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Ollagüe, the Glossary

Index Ollagüe

Ollagüe or Ullawi is a massive andesite stratovolcano in the Andes on the border between Bolivia and Chile, within the Antofagasta Region of Chile and the Potosi Department of Bolivia.[1]

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Table of Contents

  1. 169 relations: Aerial tramway, Altiplano, Altiplano–Puna volcanic complex, Alunite, Amphibole, Andean Volcanic Belt, Andes, Andesite, Antofagasta Region, Apatite, Argon–argon dating, Aucanquilcha, Autoclave, Aymara language, Back-arc region, Basaltic andesite, Biotite, Bolivia, Breccia, Calc-alkaline magma series, Caldera, Capitalism, Cenozoic, Ch'aska Urqu (Nor Lípez), Chalcedony, Chile, Cinder cone, Cirque, Clay, Colluvium, Communes of Chile, Copper, Cordillera Occidental (Central Andes), Cordillera Oriental (Bolivia), Crust (geology), Cumulate rock, Dacite, Dike (geology), Earthquake swarm, El Loa, Eocene, Evaporation, Evaporite, Fault (geology), Felsic, Ferrocarril de Antofagasta a Bolivia, Foothills, Fractional crystallization (geology), Fumarole, Gabbro, ... Expand index (119 more) »

  2. Bolivia–Chile border
  3. Volcanoes of Potosí Department

Aerial tramway

An aerial tramway, aerial tram, sky tram, aerial cablecar, aerial cableway, telepherique, or seilbahn is a type of aerial lift which uses one or two stationary ropes for support while a third moving rope provides propulsion.

See Ollagüe and Aerial tramway

Altiplano

The Altiplano (Spanish for "high plain"), Collao (Quechua and Aymara: Qullaw, meaning "place of the Qulla") or Andean Plateau, in west-central South America, is the most extensive high plateau on Earth outside Tibet. Ollagüe and Altiplano are Bolivia–Chile border.

See Ollagüe and Altiplano

Altiplano–Puna volcanic complex

The Altiplano–Puna volcanic complex, also known as APVC, is a complex of volcanic systems in the Puna of the Andes.

See Ollagüe and Altiplano–Puna volcanic complex

Alunite

Alunite is a hydroxylated aluminium potassium sulfate mineral, formula KAl3(SO4)2(OH)6.

See Ollagüe and Alunite

Amphibole

Amphibole is a group of inosilicate minerals, forming prism or needlelike crystals, composed of double chain tetrahedra, linked at the vertices and generally containing ions of iron and/or magnesium in their structures.

See Ollagüe and Amphibole

Andean Volcanic Belt

The Andean Volcanic Belt is a major volcanic belt along the Andean cordillera in Argentina, Bolivia, Chile, Colombia, Ecuador, and Peru.

See Ollagüe and Andean Volcanic Belt

Andes

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.

See Ollagüe and Andes

Andesite

Andesite is a volcanic rock of intermediate composition.

See Ollagüe and Andesite

Antofagasta Region

The Antofagasta Region (Región de Antofagasta.) is one of Chile's sixteen first-order administrative divisions.

See Ollagüe and Antofagasta Region

Apatite

Apatite is a group of phosphate minerals, usually hydroxyapatite, fluorapatite and chlorapatite, with high concentrations of OH−, F− and Cl− ion, respectively, in the crystal.

See Ollagüe and Apatite

Argon–argon dating

Argon–argon (or 40Ar/39Ar) dating is a radiometric dating method invented to supersede potassiumndashargon (K/Ar) dating in accuracy.

See Ollagüe and Argon–argon dating

Aucanquilcha

Aucanquilcha is a massive stratovolcano located in the Antofagasta Region of northern Chile, just west of the border with Bolivia and within the Alto Loa National Reserve. Ollagüe and Aucanquilcha are Pleistocene stratovolcanoes, Stratovolcanoes of Chile and volcanoes of Antofagasta Region.

See Ollagüe and Aucanquilcha

Autoclave

An autoclave is a machine used to carry out industrial and scientific processes requiring elevated temperature and pressure in relation to ambient pressure and/or temperature.

See Ollagüe and Autoclave

Aymara language

Aymara (also Aymar aru) is an Aymaran language spoken by the Aymara people of the Bolivian Andes.

