en.unionpedia.org

Mount Waesche, the Glossary

Index Mount Waesche

Mount Waesche is a mountain of volcanic origin at the southern end of the Executive Committee Range in Marie Byrd Land, Antarctica.[1]

Open in Google Maps

Table of Contents

  1. 67 relations: Aenigmatite, Aeolian processes, Antarctica, Argon–argon dating, Before Present, Benmoreite, Blue ice (glacial), Blue-ice area, Caldera, Cinder cone, Comendite, Crust (geology), Dike (geology), Drift (geology), Earthquake, Executive Committee Range, Feldspar, Fissure vent, Frost weathering, Glacial striation, Glacier, Granulite, Hawaiite, Holocene, Hyaloclastite, Ice core, Ilmenite, K–Ar dating, Lava, List of volcanoes in Antarctica, Magma, Mantle plume, Marie Byrd Land, Marie Byrd Land Volcanic Province, Moraine, Mount Berlin, Mount Hampton, Mount Sidley, Mount Takahe, Mugearite, Oligocene, Olivine, Pacific Ocean, Parasitic cone, Phenocryst, Plagioclase, Plio-Pleistocene, Pliocene, Pumice, Pyroxenite, ... Expand index (17 more) »

  2. Executive Committee Range
  3. Shield volcanoes of Antarctica
  4. Volcanoes of Marie Byrd Land

Aenigmatite

Aenigmatite, also known as cossyrite after Cossyra, the ancient name of Pantelleria, is a sodium, iron, titanium inosilicate mineral.

See Mount Waesche and Aenigmatite

Aeolian processes

Aeolian processes, also spelled eolian, pertain to wind activity in the study of geology and weather and specifically to the wind's ability to shape the surface of the Earth (or other planets).

See Mount Waesche and Aeolian processes

Antarctica

Antarctica is Earth's southernmost and least-populated continent.

See Mount Waesche and Antarctica

Argon–argon dating

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

See Mount Waesche and Argon–argon dating

Before Present

Before Present (BP) or "years before present (YBP)" is a time scale used mainly in archaeology, geology, and other scientific disciplines to specify when events occurred relative to the origin of practical radiocarbon dating in the 1950s.

See Mount Waesche and Before Present

Benmoreite

Benmoreite is a volcanic rock of intermediate composition.

See Mount Waesche and Benmoreite

Blue ice (glacial)

Blue ice occurs when snow falls on a glacier, is compressed, and becomes part of the glacier.

See Mount Waesche and Blue ice (glacial)

Blue-ice area

A blue-ice area is an ice-covered area of Antarctica where wind-driven snow transport and sublimation result in net mass loss from the ice surface in the absence of melting, forming a blue surface that contrasts with the more common white Antarctic surface.

See Mount Waesche and Blue-ice area

Caldera

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

See Mount Waesche and Caldera

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 Mount Waesche and Cinder cone

Comendite

Comendite is a hard, peralkaline igneous rock, a type of light blue grey rhyolite.

See Mount Waesche and Comendite

Crust (geology)

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

See Mount Waesche and Crust (geology)

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 Mount Waesche and Dike (geology)

Drift (geology)

In geology, drift is a name for all sediment (clay, silt, sand, gravel, boulders) transported by a glacier and deposited directly by or from the ice, or by glacial meltwater.

See Mount Waesche and Drift (geology)

Earthquake

An earthquakealso called a quake, tremor, or tembloris the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves.

See Mount Waesche and Earthquake

Executive Committee Range

The Executive Committee Range is a range consisting of five major volcanoes, which trends north-south for along the 126th meridian west, in Marie Byrd Land, Antarctica. Mount Waesche and Executive Committee Range are volcanoes of Marie Byrd Land.

See Mount Waesche and Executive Committee Range

Feldspar

Feldspar (sometimes spelled felspar) is a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium.

See Mount Waesche and Feldspar

Fissure vent

A fissure vent, also known as a volcanic fissure, eruption fissure or simply a fissure, is a linear volcanic vent through which lava erupts, usually without any explosive activity.

