The Lanterman Range () is a mountain range about long and wide, forming the southwest part of the

Bowers Mountains __NOTOC__ Bowers Mountains () is a group of north–south trending mountains in Antarctica, about 145 km (90 mi) long and 56 km (35 mi) wide, bounded by the coast on the north and by the Rennick, Canham, Black and Lillie gla ...

in Antarctica. It is bounded by the

Rennick Glacier Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches ...

Sledgers Glacier Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches ...

Black Glacier Black Glacier () is a broad tributary to the Lillie Glacier flowing northeast, marking the southeast extent of the Bowers Mountains, a major mountain range situated in the geographical location of Victoria Land, Antarctica. The glacier was first ma ...

and

Canham Glacier Canham Glacier () is a tributary glacier about long which drains the northwest part of Evans Neve in Antarctica. The glacier drains northwest between the Alamein Range and the Salamander Range of the Freyberg Mountains and enters the Rennick Glaci ...

Exploration and naming

The range was mapped by

United States Geological Survey The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, ...

(USGS) from surveys and

United States Navy The United States Navy (USN) is the maritime service branch of the United States Armed Forces and one of the eight uniformed services of the United States. It is the largest and most powerful navy in the world, with the estimated tonnage ...

air photos, 1960–62. It was named by the United States

Advisory Committee on Antarctic Names The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established ...

(US-ACAN) for Commander William Lanterman, an aerological officer for U.S. Navy

Operation Deep Freeze Operation Deep Freeze (OpDFrz or ODF) is codename for a series of United States missions to Antarctica, beginning with "Operation Deep Freeze I" in 1955–56, followed by "Operation Deep Freeze II", "Operation Deep Freeze III", and so on. (There w ...

, 1959–62.

Location

The Lanterman Range lies to the east of the

and its tributary

. The

flows past its northeast end. The

MacKinnon Glacier Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches ...

drains the range to the north into Sledgers Glacier. Glaciers draining to the west include

Orr Glacier Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches ...

Linder Glacier Linder Glacier () is a steep tributary glacier in the Lanterman Range, Bowers Mountains, Antarctica. It drains the southern slopes of Mount Bernstein and moves south to enter Hunter Glacier. The glacier was mapped by the United States Geological ...

Hunter Glacier Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches ...

Hoshko Glacier The Crown Hills () are a group of peaks and hills forming the south-east part of the Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica. Lying between Zenith Glacier and Gambone Peak, and including All Black Peak, they rise to a ...

Zenith Glacier The Crown Hills () are a group of peaks and hills forming the south-east part of the Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica. Lying between Zenith Glacier and Gambone Peak, and including All Black Peak, they rise to a ...

and

Johnstone Glacier The Crown Hills () are a group of peaks and hills forming the south-east part of the Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica. Lying between Zenith Glacier and Gambone Peak, and including All Black Peak, they rise to a ...

. The

Molar Massif Molar Massif () is a large mountain massif immediately east of the Lanterman Range in the Bowers Mountains of Antarctica. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy air photos, 1960–1964. The descriptiv ...

lies to the east. The

Crown Hills Coleman is an electoral ward and administrative division of the city of Leicester, England, consisting of the Leicester suburbs of Crown Hills and North Evington. Geography Coleman is bounded by the wards of Charnwood to the west and north, ...

form the southeastern end of the range, standing above the

to the east.

Features

Features, from north to south, include:

Carnes Crag

. A rock crag, high, in the northwest extremity of Lanterman Range, overlooking the junction of Sledgers Glacier and the Rennick Glacier. Mapped by USGS from surveys and United States Navy air photos, 1960-62. Named by US-ACAN for James J. Carnes United States Navy, chief electrician's mate with the McMurdo Station winter party, 1967.

Mount Moody

. A peak high located southeast of Carnes Crag in northwestern Lanterman Range, Bowers Mountains. Named by the northern party of

New Zealand Geological Survey Antarctic Expedition The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957 ...

(NZGSAE), 1963-64, for Lieutenant Daniel M. Moody, United States Navy, of Squadron VX-6, who flew support flights for this New Zealand expedition.

Reilly Ridge

. Prominent rock ridge about long on the northeast side of Lanterman Range, Bowers Mountains. The ridge descends from the heights just east of Mount Bernstein and forms a part of the southwest wall of Sledgers Glacier. Mapped by USGS from ground surveys and United States Navy air photos, 1960-62. Named by US-ACAN for Commander Joseph L. Reilly, United States Navy, officer in charge of the winter support party at McMurdo Station. 1964.

