Laguna Hedionda (Nor Lípez)
   HOME



picture info

Laguna Hedionda (Nor Lípez)
Laguna Hedionda (Spanish for "stinking lake") is a saline lake in the Nor Lípez Province, Potosí Department in Bolivia. It is notable for various migratory species of pink and white flamingos. Laguna Hedionda is one of the nine small saline lakes in the Andean Altiplano. It lies at an altitude of , with an area of . Salt flats and ''bofedales'' (wetlands) are spread over the periphery of the lake. It is in a very remote area where human habitation is negligible. However, llamas and alpacas are seen grazing in the area.__NOTOC__ Geography Laguna Hedionda is located in the Cordillera Occidental area of the Bolivian Altiplano of the central Andes, which is a volcanic landscape where many small closed lake basins have been noted. The central Andes of Bolivia has two other major basins, also running in a north–south direction, namely the freshwater Lake Titicaca basin and the Poopó and the Coipasa-Uyuni basins with shallow saline lakes and/or a salt crusts. Specifically, the c ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Nor Lípez Province
Nor Lípez is a province in the Bolivian department of Potosí. Its seat is Colcha "K", also called Villa Martín. The majority of the area of the province was titled as the Nor Lípez Native Community Land on 19 April 2011. One of the largest mines of Bolivia, the San Cristóbal Mine, is located near San Cristóbal in Colcha "K" municipality. Geography Some of the highest mountains of the province are listed below: Location The province is one of sixteen provinces in the Potosí Department. It is located between 20° 27' and 22° 01' South and between 66° 18' and 68° 35' West. It is bordered by the Daniel Campos Province to the north, the Republic of Chile to the west, the Enrique Baldivieso Province and Sur Lípez Province to the south, Sud Chichas Province to the east, and the Antonio Quijarro Province to the northeast. The province extends over 270 km from east to west and 210 km from north to south. Division The province comprises tw ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Coipasa Lake
__NOTOC__ Lago Coipasa is a lake in Sabaya Province, Oruro Department, Bolivia. At an elevation of 3657 m, its surface area is 806 km². It is located on the western part of Altiplano, 20 km north of Salar de Uyuni and south of the main road linking Oruro and Huara (Chile). Lake Coipasa is a tectonic saline lake with a depth of 3.5 metres that is surrounded by the Salar de Coipasa ("Coipasa Salt Flats"), and dominated by the volcanic cone of the 4,920 m high Wila Pukarani. Thousands of flamingo Flamingos or flamingoes () are a type of wading bird in the family Phoenicopteridae, which is the only extant family in the order Phoenicopteriformes. There are four flamingo species distributed throughout the Americas (including the Caribbe ...s have settled on the shores of Lake Coipasa. Gallery Coipasa lake map of the shape and depth (bathymetry) 2020.jpg, Map of the shape and depth (bathymetry) of the Coipasa lake, 2020 Lago Uru Uru Chipaya 4.jpg, The la ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Lacustrine Delta
A river delta is a landform, archetypically triangular, created by the deposition of the sediments that are carried by the waters of a river, where the river merges with a body of slow-moving water or with a body of stagnant water. The creation of a river delta occurs at the ''river mouth'', where the river merges into an ocean, a sea, or an estuary, into a lake, a reservoir, or (more rarely) into another river that cannot carry away the sediment supplied by the feeding river. Etymologically, the term ''river delta'' derives from the triangular shape (Δ) of the uppercase Greek letter delta. In hydrology, the dimensions of a river delta are determined by the balance between the watershed processes that supply sediment and the watershed processes that redistribute, sequester, and export the supplied sediment into the receiving basin. River deltas are important in human civilization, as they are major agricultural production centers and population centers. They can provide coast ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Diatom
A diatom (Neo-Latin ''diatoma'') is any member of a large group comprising several Genus, genera of algae, specifically microalgae, found in the oceans, waterways and soils of the world. Living diatoms make up a significant portion of Earth's Biomass (ecology), biomass. They generate about 20 to 50 percent of the oxygen produced on the planet each year, take in over 6.7 billion tonnes of silicon each year from the waters in which they live, and constitute nearly half of the organic material found in the oceans. The Protist shell, shells of dead diatoms are a significant component of marine sediment, and the entire Amazon basin is fertilized annually by 27 million tons of diatom shell dust transported by transatlantic winds from the African Sahara, much of it from the Bodélé Depression, which was once made up of a system of fresh-water lakes. Diatoms are unicellular organisms: they occur either as solitary cells or in Colony (biology), colonies, which can take the shape of ribb ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Sulphur
Sulfur (American spelling and the preferred IUPAC name) or sulphur (English in the Commonwealth of Nations, Commonwealth spelling) is a chemical element; it has Symbol (chemistry), symbol S and atomic number 16. It is abundance of the chemical elements, abundant, Polyvalency (chemistry), multivalent and Nonmetal (chemistry), nonmetallic. Under standard conditions for temperature and pressure, normal conditions, sulfur atoms form octasulfur, cyclic octatomic molecules with the chemical formula octasulfur, S8. Elemental sulfur is a bright yellow, crystalline solid at room temperature. Sulfur is the tenth most abundant element by mass in the universe and the fifth most common on Earth. Though sometimes found in pure, native element minerals, native form, sulfur on Earth usually occurs as sulfide minerals, sulfide and sulfate minerals. Being abundant in native form, sulfur was known in ancient times, being mentioned for its uses in Outline of ancient India, ancient India, ancient G ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Ch'iyar Quta (Nor Lípez)