See Mount Waesche and Fissure vent

Frost weathering

Frost weathering is a collective term for several mechanical weathering processes induced by stresses created by the freezing of water into ice.

See Mount Waesche and Frost weathering

Glacial striation

Glacial striations or striae are scratches or gouges cut into bedrock by glacial abrasion.

See Mount Waesche and Glacial striation

Glacier

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

See Mount Waesche and Glacier

Granulite

Granulites are a class of high-grade metamorphic rocks of the granulite facies that have experienced high-temperature and moderate-pressure metamorphism.

See Mount Waesche and Granulite

Hawaiite

Hawaiite is an olivine basalt with a composition between alkali basalt and mugearite.

See Mount Waesche and Hawaiite

Holocene

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

See Mount Waesche and Holocene

Hyaloclastite

Hyaloclastite is a volcanoclastic accumulation or breccia consisting of glass (from the Greek hyalus) fragments (clasts) formed by quench fragmentation of lava flow surfaces during submarine or subglacial extrusion.

See Mount Waesche and Hyaloclastite

Ice core

An ice core is a core sample that is typically removed from an ice sheet or a high mountain glacier.

See Mount Waesche and Ice core

Ilmenite

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

See Mount Waesche and Ilmenite

K–Ar dating

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

See Mount Waesche and K–Ar dating

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 Mount Waesche and Lava

List of volcanoes in Antarctica

This is a list of volcanoes in Antarctica.

See Mount Waesche and List of volcanoes in Antarctica

Magma

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

See Mount Waesche and Magma

Mantle plume

A mantle plume is a proposed mechanism of convection within the Earth's mantle, hypothesized to explain anomalous volcanism.

See Mount Waesche and Mantle plume

Marie Byrd Land

Marie Byrd Land (MBL) is an unclaimed region of Antarctica.

See Mount Waesche and Marie Byrd Land

Marie Byrd Land Volcanic Province

The Marie Byrd Land Volcanic Province is a volcanic field in northern Marie Byrd Land of West Antarctica, consisting of over 18 large shield volcanoes, 30 small volcanic centres and possibly many more centres buried under the West Antarctic Ice Sheet. Mount Waesche and Marie Byrd Land Volcanic Province are volcanoes of Marie Byrd Land.

See Mount Waesche and Marie Byrd Land Volcanic Province

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 Mount Waesche and Moraine

Mount Berlin

Mount Berlin is a glacier-covered volcano in Marie Byrd Land, Antarctica, from the Amundsen Sea. Mount Waesche and Mount Berlin are Polygenetic shield volcanoes, shield volcanoes of Antarctica and volcanoes of Marie Byrd Land.

See Mount Waesche and Mount Berlin

Mount Hampton

Mount Hampton is a shield volcano with a circular ice-filled caldera. Mount Waesche and Mount Hampton are Executive Committee Range, Polygenetic shield volcanoes and volcanoes of Marie Byrd Land.

See Mount Waesche and Mount Hampton

Mount Sidley

Mount Sidley is the highest dormant volcano in Antarctica, a member of the Volcanic Seven Summits, the highest volcanoes on each of the seven continents, with a summit elevation of. Mount Waesche and Mount Sidley are Executive Committee Range, Polygenetic shield volcanoes, shield volcanoes of Antarctica and volcanoes of Marie Byrd Land.

See Mount Waesche and Mount Sidley

Mount Takahe

Mount Takahe is a snow-covered shield volcano in Marie Byrd Land, Antarctica, from the Amundsen Sea. Mount Waesche and Mount Takahe are Polygenetic shield volcanoes, shield volcanoes of Antarctica and volcanoes of Marie Byrd Land.

See Mount Waesche and Mount Takahe

Mugearite

Mugearite is a type of oligoclase-bearing basalt, comprising olivine, apatite, and opaque oxides.

See Mount Waesche and Mugearite

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 Mount Waesche and Oligocene

Olivine

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

See Mount Waesche and Olivine

Pacific Ocean

The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions.

