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Chocó–Darién Moist Forests
The Chocó–Darién moist forests (NT0115) is an ecoregion in the west of Colombia and east of Panama. The region has extremely high rainfall, and the forests hold great biodiversity. The northern and southern parts of the ecoregion have been considerably modified for ranching and farming, and there are threats from logging for paper pulp, uncontrolled gold mining, coca growing and industrialisation, but the central part of the ecoregion is relatively intact. Geography Location The Chocó–Darién moist forests extend along most of the Pacific coast of Colombia and extend north into Panama along the Caribbean coast. They are bounded to the east by the Andes, which separate them from the Amazon and Orinoco ecoregions. They have an area of . In Colombia the ecoregion is in the Chocó, Cauca, Valle del Cauca and Nariño departments. In Panama it is in the Darién and Guna Yala provinces. The northern section merges into Isthmian-Atlantic moist forests to the west in the I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utría National Natural Park
The Utría National Natural Park ( es, Parque Nacional Natural Ensenada de Utría) is a national park in the Chocó Department, Colombia. It contains diverse flora and fauna in a lush, mountainous rainforest environment with some of the highest rainfall in the world, at up to annually. The park also protects the coastal marine environment, and is known for visits by humpback whales, who give birth in the lagoon after which the park is named, and sea turtles who nest on the beaches. There is accommodation for visitors, and ecotourism services are provided by the local indigenous people and members of the coastal Afro-Colombian communities. Location The Utría National Natural Park is on the Pacific coast of Colombia in the Chocó Department. It covers parts of the municipalities of Bahía Solano, Nuquí, Bojayá and Alto Baudó. The park overlaps the territory of the Emberá indigenous people, who have well-preserved cultural traditions. There are also fishing villages of Afro- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magdalena–Urabá Moist Forests
The Magdalena–Urabá moist forests (NT0137) is an ecoregion in the north of Colombia. The terrain is largely flat or undulating, but includes mountainous areas in the south. It contains moist forests and large wetlands that are important to resident and migratory birds. The ecoregion forms a bridge between the Pacific coast ecoregions of Colombia and Central America, and the ecoregions of the Andes and Amazon. It is surrounded by the more populated parts of Colombia and is threatened by farming, ranching, logging, oil exploitation and water pollution in the main rivers. Geography Location The ecoregion is in the north of Colombia, with an area of . It includes the flat landscape along the lower course of the Magdalena River, and extends west over the coastal plain to the Gulf of Urabá. To the north the ecoregion transitions into the Sinú Valley dry forests and Guajira–Barranquilla xeric scrub ecoregions. To the west it meets the Chocó–Darién moist forests, and to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laterite
Laterite is both a soil and a rock type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by intensive and prolonged weathering of the underlying parent rock, usually when there are conditions of high temperatures and heavy rainfall with alternate wet and dry periods. Tropical weathering (''laterization'') is a prolonged process of chemical weathering which produces a wide variety in the thickness, grade, chemistry and ore mineralogy of the resulting soils. The majority of the land area containing laterites is between the tropics of Cancer and Capricorn. Laterite has commonly been referred to as a soil type as well as being a rock type. This and further variation in the modes of conceptualizing about laterite (e.g. also as a complete weathering profile or theory about weathering) has led to calls for the term to be abandoned alto ... [...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] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tertiary
Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent. Historical use of the term The term Tertiary was first used by Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, the Quaternary, was applied. In the early d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serranía Del Baudó
The Serranía del Baudó is a coastal mountain range on the Pacific coast of Colombia. It is separated from the West Andes by the Atrato valley where the Atrato River flows and Quibdó is located. From the south the range extends from the Baudó River north and slightly west along the coast into Panama terminating at the Golfo de San Miguel. The range is called Serranía del Sapo when it is in Panama. Technically the landform extends south of the Baudó River down to Malaga Bay, but the area has been eroded into low hills and marshlands. From Cabo Corrientes north to Punta Ardita and on into Panama the Baudó Mountains meet the ocean in steep cliffs, rising up to as high as , with small indentations in the coast providing small pocket beaches, some sandy, but most are shingle or cobble. However, near river mouths the coast has been eroded and there are wide sandy beaches, tidal flats and even mangrove swamps. The highest point, Alto de Buey, is . Geology Geologically, the S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra Llorona De San Blas
