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Tooth Of Time
The Tooth of Time is a geological feature on the Philmont Scout Ranch located 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. 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. 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 ...
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Colfax County, New Mexico
Colfax County is a county in the U.S. state of New Mexico. As of the 2010 census, the population was 13,750. Its county seat is Raton. It is south from the Colorado state line. This county was named for Schuyler Colfax (18231885), seventeenth Vice President of the United States under U.S. President Ulysses S. Grant. Colfax County is the home of Philmont Scout Ranch and the NRA Whittington Center. History Colfax County was originally part of Taos County, one of the original nine counties created by the New Mexico Territory in 1852. In 1859, the eastern part of Taos County, including all of the territory of Colfax County, was split off to form Mora County. Colfax County was established on January 25, 1869, from the northern part of Mora County. The original county seat was the gold mining town of Elizabethtown. By 1872, when the gold rush in Elizabethtown had died down, the county seat was moved to Cimarron. Cimarron was on the stage coach route along the Mountain Branch ...
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Santa Fe Trail
The Santa Fe Trail was a 19th-century route through central North America that connected Franklin, Missouri, with Santa Fe, New Mexico. Pioneered in 1821 by William Becknell, who departed from the Boonslick region along the Missouri River, the trail served as a vital commercial highway until 1880, when the railroad arrived in Santa Fe. Santa Fe was near the end of El Camino Real de Tierra Adentro which carried trade from Mexico City. The trail was later incorporated into parts of the National Old Trails Road and U.S. Route 66. The route skirted the northern edge and crossed the north-western corner of Comancheria, the territory of the Comanche. Realizing the value, they demanded compensation for granting passage to the trail. American traders envisioned them as another market. Comanche raiding farther south in Mexico isolated New Mexico, making it more dependent on the American trade. They raided to gain a steady supply of horses to sell. By the 1840s, trail traffic through th ...
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Landforms Of Colfax County, New Mexico
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are ...
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Geography And Ecology Of Philmont Scout Ranch
Philmont Scout Ranch is located in the Sangre de Cristo Mountains of the Rocky Mountains of New Mexico. Philmont is about across (east to west) at its widest point, and about long (north to south). The southern part of the ranch is mostly grasslands/prairie, while the north is rocky and rugged, but a small part of the eastern area is prairie. Geography Philmont's lowest point is the southeast corner at and the highest point is the peak of Baldy Mountain, located on the ranch's northwest boundary, at . The average rainfall at Philmont ranges from around Base Camp to in the backcountry. There are nine major watersheds at Philmont - the Rayado River, Urraca Creek, Cimarroncito Creek, Sawmill Creek, the Cimarron (La Flecha) River, Turkey Creek, Dean Canyon, the Ponil River, and Ute Creek. Geological history The Tooth of Time, as well as Baldy Mountain, Betty's Bra, Lover's Leap, Cathedral Rock, Hogback Ridge, and many of the ridges in the northwest of the ranch, is an igneous ...
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Mount Phillips (New Mexico)
Mount Phillips, formerly called Clear Creek Mountain was renamed in 1960 in honor of the then living Waite Phillips, who donated the area to the Boy Scouts of America. It is located in Colfax County about south of Baldy Mountain in the Cimarron Range, a subrange of the Sangre de Cristo Mountains of New Mexico. Philmont Scout Ranch Mount Phillips is the second highest peak in Boy Scouts of America's Philmont Scout Ranch in the central country on the western perimeter. It is an easy hike from Comanche Peak, but it is a much steeper ascent from Clear Creek to its summit. There are four close trail camps in the area of the summit, but none have water. These are Mount Phillips, Comanche Peak, Thunder Ridge and Red Hills Camps, which, except for Red Hills Camp, are all dry. The staff camp of Clear Creek is the closest camp with water. Geology The mountain consists primarily of the metamorphic rock, pink gneiss,Mary Stuever and Daniel Shaw, ''Philmont Fieldguide'', Boy Scout ...
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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 rises abruptly, with of vertical relief (in 3 miles/4.8 km), from the Moreno Valley to the west and has a total elevation of . Philmont Scout Ranch Baldy Mountain lies on the northwestern border of the Boy Scouts of America's Philmont Scout Ranch. The valleys on the eastern side of the peak are home to some of the many small camps that are scattered throughout the Ranch. Four wheel drive roads and a radio tower exist high on the western slopes. In 1963 Norton Clapp bought around the mountain and donated it to the Boy Scouts of America. Mining Copper, gold, and silver were mined in the Baldy Mining District starting in 1866, and the top of Baldy Mountain was developed as the Mystic Lode copper mine. Other mines near Baldy Mountain we ...
