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Megantoni District, La Convención Province
Megantoni District is one of fourteen districts of La Convención Province in the Cusco Region of Peru. Megantoni occupies the northernmost part of La Convención. The district was created in 2016 from land previously belonging to Echarate District. Camisea is the capital of Megantoni and has a population of about 500 people. As of 2017, the district was not connected to the rest of Peru by road. The Urubamba River bisects the district and is a major avenue of transportation. Protected and indigenous lands Ninety-four percent of the land of Megantoni is protected for conservation or allocated to indigenous people. The majority of this land is "almost untouched" tropical rainforest and Peruvian Yungas characteristic of the Amazon Basin and the eastern flanks of the Andes. Protected lands include the Pongo de Mainique, a scenic water gap where the Urubamba River cuts through the Vilcabamba mountain range on the southern border of Megantoni. East of the Pongo, the Megantoni National ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Districts Of Peru
The districts of Peru () are the third-level country subdivisions of Peru. They are subdivisions of the provinces of Peru, provinces, which in turn are subdivisions of the larger regions of Peru, regions or departments. There are 1,838 districts in total. Overview A 1982 law requires a minimum of residents in an area for a new district to be legally established: 3,500 if it is located in the rainforest, 4,000 in the Andes highlands and 10,000 in the Chala, coastal area. In the dry Andean area, many districts have less than 3,500 inhabitants due to low population density in the area. In some cases, their populations have decreased in comparison to the days when they were founded. Districts that are located at very high altitudes tend to be scarcely populated. These districts usually are large in area, have few available land for use. Many basic government services do not reach all residents of these districts due to their difficult geography. Many lack financial means to govern th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peruvian Yungas
The Peruvian Yungas is a tropical and subtropical moist broadleaf forest ecoregion in the Yungas of Peru. Setting The Peruvian Yungas occur on the eastern slopes and valleys of the Peruvian Andes. They form a transition zone between the Southwest Amazon moist forests and Ucayali moist forests at lower elevations to the east and the Central Andean puna and wet puna at higher elevations to the west. Climate The climate in this ecoregion varies from a tropical rainforest climate in the north to a subtropical highland climate in the south. Precipitation ranges from per year. Flora This ecoregion contains over 3,000 species of plants, including 200 species of orchids. Orchid genera include ''Epidendrum'' and ''Maxillaria''. Tree ferns (''Cyathea'') and bamboo (''Chusquea'') are common. Below , the forest includes species such as cedar (''Cedrela''), trumpet tree (''Tabebuia''), and relatives of papaya (''Carica''). Above , there are scrublands and wet rocky thickets with shrubs an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cloud Forest
A cloud forest, also called a water forest, primas forest, or tropical montane cloud forest (TMCF), is a generally tropical or subtropical, evergreen, montane, moist forest characterized by a persistent, frequent or seasonal low-level cloud cover, usually at the canopy level, formally described in the ''International Cloud Atlas'' (2017) as silvagenitus. Cloud forests often exhibit an abundance of mosses covering the ground and vegetation, in which case they are also referred to as mossy forests. Mossy forests usually develop on the saddles of mountains, where moisture introduced by settling clouds is more effectively retained. Cloud forests are among the most biodiversity rich ecosystems in the world with a large amount of species directly or indirectly depending on them. Other moss forests include black spruce/feathermoss climax forest, with a moderately dense canopy and a forest floor of feathermosses including ''Hylocomium splendens'', ''Pleurozium schreberi'' and ''Ptil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wildlife Conservation Society
The Wildlife Conservation Society (WCS) is a non-governmental organization headquartered at the Bronx Zoo in New York City, that aims to conserve the world's largest wild places in 14 priority regions. Founded in 1895 as the New York Zoological Society (NYZS), the organization is now led by President and CEO Cristián Samper. WCS manages four New York City wildlife parks in addition to the Bronx Zoo: the Central Park Zoo, New York Aquarium, Prospect Park Zoo and Queens Zoo. Together these parks receive 4 million visitors per year."About Us" ''WCS.org'', accessed 23 November 2020 All of the New York City facilities are accredited by the (AZA). H ...
