Daniell Peninsula: Difference between revisions

Content deleted Content added

Inline

Latest revision as of 06:44, 20 April 2024

Daniell Peninsula (72°50′S 169°35′E / 72.833°S 169.583°E / -72.833; 169.583) is the large peninsula between Cape Daniell and Cape Jones on the coast of Victoria Land, Antarctica. It is an elongated basalt dome similar to Adare Peninsula and Hallett Peninsula and rises to 2,000 metres (6,600 ft). It is partly separated from the Victory Mountains by Whitehall Glacier, which is afloat in its lower reaches, but is joined to these mountains by the higher land in the vicinity of Mount Prior. It was named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1957–58, after Cape Daniell, and by analogy with the Adare and Hallett peninsulas.^[1]

Geology

The Daniell Peninsula consists of at least four overlapping shield volcanoes that form part of the Hallett Volcanic Province of the McMurdo Volcanic Group.^[2]^[3] Mount Brewster forms the central portion of the Daniell Peninsula and rises to an elevation of 2,026 m (6,647 ft), forming the highest point on the peninsula.^[3] K–Ar or Rb–Sr dating has given an age of 12.4 ± 0.2 million years for Mount Brewster pantelleritic trachyte and an age of 6.9 ± 0.3 million years for Mount Brewster hawaiite lava.^[4]

A second shield volcano forming the southern end of the peninsula is deeply dissected by the Mandible Cirque. It contains the small satellite vent of Tousled Peak and the prominent ice-draped cone-like peak of Mount Lubbock.^[3] A dike cutting Mandible Cirque comenditic trachyte has given an age of 9.5 ± 0.1 million years.^[4]

The Cape Daniell shield volcano at the northern end of the Daniell Peninsula has an elevation of 1,910 m (6,270 ft), with its highest point being an unnamed peak. The summit area contains a flat region several kilometres wide that might be a small ice-filled caldera.^[3] Cape Daniell trachyte lava has an age of 5.8 ± 0.1 million years while Cape Daniell benmoreite lava has an age of 5.6 ± 0.5 million years.^[4]

Geography

The Daniell Peninsula extends along the west coast of the Ross Sea to the east of the Victory Mountains. The Borchgrevink Glacier flows down the southwestern coast of the peninsula, from which it is fed by the Langevad Glacier and the Bargh Glacier.^[5] Mount Prior looks over the point where the Humphries Glacier flowing southwest joins the Borchgrevink Glacier. The Humphries Glacier is saddled with the Whitehall Glacier, which flows north from below Mount Brewster along the east coast of the peninsula to enter Tucker Inlet at the north of the peninsula.^[6] Cape Jones is the southernmost point of the Peninsula. North of Cape Jones are Mount Lubbock, Touried Peak, Narrow Neck, the Mandible Cirque and Cape Phillips.^[5] Cape Daniell on the northeast of the peninsula marks the mouth of the Tucker Inlet, opposite Cape Wheatstone on the Hallett Peninsula to the north.^[6]

Features

Named features of the Daniell Peninsula include:

Mount Prior

72°58′S 168°47′E / 72.967°S 168.783°E / -72.967; 168.783. A mountain, 1,220 metres (4,000 ft) high, about 10 nautical miles (19 km; 12 mi) west of Mount Brewster, rising at the head of Whitehall Glacier in the west part of Daniell Peninsula. Named by New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1957–58, for George T. Prior of the Mineral Department, British Museum, who studied and analyzed the rocks obtained from this region by the British National Antarctic Expedition (BrNAE), 1901-04.^[7]

Mount Brewster

72°57′S 169°23′E / 72.950°S 169.383°E / -72.950; 169.383. A small peak, 2,025 metres (6,644 ft) high, that rises above the general level of the central part of Daniell Peninsula and marks its greatest elevation. Named in 1841 by Sir James Clark Ross for Sir David Brewster, Scottish physicist.^[8]