Sierra (Spanish for "mountain range" and "saw", from Latin '' serra'') may refer to the following: Places Mountains and mountain ranges * Sierra de Juárez, a mountain range in Baja California, Mexico * Sierra de las Nieves, a mountain range in Andalusia, Spain * Sierra Madre (other), various mountain ranges ** Sierra Madre (Philippines), a mountain range in the east of Luzon, Philippines * Sierra mountains (other) * Sierra Nevada, a mountain range in the U.S. states of California and Nevada * Sierra Nevada (Spain), a mountain range in Andalusia, Spain * Sierra de San Pedro Mártir, a mountain range in Baja California, Mexico * Sierra Maestra, a mountain range in Cuba Other places Africa * Sierra Leone, a country located on the coast of West Africa Asia * Sierra Bullones, Bohol, Philippines Europe * Sierra Nevada National Park (Spain), Andalusia, Spain * Sierra Nevada Observatory, Granada, Spain North America * High Sierra Trail, California, United States ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serranía Del Darién
The Serranía del Darién is a small mountain range on the border between Colombia and Panamá in the area called the Darién Gap. It is located in the southeastern part of the Darién Province of Panamá and the northwestern part of the Chocó Department of Colombia. There are two major protected areas here: Darién National Park in Panamá and Los Katíos National Park in Colombia. Serranía del Darién range's average elevation above sea level is . These mountains have sparse settlements, with just two people living in every square kilometer. This lack of human settlements is reflected in the fact that the nearest town with a population of 50,000 is over 12 hours by road. Geological hazards The Serranía del Darién is notorious for strong earthquakes; on average earthquakes measuring between 6 and 7 occur here every 50 years. The area is also susceptible to floods and landslides, both of which have been classified as medium to high intensity hazards for the region. Climate S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cerro Torrá
Cerro is Spanish for "hill" or "mountain". Toponyms ;Bolivia: * Cerro Rico, the "Rich Mountain" containing silver ore near Potosi, Bolivia ;Brazil: *Cerro Branco, a municipality of Rio Grande do Sul *Cerro Grande, Rio Grande do Sul, a municipality of Rio Grande do Sul * Cerro Largo, a municipality of Rio Grande do Sul ;Chile * Cerro de Los Inocentes, in the Juan Fernández Islands ;Cuba: * Cerro, Havana, a district (''municipio'') ;Italy: *Cerro (Bottanuco), a subdivision of Bottanuco in the province of Bergamo *Cerro al Lambro, in the province of Milano *Cerro al Volturno, in the province of Isernia *Cerro Maggiore, in the province of Milano *Cerro Tanaro, in the province of Asti *Cerro Veronese, in the province of Verona ;Mexico: * Cerro Potosí ;United States: * Cerro, New Mexico ;Uruguay: * Cerro Largo Department * Villa del Cerro, in Montevideo * Fortaleza del Cerro, in Montevideo Football clubs * C.A. Cerro, a football club from Montevideo, Uruguay * Club Cerro Cor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cordillera Occidental (Colombia)
The Cordillera Occidental ( en, Western Ranges) is the lowest in elevation of the three branches of the Colombian Andes. The average altitude is and the highest peak is Cerro Tatamá at . The range extends from south to north dividing from the Colombian Massif in Nariño Department, passes north through Cauca, Valle del Cauca, Risaralda, Chocó, and Caldas Departments to the Paramillo Massif in Antioquia and Córdoba Departments. From this massif the range divides further to form the Serranías de Ayapel, San Jerónimo and Abibe. Only to recede into the Caribbean plain and the Sinú River valley. Geography The western part of the mountain range belongs to the Pacific region of Colombia and its Chocó–Darién moist forests ecoregion, with the San Juan River being the main watershed, while the eastern part belongs to the Cauca River basin. The northern and northwestern parts belong to the Atlantic Slope, with the Atrato and Sinú Rivers being the main water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Ecuador Moist Forests
The Western Ecuador Moist Forests (NT0178), also known as thPacific Forest of Ecuador is an ecoregion in the plains and western foothills of the Andes of southern Colombia and Ecuador. At one time this region contained dense forests with highly diverse flora and fauna, and many endemic species. Most of the original habitat has now been destroyed, and the ecoregion is one of the most threatened in the world. Geography Location The Western Ecuador moist forests ecoregion covers land to the west of the Andes in Ecuador and southern Colombia. In the northwest and the extreme southwest the ecoregion extends to the Pacific Ocean. The ecoregion is bounded on the north by the Patía River. It extends through the provinces of Esmeraldas, Manabí and Guayas, reaching the Gulf of Guayaquil in the south, and the foothills on the Andes in the east. It varies in width from . It has an area of . In the extreme north the ecoregion transitions into the Chocó–Darién moist forests ecoreg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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