Miller Range

Mountain range in Antarctica


title: "Miller Range" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["mountain-ranges-of-oates-land"] description: "Mountain range in Antarctica" topic_path: "general/mountain-ranges-of-oates-land" source: "https://en.wikipedia.org/wiki/Miller_Range" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Mountain range in Antarctica ::

::data[format=table title="Infobox mountain"]

FieldValue
photoFile:Miller Range, Antarctica - Searching for meteorites (2).jpg
photo_captionThe ANSMET team searches for meteorites on the blue ice field in the Miller Range 3 January 2016
mapAntarctica
native_name
native_name_lang
location
country_type
country
state
region
district
part
settlement_typeUse settlement_type= instead of city_type= (deprecated).
settlement
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| name = | other_name = | photo = File:Miller Range, Antarctica - Searching for meteorites (2).jpg | photo_size = | photo_upright = | photo_alt = | photo_caption = The ANSMET team searches for meteorites on the blue ice field in the Miller Range 3 January 2016 | map = Antarctica | highest = | highest_location = | elevation = | elevation_m = | elevation_ft = | elevation_ref = | elevation_system = | prominence = | prominence_m = | prominence_ft = | prominence_ref = | parent_peak = | isolation = | isolation_km = | isolation_mi = | isolation_parent = | isolation_ref = | listing = | coordinates = | coordinates_ref = | length = | length_km = | length_mi = | length_orientation = | length_ref = | width = | width_km = | width_mi = | width_orientation = | width_ref = | area = | area_km2 = | area_mi2 = | area_ref = | volume = | volume_km3 = | volume_mi3 = | volume_ref = | etymology = | nickname = | native_name = | native_name_lang = | translation = | pronunciation = | authority = | location = | country_type = | country = | state_type = | state = | region_type = | region = | district_type = | district = | part_type = | part = | settlement_type = Use settlement_type= instead of city_type= (deprecated). | settlement = | range_coordinates = | range_coordinates_ref = | range = | borders_on = | grid_ref_UK = | grid_ref_UK_ref = | grid_ref_Ireland = | grid_ref_Ireland_ref = | topo_maker = | topo_map = | biome = | formed_by = | orogeny = | age = | type = | geology = | volcanic_region = | volcanic_arc = | volcanic_belt = | volcanic_field = | volcanic_arc/belt = | last_eruption = | first_ascent = | easiest_route = | normal_route = | access = | embedded = | module = The Miller Range () is a mountain range extending south from Nimrod Glacier for 80 km along the western edge of the Marsh Glacier in Antarctica.

Name

The range is named for J.H. "Bob", now Sir Joseph Holmes Miller, a member of the New Zealand party of the Commonwealth Trans-Antarctic Expedition (1958) who, with G.W. Marsh, mapped this area.

Location

The Miller Range is in the Transantarctic Mountains to the east of the Ross Ice Shelf. It runs from north to south, and is about 80 km long and up to 30 km wide. The maximum elevation above the ice sheet is about 1700 m. There are signs of glaciation on the highest points of the range.

The Miller Range is separated by about 20 km from the adjacent ranges of the Transantarctic Mountains by the Nimrod and Marsh glaciers. The Marsh Glacier to the east and Nimrod Glacier to the west both flow north and converge just north of the range. The Queen Elizabeth Range is east of the Miller Range, on the other side of Marsh Glacier. The Cobham Range is to the northeast and the Geologists Range to the northwest, both on the other side of the Nimrod Glacier.

Geology

The Miller Range was part of the Mawson Continent. There is evidence that suggests that the Miller Range terrain was accreted to the GawlerAdélie Craton during the 1730–1690 Ma Kimban–Nimrod Orogeny, with a suture zone that may be at or near the location of the Nimrod Group.

The range is in the Beardmore-Nimrod Glacier area, which has a basement complex of igneous, metamorphic and sedimentary rocks. This is unconformably overlain by a thick sequence of sedimentary rocks, mostly from the Devonian to Triassic and of continental origin. The Miller Range differs from its neighbors in being composed only of the basement complex, which holds regional metamorphic rocks of the Nimrod Group, with Hope Granite intrusions. Metamorphic rocks of the Nimrod Group include mica schists, metaquartzites, banded gneisses, augen gneisses and marbles, all mostly derived from sedimentary sources, and amphibolites derived from basaltic rocks.

Glaciers

The Marsh Glacier lies to the east and Nimrod Glacier to the west, both of which flow north and converge just north of the range. Argo Glacier, which flows east into Marsh Glacier, divides the southern part of the range from the central part. Argosy Glacier, fed from the south by Ascent Glacier, also flows east into Marsh Glacier, and divides the central part of the range from the northern part. Skua Glacier and Astro Glacier flow northeast through the northern portion of the range into Marsh Glacier.

Cirques

Dike Cirque

Hockey Cirque

Strawberry Cirque

Southern section

::figure[src="https://upload.wikimedia.org/wikipedia/commons/c/c0/Miller_Range,Antarctica-_Snow_Machines.jpg" caption="Aboard snow machines, the team traverses a pass toward the blue ice field in the distance."] ::

The southern section is to the south of Argo Glacier.

Gerard Bluffs

Augen Bluffs

Isocline Hill

Orr Peak

Central section

::figure[src="https://upload.wikimedia.org/wikipedia/commons/c/c5/Miller_Range,Antarctica-_Moraines.jpg" caption="Blue ice field in the Miller Range, near the edge of a moraine."] ::

The Central section is between Argo Glacier and Argosy Glacier.

Milan Ridge

Greene Ridge

Martin Dome

Ong Valley

Macdonald Bluffs

Kreiling Mesa

Northern Section

The Northern section is to the north of Argosy Glacier.

Aurora Heights

Lookout Dome

Turner Hills

Tricorn Peak

Snowshoe Pass

Rust Bluff

Corner Nunatak

References

Sources

  • {{citation|url=https://pubs.usgs.gov/fedgov/70039167/report.pdf |accessdate=2023-12-03 |edition=2 |editor-last=Alberts |title=Geographic Names of the Antarctic |editor-first=Fred G. |publisher=United States Board on Geographic Names |year=1995}}
  • {{citation |url=https://core.ac.uk/download/pdf/159577711.pdf |accessdate=2023-12-12 |publisher=Institute of Polar Studies |last=Gunner |first=John D. |year=1969 |title=Petrography of Metamomorphic Rocks from the Miller Range, Antarctica}}
  • {{citation |url=https://commons.wikimedia.org/wiki/File:C83165s1_Ant.Map_Mount_Rabot.jpg |accessdate=2023-12-12 |title=Mount Rabot |publisher=USGS United States Geologic Survey |year=1960 |ref= }}
  • {{citation |doi=10.1144/SP323.16 |publisher=Geological Society, London |work=Special Publications |year=2009 |volume=323 |pages=319–355 |last1=Payne |first1=Justin L. |first2= Martin |last2=Hand |first3=Karin M. |last3=Barovich |first4=Anthony |last4=Reid |first5=David A. D. |last5=Evans |title=Correlations and reconstruction models for the 2500–1500 Ma evolution of the Mawson Continent|issue=1 |bibcode=2009GSLSP.323..319P }}

::callout[type=info title="Wikipedia Source"] This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page. ::

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