Cape Jones

73°17′S 169°13′E / 73.283°S 169.217°E / -73.283; 169.217. The cape lying immediately southeast of Mount Lubbock and marking the south tip of Daniell Peninsula. Discovered in January 1841 by Sir James Clark Ross who named it for Captain William Jones, Royal Navy.^[9]

Mount Lubbock

73°13′S 169°08′E / 73.217°S 169.133°E / -73.217; 169.133. A coastal peak, 1,630 metres (5,350 ft) high, rising immediately north of Cape Jones at the south end of Daniell Peninsula. Discovered in January 1841 by Sir James Clark Ross who named it for Sir John Lubbock, treasurer of the Royal Society.^[10]

Touried Peak

73°11′S 169°01′E / 73.183°S 169.017°E / -73.183; 169.017. Small ice-covered peak, 1,220 metres (4,000 ft) high, situated 3.5 nautical miles (6.5 km; 4.0 mi) northwest of the summit of Mount Lubbock in the south end of Daniell Peninsula, Victoria Land. The name given by New Zealand Antarctic Place Names Committee (NZ-APC) in 1966 is descriptive of the exceptionally broken ice summit.^[11]

Narrow Neck

73°06′S 169°03′E / 73.100°S 169.050°E / -73.100; 169.050. A narrow, but elevated isthmus or neck of land between Langevad Glacier and Mandible Cirque in the south part of Daniell Peninsula. The feature serves to join Tousled Peak and the Mount Lubbock vicinity to the main mass of Daniell Peninsula. The descriptive name was applied by NZ-APC in 1966.^[12]

Mandible Cirque

73°07′S 169°15′E / 73.117°S 169.250°E / -73.117; 169.250. A spectacular cirque indenting the coast of Daniell Peninsula 5 nautical miles (9.3 km; 5.8 mi) west-southwest of Cape Phillips. Named in 1966 by the NZ-APC for its appearance in plan and oblique views.^[13]

Cape Phillips

73°04′S 169°36′E / 73.067°S 169.600°E / -73.067; 169.600. A cape approximately midway along the east side of Daniell Peninsula, 8 nautical miles (15 km; 9.2 mi) southeast of Mount Brewster. Discovered in January 1841 by Sir James Clark Ross who named it for Lieutenant Charles G. Phillips of the Terror.^[14]

Cape Daniell

72°43′S 169°55′E / 72.717°S 169.917°E / -72.717; 169.917. A cape at the northeast extremity of Daniell Peninsula which marks the south side of the entrance to Tucker Inlet. Discovered, January 15, 1841, by Sir James Clark Ross who named it for Professor John Frederic Daniell, chemist of King's College, Cambridge University, and Foreign Secretary of the Royal Society.^[1]

References

^ ^a ^b Alberts 1995, p. 172.
^ Riffenburgh, Beau (2007). Encyclopedia of the Antarctic. Vol. 1. Taylor & Francis. p. 639. ISBN 978-0-415-97024-2.
^ ^a ^b ^c ^d Smellie, J. L.; Rocchi, S.; Armienti, P. (2011). "Late Miocene volcanic sequences in northern Victoria Land, Antarctica: products of glaciovolcanic eruptions under different thermal regimes". Bulletin of Volcanology. Springer: 4, 5. ISSN 0258-8900.
^ ^a ^b ^c "K/Ar and Rb/Sr dating of McMurdo Volcanic Group (north of Campbell Glacier)" (PDF). Geological Society of America. p. 1.
^ ^a ^b Coulman Island USGS.
^ ^a ^b Cape Hallet USGS.
^ Alberts 1995, p. 592.
^ Alberts 1995, pp. 92–93.
^ Alberts 1995, p. 376.
^ Alberts 1995, p. 446.
^ Alberts 1995, p. 755.
^ Alberts 1995, p. 517.
^ Alberts 1995, p. 458.
^ Alberts 1995, p. 573.

