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Chicoma Mountain
Chicoma Mountain (; also spelled Tschicoma or Tchicoma) is the highest point in the Jemez Mountains, a prominent mountain range in the U.S. State of New Mexico. The tree line in this area is exceptionally high, and the mountain is forested almost all the way to its summit which is conspicuous from the towns of Los Alamos, Santa Fe, and Española and other areas in the valley of the Rio Grande in northern New Mexico. Like the rest of the Jemez, it is of volcanic origin; it lies on the northeast rim of the Valles Caldera, one of the best examples of a caldera in the United States. The mountain is sacred to many of the Puebloan peoples of New Mexico, who traditionally regarded it as the "center of all." Much of it lies within the territory of the Santa Clara Pueblo. Access by hikers, hunters, and others, is correspondingly limited, although the summit can be reached via public lands on the north side. The Puye Cliff Dwellings in Santa Clara Canyon are an archaeological site o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jemez Mountains
The Jemez Mountains are a group of mountains in Rio Arriba, Sandoval, and Los Alamos counties, New Mexico, United States. Numerous Puebloan Indian tribes have lived in the Jemez Mountains region since before the Spanish arrived in New Mexico. The Pueblo Indians of this region are the Towa-speaking Jemez people for which this mountain range is named, the Keres-speaking Keresan Indians, and the Tewa-speaking Tewa Indians. Tsąmpiye'ip'įn is the Tewa language name for the Jemez Mountains. The highest point in the range is Chicoma Mountain (also spelled as Tschicoma or Tchicoma) at an elevation of . The town of Los Alamos and the Los Alamos National Laboratory adjoin the eastern side of the range while the town of Jemez Springs is to the west. Pajarito Mountain Ski Area is the only ski area in the Jemez. New Mexico State Highway 4 is the primary road that provides vehicular access to locations in the Jemez Mountains. Geology The Jemez Mountains lie to the north of the Alb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Religious Places Of The Indigenous Peoples Of North America
Religion is usually defined as a social-cultural system of designated behaviors and practices, morals, beliefs, worldviews, texts, sanctified places, prophecies, ethics, or organizations, that generally relates humanity to supernatural, transcendental, and spiritual elements; however, there is no scholarly consensus over what precisely constitutes a religion. Different religions may or may not contain various elements ranging from the divine, sacred things, faith,Tillich, P. (1957) ''Dynamics of faith''. Harper Perennial; (p. 1). a supernatural being or supernatural beings or "some sort of ultimacy and transcendence that will provide norms and power for the rest of life". Religious practices may include rituals, sermons, commemoration or veneration (of deities or saints), sacrifices, festivals, feasts, trances, initiations, funerary services, matrimonial services, meditation, prayer, music, art, dance, public service, or other aspects of human culture. Religions have sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of New Mexico
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Santa Fe National Forest
The Santa Fe National Forest is a protected United States National Forest, national forest in northern New Mexico in the Southwestern United States. It was established in 1915 and covers . Elevations range from 5,300 feet (1600 m) to 13,103 feet (4000 m) at the summit of Truchas Peak, located within the Pecos Wilderness. The Jemez, Coyote, and Cuba districts are located in the Jemez Mountains; the Pecos/Las Vegas district is located in the Sangre de Cristo Mountains; and the Española district is located in both mountain ranges. In descending order of land area the forest lies in parts of Rio Arriba County, New Mexico, Rio Arriba, San Miguel County, New Mexico, San Miguel, Sandoval County, New Mexico, Sandoval, Santa Fe County, New Mexico, Santa Fe, Mora County, New Mexico, Mora, and Los Alamos County, New Mexico, Los Alamos counties. Forest headquarters are located in the city of Santa Fe, New Mexico, Santa Fe. Santa Fe National Forest was established on July 1, 1915 by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puye Cliff Dwellings
