|
Sierra De Chuacús
The Sierra de Chuacús is situated in the Guatemalan highlands, central highlands of Guatemala, and runs southeast from El Quiché to Baja Verapaz. Its northwestern border is marked by the Chixoy River basin in Uspantán, which separates it from the Sierra de los Cuchumatanes. Its eastern border is marked by the Salamá River which separates it from the Sierra de las Minas. Its southeastern border is defined by the Motagua River valley. The main crest of the Sierra the Chuacús is located along the El Quiché and Baja Verapáz border, and extends at an elevation above 2,100 m for more than 50 km. Its highest peak reaches up to 2504 m. Located between the Motagua Fault and the Chixoy-Polochic Fault, the Chuacús mountains were formed by complex tectonic and geological processes that started in the Late Cretaceous. References See also *Geography of Guatemala *Guatemalan highlands Mountain ranges of Guatemala, Chuacus {{Guatemala-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
El Quiché
EL, El or el may refer to: Arts and entertainment Fictional entities * El, a character from the manga series ''Shugo Chara!'' by Peach-Pit * Eleven (''Stranger Things'') (El), a fictional character in the TV series ''Stranger Things'' * El, family name of Kal-El (Superman) and his father Jor-El in the Superman dynasty * E.L. Faldt, character in the road comedy film '' Road Trip'' Music * Él Records, an independent record label from the UK founded by Mike Alway * ''Él ''(Lucerito album), a 1982 album by Lucerito * "Él", Spanish song by Rubén Blades from the album '' Caminando'' * "Él" (Lucía song), the Spanish entry performed by Lucía in the Eurovision Song Contest 1982 Other media * ''Él'', 1926 autobiographical novel by Mercedes Pinto * ''Él'' (film), a 1953 film by Luis Buñuel based on the 1926 novel * ''Él'' (visual novel), a 1991 Japanese adult visual novel * EL TV, an Azerbaijani regional television channel Companies and organizations * Estée Lauder Co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baja Verapaz
Baja Verapaz () is a department in Guatemala. In 2018, the population of the department was 299,476. The capital is Salamá. 78.5% of the department’s population identifies as Maya, with 53% belonging to the Achi linguistic group. Baja Verapaz contains the Mario Dary Biotope Preserve, preserving the native flora and fauna of the region, especially the endangered national bird of Guatemala, the Resplendent Quetzal. Municipalities *Cubulco * Granados *Purulhá *Rabinal *Salamá * San Jerónimo *San Miguel Chicaj *Santa Cruz El Chol Santa Cruz El Chol () is a municipality in the Baja Verapaz department of Guatemala. It is situated at 1008 m above sea level and contains about 8817 people. It covers a terrain of 140 km² and its annual festival is held from December 6-Dec ... References External linksBaja Verapaz Website Departments of Guatemala {{Guatemala-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guatemalan Highlands
The Guatemalan Highlands is an upland region in southern Guatemala which lies between the Sierra Madre de Chiapas to the south and the Petén lowlands to the north. Geographic description The Highlands lie between 6360 ft and 13780 ft and are made up of a series of high valleys enclosed by mountains. There are volcanoes which are both active and extinct. The local name for the region is ''Altos,'' meaning "highlands." The relief of the mountainous country which is north of the Highlands and drains into the Atlantic is varied by terraces, ridges, and underfalls. Its general configuration is compared by E. Reclus to the appearance of "a stormy sea breaking into parallel billows".''Universal Geography'', ed. E. G. Ravenstein, div. xxxiii., p. 212 A range called the Sierra de Chamá travels eastward towards Belize and is connected by low hills with the Cockscomb Mountains. The Sierra de Santa Cruz, a similar range, continues east to Cape Cocoli between the Polochic and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guatemala
Guatemala, officially the Republic of Guatemala, is a country in Central America. It is bordered to the north and west by Mexico, to the northeast by Belize, to the east by Honduras, and to the southeast by El Salvador. It is hydrologically bordered to the south by the Pacific Ocean and to the northeast by the Gulf of Honduras. The territory of modern Guatemala hosted the core of the Maya civilization, which extended across Mesoamerica; in the 16th century, most of this was Spanish conquest of Guatemala, conquered by the Spanish and claimed as part of the viceroyalty of New Spain. Guatemala attained independence from Spain and Mexico in 1821. From 1823 to 1841, it was part of the Federal Republic of Central America. For the latter half of the 19th century, Guatemala suffered instability and civil strife. From the early 20th century, it was ruled by a series of dictators backed by the United States. In 1944, authoritarian leader Jorge Ubico was overthrown by a pro-democratic m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chixoy River
The Chixoy River or Río Chixoy is a river in Guatemala. The river is called Río Negro from its sources in the highlands of Huehuetenango and El Quiché until it reaches the Chixoy hydroelectric dam (located at ), where the Río Salamá and Rio Carchela converge with the Río Negro. After the Chixoy dam, the river is called Río Chixoy and flows northwards, marking the departmental limits between Alta Verapaz and El Quiché, until it reaches the border with Mexico. It continues along the border for another as the Salinas river until it finally converges with the Río la Pasión (at ) to form the Usumacinta river which flows into the Gulf of Mexico The Gulf of Mexico () is an oceanic basin and a marginal sea of the Atlantic Ocean, mostly surrounded by the North American continent. It is bounded on the northeast, north, and northwest by the Gulf Coast of the United States; on the southw .... The Chixoy river's water discharge of is Guatemala's highest. This was one o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra De Los Cuchumatanes