Sources

Alberts, Fred G., ed. (1995), Geographic Names of the Antarctic (PDF) (2 ed.), United States Board on Geographic Names, retrieved 2024-01-21 This article incorporates public domain material from websites or documents of the United States Board on Geographic Names.
Cape Hallet, USGS: United States Geological Survey, retrieved 2024-01-24
Coulman Island, USGS: United States Geological Survey, retrieved 2024-01-24

This article incorporates public domain material from websites or documents of the United States Geological Survey.

[FOOTNOTEAlberts1995172-1] Alberts 1995, p. 172.

[QH-2] Riffenburgh, Beau (2007). Encyclopedia of the Antarctic. Vol. 1. Taylor & Francis. p. 639. ISBN 978-0-415-97024-2.

[DP-3] Smellie, J. L.; Rocchi, S.; Armienti, P. (2011). "Late Miocene volcanic sequences in northern Victoria Land, Antarctica: products of glaciovolcanic eruptions under different thermal regimes". Bulletin of Volcanology. Springer: 4, 5. ISSN 0258-8900.

[CA-4] "K/Ar and Rb/Sr dating of McMurdo Volcanic Group (north of Campbell Glacier)" (PDF). Geological Society of America. p. 1.

[FOOTNOTECoulman_Island_USGS-5] Coulman Island USGS.

[FOOTNOTECape_Hallet_USGS-6] Cape Hallet USGS.

[FOOTNOTEAlberts1995592-7] Alberts 1995, p. 592.

[FOOTNOTEAlberts199592–93-8] Alberts 1995, pp. 92–93.

[FOOTNOTEAlberts1995376-9] Alberts 1995, p. 376.

[FOOTNOTEAlberts1995446-10] Alberts 1995, p. 446.

[FOOTNOTEAlberts1995755-11] Alberts 1995, p. 755.

[FOOTNOTEAlberts1995517-12] Alberts 1995, p. 517.

[FOOTNOTEAlberts1995458-13] Alberts 1995, p. 458.

[FOOTNOTEAlberts1995573-14] Alberts 1995, p. 573.

[1]

[2]

[3]

[4]

[5]

[6]

[7]

[8]

[9]

[10]

[11]

[12]

[13]

[14]

