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It is the most visually prominent peak in the range when viewed from the south, for example, from Albuquerque. From many other directions it is less prominent or not visible, due to its location in the center of the Valles Caldera, well away from the caldera's rim. Redondo Peak is an example of the volcanic feature known as a resurgent dome.
The highest point in the caldera is Redondo Peak, an 11,254-foot (3,430 m) resurgent lava dome located entirely within the caldera and surrounded by moat-like flows of rhyolitic solidified lavas. [5] Located within the caldera are several grass valleys , or valles , the largest of which is Valle Grande ( locally / ˈ v aɪ . eɪ ˈ ɡ r ɑː n ...
Redondo Peak, the second-highest summit in the range at 11,254 ft (3431 m), is a resurgent dome in the middle of the Valles Caldera, which also contains several smaller volcanos. In the Jemez Mountains, the Quaternary volcanic field, encompasses the Valles caldera and the connected Bandelier Tuff. [16]
The highest point in the county is the summit of Redondo Peak, at 11,254 feet (3,430 m). A relatively small portion of the county exists as a geographically separate exclave between Los Alamos County and Santa Fe County.
Like the rest of the Jemez, it is of volcanic origin; it lies on the northeast rim of the Valles Caldera, one of the best examples of a caldera in the United States. The mountain is sacred to many of the Puebloan peoples of New Mexico, who traditionally regarded it as the "center of all." Much of it lies within the territory of the Santa Clara ...
It has a maximum thickness of 1,050 m (3,440 ft). It overlies the Santa Fe, Keres, and Polvadera Groups to the east and south of the caldera and older rocks ranging in age from Paleoproterozoic to Permian to the west and north. It forms the upper surfaces of the Pajarito Plateau east of the caldera and the Jemez Plateau west of the caldera. [6]
Many geological features in Western United States have a Northeastern orientation, the North American craton motion has the same orientation as well. [1] For example: the Trans-Challis fault zone, Idaho; the Snake River in Oregon; the Garlock Fault, California; the Colorado River in Utah; the Colorado Mineral Belt; Crater Flat-Reveille Range-Lunar Crater lineament, the Northwestern Nevada ...
Peter D. Rowley; Charles G. Cunningham; John J. Anderson; Thomas A. Steven; Jeremiah B. Workman & Lawrence W. Snee (May 6, 2002), "Geology and Mineral Resources of the Marysvale Volcanic Field, Southwestern Utah" (PDF), in Lund, W.R. (ed.), Field Guide to Geologic Excursions in Southwestern Utah and Adjacent Areas of Arizona and Nevada, Geological Society of America 2002 Rocky Mountain Section ...