Cathedral Cliff facts for kids

Quick facts for kids Cathedral Cliff
Southeast aspect
Highest point
Elevation	5,810 ft (1,770 m)
Prominence	360 ft (110 m)
Isolation	1.16 mi (1.87 km)
Parent peak	Table Mesa ( 5,850 ft)
Geography
Cathedral Cliff Location in New Mexico Cathedral Cliff Location in the United States
Location	San Juan County, New Mexico, US
Parent range	Chuska Mountains Colorado Plateau
Topo map	USGS Table Mesa
Geology
Age of rock	Oligocene
Mountain type	Volcanic plug
Type of rock	Volcanic breccia

Cathedral Cliff is a 5,810-foot (1,770 meter) elevation volcanic plug located on Navajo Nation land in San Juan County of northwest New Mexico, United States. It is a prominent landmark set alongside U.S. Route 491, approximately 13 miles south of the community of Shiprock, New Mexico. Cathedral Cliff is one of the phreatomagmatic diatremes of the Four Corners area, and with significant relief as it rises 400 feet (122 meters) above the high-desert plain. It is situated about 9.5 miles (15.3 km) southeast of Shiprock, the most famous of these diatremes. Cathedral Cliff is set in the northeastern part of the Navajo Volcanic Field, a volcanic field that includes intrusions and flows of minette and other unusual igneous rocks which formed around 30 million years ago during the Oligocene. Its nearest higher neighbor is Table Mesa, one mile to the southwest, and Barber Peak is set 1.5 mile to the southeast.

Climate

According to the Köppen climate classification system, Cathedral Cliff is located in a semi-arid climate zone with cold winters and hot summers. Precipitation runoff from this feature drains into Dead Mans Wash, which is part of the San Juan River drainage basin.