__NOTOC__ Ch'iyar Quta (Aymara ''ch'iyara'' black, ''quta'' lake, "black lake", hispanicized spellings ''Chiar Kkota, Chiar Khota, Chiar Kota'') is a Bolivian lake located in the San Pedro de Quemes Municipality, Nor Lípez Province of the Potosí Department near the border to Chile Chile, officially the Republic of Chile, is a country in western South America. It is the southernmost country in the world and the closest to Antarctica, stretching along a narrow strip of land between the Andes, Andes Mountains and the Paci .... It is situated at a height of about south west of Laguna Hedionda and east of Mount Araral. See also * Lake Kara * Laguna Pastos Grande References Lakes of Potosí Department {{Potosí-geo-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Volcano
A volcano is commonly defined as a vent or fissure 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 are diverging or converging, and because most of Earth's plate boundaries are underwater, most volcanoes are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes resulting from divergent tectonic activity are usually non-explosive whereas those resulting from convergent tectonic activity cause violent eruptions."Mid-ocean ridge tectonics, volcanism and geomorphology." Geology 26, no. 455 (2001): 458. https://macdonald.faculty.geol.ucsb.edu/papers/Macdonald%20Mid-Ocean%20Ridge%20Tectonics.pdf Volcanoes can also form where there is str ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Ollagüe
Ollagüe () or Ullawi () is a massive andesite stratovolcano in the Andes on the Bolivia–Chile border, within the Antofagasta Region of Chile and the Potosí Department, Potosi Department of Bolivia. Part of the Central Volcanic Zone of the Andes, its highest summit is above sea level and features a summit crater that opens to the south. The western rim of the summit crater is formed by a compound of lava domes, the youngest of which features a vigorous fumarole that is visible from afar. Ollagüe is mostly of Pleistocene age. It started developing more than one million years ago, forming the so-called Vinta Loma and Santa Rosa series mostly of Andesite, andesitic lava flows. A fault (geology), fault bisects the edifice and two large landslides occurred in relation to it. Later two groups of Dacite, dacitic lava domes formed, Ch'aska Urqu (Nor Lípez), Ch'aska Urqu on the southeastern slope and La Celosa on the northwestern. Another centre named La Poruñita formed at that ti ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Tocorpuri
Tocorpuri is a volcano on the border between Chile and Bolivia. Its peak height is most recently given as and it features a wide summit crater. The volcano consists mainly of lava flows and pyroclastic deposits and is subdivided into two separate edifices. Just west of Tocorpuri, the La Torta lava dome is a high flat-topped structure. The volcanoes are formed by andesitic, dacitic and rhyolitic rocks. The Tocorpuri volcanoes developed in the late Pleistocene in three separate stages and were subject to glaciation and tectonic faulting. The most recent eruption generated the La Torta lava dome 34,000 ± 7,000 years ago; presently there is geothermal activity which may be connected to that of the neighbouring El Tatio geothermal field. Geomorphology Tocorpuri lies in northern Chile, about east of Calama. The border with Bolivia runs around the eastern side of Tocorpuri's summit crater. The area lies in Chile's Antofagasta Department and on Bolivia's Potosí Department and ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Michincha
Michincha is a stratovolcano on the border of Bolivia and Chile. It is part of an east–west trending ridge of stratovolcanoes. To its east lies Olca Olca is a stratovolcano on the border of Chile and Bolivia. It lies in the middle of a 15 km long ridge composed of several stratovolcanos. Cerro Minchincha lies to the west and Paruma to the east. It is also close to the pre-Holocene Cerro .... The only historical activity from the complex was a flank eruption from 1865 to 1867. Sources Stratovolcanoes of Chile Subduction volcanoes Volcanoes of Potosí Department Mountains of Tarapacá Region Polygenetic volcanoes Bolivia–Chile border International mountains of South America Volcanoes of Tarapacá Region Holocene stratovolcanoes Five-thousanders of the Andes {{chile-mountain-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Andes Mountains
The Andes ( ), Andes Mountains or Andean Mountain Range (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long and wide (widest between 18°S and 20°S latitude) and has an average height of about . The Andes extend from south to north through seven South American countries: Argentina, Chile, Bolivia, Peru, Ecuador, Colombia, and Venezuela. Along their length, the Andes are split into several ranges, separated by intermediate depressions. The Andes are the location of several high plateaus—some of which host major cities such as Quito, Bogotá, Cali, Arequipa, Medellín, Bucaramanga, Sucre, Mérida, El Alto, and La Paz. The Altiplano Plateau is the world's second highest after the Tibetan Plateau. These ranges are in turn grouped into three major divisions based on climate: the Tropical Andes, the Dry Andes, and the Wet Andes. The Andes are the highest mountain r ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]