Shackleton Range, Eastern Antarctica, Antarcticai
Regional Level Types | |
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Shackleton Range | Mountain Range |
Eastern Antarctica | Region |
Antarctica | Continent |
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Latitude & Longitude (WGS84):
80° 30' South , 25° 0' West
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:
The Shackleton Range is a mountain range in Antarctica. Rising at Holmes Summit to 1,875 metres (6,152 ft), it extends in an east-west direction for about 160 kilometres (99 mi) between the Slessor and Recovery glaciers.
The range was named after Sir Ernest Shackleton, leader of the British Imperial Trans-Antarctic Expedition (or "Shackleton's Expedition") of 1914-16.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
Mineral list contains entries from the region specified including sub-localities1 valid mineral.
Detailed Mineral List:
ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 Reference: Grew, E. S., and M. Halpern. 1979. Rubidium-strontium dates from the Shackleton Range Metamorphic Complex in the Mount Provender area, Shackleton Range, Antarctica. Journal of Geology, 87: 325-32. |
ⓘ 'Hornblende' Reference: Grew, E. S., and M. Halpern. 1979. Rubidium-strontium dates from the Shackleton Range Metamorphic Complex in the Mount Provender area, Shackleton Range, Antarctica. Journal of Geology, 87: 325-32. |
ⓘ Kyanite Formula: Al2(SiO4)O Reference: Grew, E. S., and M. Halpern. 1979. Rubidium-strontium dates from the Shackleton Range Metamorphic Complex in the Mount Provender area, Shackleton Range, Antarctica. Journal of Geology, 87: 325-32. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 9 - Silicates | |||
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ⓘ | Kyanite | 9.AF.15 | Al2(SiO4)O |
Unclassified Minerals, Rocks, etc. | |||
ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
ⓘ | 'Hornblende' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
O | Oxygen | |
O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
O | ⓘ Kyanite | Al2(SiO4)O |
F | Fluorine | |
F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Mg | Magnesium | |
Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Al | Aluminium | |
Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Al | ⓘ Kyanite | Al2(SiO4)O |
Si | Silicon | |
Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Si | ⓘ Kyanite | Al2(SiO4)O |
K | Potassium | |
K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Ti | Titanium | |
Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Fe | Iron | |
Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A)BRAUN, H.-M., KLEINSCHMIDT, G. & SPAETH, G. (1988): Strukturgeologie der Shackleton Range. Ber. Polarforsch. 58: 208-218.
BUGGISCH, W., KLEINSCHMIDT, G., KREUZER, H. & KRUMM, S. (1990): Stratigraphy, metamorphism and nappe-tectonics in the Shackleton Range (Antarctica). Geodät. geophys. Veröff. R. I, 15: 64-86.
BUGGISCH, W., KLEINSCHMIDT, G., HÖHNDORF, A. & POHL, J. (1994): Stratigraphy and facies of sediments and low-grade metasediments in the Shackleton Range, Antartica. Polarforsch. 63: 9-32.
KLEINSCHMIDT, G. & BUGGISCH, W. (1994): Plate-tectonic implications of the structure of the Shackleton Range. Polarforsch. 63: 57-62.
CLARKSON, P. et al. (Ed.: THOMSON, J.W. et al.) (1995): Geological map of the Shackleton Range, Antarctica. BAS GEOMAP Ser., Sheet 4, 1:250000, Cambridge (Brit. Antarct. Surv.).
TALARICO, F., HENJES-KUNST, F. & KLEINSCHMIDT, G., (1999): An ophiolitic complex in the northern Shackleton Range, Antarctica. In: EUG 10 StrasbourgMarch 28th - April 1st 1999. J. Conf. Abstr. 4 (1): 122.
TALARICO, F., KLEINSCHMIDT, G. & HENJES-KUNST, F. (1999): An ophiolitic complex in the northern Shackleton Range, Antarctica. Terra Antartica 6: 293-315.
TESSENSOHN, F., KLEINSCHMIDT, G. & BUGGISCH, W. (1999): Permo-Carboniferous glacial beds in the Shackleton Range, Antarctica. Terra Antartica 6: 337-344.
KLEINSCHMIDT, G., HENJES-KUNST, F., & TESSENSOHN, F. (2001): Nappe tectonics in the central Shackleton Range, Antarctica. Z. dt. Geol. Ges. 152: 227-248.
KROHNE, N., LISKER, F., KLEINSCHMIDT, G., KLÜGEL, A., LÄUFER, A., ESTRADA, S. & SPIEGEL, C. (2016): The Shackleton Range (East Antarctica): an alien block at the rim of Gondwana? Geol. Mag., 24 pp. doi:10.1017/0016756816001011.
Other Databases
Wikipedia: | https://en.wikipedia.org/wiki/Shackleton_Range |
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Wikidata ID: | Q1550766 |
Localities in this Region
- Eastern Antarctica
- Shackleton Range
Other Regions, Features and Areas containing this locality
Antarctic MeteoritesGroup of Meteorite Fall Locations
Antarctic PlateTectonic Plate
Antarctica
- Western Antarctica
- Transantarctic MountainsMountain Range
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