range, and Abajo Mountains, ranges that dominate many views in southeastern Utah, are formed about igneous rocks that were intruded in the interval from 20 to 31 million years: some igneous intrusions in these mountains…

Altitud media: 1.512 m

Altitud media: 1.424 m

Altitud media: 1.851 m

Altitud media: 1.806 m

Altitud media: 1.406 m

Altitud media: 2.024 m

Altitud media: 1.851 m

Younger igneous rocks form spectacular topographic features. The Henry Mountains, La Sal Range, and Abajo Mountains, ranges that dominate many views in southeastern Utah, are formed about igneous rocks that were intruded in the interval from 20 to 31 million years: some igneous intrusions in these mountains…

Altitud media: 1.512 m

Altitud media: 1.398 m

Altitud media: 1.627 m

Altitud media: 1.422 m

Altitud media: 1.424 m

Monticello is located at the base of the Abajo Mountains, or the Blue Mountains, which are part of the Manti-La Sal National Forest. The elevation of Monticello is 7,069 feet (2,155 m). From Monticello, a tree formation on the Blue Mountains can be seen, which resembles a horse's head and neck, which can be…

Altitud media: 2.145 m

Altitud media: 2.098 m