@@ Line 1: / Line 1: @@
+{{short description|Peninsula in Ross Dependency, Antarctica}}
-'''Daniell Peninsula''' ({{Coord|72|50|S|169|35|E|source:GNIS|display=inline,title}}) is the large peninsula between [[Cape Daniell]] and [[Cape Jones]] on the coast of [[Victoria Land]]. It is partly separated from the [[Victory Mountains]] by [[Whitehall Glacier]], which is afloat in its lower reaches, but is joined to these mountains by the higher land in the vicinity of [[Mount Prior]]. It was named by the [[New Zealand Geological Survey Antarctic Expedition]], 1957–58, after Cape Daniell, and by analogy with Adare and Hallett peninsulas.<ref>{{usgs-gazetteer|id=3505}}</ref>
+'''Daniell Peninsula''' ({{Coord|72|50|S|169|35|E|source:GNIS|display=inline,title}}) is the large peninsula between Cape Daniell and Cape Jones on the coast of [[Victoria Land]], Antarctica.
+It is an elongated basalt dome similar to [[Adare Peninsula]] and [[Hallett Peninsula]] and rises to {{convert|2,000|m}}.
+It is partly separated from the [[Victory Mountains]] by [[Whitehall Glacier]], which is afloat in its lower reaches, but is joined to these mountains by the higher land in the vicinity of Mount Prior. It was named by the [[New Zealand Geological Survey Antarctic Expedition]] (NZGSAE), 1957–58, after Cape Daniell, and by analogy with the [[Adare Peninsula|Adare]] and [[Hallett Peninsula|Hallett]] peninsulas.{{sfn|Alberts|1995|p=172}}
+{{TOC limit|2}}
 ==Geology==
-The peninsula is an elongated volcanic complex, consisting of at least four overlapping [[shield volcano]]es that form part of the Hallett Volcanic Province of the [[McMurdo Volcanic Group]].<ref name="QH">{{cite book|last1=Riffenburgh|first1=Beau|title=Encyclopedia of the Antarctic|publisher=[[Taylor & Francis]]|year=2007|page=639|volume=1|isbn=0-415-97024-5}}</ref><ref name="DP">{{cite journal|last1=Smellie|first1=J. L.|last2=Rocchi|first2=S.|last3=Armienti|first3=P.|title=Late Miocene volcanic sequences in northern Victoria Land, Antarctica: products of glaciovolcanic eruptions under different thermal regimes|journal=[[Bulletin of Volcanology]]|publisher=[[Springer Science+Business Media|Springer]]|year=2011|pages=4, 5|issn=0258-8900}}</ref> [[Mount Brewster (Antarctica)|Mount Brewster]] forms the central portion of the Daniell Peninsula and rises to an elevation of {{Convert|2026|m|ft|abbr=on}}, forming the highest point on the peninsula.<ref name="DP"/> [[K–Ar dating|K–Ar]] or [[Rubidium–strontium dating|Rb–Sr]] dating has given 12.4 ± 0.2 million years for Mount Brewster [[pantelleritic]] [[trachyte]] and 6.9 ± 0.3 million years for Mount Brewster [[hawaiite]] lava.<ref name="CA">{{cite web|url=https://www.geosociety.org/datarepository/1999/9954.pdf|title=K/Ar and Rb/Sr dating of McMurdo Volcanic Group (north of Campbell Glacier)|publisher=[[Geological Society of America]]|page=1}}</ref>
+The Daniell Peninsula consists of at least four overlapping [[shield volcano]]es that form part of the Hallett Volcanic Province of the [[McMurdo Volcanic Group]].<ref name="QH">{{cite book|last1=Riffenburgh|first1=Beau|title=Encyclopedia of the Antarctic|publisher=[[Taylor & Francis]]|year=2007|page=639|volume=1|isbn=978-0-415-97024-2}}</ref><ref name="DP">{{cite journal|last1=Smellie|first1=J. L.|last2=Rocchi|first2=S.|last3=Armienti|first3=P.|title=Late Miocene volcanic sequences in northern Victoria Land, Antarctica: products of glaciovolcanic eruptions under different thermal regimes|journal=[[Bulletin of Volcanology]]|publisher=[[Springer Science+Business Media|Springer]]|year=2011|pages=4, 5|issn=0258-8900}}</ref> Mount Brewster forms the central portion of the Daniell Peninsula and rises to an elevation of {{Convert|2026|m|ft|abbr=on}}, forming the highest point on the peninsula.<ref name="DP"/> [[K–Ar dating|K–Ar]] or [[Rubidium–strontium dating|Rb–Sr]] dating has given an age of 12.4 ± 0.2 million years for Mount Brewster [[pantelleritic]] [[trachyte]] and an age of 6.9 ± 0.3 million years for Mount Brewster [[hawaiite]] lava.<ref name="CA">{{cite web|url=https://www.geosociety.org/datarepository/1999/9954.pdf|title=K/Ar and Rb/Sr dating of McMurdo Volcanic Group (north of Campbell Glacier)|publisher=[[Geological Society of America]]|page=1}}</ref>
