Cerro De Coxóm

	Cerro De Coxóm Cerro de Coxóm is a stratovolcano in Totonicapán in western Guatemala. The volcano is located at the eastern edge of the valley of Quetzaltenango. See also * List of volcanoes in Guatemala This is a list of active, dormant, and extinct volcanoes in Guatemala. Volcanoes See also * Central America Volcanic Arc * List of volcanoes in El Salvador * List of volcanoes in Honduras * List of volcanoes in Mexico Footnotes ... References Mountains of Guatemala Stratovolcanoes of Guatemala {{Guatemala-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	Totonicapán Department Totonicapán is one of the 22 departments of Guatemala. The capital is the city of Totonicapán. History Historical chronicler Francisco Antonio de Fuentes y Guzmán, described the municipalities of Totonicapán in his 1689 “Recordación Florida.” This record confirms the area's pre-Columbian origins. In July, 1820, the indigenous residents of Totonicapán revolted against the government in response to excessive tributes imposed by the Spanish King Ferdinand VII. The Totonicapán Uprising of 1820 was led by Atanasio Tzul and Lucas Aguilar. After toppling the local government, Tzul declared himself king of the breakaway province, with Aguilar as president. The mayor of neighboring Quetzaltenango, Prudencio Cózar, along with hundreds of armed men, led an invasion to put down the rebellion. The rebel government lasted about 20 days. The rebels were captured, whipped, and imprisoned. The rebellion is widely celebrated in Guatemala as the opening volley in the independence s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	Guatemala Guatemala ( ; ), officially the Republic of Guatemala ( es, República de Guatemala, links=no), is a country in Central America. It is bordered to the north and west by Mexico; to the northeast by Belize and the Caribbean; to the east by Honduras; to the southeast by El Salvador and to the south by the Pacific Ocean. With an estimated population of around million, Guatemala is the most populous country in Central America and the 11th most populous country in the Americas. It is a representative democracy with its capital and largest city being Nueva Guatemala de la Asunción, also known as Guatemala City, the most populous city in Central America. The territory of modern Guatemala hosted the core of the Maya civilization, which extended across Mesoamerica. In the 16th century, most of this area was conquered by the Spanish and claimed as part of the viceroyalty of New Spain. Guatemala attained independence in 1821 from Spain and Mexico. In 1823, it became part of the Fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Stratovolcano A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Stratovolcano A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Quetzaltenango Quetzaltenango (, also known by its Maya name Xelajú or Xela ) is both the seat of the namesake Department and municipality, in Guatemala. The city is located in a mountain valley at an elevation of above sea level at its lowest part. It may reach above within the city. The Municipality of Quetzaltenango consists of an area of . Municipalities abutting the municipality of Quetzaltenango include Salcajá, Cantel, Almolonga, Zunil, El Palmar, Concepción Chiquirichapa, San Mateo, La Esperanza, and Olintepeque in Quetzaltenango department and San Andrés Xecul in Totonicapán department. History In Pre-Columbian times Quetzaltenango was a city of the Mam Maya people called Xelajú, although by the time of the Spanish Conquest it had become part of the K'iche' Kingdom of Q'umarkaj. The name may be derived from ''xe laju' noj'' meaning "under ten mountains". The city was said to have already been over 300 years old when the Spanish first arrived. With the help of his all ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	List Of Volcanoes In Guatemala This is a list of active, dormant, and extinct volcanoes in Guatemala. Volcanoes See also * Central America Volcanic Arc * List of volcanoes in El Salvador * List of volcanoes in Honduras * List of volcanoes in Mexico Footnotes References {{Central American volcanoes Guatemala List Volcanoes 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 a ... ... [...More Info...] [...Related Items...] OR:* [Wikipedia] [Google] [Baidu]
picture info	Mountains Of Guatemala 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]