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Stockade
A stockade is an enclosure of palisades and tall walls, made of logs placed side by side vertically, with the tops sharpened as a defensive wall. Etymology ''Stockade'' is derived from the French word ''estocade''. The French word was derived from the Spanish word ''estacada''. As a frontier outpost It was used as an outpost because it provided cover and was safe to look at things through. As a security fence The troops or settlers would build a stockade by clearing a space of woodland and using the trees whole or chopped in half, with one end sharpened on each. They would dig a narrow trench around the area, and stand the sharpened logs side-by-side inside it, encircling the perimeter. Sometimes they would add additional defence by placing sharpened sticks in a shallow secondary trench outside the stockade. In colder climates sometimes the stockade received a coating of clay or mud that would make the crude wall wind-proof. Builders could also place stones or thick mud la ...
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Philmont Scout Ranch Camps
Philmont Scout Ranch camps are a group of backpacking camps located in Philmont Scout Ranch, a large property in Colfax County, New Mexico, Colfax County near Cimarron, New Mexico, owned by the Boy Scouts of America and used as a backpacking reservation. Philmont operates from one large Philmont Scout Ranch camps#Base Camp, Base Camp which includes camping headquarters, the Philmont Training Center and Villa Philmonte, the Philmont Museum and Seton Memorial Library, Seton Museum, fire response facilities, cattle headquarters, and an administration area.
Official Philmont web site
As of 2022, there are 71 Philmont Scout Ranch camps#Trail camps, trail camps and 36 Philmont Scout Ranch camps#Staffed camps, staffed camps. Philmont's camps are generally set no more than a couple of miles apart. Old camps are closed or relocated and new camps are opened every ...
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Philmont Scout Ranch Tooth Of Time Panoramic View
Philmont Scout Ranch is a ranch located in Colfax County, New Mexico, near the village of Cimarron, New Mexico, Cimarron; it covers of wilderness in the Sangre de Cristo Mountains on the east side of the Cimarron_Range,_New_Mexico, Cimarron Range of the Rocky Mountains. Donated by oil baron Waite Phillips, the ranch is owned and operated by the Boy Scouts of America. It is a National High Adventure Base where crews of Scouts and Venturers take part in Backpacking (wilderness), backpacking treks and other outdoor education, outdoor activities. By land area, it is one of the largest youth camps in the world. During the 2019 season, between June 8 and August 22, an estimated 24,000 Scouts and adult leaders backpacked through the Ranch's extensive backcountry. That same year 1,302 staff were responsible for the Ranch's summer operations. Philmont is also home to the Philmont Training Center, the National Scouting Museum and the Seton Memorial Library. The Training Center is the pr ...
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Lonesome Dove (TV Miniseries)
''Lonesome Dove'' is a 1989 American epic film, epic Western (genre), Western adventure fiction, adventure television miniseries directed by Simon Wincer. It is a four-part film adaptation, adaptation of the 1985 Lonesome Dove, novel of the same name by Larry McMurtry and is the first installment in the Lonesome Dove series, ''Lonesome Dove'' series. The novel was based upon a screenplay by Peter Bogdanovich and McMurtry. The miniseries stars an ensemble cast headed by Robert Duvall as Augustus McCrae and Tommy Lee Jones as Woodrow Call. The series was originally broadcast by CBS from February 5 to 8, 1989, drawing a huge viewing audience, earning numerous awards, and reviving both the television Western and the miniseries. An estimated 26 million homes tuned in to watch ''Lonesome Dove'', unusually high numbers for a Western at that time. The Western genre was considered dead by most people, as was the miniseries. By the show's end, it had earned huge ratings and virtually revamp ...
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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 particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ...
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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 natural satellites. Besides molten rock, magma may also contain suspended crystals and gas bubbles. Magma is produced by melting of the mantle or the crust in various tectonic settings, which on Earth include subduction zones, continental rift zones, mid-ocean ridges and hotspots. Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush zones. During magma's storage in the crust, its composition may be modified by fractional crystallization, contamination with crustal melts, magma mixing, and degassing. Following its ascent through the crust, magma may feed a volcano and be extruded as lava, or it may solidify underground to form an intrusion, such as a ...
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