-A second shield volcano forming the southern end of the peninsula is deeply dissected by the [[Mandible Cirque]]. It contains the small satellite vent of [[Tousled Peak]] and the prominent ice-draped cone-like peak of [[Mount Lubbock]].<ref name="DP"/> A [[dike (geology)|dike]] cutting Mandible Cirque [[comenditic]] trachyte has given an age of 9.5 ± 0.1 million years.<ref name="CA"/>
+A second shield volcano forming the southern end of the peninsula is deeply dissected by the [[Mandible Cirque]]. It contains the small satellite vent of Tousled Peak and the prominent ice-draped cone-like peak of Mount Lubbock.<ref name="DP"/> A [[dike (geology)|dike]] cutting Mandible Cirque [[comenditic]] trachyte has given an age of 9.5 ± 0.1 million years.<ref name="CA"/>
 The Cape Daniell shield volcano at the northern end of the Daniell Peninsula has an elevation of {{Convert|1910|m|ft|abbr=on}}, with its highest point being an unnamed peak. The summit area contains a flat region several kilometres wide that might be a small ice-filled [[caldera]].<ref name="DP"/> Cape Daniell trachyte lava has an age of 5.8 ± 0.1 million years while Cape Daniell [[benmoreite]] lava has an age of 5.6 ± 0.5 million years.<ref name="CA"/>
+==Geography==
+[[File:C72189s1 Ant.Map Cape Hallet.jpg|thumb|North of peninsula in south of map]]
+[[File:C73189s1 Ant.Map Coulman Island.jpg|thumb|South of peninsula in north of map]]
+The Daniell Peninsula extends along the west coast of the [[Ross Sea]] to the east of the [[Victory Mountains]].
+The [[Borchgrevink Glacier]] flows down the southwestern coast of the peninsula, from which it is fed by the [[Langevad Glacier]] and the [[Bargh Glacier]].{{sfn|Coulman Island USGS}}
+Mount Prior looks over the point where the [[Humphries Glacier]] flowing southwest joins the Borchgrevink Glacier.
+The Humphries Glacier is saddled with the [[Whitehall Glacier]], which flows north from below Mount Brewster along the east coast of the peninsula to enter [[Tucker Inlet]] at the north of the peninsula.{{sfn|Cape Hallet USGS}}
+Cape Jones is the southernmost point of the Peninsula.
+North of Cape Jones are Mount Lubbock, Touried Peak, Narrow Neck, the Mandible Cirque and Cape Phillips.{{sfn|Coulman Island USGS}}
+Cape Daniell on the northeast of the peninsula marks the mouth of the Tucker Inlet, opposite [[Cape Wheatstone]] on the [[Hallett Peninsula]] to the north.{{sfn|Cape Hallet USGS}}
+==Features==
+Named features of the Daniell Peninsula include:
+===Mount Prior===
+{{coord|72|58|S|168|47|E}}.
+A mountain, {{convert|1,220|m}} high, about {{convert|10|nmi}} west of Mount Brewster, rising at the head of Whitehall Glacier in the west part of Daniell Peninsula.
+Named by [[New Zealand Geological Survey Antarctic Expedition]] (NZGSAE), 1957–58, for George T. Prior of the Mineral Department, British Museum, who studied and analyzed the rocks obtained from this region by the [[British National Antarctic Expedition]] (BrNAE), 1901-04.{{sfn|Alberts|1995|p=592}}
+===Mount Brewster===
+[[File:David Brewster 1618.jpg|thumb|David Brewster]]
+{{coord|72|57|S|169|23|E}}.
+A small peak, {{convert|2,025|m}} high, that rises above the general level of the central part of Daniell Peninsula and marks its greatest elevation.