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Biodiversity Hotspot
A biodiversity hotspot is a biogeographic region with significant levels of biodiversity that is threatened by human habitation. Norman Myers wrote about the concept in two articles in ''The Environmentalist'' in 1988 and 1990, after which the concept was revised following thorough analysis by Myers and others into “Hotspots: Earth’s Biologically Richest and Most Endangered Terrestrial Ecoregions” and a paper published in the journal ''Nature'', both in 2000. To qualify as a biodiversity hotspot on Myers' 2000 edition of the hotspot map, a region must meet two strict criteria: it must contain at least 1,500 species of vascular plants (more than 0.5% of the world's total) as endemics, and it has to have lost at least 70% of its primary vegetation. Globally, 36 zones qualify under this definition. These sites support nearly 60% of the world's plant, bird, mammal, reptile, and amphibian species, with a high share of those species as endemics. Some of these hotspots support up ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southwest Amazon Moist Forests
The Southwest Amazon moist forests (NT0166) is an ecoregion located in the Upper Amazon basin. The forest is characterized by a relatively flat landscape with alluvial plains dissected by undulating hills or high terraces. The biota of the southwest Amazon moist forest is very rich because of these dramatic edaphic and topographical variations at both the local and regional levels. This ecoregion has the highest number of both mammals and birds recorded for the Amazonian biogeographic realm: 257 with 11 endemic species for mammals and 782 and 17 endemics for birds. The inaccessibility of this region, along with few roads, has kept most of the habitat intact. Also, there are a number of protected areas, which preserve this extremely biologically rich ecoregion. Location The southwest Amazon moist forest region covers an extensive area of the Upper Amazon Basin comprising four sub-basins: (1) both the Pastaza- Marañon and (2) Ucayali River sub-basins drain into the Upper ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Machiguenga Communal Reserve
The Machiguenga Communal Reserve (''Reserva Comunal Machiguenga'') is a protected area in Peru located in the Cusco Region, La Convención Province, Megantoni district. See also * Machiguenga * Natural and Cultural Peruvian Heritage * Megantoni National Sanctuary Megantoni National Sanctuary (''Santuario Nacional de Megantoni'') is a protected area in Peru situated in the Cusco Region, La Convención Province, Echarate and Megantoni districts. It protects a part of the Peruvian Yungas ecoregion. See als ... External links www.parkswatch.org / Machiguenga Communal Reserve {{coord, 11.7556, S, 73.5682, W, source:wikidata, display=title Communal reserves of Peru Geography of Cusco Region ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otishi National Park
Otishi National Park ( es, Parque Nacional Otishi) is a protected area in Peru, located in the regions of Junín and Cusco. It protects part of the Vilcabamba mountain range, preserving the wildlife and geological formations in this area. See also *Asháninka * Machiguenga The Machiguenga (also Matsigenka, Matsigenga) are an indigenous people who live in the high jungle, or''montaña'', area on the eastern slopes of the Andes and in the Amazon Basin jungle regions of southeastern Peru. Their population in 2020 amou ... References National parks of Peru Geography of Junín Region Geography of Cusco Region Protected areas established in 2003 Tourist attractions in Cusco Region Tourist attractions in Junín Region {{Cusco-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Megantoni National Sanctuary
Megantoni National Sanctuary (''Santuario Nacional de Megantoni'') is a protected area in Peru situated in the Cusco Region, La Convención Province, Echarate and Megantoni districts. It protects a part of the Peruvian Yungas ecoregion. See also * Machiguenga Communal Reserve * Natural and Cultural Peruvian Heritage This is a list of protected areas in Peru. Natural heritage The Constitution of Peru of 1993 recognized the natural resources and ecosystem variety of its country as a heritage. In 1990, the National System of Natural Areas that are protecte ... References External links www.enjoyperu.com / Megantoni National Sanctuary(Spanish) {{coord, 12.2206, S, 72.3614, W, source:wikidata, display=title National sanctuaries of Peru Geography of Cusco Region Protected areas established in 2004 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vilcabamba Mountain Range
The Vilcabamba mountain range is located in the region of Cusco, Peru, in the provinces of Anta, La Convención and Urubamba. It extends between 13°10' and 13°27'S. and 72°30' and 73°15'W for about 85 km.usgs.gov USGS, Peruvian Cordilleras Its highest peak is Salcantay, which is 6,271 m (20,574 ft) above sea level. Toponyms Most of the names in the range originate from . They used to be spelled according to a mainly Spanish-based orthography which is incompatible with the normalized spellings of these languages and Law 29735 which regulates the 'use, preservation, development, recovery, promotion and diffusion of the originary languages of Peru'. According to Arti ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Water Gap
A water gap is a gap that flowing water has carved through a mountain range or mountain ridge and that still carries water today. Such gaps that no longer carry water currents are called wind gaps. Water gaps and wind gaps often offer a practical route for road and rail transport to cross the mountain barrier. Geology A water gap is usually an indication of a river that is older than the current topography. The likely occurrence is that a river established its course when the landform was at a low elevation, or by a rift in a portion of the crust of the earth having a very low stream gradient and a thick layer of unconsolidated sediment. In a hypothetical example, a river would have established its channel without regard for the deeper layers of rock. A later period of uplift would cause increased erosion along the riverbed, exposing the underlying rock layers. As the uplift continued, the river, being large enough, would continue to erode the rising land, cutting thr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