See Mount Waesche and Pacific Ocean

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 Mount Waesche and Parasitic cone

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 Mount Waesche and Phenocryst

Plagioclase

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

See Mount Waesche and Plagioclase

Plio-Pleistocene

The Plio-Pleistocene is an informally described geological pseudo-period, which begins about 5 million years ago (Mya) and, drawing forward, combines the time ranges of the formally defined Pliocene and Pleistocene epochs—marking from about 5 Mya to about 12 kya.

See Mount Waesche and Plio-Pleistocene

Pliocene

The Pliocene (also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58 million years ago.

See Mount Waesche and Pliocene

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 Mount Waesche and Pumice

Pyroxenite

Pyroxenite is an ultramafic igneous rock consisting essentially of minerals of the pyroxene group, such as augite, diopside, hypersthene, bronzite or enstatite.

See Mount Waesche and Pyroxenite

Quartz

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

See Mount Waesche and Quartz

Radar

Radar is a system that uses radio waves to determine the distance (ranging), direction (azimuth and elevation angles), and radial velocity of objects relative to the site.

See Mount Waesche and Radar

Rhyolite

Rhyolite is the most silica-rich of volcanic rocks.

See Mount Waesche and Rhyolite

Roche moutonnée

In glaciology, a roche moutonnée (or sheepback) is a rock formation created by the passing of a glacier.

See Mount Waesche and Roche moutonnée

Ross Ice Shelf

The Ross Ice Shelf is the largest ice shelf of Antarctica (an area of roughly and about across: about the size of France).

See Mount Waesche and Ross Ice Shelf

Russell R. Waesche

Russell Randolph Waesche, Sr. (6 January 1886 – 17 October 1946) served as the eighth Commandant of the United States Coast Guard from 1936 to 1946, overseeing the service during World War II. He was the U.S. Coast Guard's longest serving commandant, having served ten years in that post. In addition, he was the first officer to hold the ranks of vice admiral and admiral within the Coast Guard.

See Mount Waesche and Russell R. Waesche

Scoria

Scoria is a pyroclastic, highly vesicular, dark-colored volcanic rock formed by ejection from a volcano as a molten blob and cooled in the air to form discrete grains called clasts.

See Mount Waesche and Scoria

Shield volcano

A shield volcano is a type of volcano named for its low profile, resembling a shield lying on the ground.

See Mount Waesche and Shield volcano

Solifluction

Solifluction is a collective name for gradual processes in which a mass moves down a slope ("mass wasting") related to freeze-thaw activity.

See Mount Waesche and Solifluction

Surface exposure dating

Surface exposure dating is a collection of geochronological techniques for estimating the length of time that a rock has been exposed at or near Earth's surface.

See Mount Waesche and Surface exposure dating

Tephra

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

See Mount Waesche and Tephra

Tuff

Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption.

See Mount Waesche and Tuff

Vitrophyre

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

See Mount Waesche and Vitrophyre

Volcanic ash

Volcanic ash consists of fragments of rock, mineral crystals, and volcanic glass, produced during volcanic eruptions and measuring less than 2 mm (0.079 inches) in diameter.

See Mount Waesche and Volcanic ash

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.

See Mount Waesche and Volcanic bomb

West Antarctic Ice Sheet

The West Antarctic Ice Sheet (WAIS) is the segment of the continental ice sheet that covers West Antarctica, the portion of Antarctica on the side of the Transantarctic Mountains that lies in the Western Hemisphere.

See Mount Waesche and West Antarctic Ice Sheet

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.

See Mount Waesche and Xenolith

See also

Executive Committee Range

Shield volcanoes of Antarctica

Volcanoes of Marie Byrd Land

References

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

, Quartz, Radar, Rhyolite, Roche moutonnée, Ross Ice Shelf, Russell R. Waesche, Scoria, Shield volcano, Solifluction, Surface exposure dating, Tephra, Tuff, Vitrophyre, Volcanic ash, Volcanic bomb, West Antarctic Ice Sheet, Xenolith.