+Named in 1841 by Sir [[James Clark Ross]] for Sir [[David Brewster]], Scottish physicist.{{sfn|Alberts|1995|pp=92–93}}
+===Cape Jones===
+{{coord|73|17|S|169|13|E}}.
+The cape lying immediately southeast of Mount Lubbock and marking the south tip of Daniell Peninsula.
+Discovered in January 1841 by Sir James Clark Ross who named it for Captain William Jones, Royal Navy.{{sfn|Alberts|1995|p=376}}
+===Mount Lubbock===
+{{coord|73|13|S|169|08|E}}.
+A coastal peak, {{convert|1,630|m}} high, rising immediately north of Cape Jones at the south end of Daniell Peninsula.
+Discovered in January 1841 by Sir James Clark Ross who named it for [[John Lubbock, 1st Baron Avebury|Sir John Lubbock]], treasurer of the Royal Society.{{sfn|Alberts|1995|p=446}}
+===Touried Peak===
+{{coord|73|11|S|169|01|E}}.
+Small ice-covered peak, {{convert|1,220|m}} high, situated {{convert|3.5|nmi}} northwest of the summit of Mount Lubbock in the south end of Daniell Peninsula, Victoria Land.
+The name given by [[New Zealand Antarctic Place Names Committee]] (NZ-APC) in 1966 is descriptive of the exceptionally broken ice summit.{{sfn|Alberts|1995|p=755}}
+===Narrow Neck===
+{{coord|73|06|S|169|03|E}}.
+A narrow, but elevated isthmus or neck of land between Langevad Glacier and Mandible Cirque in the south part of Daniell Peninsula.
+The feature serves to join Tousled Peak and the Mount Lubbock vicinity to the main mass of Daniell Peninsula.
+The descriptive name was applied by NZ-APC in 1966.{{sfn|Alberts|1995|p=517}}
+===Mandible Cirque===
+{{main|Mandible Cirque}}
+{{coord|73|07|S|169|15|E}}.
+A spectacular cirque indenting the coast of Daniell Peninsula {{convert|5|nmi}} west-southwest of Cape Phillips.
+Named in 1966 by the NZ-APC for its appearance in plan and oblique views.{{sfn|Alberts|1995|p=458}}
+===Cape Phillips===
+{{coord|73|04|S|169|36|E}}.
+A cape approximately midway along the east side of Daniell Peninsula, {{convert|8|nmi}} southeast of Mount Brewster.
+Discovered in January 1841 by Sir James Clark Ross who named it for Lieutenant Charles G. Phillips of the Terror.{{sfn|Alberts|1995|p=573}}
+===Cape Daniell===
+{{coord|72|43|S|169|55|E}}.
+A cape at the northeast extremity of Daniell Peninsula which marks the south side of the entrance to Tucker Inlet.
+Discovered, January 15, 1841, by Sir James Clark Ross who named it for Professor [[John Frederic Daniell]], chemist of King's College, Cambridge University, and Foreign Secretary of the Royal Society.{{sfn|Alberts|1995|p=172}}
 ==References==
 {{reflist}}
+==Sources==
-[[Category:Peninsulas of Antarctica]]
+{{refbegin}}
-[[Category:Landforms of Victoria Land]]
+*{{citation|url=https://pubs.usgs.gov/fedgov/70039167/report.pdf |accessdate=2024-01-21  |edition=2
+ |editor-last=Alberts |title=Geographic Names of the Antarctic |editor-first=Fred G.
+ |publisher=United States Board on Geographic Names |year=1995}}  {{Include-USGov |agency=United States Board on Geographic Names}}
+*{{citation |url=https://commons.wikimedia.org/wiki/File:C72189s1_Ant.Map_Cape_Hallet.jpg |accessdate=2024-01-24
+ |title=Cape Hallet |publisher=USGS: United States Geological Survey |ref={{harvid|Cape Hallet USGS}} }}
+*{{citation |url=https://commons.wikimedia.org/wiki/File:C73189s1_Ant.Map_Coulman_Island.jpg |accessdate=2024-01-24
+ |title=Coulman Island |publisher=USGS: United States Geological Survey |ref={{harvid|Coulman Island USGS}} }}
+{{refend}}
+{{Include-USGov |agency=United States Geological Survey}}
+[[Category:Peninsulas of Victoria Land]]
 [[Category:Borchgrevink Coast]]
 [[Category:Volcanoes of Victoria Land]]
-[[Category:Shield volcanoes]]
+[[Category:Miocene shield volcanoes]]
-[[Category:Miocene volcanoes]]
+[[Category:Shield volcanoes of Antarctica]]
-{{BorchgrevinkCoast-geo-stub}}