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Tusas Mountains information


Tusas Mountains
Brazos Cliffs and Valley, New Mexico
Highest point
Peak11,407 ft (3,477 m), Grouse Mesa[1]
Dimensions
Length67 mi (108 km) north-south
Width59 mi (95 km) east-west
Area2,709 sq mi (7,020 km2)
Geography
Tusas Mountains is located in New Mexico
Tusas Mountains
Tusas Mountains
CountryUnited States
StateNew Mexico
Range coordinates36°28′47″N 106°15′06″W / 36.47972°N 106.25167°W / 36.47972; -106.25167[2]

The Tusas Mountains are a mountain range in northern New Mexico, extending slightly into southern Colorado. They are considered the southeasternmost part of the San Juan Mountains.[1] Grouse Mesa, 11,407 feet (3,477 m),[3] is the highest peak in the range.[1] The mountains are located to the west of Taos and northwest of Santa Fe. The Tusas Mountains are a wide region of upland mesas and gently sloping mountains, dissected in places by deep canyons.[4]

  1. ^ a b c "Tusas Mountains". Peakbagger. Retrieved 2019-09-21.
  2. ^ "Tusas Mountains". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. 2011-12-13. Retrieved 2019-09-21.
  3. ^ "Grouse Mesa". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. 1980-11-13. Retrieved 2019-09-21.
  4. ^ Julyan 2006, p. 69–70.

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The Burned Mountain Formation is a geologic formation that crops out in the Tusas Mountains of northern New Mexico. It has a U-Pb radiometric age of 1700...

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Maquinita Granodiorite

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Granodiorite is a Precambrian pluton that crops out in the northern Tusas Mountains of New Mexico. It has a radiometric age of 1.755 billion years, corresponding...

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Rio Grande rift

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Luis, which is bounded by the San Juan and Tusas mountains on the west and the Sangre de Cristo Mountains in the east. The Albuquerque basin is the largest...

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Los Pinos Formation

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volcaniclastic, with interbedded tuffs and basalt flows. It crops out in the Tusas Mountains of New Mexico. The type section is located along Los Pinos Creek, near...

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Moppin Complex

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The Moppin Complex is a Precambrian geologic complex found in the Tusas Mountains of northern New Mexico. It has not been directly dated, but is thought...

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Big Rock Formation

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The Big Rock Formation is a formation that crops out in the Tusas Mountains of northern New Mexico. Detrital zircon geochronology gives a maximum age...

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Ortega Formation

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Mountains in his definition, assigning the schist to the Rinconada schist member, and including the feldspathic Petaca Schist in the Tusas Mountains....

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Geology of New Mexico

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terranes—sections of continental crust—that joined. Metavolcanic rocks in the Tusas Mountains may be among the oldest, which are intruded by 1.65 billion year old...

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Tres Piedras Orthogneiss

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Moppin Complex to the west in the Tusas Mountains. It may correlate with the San Miguel gneiss in the Nacimiento Mountains. The pluton is interpreted as possibly...

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Hondo Group

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about 2,200 meters (7,200 feet). The upper section is absent in the Tusas Mountains, where the Hondo Group is essentially synonymous with the Ortega Formation...

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Abiquiu Formation

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broad belt from the southwest flank of the Tusas Mountains to the Jarosa area in the northwest Jemez Mountains. The formation reaches a maximum thickness...

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Wild Rivers Recreation Area

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off of NM 522. It is located west of the Sangre de Cristo Mountains, east of the Tusas Mountains on the Taos Plateau volcanic field. The Rio Grande and Red...

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El Rito Formation

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out over a narrow belt from the southern Tusas Mountains to upper Coyote Creek. In the southern Tusas Mountains, it fills narrow paleovalleys eroded in...

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Cerro Pedernal

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Spanish for "flint hill". The mesa lies on the north flank of the Jemez Mountains, south of Abiquiu Lake, in the Coyote Ranger District of the Santa Fe...

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Vadito Group

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Burned Mountain Formation in the Tusas Mountains, and the upper Vadito Group is assigned to the Glenwoody Formation in the Picuris Mountains. The Burnt...

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Rinconada Formation

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inverted syncline in the northern Picuris Mountains. It is missing from the Hondo Group in the Tusas Mountains. Detrital zircon geochronology establishes...

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Glenwoody Formation

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Yavapai orogeny. It likely correlates with the Burned Mountain Formation in the Tusas Mountains. The formation has a characteristic manganese-rich zone...

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Latir volcanic field

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Latir field are found on the west side of the Rio Grande rift in the Tusas Mountains. The oldest rocks in the field have been dated to the Paleoproterozoic...

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Marquenas Formation

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Vadito Group, likely correlating with the Big Rock Formation of the Tusas Mountains. However, detrital zircon geochronology establishes a maximum age of...

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Uncompahgre Formation

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deformation along the Proterozoic Spring Creek shear zone of the northern Tusas Mountains, New Mexico" (PDF). New Mexico Geological Society Field Conference...

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