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Gamburtsev Mountain Range

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they are there; we've seen them under the ice. Not only are they similar in dimension to the European Alps, but they are also similar in aspect: we see very sharp peaks and valleys which are remarkably similar to the Alps themselves. It all adds to the mystery – from the tectonic perspective of how these mountains were created; and from the glacial history perspective of how the East Antarctic ice sheet was formed and didn't erode these peaks."
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The team's next goal is to drill through the ice and collect the first Gamburtsev rock samples. "Amazingly, we have samples of the moon but none of the Gamburtsevs," said Robin Bell, a geophysicist at Columbia University's Lamont–Doherty Earth Observatory. "With these rock samples we will be able to
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that picked up earthquake signals passing through the rock from the opposite side of the planet. Despite the extreme temperatures — around −30 °C at the two base camps as reported by AGAP US co-leader Dr Robin Bell — liquid water was detected in the valleys three kilometres beneath the team.
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Scientists announced the completion of their mission on 25 February 2009. Modern-day remote-sensing technology revealed a very jagged landscape. The gathered data will be analysed by researchers in the following months. Dr Fausto Ferraccioli from the British Antarctic Survey said: "We can confirm
302:. This early range was eroded above the surface but left a deep cold root, which is visible today in seismic images, reaching down into the Earth's mantle. About 250-100 million years ago, the crust started to pull apart in a series of rifting events close to the east of this old root. A forked 168:. It is approximately 1,200 kilometres (750 mi) long, and the mountains are believed to be about 2,700 metres (8,900 ft) high, although they are completely covered by over 600 metres (2,000 ft) of ice and snow. The Gamburtsev Mountain Range is about the same size as the European 318:. Further uplift still was achieved as deep valleys were later cut erosion lightening the overall mass of the system. Around 35 million years ago, the glaciers merged to form the East Antarctic Ice Sheet, burying the Gamburtsev Range in the process. 172:. As of 2008, it was unknown how the mountains were formed due to the lack of data. Studies conducted during the International Polar year demonstrated that ancient plate collisions produced a core that was rejuvenated in the early to mid-Mesozoic 298:
The result of the 2007–2009 study has found that the Gamburtsev are very old, first forming around a billion years ago when continental drift pushed two plates together to form the super-continent of
271:. The local gravitational and magnetic fields were also measured. 120,000 km were flown, with over 20% of the East Antarctic Ice Sheet being explored during the course of the mission. 737: 175:. The main features of the range formed before 34 million years ago, when the area was covered by the present ice sheet. Current models suggest that the 267:. Two field camps were established deep within the Antarctic interior and aircraft flew across the ice, mapping the shape of the sub-glacials using an 1106: 282:
By December, 2009, data analyzed so far from the AGAP project indicate the mountain range is generally oriented southwest to northeast, and arose from
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within it. This rifting warmed and rejuvenated the root, giving it the buoyancy to be lifted up to re-establish the mountains as an 800 km long
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Ferraccioli added: "Up until now we just had an ambitious plan. Now we have all this remarkable data to pore over."