See Ollagüe and Aymara language

Back-arc region

The back-arc region is the area behind a volcanic arc.

See Ollagüe and Back-arc region

Basaltic andesite

Basaltic andesite is a volcanic rock that is intermediate in composition between basalt and andesite.

See Ollagüe and Basaltic andesite

Biotite

Biotite is a common group of phyllosilicate minerals within the mica group, with the approximate chemical formula.

See Ollagüe and Biotite

Bolivia

Bolivia, officially the Plurinational State of Bolivia, is a landlocked country located in western-central South America.

See Ollagüe and Bolivia

Breccia

Breccia is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix.

See Ollagüe and Breccia

Calc-alkaline magma series

The calc-alkaline magma series is one of two main subdivisions of the subalkaline magma series, the other subalkaline magma series being the tholeiitic series.

See Ollagüe and Calc-alkaline magma series

Caldera

A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption.

See Ollagüe and Caldera

Capitalism

Capitalism is an economic system based on the private ownership of the means of production and their operation for profit.

See Ollagüe and Capitalism

Cenozoic

The Cenozoic is Earth's current geological era, representing the last 66million years of Earth's history.

See Ollagüe and Cenozoic

Ch'aska Urqu (Nor Lípez)

Ch'aska Urqu (Quechua ch'aska star; tousled, urqu mountain, "star mountain" or "tousled mountain", also spelled Chasca Orkho) is a mountain in the Andes of Bolivia, about high.

See Ollagüe and Ch'aska Urqu (Nor Lípez)

Chalcedony

Chalcedony is a cryptocrystalline form of silica, composed of very fine intergrowths of quartz and moganite.

See Ollagüe and Chalcedony

Chile

Chile, officially the Republic of Chile, is a country in western South America.

See Ollagüe and Chile

Cinder cone

A cinder cone (or scoria cone) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent.

See Ollagüe and Cinder cone

Cirque

A (from the Latin word) is an amphitheatre-like valley formed by glacial erosion.

See Ollagüe and Cirque

Clay

Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, Al2Si2O5(OH)4).

See Ollagüe and Clay

Colluvium

Colluvium (also colluvial material or colluvial soil) is a general name for loose, unconsolidated sediments that have been deposited at the base of hillslopes by either rainwash, sheetwash, slow continuous downslope creep, or a variable combination of these processes.

See Ollagüe and Colluvium

Communes of Chile

A commune (comuna) is the smallest administrative subdivision in Chile.

See Ollagüe and Communes of Chile

Copper

Copper is a chemical element; it has symbol Cu and atomic number 29.

See Ollagüe and Copper

Cordillera Occidental (Central Andes)

Eastern Cordillera in white, Altiplano in gray, and '''Western Cordillera''' in white The Cordillera Occidental or Western Cordillera of Bolivia is part of the Andes (that is also part of the American Cordillera), a mountain range characterized by volcanic activity, making up the natural border with Chile and starting in the north with Juqhuri and ending in the south at the Licancabur volcano, which is on the southern limit of Bolivia with Chile.

See Ollagüe and Cordillera Occidental (Central Andes)

Cordillera Oriental (Bolivia)

The Cordillera Oriental or Eastern Cordillera is a set of parallel mountain ranges of the Bolivian Andes, emplaced on the eastern and north eastern margin of the Andes.

See Ollagüe and Cordillera Oriental (Bolivia)

Crust (geology)

In geology, the crust is the outermost solid shell of a planet, dwarf planet, or natural satellite.

See Ollagüe and Crust (geology)

Cumulate rock

Cumulate rocks are igneous rocks formed by the accumulation of crystals from a magma either by settling or floating.

See Ollagüe and Cumulate rock

Dacite

Dacite is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides.

See Ollagüe and Dacite

Dike (geology)

In geology, a dike or dyke is a sheet of rock that is formed in a fracture of a pre-existing rock body.

See Ollagüe and Dike (geology)

Earthquake swarm

In seismology, an earthquake swarm is a sequence of seismic events occurring in a local area within a relatively short period.

See Ollagüe and Earthquake swarm

El Loa

El Loa Province (Provincia El Loa) is one of three provinces of the northern Chilean region of Antofagasta (II).

See Ollagüe and El Loa

Eocene

The Eocene is a geological epoch that lasted from about 56 to 33.9 million years ago (Ma).