The Puye Cliff Dwellings are the ruins of an abandoned pueblo, located in Santa Clara Canyon on Santa Clara Pueblo land near Española, New Mexico. The site was declared a National Historic Landmark in 1966. Ancient pueblo dwellings Between 900 and 1580, up to 1500 Pueblo people lived in the area where they hunted game and cultivated food. Native peoples first settled in the area in the late 10th century of the Pueblo II Era, living in dispersed farmstead dwellings at the east side of the Jemez Mountains. Their settlements increased and changed over time in the Pueblo III Era, when they lived in larger, concentrated villages of Otowi, Puye, Shufinne, Tsankawi, Tsirege, and Tyuonyi.''Puye Cliff Dwellings History.'' Puye Cliffs. Retrieved 10-14-2011. The Puye Cliffs complex, the largest complex on the |
Santa Clara Pueblo
Santa Clara Pueblo (in Tewa: Khaʼpʼoe Ówîngeh ɑ̀ʔp’òː ʔówîŋgè ″Singing Water Village″, also known as ″Village of Wild Roses″ is a census-designated place (CDP) in Rio Arriba County, New Mexico, United States and a federally recognized tribe of Native American Pueblo people. The pueblo is a member of the Eight Northern Pueblos, and the people are from the Tewa ethnic group of Native Americans who speak the Rio Grande Tewa language. The pueblo is on the Rio Grande, between Ohkay Owingeh (formerly San Juan Pueblo) to the north and San Ildefonso Pueblo (P'ohwhóge Owingeh) to the south. Santa Clara Pueblo is famous for producing hand-crafted pottery, specifically blackware and redware with deep engravings. The pueblo is listed on the National Register of Historic Places. Geography Santa Clara Pueblo is located at (35.971124, -106.089111), approximately 1.5 miles south of Española on NM 30. According to the United States Census Bureau, the CDP has a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puebloan Peoples
The Puebloans or Pueblo peoples, are Native Americans in the Southwestern United States who share common agricultural, material, and religious practices. Currently 100 pueblos are actively inhabited, among which Taos, San Ildefonso, Acoma, Zuni, and Hopi are the best-known. Pueblo people speak languages from four different language families, and each Pueblo is further divided culturally by kinship systems and agricultural practices, although all cultivate varieties of maize. Pueblo peoples have lived in the American Southwest for millennia and descend from Ancestral Pueblo peoples. The term ''Anasazi'' is sometimes used to refer to ancestral Pueblo people but it is now largely minimized. ''Anasazi'' is a Navajo word that means ''Ancient Ones'' or ''Ancient Enemy'', hence Pueblo peoples' rejection of it (see exonym). ''Pueblo'' is a Spanish term for "village." When Spaniards entered the area, beginning in the 16th-century with the founding of Nuevo México, they came across ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valles Caldera
Valles Caldera (or Jemez Caldera) is a wide volcanic caldera in the Jemez Mountains of northern New Mexico. Hot springs, streams, fumaroles, natural gas seeps and volcanic domes dot the caldera floor landscape. The highest point in the caldera is Redondo Peak, an resurgent lava dome located entirely within the caldera. Also within the caldera are several grass valleys, or ''valles'', the largest of which is Valle Grande ( ), the only one accessible by a paved road. In 1975, Valles Caldera was designated as a National Natural Landmark by the National Park Service with much of the caldera being within the Valles Caldera National Preserve, a unit of the National Park System. History Use of Valles Caldera dates back to the prehistoric times: spear points dating to 11,000 years ago have been discovered.Anscheutz, Kurt F. and Merlan, Thomas (2007)"More than a scenic mountain landscape: Valles Caldera National Preserve land use history" U.S. Department of Agriculture Rocky Mountain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Arriba County, New Mexico
Rio Arriba County is a county in the U.S. state of New Mexico. As of the 2010 census, the population was 40,246. Its county seat is Tierra Amarilla. Its northern border is the Colorado state line. Rio Arriba County comprises the Española, NM Micropolitan Statistical Area, which is also included in the Albuquerque- Santa Fe-Las Vegas, NM Combined Statistical Area. History The county was one of nine originally created for the Territory of New Mexico in 1852. Originally extending west to the California line, it included the site of present-day Las Vegas, Nevada. The county seat was initially sited at San Pedro de Chamita, and shortly afterwards at Los Luceros. In 1860 the seat was moved to Plaza del Alcalde. Since 1880 Tierra Amarilla has been the county seat. The Battle of Embudo Pass took place in the southern part of the county during the Mexican–American War in January 1847. Geography According to the U.S. Census Bureau, the county has a total area of , of which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
