Tooth of Time

The Tooth of Time is geological feature on the Philmont Scout Ranch located five miles (8.0 km) southwest of Cimarron, New Mexico, United States, and is one of Philmont's most popular sights. It is an igneous intrusion of dacite porphyry formed in the Paleogene Period of the Cenozoic Era some 22-40 million years ago.

Tooth of Time
Tooth of Time from the South
Highest point
Elevation9,003 ft (2,744 m) [1]
Prominence203 ft (62 m) [1]
Coordinates36°26′53″N 105°0′29″W [1]
Geography
Tooth of Time
Tooth of Time
Tooth of Time (the United States)
Parent rangeCimarron Range, Sangre de Cristo Mountains
Topo mapUSGS Tooth of Time
Climbing
Easiest routeScramble

Santa Fe Trail

The Tooth rises prominently from the valley floor, some 2,500 feet (760 m) below, creating a sheer vertical face unable to support substantial plant life. Both its pinkish-gray color and its unusual shape make it a particularly notable geological landmark. It was well known among the overland traders on the Santa Fe Trail, who used it to mark the final seven-day push to Santa Fe, New Mexico.

Geology

The Tooth was formed when magma from deep within the Earth rose through older rock layers and slowly cooled. Over many thousands of years, the older sedimentary rock eroded and left the harder igneous formation. The sedimentary rock acted as a mold for the intrusive magma, causing it to harden and cool where the sedimentary rock was strongest.

The Tooth sits atop a prominent ridge created through the process mentioned above. In the fourth episode of the TV mini-series western Lonesome Dove, the Tooth is readily visible as Pea Eye Parker, one of the protagonists, walks across the plain towards the cattle herd.

Climbing
Panoramic view from top of the Tooth of Time.

The Tooth of Time is located on the east end of Tooth of Time Ridge, while Shaefer's Peak is located on the west end of the ridge. A trail extends about 3.5 miles from Shaefer's Pass to the Tooth Ridge campsite, located at the base of the Tooth of Time, with a short scramble ascending the Tooth. Another trail, known as the Stockade Trail, extends along the steeper back side and terminates at an animal stockade along a road.[2] The first roped ascent of the main face was completed in July, 1972 by Lee Davis, Rick Barrett and Randy Wright.[3]

gollark: Huh, it says on Wikipedia (all hail Wikipedia) that the Earth is already 30% oxygen.
gollark: Not all of it. Probably not the mantle.
gollark: I'm trying to look up the composition of the Earth, because I figure a good way to remove the oxygen would be to react it with some readily available metal or whatever.
gollark: Use it directly, I mean.
gollark: Though I guess you just need to reduce it to 10% or so to stop humans from being able to use it.

See also

References
  1. Tooth of Time - Peakbagger.com
  2. Tooth of Time : Climbing, Hiking & Mountaineering : SummitPost
  3. Climbing Magazine, Sept/Oct 1972
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.