See Ollagüe and Eocene

Evaporation

Evaporation is a type of vaporization that occurs on the surface of a liquid as it changes into the gas phase.

See Ollagüe and Evaporation

Evaporite

An evaporite is a water-soluble sedimentary mineral deposit that results from concentration and crystallization by evaporation from an aqueous solution.

See Ollagüe and Evaporite

Fault (geology)

In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

See Ollagüe and Fault (geology)

Felsic

In geology, felsic is a modifier describing igneous rocks that are relatively rich in elements that form feldspar and quartz.

See Ollagüe and Felsic

Ferrocarril de Antofagasta a Bolivia

The Ferrocarril de Antofagasta a Bolivia (British company name: Antofagasta (Chili) & Bolivia Railway or FCAB for short) is a private railway operating in the northern provinces of Chile.

See Ollagüe and Ferrocarril de Antofagasta a Bolivia

Foothills or piedmont are geographically defined as gradual increases in elevation at the base of a mountain range, higher hill range or an upland area.

See Ollagüe and Foothills

Fractional crystallization (geology)

Fractional crystallization, or crystal fractionation, is one of the most important geochemical and physical processes operating within crust and mantle of a rocky planetary body, such as the Earth.

See Ollagüe and Fractional crystallization (geology)

Fumarole

A fumarole (or fumerole) is a vent in the surface of the Earth or another rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids.

See Ollagüe and Fumarole

Gabbro

Gabbro is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface.

See Ollagüe and Gabbro

Galán

Cerro Galán is a caldera in the Catamarca Province of Argentina. Ollagüe and Galán are polygenetic volcanoes.

See Ollagüe and Galán

Glacial period

A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances.

See Ollagüe and Glacial period

Glacier

A glacier is a persistent body of dense ice that is constantly moving downhill under its own weight.

See Ollagüe and Glacier

Graben

In geology, a graben is a depressed block of the crust of a planet or moon, bordered by parallel normal faults.

See Ollagüe and Graben

Gully

A gully is a landform created by running water, mass movement, or commonly a combination of both eroding sharply into soil or other relatively erodible material, typically on a hillside or in river floodplains or terraces.

See Ollagüe and Gully

Gypsum

Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula.

See Ollagüe and Gypsum

Height above mean sea level

Height above mean sea level is a measure of a location's vertical distance (height, elevation or altitude) in reference to a vertical datum based on a historic mean sea level.

See Ollagüe and Height above mean sea level

Highway

A highway is any public or private road or other public way on land.

See Ollagüe and Highway

Holocene

The Holocene is the current geological epoch, beginning approximately 11,700 years ago.

See Ollagüe and Holocene

Hydrothermal circulation

Hydrothermal circulation in its most general sense is the circulation of hot water (Ancient Greek ὕδωρ, water,Liddell, H.G. & Scott, R. (1940). A Greek-English Lexicon. revised and augmented throughout by Sir Henry Stuart Jones. with the assistance of. Roderick McKenzie. Oxford: Clarendon Press.

See Ollagüe and Hydrothermal circulation

Hypoxia (medicine)

Hypoxia is a condition in which the body or a region of the body is deprived of adequate oxygen supply at the tissue level.

See Ollagüe and Hypoxia (medicine)

Ignimbrite

Ignimbrite is a type of volcanic rock, consisting of hardened tuff.

See Ollagüe and Ignimbrite

Ilmenite

Ilmenite is a titanium-iron oxide mineral with the idealized formula.

See Ollagüe and Ilmenite

Industrialisation

Industrialisation (UK) or industrialization (US) is the period of social and economic change that transforms a human group from an agrarian society into an industrial society.

See Ollagüe and Industrialisation

International Journal of Earth Sciences

International Journal of Earth Sciences is a peer-reviewed scientific journal published monthly by Springer Science+Business Media.

See Ollagüe and International Journal of Earth Sciences

Intervocalic consonant

In phonetics and phonology, an intervocalic consonant is a consonant that occurs between two vowels.

See Ollagüe and Intervocalic consonant

Irruputuncu

Irruputuncu is a volcano in the commune of Pica, Tamarugal Province, Tarapacá Region, Chile, as well as San Pedro de Quemes Municipality, Nor Lípez Province, Potosí Department, Bolivia. Ollagüe and Irruputuncu are Bolivia–Chile border, International mountains of South America, polygenetic volcanoes, Stratovolcanoes of Chile and volcanoes of Potosí Department.

