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The Tooth of Time is a geological feature on the
Philmont Scout Ranch Philmont Scout Ranch is a ranch located in Colfax County, New Mexico, near the village of Cimarron; it covers of wilderness in the Sangre de Cristo Mountains on the east side of the Cimarron Range of the Rocky Mountains. Donated by oil baro ...
located southwest of
Cimarron, New Mexico Cimarron is a village in Colfax County, New Mexico, United States, which sits on the eastern slopes of the Sangre de Cristo Mountains. The population was 1,021 at the 2010 census, making it the fourth most populous municipality in Colfax County. ...
, United States, and is one of Philmont's most popular sights. It is an
igneous Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma o ...
intrusion In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and com ...
of
dacite Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained ( aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhy ...
porphyry formed in the
Paleogene The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the beginning of ...
Period of the
Cenozoic The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configu ...
Era some 22-40 million years ago.


Santa Fe Trail

The Tooth rises prominently from the valley floor, some 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 Santa Fe ( ; , Spanish for 'Holy Faith'; tew, Oghá P'o'oge, Tewa for 'white shell water place'; tiw, Hulp'ó'ona, label= Northern Tiwa; nv, Yootó, Navajo for 'bead + water place') is the capital of the U.S. state of New Mexico. The name “S ...
.


Geology

The Tooth was formed when
magma Magma () is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natura ...
from deep within the Earth rose through older rock layers and slowly cooled. Over many thousands of years, the older
sedimentary rock Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particle ...
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

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.Tooth of Time : Climbing, Hiking & Mountaineering : SummitPost
/ref> The first roped ascent of the main face was completed in July, 1972 by Lee Davis, Rick Barrett and Randy Wright.Climbing Magazine, Sept/Oct 1972


See also

*
Baldy Mountain (Colfax County, New Mexico) Baldy Mountain (official name), Baldy Peak, Mount Baldy, or Old Baldy is the highest peak in the Cimarron Range, a subrange of the Sangre de Cristo Mountains of New Mexico. It is located in Colfax County, about northeast of Eagle Nest. It rise ...
* Mount Phillips (New Mexico) * Geography and ecology of Philmont Scout Ranch


References


External links


Satellite image of Tooth Ridge

Official website of Philmont Scout Ranch
{{DEFAULTSORT:Tooth Of Time Landforms of Colfax County, New Mexico
Cimarron, New Mexico Cimarron is a village in Colfax County, New Mexico, United States, which sits on the eastern slopes of the Sangre de Cristo Mountains. The population was 1,021 at the 2010 census, making it the fourth most populous municipality in Colfax County. ...
Rock formations of New Mexico Santa Fe Trail