Patilla Pata
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Patilla Pata is a
stratovolcano A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with ...
in the
Oruro Department Oruro (; Quechua: ''Uru Uru''; Aymara: ''Ururu'') is a department of Bolivia, with an area of . Its capital is the city of Oruro. According to the 2012 census, the Oruro department had a population of 494,178. Provinces of Oruro The depar ...
in
Bolivia Bolivia, officially the Plurinational State of Bolivia, is a landlocked country located in central South America. The country features diverse geography, including vast Amazonian plains, tropical lowlands, mountains, the Gran Chaco Province, w ...
. It is situated in the
Sajama Province Sajama is a province in the northwestern parts of the Bolivian Oruro Department. Location ''Sajama'' province is one of the sixteen provinces in the Oruro Department. It is located between 17° 39' and 18° 39' South and between 67° 38' and 68° ...
, in the west of the Curahuara de Carangas Municipality, at the border with
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 ...
. Patilla Pata lies south-west of the mountain Jisk'a Kunturiri, north-east of the lake Q'asiri Quta ''(Khasiri Kkota)'' and the mountain Qullqi Warani, west of the little lake Sura Pata, south-east of the mountains Laram Q'awa, Kunturiri and Milluni and south of the little lake named Ch'iyar Quta. The river Junt'uma K'uchu (Aymara ''junt'u'' warm, hot, ''uma'' water, ''k'uchu'' corner, "warm water corner", ''Junthuma Khuchu'') originates south of Patilla Pata. It flows to the south-east as a right affluent of the Sajama River. (unnamed, south of ''Chiar Kkota'') The date of its last eruption is unclear, but it is unlikely to be during the
Holocene The Holocene () is the current geologic time scale, geological epoch, beginning approximately 11,700 years ago. It follows the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene to ...
as the mountain is heavily glaciated. The composition of the volcano is largely
andesitic Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predomina ...
, but there are also a number of
basaltic Basalt (; ) is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron ( mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90% ...
lava Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a Natural satellite, moon onto its surface. Lava may be erupted at a volcano or through a Fissure vent, fractu ...
flows.


See also

* Jach'a Kunturiri * Sajama *
List of volcanoes in Bolivia The country of Bolivia hosts numerous activeIn vulcanology and this article active volcanoes are those with Holocene eruption, that means eruptions in the last 10,000 years. and extinct volcanoes across its territory. The active volcanoes are i ...


References


Sources

* Stratovolcanoes of Bolivia Subduction volcanoes Polygenetic volcanoes Volcanoes of Oruro Department Volcanoes of La Paz Department (Bolivia) Pleistocene stratovolcanoes {{Oruro-geo-stub