See Ollagüe and Irruputuncu

Journal of Petrology

The Journal of Petrology is a monthly peer-reviewed academic journal focused on the field of igneous and metamorphic petrology and petrogenesis.

See Ollagüe and Journal of Petrology

Journal of Volcanology and Geothermal Research

Journal of Volcanology and Geothermal Research is a scientific journal that publishes recent research on the fields of volcanology and geothermal activity, as well as the societal and environmental impact of these phenomenon.

See Ollagüe and Journal of Volcanology and Geothermal Research

Kaolinite

Kaolinite (also called kaolin) is a clay mineral, with the chemical composition: Al2Si2O5(OH)4.

See Ollagüe and Kaolinite

K–Ar dating

Potassium–argon dating, abbreviated K–Ar dating, is a radiometric dating method used in geochronology and archaeology.

See Ollagüe and K–Ar dating

Lake Tauca

Lake Tauca is a former lake in the Altiplano of Bolivia.

See Ollagüe and Lake Tauca

Land mine

A land mine, or landmine, is an explosive weapon concealed under or camouflaged on the ground, and designed to destroy or disable enemy targets, ranging from combatants to vehicles and tanks, as they pass over or near it.

See Ollagüe and Land mine

Landsat program

The Landsat program is the longest-running enterprise for acquisition of satellite imagery of Earth.

See Ollagüe and Landsat program

Landslide

Landslides, also known as landslips, or rockslides, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows.

See Ollagüe and Landslide

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 moon onto its surface.

See Ollagüe and Lava

Lava dome

In volcanology, a lava dome is a circular, mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano.

See Ollagüe and Lava dome

Lava lake

Lava lakes are large volumes of molten lava, usually basaltic, contained in a volcanic vent, crater, or broad depression.

See Ollagüe and Lava lake

Lineament

See also Line (geometry) A lineament is a linear feature in a landscape which is an expression of an underlying geological structure such as a fault.

See Ollagüe and Lineament

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.

See Ollagüe and List of volcanoes in Bolivia

List of volcanoes in Chile

The Smithsonian Institution's Global Volcanism Program lists 105 volcanoes in Chile that have been active during the Holocene.

See Ollagüe and List of volcanoes in Chile

Little Ice Age

The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region.

See Ollagüe and Little Ice Age

Llama

The llama (Lama glama) is a domesticated South American camelid, widely used as a meat and pack animal by Andean cultures since the pre-Columbian era.

See Ollagüe and Llama

Mafic

A mafic mineral or rock is a silicate mineral or igneous rock rich in magnesium and iron.

See Ollagüe and Mafic

Magma

Magma is the molten or semi-molten natural material from which all igneous rocks are formed.

See Ollagüe and Magma

Magma chamber

A magma chamber is a large pool of liquid rock beneath the surface of the Earth.

See Ollagüe and Magma chamber

Magnetite

Magnetite is a mineral and one of the main iron ores, with the chemical formula.

See Ollagüe and Magnetite

Mantle wedge

A mantle wedge is a triangular shaped piece of mantle that lies above a subducting tectonic plate and below the overriding plate.

See Ollagüe and Mantle wedge

Medicine Lake Volcano

Medicine Lake Volcano is a large shield volcano in northeastern California about northeast of Mount Shasta.

See Ollagüe and Medicine Lake Volcano

Metasomatism (from the Greek μετά metá "change" and σῶμα sôma "body") is the chemical alteration of a rock by hydrothermal and other fluids.

See Ollagüe and Metasomatism

Mining

Mining is the extraction of valuable geological materials and minerals from the surface of the Earth.

See Ollagüe and Mining

Miocene

The Miocene is the first geological epoch of the Neogene Period and extends from about (Ma).

See Ollagüe and Miocene

Monogenetic volcanic field

A monogenetic volcanic field is a type of volcanic field consisting of a group of small monogenetic volcanoes, each of which erupts only once, as opposed to polygenetic volcanoes, which erupt repeatedly over a period of time.

See Ollagüe and Monogenetic volcanic field

Moraine

A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet.

