TheCarrizo Mountains (36°50' N, 109°7'W) is a small, mostly circular mountain range 15 to 20 km (9.3 to 12.4 mi) in diameter located on theColorado Plateau in northeasternArizona. The range is about 20 km (12 mi) southwest of theFour Corners. The highest summit, Pastora Peak, is 2,869 m (9,413 ft) in elevation, whereas elevations on the surrounding plateau are near 1,800 m (5,900 ft).
The mountains are within theNavajo Nation.Teec Nos Pos, Arizona, the closest community, is adjacent at the northern foothills, on Teec Nos Pos Wash, from Pastora Peak, about 5-mi miles to the north from the mountain's perimeter; Teec Nos Pos had about 800 inhabitants in the 2000 census.
The Carrizo Mountains primarily consist ofigneous rocks that intrudedPermian throughCretaceous marine strata. The most common igneous rock type isporphyritichornblendediorite. Intrusive forms includelaccoliths,stocks,sills, anddikes.Ages of the igneous rocks range from 70 to 74 million years.
Similar igneous-cored ranges of theColorado Plateau, including theHenry Mountains,Abajo Mountains andLa Sal Range, formed ca. 31 to 20 million years ago, making them distinctly younger than the late Cretaceous intrusions of the Carrizo Mountains. Radiometric ages of igneous intrusions inSleeping Ute Mountain are essentially identical to those of the diorite intrusions in the Carrizos. Both the Carrizo Mountains and Sleeping Ute Mountain are located along the southwest extension of theColorado Mineral Belt, a 250-mile long lineament characterized by igneous rocks associated with abundant ore deposits. Large ore deposits have not been found in the igneous rocks of the Carrizo Mountains, although small deposits ofuranium,vanadium,copper andsilver have been found in the sedimentary rocks of theMorrison Formation.
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