Coronado Cave
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Coronado Cave
Coronado Cave () is located in Cochise County in southern Arizona near the Mexican border. Walking in the cave is rather easy and the temperature is consistent. Some rooms require crawling in order to enter. The cave has both stalactites and stalagmites A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically .... The cave has been measured to be approximately 600 feet long, 70 feet wide and 20 feet tall with several passages and crawl ways. Access Visitors must stop at the visitor center and obtain a free cave permit. From the parking lot visitors can travel west on a well marked trail for 0.75 miles until reaching the cave. References {{Reflist Caves of Arizona Landforms of Cochise County, Arizona Limestone caves Wild caves ...
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Coronado Cave
Coronado Cave () is located in Cochise County in southern Arizona near the Mexican border. Walking in the cave is rather easy and the temperature is consistent. Some rooms require crawling in order to enter. The cave has both stalactites and stalagmites A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically .... The cave has been measured to be approximately 600 feet long, 70 feet wide and 20 feet tall with several passages and crawl ways. Access Visitors must stop at the visitor center and obtain a free cave permit. From the parking lot visitors can travel west on a well marked trail for 0.75 miles until reaching the cave. References {{Reflist Caves of Arizona Landforms of Cochise County, Arizona Limestone caves Wild caves ...
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Coronado Cave Entrance
Coronado may refer to: People * Coronado (surname) * Francisco Vázquez de Coronado (1510–1554), Spanish explorer often referred to simply as "Coronado" * Coronado Chávez (1807–1881), President of Honduras from 1845 to 1847 Places United States * Coronado Butte, a summit in the Grand Canyon, Arizona * Coronado, California, a city * Coronado Heights, Kansas, a hill with a public park * Coronado, Kansas, an unincorporated community * Coronado Cave, Arizona * Coronado Historic Site, New Mexico * Coronado National Forest, in Arizona and New Mexico Mexico * Coronado Municipality, Chihuahua, Mexico * Coronado Islands, island group in Tijuana municipality, Baja California, Mexico * Isla Coronado, an island and volcano in Ensenada municipality, Baja California, Mexico * Isla Coronados, Loreto Municipality, Baja California Sur, Mexico Elsewhere * Coronado, Alberta, Canada, a locality * Vázquez de Coronado (canton), commonly shortened to Coronado, a canton in Costa Rica * Coronado ...
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Cochise County, Arizona
Cochise County () is a county in the southeastern corner of the U.S. state of Arizona. It is named after the Native American chief Cochise. The population was 125,447 at the 2020 census. The county seat is Bisbee and the most populous city is Sierra Vista. Cochise County includes the Sierra Vista-Douglas, Arizona Metropolitan Statistical Area. The county borders southwestern New Mexico and the northwestern Mexican state of Sonora. History In 1528 Spanish Explorers: Álvar Núñez Cabeza de Vaca, Estevanico, and Fray Marcos de Niza survived a shipwreck off the Texas coast. Captured by Native Americans, they spent eight years finding their way back to Mexico City, via the San Pedro Valley. Their journals, maps, and stories led to the Cibola, seven cities of gold myth. The Expedition of Francisco Vásquez de Coronado in 1539 using it as his route north through what they called the Guachuca Mountains of Pima ( Tohono O'odham) lands and later part of the mission routes north, ...
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Stalactites
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" ...
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Stalagmites
A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). The corresponding formation hanging down from the ceiling of a cave is a stalactite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground", another is that, as with ants in the pants, the mites go up and the tights (tites) come down. Formation and type Limestone stalagmites The most common stalagmites are speleothems, which usually form in limestone caves. Stalagmite formation occurs only under certain pH conditions within the cavern. They form through deposition of calcium carbonate ...
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Caves Of Arizona
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ...
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Landforms Of Cochise County, Arizona
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 the fo ...
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Limestone Caves
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone co ...
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