Rowell Peak

. The highest peak high on Reilly Ridge. Named by the

New Zealand Antarctic Place-Names Committee New Zealand Antarctic Place-Names Committee (NZ-APC) is an adjudicating committee established to authorize the naming of features in the Ross Dependency on the Antarctic continent. It is composed of the members of the New Zealand Geographic Board pl ...

(NZ-APC) in 1983 after A.J. Rowell, geologist, a member of R.A. Cooper's NZARP geological party to the area, 1981-82.

Mount Bernstein

. A prominent mountain, high, which forms a part of the northern wall of Linder Glacier. Mapped by the USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for the late Captain Fred J. Bernstein, Assistant Chief of Staff for Operations and Plans, United States Navy Support Force, Antarctica, 1967 and 1968.

Gateway Hills

. A prominent pair of hills high immediately west of Husky Pass at the head of Sledgers Glacier. So named by the NZ-APC in 1983 on a proposal by geologist M.G. Laird because the hills bound the southern entrance to Sledgers Glacier.

Mount Lugering

. Mountain nearly high on the west side of Lanterman Range. It marks the north side of the terminus of Hunter Glacier where it joins Rennick Glacier. Mapped by USGS from ground surveys and United States Navy air photos, 1960-62. Named by US-ACAN for utilitiesman Donald R. Lugering, United States Navy, of the South Pole Station winter party, 1965.

References

Sources

* *

* Gunter Faure, Teresa M. Mensing,
The Transantarctic Mountains: Rocks, Ice, Meteorites and Water
', P 115 * G. Di Vincenzo, R. Palmeri, F. Talarico, P.A.M. Andriessen, G.A. Ricci,
Petrology and Geochronology of Eclogites from the Lanterman Range, Antarctica
', Journal of Petrology, Volume 38, Issue 10, October 1997, Pages 1391–1417, https://doi.org/10.1093/petroj/38.10.1391 * R. Palmeri, F.M. Talarico, C.A. Ricci,
Ultrahigh‐pressure metamorphism at the Lanterman Range (northern Victoria Land, Antarctica)
'', Geological JournalVolume46, Issue2‐3 Special Issue: Extreme metamorphism and continental dynamics: Guest Edited by M. Santosh, March ‐ June 2011, Pages 126–136, https://doi.org/10.1002/gj.1243 * Ruppel, Antonia; Läufer, Andreas; Crispini, Laura; Capponi, Giovanni; Lisker, Frank,
A high-resolution aeromagnetic survey over the Lanterman Range, northern Victoria Land, Antarctica
', 19th EGU General Assembly, EGU2017, proceedings from the conference held 23-28 April, 2017 in Vienna, Austria., p.14182 * Capponi, Giovanni & Crispini, Laura & Meccheri, Marco. (1999),
The metaconglomerates of the eastern Lanterman Range (northern Victoria Land, Antarctica): New constraints for their interpretation
', ANTARCTIC SCIENCE. 11. 217–227. https://doi.org/10.1017/S0954102099000280 * Kim, D., Kim, T., Lee, J. et al.,
Microfabrics of omphacite and garnet in eclogite from the Lanterman Range, northern Victoria Land, Antarctica
', Geosci J 22, 939–953 (2018) https://doi.org/10.1007/s12303-018-0055-7 * Ghiribelli, Barbara; Frezzotti, Maria-Luce; Palmeri, Rosaria,
Coesite in eclogites of the Lanterman Range (Antarctica): Evidence from textural and Raman studies
', European Journal of Mineralogy Volume 14 Number 2 (2002), p. 355 - 360, Mar 22, 2002, https://doi.org/10.1127/0935-1221/2002/0014-0355 * Christopher J. Adams,
Style of Uplift of Paleozoic Terranes in Northern Victoria Land, Antarctica: Evidence from K-Ar Age Patterns
', Fütterer, D K, Damaske, D, Kleinschmidt, G, Miller, H & Tessensohn, F (eds.), Antarctica: contributions to global earth sciences, Springer, Berlin, Heidelberg, New York, 45-54 http://dx.doi.org/10.1007/3-540-32934-X * J. D. Bradshaw, S. D. Weaver, M. G. Laird,

', CircumPacific Council for Energy and Mineral Resources 2008 – Tectonostratigrahic Terranes of the Circum-Pacific Region, Earth Science Series, Number 1, 1985. * Crispini, L.; Capponi, G.; Federico, L.; and Talarico, F., '
Gold bearing v Gold bearing veining link eining linked to transcrustal fault z anscrustal fault Zones in the ones in the Transantar ansantarctic Mountains (nor ctic Mountains (northern Vict thern Victoria Land, Antar oria Land, Antarctica)
'', (2007). Related Publications from ANDRILL Affiliates. 20. https://digitalcommons.unl.edu/andrillaffiliates/20 {{refend Mountain ranges of Victoria Land Pennell Coast