227:, so called, the AGAP project was a multinational effort to gather information about the Gamburtsev mountain chain. 1207: 1121: 214: 151: 1202: 1085: 863: 784: 155: 1075: 705: 606:"Researchers Unravel Origins of Antarctica's Ice-Covered Mountains – the Earth Institute – Columbia University" 559:"U.S.-led, International Research Team Confirms Alps-like Mountain Range Exists under East Antarctic Ice Sheet" 420:"Dispatches from the Bottom of the Earth: An Antarctic Expedition in Search of Large Mountains Encased in Ice" 1065: 1027: 838: 248: 518:"The Gamburtsev Mountains: Integrated International Exploration of the Earths Most Enigmatic Mountain Range" 976: 906: 853: 826: 53: 1302: 1090: 1022: 911: 184: 487: 1172: 1157: 1116: 1080: 777: 749: 390:"20 лет открытию Полюса недоступности Антарктиды: Метеорология и Гидрология. 1979, №3. Гидрометеоиздат" 290:
constrain when this ancient piece of crust was rejuvenated and grew to a magnificent mountain range."
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was formed from the glaciers that began sliding down the Gamburtsev range at the end of the
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Heeszel, D.; Wiens, D.; Nyblade, A.; Hansen4, S.; Kanao, M.; An, M.; Zhao, Y. (2013).
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The Gamburtsev mountains and the origin and early evolution of the Antarctic Ice Sheet
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The AGAP project comprised scientists, engineers, pilots and support staff from
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Map of Antarctica, showing Dome A and the Gamburtsev Mountain Range
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runs along the northern side of the mountains containing lakes
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form an east extension of Gamburtsev Subglacial Mountains.
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Subglacial mountain range located in East Antarctica
1107:Council of Managers of National Antarctic Programs 411: 481: 1320: 515: 363:Australian Antarctic Data Centre (2000-01-01). 494:459, 690–693 (2009-06-04), accessed 2009-06-09 785: 738:A SciencePoles.org interview of Dr Robin Bell 676:"Gamburtsev 'ghost mountains mystery solved'" 579: 538: 337: 625:Journal of Geophysical Research: Solid Earth 417: 659:: CS1 maint: numeric names: authors list ( 792: 778: 644: 274:Information was recorded on a network of 667: 612: 504:Vostok Subglacial Highlands: Antarctica 394:Arctic and Antarctic Research Institute 218:Gamburtsev Mountain Range in Antarctica 14: 1321: 733:A BBC article about the mountain range 773: 573: 333: 331: 1298: 673: 674:Amos, Jonathan (17 November 2011). 551: 464:"'Ghost peaks' emerge from the ice" 24: 582:"Data to expose 'ghost mountains'" 541:"Expedition set for 'ghost peaks'" 509: 340:"Survey targets 'ghost' mountains" 328: 200: 154:. The range was discovered by the 25: 1345: 694: 365:"Gamburtsev Subglacial Mountains" 356: 1297: 1288: 1287: 1047: 757: 711:Lamont Doherty Earth Observatory 199: 192: 152:Southern Pole of Inaccessibility 598: 156:3rd Soviet Antarctic Expedition 133:Gamburtsev Subglacial Mountains 18:Gamburtsev Subglacial Mountains 799: 532: 516:Bryan C. Storey (2006-03-23). 497: 382: 13: 1: 1329:Mountain ranges of Antarctica 743:BBC article on recent results 716:Australian Antarctic Division 321: 230: 48:3,400 m (11,200 ft) 580:Jonathan Amos (2009-12-18). 539:Jonathan Amos (2008-10-14). 338:Jonathan Amos (2006-12-13). 146:, just underneath the lofty 7: 706:National Science Foundation 418:Robin E Bell (2008-11-12). 185:Vostok Subglacial Highlands 100:1,200 km (750 mi) 10: 1350: 1283: 1236: 1135: 1099: 1056: 1045: 1000: 949: 872: 807: 293: 158:in 1958 and is named for 129:Gamburtsev Mountain Range 117: 109: 104: 96: 91: 52: 42: 37: 33:Gamburtsev Mountain Range 32: 957:Antarctic/Southern Ocean 701:British Antarctic Survey 522:International Polar Year 225:International Polar Year 177:East Antarctic ice sheet 223:As part of the 2007–09 166:Grigoriy A. Gamburtsev 422:. 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Index

Gamburtsev Subglacial Mountains
Elevation
Coordinates
80°30′S 76°00′E / 80.500°S 76.000°E / -80.500; 76.000
subglacial
mountain range
East Antarctica
Dome A
Southern Pole of Inaccessibility
3rd Soviet Antarctic Expedition
Soviet
geophysicist
Grigoriy A. Gamburtsev
Alps

East Antarctic ice sheet
Eocene
Vostok Subglacial Highlands
Gamburtsev Mountain Range in Antarctica
class=notpageimage|
International Polar Year
Australia
Canada
China
Germany
Japan
United Kingdom
United States
ice-penetrating radar
seismometers

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