See Ollagüe and Moraine

Mount Mazama

Mount Mazama (Tum-sum-ne in the Native American language Klamath) is a complex volcano in the western U.S. state of Oregon, in a segment of the Cascade Volcanic Arc and Cascade Range.

See Ollagüe and Mount Mazama

National Geology and Mining Service

Santiago. The National Geology and Mining Service (Servicio Nacional de Geología y Minería; SERNAGEOMIN) is a Chilean government agency.

See Ollagüe and National Geology and Mining Service

Nazca Plate

The Nazca Plate or Nasca Plate, named after the Nazca region of southern Peru, is an oceanic tectonic plate in the eastern Pacific Ocean basin off the west coast of South America.

See Ollagüe and Nazca Plate

Nor Lípez Province

Nor Lípez is a province in the Bolivian department of Potosí.

See Ollagüe and Nor Lípez Province

Nuclear fallout

Nuclear fallout is the residual radioactive material propelled into the upper atmosphere following a nuclear blast, so called because it "falls out" of the sky after the explosion and the shock wave has passed.

See Ollagüe and Nuclear fallout

Olca

Olca is a stratovolcano on the border of Chile and Bolivia. Ollagüe and Olca are Bolivia–Chile border, International mountains of South America, Pleistocene stratovolcanoes, polygenetic volcanoes, Stratovolcanoes of Chile, volcanoes of Antofagasta Region and volcanoes of Potosí Department.

See Ollagüe and Olca

Oligocene

The Oligocene is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present (to). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain.

See Ollagüe and Oligocene

Olivine

The mineral olivine is a magnesium iron silicate with the chemical formula.

See Ollagüe and Olivine

Ollagüe, Chile

Ollagüe is a Chilean frontier village and commune in El Loa Province, Antofagasta Region.

See Ollagüe and Ollagüe, Chile

Opal

Opal is a hydrated amorphous form of silica (SiO2·nH2O); its water content may range from 3% to 21% by weight, but is usually between 6% and 10%.

See Ollagüe and Opal

Oral tradition

Oral tradition, or oral lore, is a form of human communication in which knowledge, art, ideas and culture are received, preserved, and transmitted orally from one generation to another.

See Ollagüe and Oral tradition

Paleozoic

The Paleozoic (or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon.

See Ollagüe and Paleozoic

Parasitic cone

A parasitic cone (also adventive cone or satellite cone) is the cone-shaped accumulation of volcanic material not part of the central vent of a volcano.

See Ollagüe and Parasitic cone

Parinacota (volcano)

Parinacota (in Hispanicized spelling), Parina Quta or Parinaquta is a dormant stratovolcano on the border of Bolivia and Chile. Ollagüe and Parinacota (volcano) are Bolivia–Chile border, International mountains of South America, Pleistocene stratovolcanoes, polygenetic volcanoes and Stratovolcanoes of Chile.

See Ollagüe and Parinacota (volcano)

Pelcoya Canton

Pelcoya is one of the cantons of the San Pedro de Quemes Municipality, the second municipal section of the Nor Lípez Province in the Potosí Department of Bolivia.

See Ollagüe and Pelcoya Canton

Peru–Chile Trench

The Peru–Chile Trench, also known as the Atacama Trench, is an oceanic trench in the eastern Pacific Ocean, about off the coast of Peru and Chile.

See Ollagüe and Peru–Chile Trench

Phenocryst

Swiss side of the Mont Blanc massif, has large white phenocrysts of plagioclase (that have trapezoid shapes when cut through). 1 euro coin (diameter 2.3 cm) for scale. A phenocryst is an early forming, relatively large and usually conspicuous crystal distinctly larger than the grains of the rock groundmass of an igneous rock.

See Ollagüe and Phenocryst

Phreatomagmatic eruption

Phreatomagmatic eruptions are volcanic eruptions resulting from interaction between magma and water.

See Ollagüe and Phreatomagmatic eruption

Plagioclase

Plagioclase is a series of tectosilicate (framework silicate) minerals within the feldspar group.

See Ollagüe and Plagioclase

Planchón-Peteroa

Planchón-Peteroa is a complex volcano extending in a north–south direction along the border between Argentina and Chile. Ollagüe and Planchón-Peteroa are International mountains of South America and polygenetic volcanoes.

