The Ellsworth Mountains are the highest
mountain range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have aris ...
s in
Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean (also known as the Antarctic Ocean), it contains the geographic South Pole. ...
, forming a long and wide chain of
mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher t ...
s in a north to south configuration on the western margin of the
Ronne Ice Shelf in
Marie Byrd Land. They are bisected by
Minnesota Glacier to form the
Sentinel Range to the north and the
Heritage Range to the south. The former is by far the higher and more spectacular with
Mount Vinson () constituting the highest point on the continent.
[Bockheim, J.G., Schaefer, C.E., 2015. ''Soils of Ellsworth Land, the Ellsworth Mountains''. In: Bockheim, J.G. (Ed.), ''The Soils of Antarctica. World Soils Book Series'', Springer, Switzerland, pp. 169–181.] The mountains are located within the
Chilean Antarctic territorial claim but outside of the
Argentinian and
British ones.
Discovery
The mountains were discovered on November 23, 1935, by the American explorer
Lincoln Ellsworth
Lincoln Ellsworth (May 12, 1880 – May 26, 1951) was an American polar explorer, engineer, surveyor, and author. He led the first Arctic and Antarctic air crossings.
Early life
Linn Ellsworth was born in Chicago, Illinois on May 12, 1880. His ...
in the course of a trans-Antarctic flight from
Dundee Island
Dundee Island () is an ice-covered island lying east of the northeastern tip of the Antarctic Peninsula and south of Joinville Island, Antarctica.
Location
Dundee Island is in the Joinville Island group in Graham Land.
It is south of Joinvi ...
to the
Ross Ice Shelf. He gave them the descriptive name Sentinel Range.
[
The mountains were mapped in detail by the U.S. Geological Survey from ground surveys and U.S. Navy aerial photography, 1958–1966. When it became evident that the mountains comprise two distinct ranges, the US-ACAN restricted the application of Sentinel Range to the high northern one and gave the name Heritage Range to the southern one; the Committee recommended the name of the discoverer for this entire group of mountains.][
]
Geology
Geologically, the Ellsworth Mountains occupy a discrete block of continental crust
Continental crust is the layer of igneous, metamorphic, and sedimentary rocks that forms the geological continents and the areas of shallow seabed close to their shores, known as '' continental shelves''. This layer is sometimes called '' si ...
known as the Ellsworth-Whitmore Mountain terrane. This terrane was part of the early Paleozoic
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three Era (geology), geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma a ...
amalgamation of Gondwana
Gondwana ( ; ) was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia (continent), Australia, Zea ...
and consists of a thick section of folded Cambrian
The Cambrian ( ) is the first geological period of the Paleozoic Era, and the Phanerozoic Eon. The Cambrian lasted 51.95 million years from the end of the preceding Ediacaran period 538.8 Ma (million years ago) to the beginning of the Ordov ...
–Permian
The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years, from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the s ...
strata
In geology and related fields, a stratum (: strata) is a layer of Rock (geology), rock or sediment characterized by certain Lithology, lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by v ...
, which accumulated on Grenville-age continental crust. It was likely once part of the Cape Fold Belt that was detached from southern Africa
Africa is the world's second-largest and second-most populous continent after Asia. At about 30.3 million km2 (11.7 million square miles) including adjacent islands, it covers 20% of Earth's land area and 6% of its total surfac ...
during the breakup of Gondwana and later incorporated into Antarctica.[Craddock, J.P., Schmitz, M.D., Crowley, J.L., Larocque, J., Pankhurst, R.J., Juda, N., Konstantinou, A. and Storey, B., 2017. ''Precise U-Pb zircon ages and geochemistry of Jurassic granites, Ellsworth-Whitmore terrane, central Antarctica''. ''Geological Society of America Bulletin'', 129(1-2), pp.118-136.]
The stratigraphy
Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks.
Stratigraphy has three related subfields: lithost ...
consists of the thick Early Cambrian-Middle Cambrian
Middle or The Middle may refer to:
* Centre (geometry), the point equally distant from the outer limits.
