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Cuexcomate
Cuexcomate () is an inactive geyser in Puebla city, Puebla state, Mexico. The sinter cone that the geyser built up around its vent is tall and has a diameter of . A central crater within the cone is up to wide and deep (extending below ground level). Cuexcomate's name is derived from the Nahuatl term '' cuezcomatl'' "a large earthen jar used to store grain", because of its resemblance to such a vessel. Historically, it has been cited that the geyser was formed before the 1064 eruption of the Popocatépetl, an active volcano and the second highest peak in Mexico, which likely activated geothermal spring circulation that cut upward through Mesozoic limestone and deposited the geyser and the springs around it. The geyser's rock composition is 99% calcite, differing thus from typical silica sinter deposits. Cuexcomate has been mistakenly called 'the smallest volcano in the world' because of the popular belief that it was indeed a volcano, based only on the shape of the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cuexcomate Completo
Cuexcomate () is an inactive geyser in Puebla, Puebla, Puebla city, Puebla state, Mexico. The Geyserite, sinter cone that the geyser built up around its vent is tall and has a diameter of . A central crater within the cone is up to wide and deep (extending below ground level). Cuexcomate's name is derived from the Nahuatl language, Nahuatl term ''wiktionary:cuezcomatl, cuezcomatl'' "a large earthen jar used to store grain", because of its resemblance to such a vessel. Historically, it has been cited that the geyser was formed before the 1064 eruption of the Popocatépetl, an active volcano and the second highest mountain, peak in Mexico, which likely activated geothermal spring circulation that cut upward through Mesozoic limestone and deposited the geyser and the springs around it. The geyser's rock composition is 99% calcite, differing thus from typical Geyserite, silica sinter deposits. Cuexcomate has been mistakenly called 'the smallest volcano in the world' becaus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cuexcomate Cima
Cuexcomate () is an inactive geyser in Puebla city, Puebla state, Mexico. The sinter cone that the geyser built up around its vent is tall and has a diameter of . A central crater within the cone is up to wide and deep (extending below ground level). Cuexcomate's name is derived from the Nahuatl term '' cuezcomatl'' "a large earthen jar used to store grain", because of its resemblance to such a vessel. Historically, it has been cited that the geyser was formed before the 1064 eruption of the Popocatépetl, an active volcano and the second highest peak in Mexico, which likely activated geothermal spring circulation that cut upward through Mesozoic limestone and deposited the geyser and the springs around it. The geyser's rock composition is 99% calcite, differing thus from typical silica sinter deposits. Cuexcomate has been mistakenly called 'the smallest volcano in the world' because of the popular belief that it was indeed a volcano, based only on the shape of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puebla (city)
Puebla de Zaragoza (; nah, Cuetlaxcoapan), formally Heroica Puebla de Zaragoza, formerly Puebla de los Ángeles during colonial times, or known in English simply as Puebla, is the seat of Puebla Municipality. It is the capital and largest city of the state of Puebla, and the fourth largest city in Mexico, after Mexico City, Monterrey, and Guadalajara. A viceregal era planned city, it is located in the southern part of Central Mexico on the main route between Mexico City and Mexico's main Atlantic port, Veracruz—about east southeast of Mexico City and about west of Veracruz. The city was founded in 1531 in an area called Cuetlaxcoapan, which means "where serpents change their skin", between two of the main indigenous settlements at the time, Tlaxcala and Cholula. This valley was not populated in the 16th century, as in the pre-Hispanic period this area was primarily used for the "flower wars" between a number of populations. Due to its history and architectural styles rang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puebla, Puebla
Puebla de Zaragoza (; nah, Cuetlaxcoapan), formally Heroica Puebla de Zaragoza, formerly Puebla de los Ángeles during colonial times, or known in English simply as Puebla, is the seat of Puebla Municipality. It is the capital and largest city of the state of Puebla, and the fourth largest city in Mexico, after Mexico City, Monterrey, and Guadalajara. A viceregal era planned city, it is located in the southern part of Central Mexico on the main route between Mexico City and Mexico's main Atlantic port, Veracruz—about east southeast of Mexico City and about west of Veracruz. The city was founded in 1531 in an area called Cuetlaxcoapan, which means "where serpents change their skin", between two of the main indigenous settlements at the time, Tlaxcala and Cholula. This valley was not populated in the 16th century, as in the pre-Hispanic period this area was primarily used for the "flower wars" between a number of populations. Due to its history and architectural styles rang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Puebla
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cholula, Puebla
Cholula (), officially Cholula de Rivadavia, is a city and district located in the metropolitan area of Puebla, Mexico. Cholula is best known for its Great Pyramid, with the Iglesia de Nuestra Señora de los Remedios sanctuary on top, as well as its numerous churches. The city and district of Cholula are divided into two: San Pedro Cholula and San Andrés Cholula. Surrounding the city proper is a number of more rural communities which belong to the municipalities of San Andrés and San Pedro. The city itself is divided into eighteen neighborhoods or barrios, each with a patron saint. This division has pre-Hispanic origins as does the division into two municipalities. The city is unified by a complicated system of shared religious responsibilities, called ''cargas'', which function mostly to support a very busy calendar of saints' days and other festivals which occur in one part or another almost all year round. The most important of these festivals is that dedicated to the Vir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcite
Calcite is a Carbonate minerals, carbonate mineral and the most stable Polymorphism (materials science), polymorph of calcium carbonate (CaCO3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on the Mohs scale of mineral hardness, based on Scratch hardness, scratch hardness comparison. Large calcite crystals are used in optical equipment, and limestone composed mostly of calcite has numerous uses. Other polymorphs of calcium carbonate are the minerals aragonite and vaterite. Aragonite will change to calcite over timescales of days or less at temperatures exceeding 300 °C, and vaterite is even less stable. Etymology Calcite is derived from the German ''Calcit'', a term from the 19th century that came from the Latin word for Lime (material), lime, ''calx'' (genitive calcis) with the suffix "-ite" used to name minerals. It is thus etymologically related to chalk. When applied by archaeology, archaeologists and stone trade pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles, like the dinosaurs; an abundance of conifers and ferns; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest well-documented mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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