See Ollagüe and Planchón-Peteroa

Pleistocene

The Pleistocene (often referred to colloquially as the Ice Age) is the geological epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations.

See Ollagüe and Pleistocene

Plinian eruption

Plinian eruptions or Vesuvian eruptions are volcanic eruptions marked by their similarity to the eruption of Mount Vesuvius in 79 AD, which destroyed the ancient Roman cities of Herculaneum and Pompeii.

See Ollagüe and Plinian eruption

Potassium

Potassium is a chemical element; it has symbol K (from Neo-Latin kalium) and atomic number19.

See Ollagüe and Potassium

Potassium nitrate

Potassium nitrate is a chemical compound with a sharp, salty, bitter taste and the chemical formula.

See Ollagüe and Potassium nitrate

Potosí Department

Potosí (Quechua: P'utuqsi; Aymara: Putusi) is a department in southwestern Bolivia.

See Ollagüe and Potosí Department

Proterozoic

The Proterozoic is the third of the four geologic eons of Earth's history, spanning the time interval from 2500 to 538.8Mya, the longest eon of the Earth's geologic time scale.

See Ollagüe and Proterozoic

Provinces of Chile

A province is a second-level administrative division in Chile.

See Ollagüe and Provinces of Chile

Pumice

Pumice, called pumicite in its powdered or dust form, is a volcanic rock that consists of extremely vesicular rough-textured volcanic glass, which may or may not contain crystals.

See Ollagüe and Pumice

Putana

In Hinduism, Pūtanā is a rakshasi (demoness), who was killed by the infant-god Krishna.

See Ollagüe and Putana

Pyroclastic flow

A pyroclastic flow (also known as a pyroclastic density current or a pyroclastic cloud) is a fast-moving current of hot gas and volcanic matter (collectively known as tephra) that flows along the ground away from a volcano at average speeds of but is capable of reaching speeds up to.

See Ollagüe and Pyroclastic flow

Pyroclastic rock

Pyroclastic rocks are clastic rocks composed of rock fragments produced and ejected by explosive volcanic eruptions.

See Ollagüe and Pyroclastic rock

Pyroxene

The pyroxenes (commonly abbreviated Px) are a group of important rock-forming inosilicate minerals found in many igneous and metamorphic rocks.

See Ollagüe and Pyroxene

Quartz

Quartz is a hard, crystalline mineral composed of silica (silicon dioxide).

See Ollagüe and Quartz

Radiometric dating

Radiometric dating, radioactive dating or radioisotope dating is a technique which is used to date materials such as rocks or carbon, in which trace radioactive impurities were selectively incorporated when they were formed.

See Ollagüe and Radiometric dating

Rhyolite

Rhyolite is the most silica-rich of volcanic rocks.

See Ollagüe and Rhyolite

Ruins

Ruins are the remains of a civilization's architecture.

See Ollagüe and Ruins

Salar de Ascotán

Salar de Ascotán, also known as Salar de Cebollar, is a salt flat in northern Chile. Ollagüe and Salar de Ascotán are volcanoes of Antofagasta Region.

See Ollagüe and Salar de Ascotán

Salar de Carcote

Salar de Carcote, also known as Salar de San Martín, is a salt flat in northern Chile.

See Ollagüe and Salar de Carcote

Salt pan (geology)

Natural salt pans or salt flats are flat expanses of ground covered with salt and other minerals, usually shining white under the sun.

See Ollagüe and Salt pan (geology)

San Pedro (Chile volcano)

San Pedro is a Holocene composite volcano in northern Chile and at in elevation one of the highest active volcanoes in the world. Ollagüe and San Pedro (Chile volcano) are Pleistocene stratovolcanoes, Stratovolcanoes of Chile and volcanoes of Antofagasta Region.

See Ollagüe and San Pedro (Chile volcano)

Scree

Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall.

See Ollagüe and Scree

Sector collapse

A sector collapse or lateral collapse is the structural failure and subsequent collapse of part of a volcano.

See Ollagüe and Sector collapse

Silicic acid

In chemistry, a silicic acid is any chemical compound containing the element silicon attached to oxide and hydroxyl groups, with the general formula or, equivalently,.

See Ollagüe and Silicic acid

Slab (geology)

In geology, the slab is a significant constituent of subduction zones.

See Ollagüe and Slab (geology)

Snow

Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes.