Places
* Middle (sheading), a subdivision of the Isle of Man
* Middle Bay (disambiguation)
* Middle Brook (disambiguation)
* Middle Creek (di ...
Heritage Group overlain by the thick Late Cambrian
The Furongian is the fourth and final Epoch (geology), epoch and Series (stratigraphy), series of the Cambrian. It lasted from to million years ago. It succeeds the Miaolingian series of the Cambrian and precedes the Lower Ordovician Tremadocia ...
-Devonian
The Devonian ( ) is a period (geology), geologic period and system (stratigraphy), system of the Paleozoic era (geology), era during the Phanerozoic eon (geology), eon, spanning 60.3 million years from the end of the preceding Silurian per ...
Crashsite Group; the thick Permo-Carboniferous Whiteout Conglomerate (black diamictite) from Gondawanaland glaciation; and the thick Permian
The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years, from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the s ...
Polarstar Formation consisting of black argillite
Argillite () is a fine-grained sedimentary rock composed predominantly of Friability, indurated clay particles. Argillaceous rocks are basically lithified muds and Pelagic sediment, oozes. They contain variable amounts of silt-sized particles. T ...
, siltstone, sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ...
, and coal. Within the Heritage Group is the Union Glacier Formation of ashflow tuff-lahar
A lahar (, from ) is a violent type of mudflow or debris flow composed of a slurry of Pyroclastic rock, pyroclastic material, rocky debris and water. The material flows down from a volcano, typically along a valley, river valley.
Lahars are o ...
deposits, the Hyde Glacier Formation of graywacke-argillite-conglomerate, the Drake Icefall Formation of black shales and marble, the Conglomerate Ridge Formation of conglomerate and quartzite, the Liberty Hills-Springer Peak-Frazier Ridge Formations of quartzite-argillite, and the Minaret Formation of marble. Within the Crashsite Group is the Howard Nunataks Formation of quartzites, the Mt. Liptak Formation of quartzites, and the Mount Wyatt Earp Formation of quartzites. Major deformation of the sedimentary rocks occurred during the Gondwanide orogeny, followed by later uplift.
Climate
Temperatures in the Ellsworth Mountains average around . The best time for expeditions is November through January, mid-summer in the Southern Hemisphere. Arranging an outing here is a difficult task, requiring either official scientific sponsorship or considerable financial resources.
Maps
Northern-Sentinel-Map.jpg , Northern Sentinel Range, USGS map
Vinson-Map.jpg , Central and southern Sentinel Range, USGS map
Union-Glacier.jpg , Northern Heritage Range, USGS map
Liberty-Hills.jpg , Southern Heritage Range, USGS map
Antarctic Digital Database (ADD).
Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly updated.
See also
* Ellsworth Subglacial Highlands
* Antarctic Ice Marathon
* Union Glacier Camp
* Pirrit Hills
Gallery
Vinson-Massif.jpg , The central part of the mountains with Vinson Plateau
Vinson Plateau is the summit plateau of Vinson Massif, Sentinel Range in Ellsworth Mountains, Antarctica. It extends for 9 km between Goodge Col and Hammer Col linking it to the north-central part of Sentinel Range to the north-northwest an ...
, NASA satellite image
Mount Gardner from SW by Christian Stangl (flickr).jpg , Mount Gardner
Mount Press, Ellsworth Mountains, Antarctica.jpg , Mount Press
Mount Shinn from North East by Christian Stangl (flickr).jpg , Mount Shinn
Mount Tyree (Antarctica) from East by Christian Stangl (flickr).jpg , Mount Tyree
File:Mount Vinson from NW at Vinson Plateau by Christian Stangl (flickr).jpg , Mount Vinson
References
External links
Geologic Map of the Ellsworth Mountains
Scientific Committee on Antarctic Research (SCAR)
Ellsworth Mountains.
SCAR Composite Gazetteer of Antarctica
{{Authority control
West Antarctica
Mountain ranges of Ellsworth Land
Filchner-Ronne Ice Shelf