The Sierra de los Cuchumatanes, in western Guatemala, is the highest non-volcanic mountain range in Central America. Etymology The name "Cuchumatán" is derived from the Mam words ''cuchuj'' (to join or unite) and ''matán'' (with superior force) and means "that which was brought together by superior force". Cuchumatán may also be a derivation of the Nahuatl word ''kochmatlán'', which means "place of the parrot hunters". Geography The mountains' elevations range from to over , and the range covers an area of .Lovell 2005:11 With an area of lying above , it is also the most extensive highland region in Central America. The Sierra lies in western Guatemala in the departments of Huehuetenango and El Quiché. Its western and south-western borders are marked by the Seleguá River, which separates it from the Sierra Madre volcanic chain. Its southern border is defined by the Río Negro, which flows into the Chixoy River, which turns northwards and separates the Cuchumatanes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salamá River
The Salamá River is a river in Guatemala. It is a tributary of the Chixoy River. The river is fed by a number of streams running down the slopes of the Sierra de las Minas and Sierra de Chuacús and flows in a north-westerly direction through the town of Salamá until it joins the Chixoy River. References External links Map of Guatemala including the river Rivers of Guatemala Usumacinta River {{Guatemala-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra De Las Minas
Sierra de las Minas is a mountain range in eastern Guatemala which extends 130 km west of the Lake Izabal. It is 15–30 km wide and bordered by the valleys of the Polochic River in the north and the Motagua River in the south. Its western border is marked by the Salamá River valley which separates it from the Chuacús mountain range. The highest peak is Cerro Raxón at 3,015 m. The Sierras (Chuacús) rich deposits of jade and marble have been mined for centuries. The small scale mining activities explain the name of the mountain range. The range has several different habitats, including Mesoamerica's largest cloud forests and is home to a great variety of wildlife. A large part of the Sierra de las Minas was declared a biosphere reserve in 1990. Biosphere reserve In 1990, a substantial part of the Sierra de las Minas (, including the buffer zones and transition areas) was designated a biosphere reserve. Habitats and land cover types Due to its size and great va ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Motagua River
The Motagua River () is a river in Guatemala. It rises in the Western Highlands of Guatemala and runs in an easterly direction to the Gulf of Honduras. The Motagua River basin covers an area of and is the largest in Guatemala. The Motagua River valley contains sources of jadeitite, which has been used by many Indigenous communities that have inhabited the region. The Motagua River is also one of the most plastic-emitting rivers in the world, contributing around two percent of global plastic pollution emissions into oceans annually. Conservation efforts have been driven by the government and non-governmental organizations to ensure safe water and clean oceans. Course The river begins in the Western Highlands of Guatemala and runs along the Atlantic slope. Traveling in an easterly direction, it passes through 14 of Guatemala's departments and contains seven distinct ecoregions. Along its course, water flows in from 29 other major rivers. The final few kilometres of the riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Motagua Fault
The Motagua Fault (also, Motagua Fault Zone) is a major, active fault, active left lateral-moving transform fault which cuts across Guatemala. It forms part of the tectonic boundary between the North American plate and the Caribbean plate. It is considered the onshore continuation of the Swan Islands Transform Fault and Cayman Trough, Cayman trench, which run under the Caribbean Sea. Its western end appears not to continue further than its surface trace, where it is covered by Cenozoic volcanics. The measured length of the fault is approximately 350 km and is the longest fault in Guatemala. Motion of the fault and others in the plate boundary have formed north–south trending grabens across the region that show evidence of counter-clockwise rotation over time. Guatemala City lies in one of these grabens, which may contribute to the seismic hazard posed to the city's inhabitants. The Motagua Fault is regarded by some geologists as part of a system of faults designated the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chixoy-Polochic Fault
The Chixoy-Polochic Fault, also known as Cuilco-Chixoy-Polochic Fault, is a major fault zone in Guatemala and southeast Mexico. It runs in a light arc from the east coast of Guatemala to Chiapas, following the deep valleys of the Polochic River, Chixoy River and Cuilco River. Extent, slip rate and total displacement The Chixoy-Polochic Fault is a large, dominantly strike-slip, left-lateral fault that runs largely parallel to the Motagua Fault situated some 45 km to its south. Both fault zones are onshore extensions of the Bartlett Deep, or Cayman Trench of the Caribbean Sea, which marks the tectonic boundary between the Caribbean plate and the North American plate. Both faults connect at sea west of the Guatemalan coast. To the west, the Polochic fault may branch onto the Tonala fault of western Chiapas. It does not continue at sea across the Pacific coastal plain and marine shelf. The Chixoy-Polochic fault has total displacement of 125 km, well constrained by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the more recent of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period. Climate During the Late Cretaceous, the climate was warmer than present, although throughout the period a cooling trend is evident. The tropics became restricted to equatorial regions and northern latitudes experienced markedly more seasonal climatic conditions. Geography Due to plate tectonics, the Americas were gradually moving westward, causing the Atlantic Ocean to expand. The Western Interior Seaway divided North America into eastern and western halves; Appalachia and Laramidia. India maintained a northward course towards Asia. In the Southern Hemisphere, Aus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