See Ollagüe and Snow

Snow line

The climatic snow line is the boundary between a snow-covered and snow-free surface.

See Ollagüe and Snow line

Solar irradiance

Solar irradiance is the power per unit area (surface power density) received from the Sun in the form of electromagnetic radiation in the wavelength range of the measuring instrument.

See Ollagüe and Solar irradiance

South America

South America is a continent entirely in the Western Hemisphere and mostly in the Southern Hemisphere, with a considerably smaller portion in the Northern Hemisphere.

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South American Plate

The South American Plate is a major tectonic plate which includes the continent of South America as well as a sizable region of the Atlantic Ocean seabed extending eastward to the African Plate, with which it forms the southern part of the Mid-Atlantic Ridge.

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Stratovolcano

A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra.

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Subduction

Subduction is a geological process in which the oceanic lithosphere and some continental lithosphere is recycled into the Earth's mantle at convergent boundaries.

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Suffix

In linguistics, a suffix is an affix which is placed after the stem of a word.

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Sulfur

Sulfur (also spelled sulphur in British English) is a chemical element; it has symbol S and atomic number 16.

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Tata Sabaya

Tata Sabaya is a high volcano in Bolivia. Ollagüe and Tata Sabaya are Five-thousanders of the Andes.

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Technical report

A technical report (also scientific report) is a document that describes the process, progress, or results of technical or scientific research or the state of a technical or scientific research problem.

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Tephra

Tephra is fragmental material produced by a volcanic eruption regardless of composition, fragment size, or emplacement mechanism.

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Thematic Mapper

A Thematic Mapper (TM) is one of the Earth observing sensors introduced in the Landsat program.

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Three Sisters (Oregon)

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Titanite

Titanite, or sphene, is a calcium titanium nesosilicate mineral, CaTiSiO5.

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Train station

A train station, railroad station, or railroad depot (mainly North American terminology) and railway station (mainly UK and other Anglophone countries) is a railway facility where trains stop to load or unload passengers, freight, or both.

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U-shaped valley

U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation.

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Ultra-prominent peak

An ultra-prominent peak, or ultra for short, is a mountain summit with a topographic prominence of or more; it is also called a P1500.

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Unconformity

An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous.

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Vitrophyre

A vitrophyre is a porphyritic volcanic rock in which phenocrysts are embedded in a glassy matrix.

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Volcanic arc

A volcanic arc (also known as a magmatic arc) is a belt of volcanoes formed above a subducting oceanic tectonic plate, with the belt arranged in an arc shape as seen from above.

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Volcanic bomb

A volcanic bomb or lava bomb is a mass of partially molten rock (tephra) larger than 64 mm (2.5 inches) in diameter, formed when a volcano ejects viscous fragments of lava during an eruption.

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Volcanic crater

A volcanic crater is an approximately circular depression in the ground caused by volcanic activity.

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Volcano

A volcano is a rupture 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.

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Wanaku (Potosí)

Wanaku (Quechua for guanaco, Hispanicized spelling Huanaco, Huanacu) is a mountain in the Andes of Bolivia, about high.

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War of the Pacific

The War of the Pacific (Guerra del Pacífico), also known as the Nitrate War (Guerra del salitre) and by multiple other names, was a war between Chile and a Bolivian–Peruvian alliance from 1879 to 1884.

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Water

Water is an inorganic compound with the chemical formula.

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Xenolith

A xenolith ("foreign rock") is a rock fragment (country rock) that becomes enveloped in a larger rock during the latter's development and solidification.

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Yeísmo

Yeísmo (literally "Y-ism") is a distinctive feature of certain dialects of the Spanish language, characterized by the loss of the traditional palatal lateral approximant phoneme (written) and its merger into the phoneme (written). It is an example of delateralization.

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Zircon

Zircon is a mineral belonging to the group of nesosilicates and is a source of the metal zirconium.

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1980 eruption of Mount St. Helens

On March27, 1980, a series of volcanic explosions and pyroclastic flows began at Mount St. Helens in Skamania County, Washington, United States.

See Ollagüe and 1980 eruption of Mount St. Helens

See also

Bolivia–Chile border

Volcanoes of Potosí Department

References

[1] https://en.wikipedia.org/wiki/Ollagüe

Also known as Ollaguee.

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