Antarctic geomorphological and glaciological 1:250000 map series:: Mount Murchison quadrangle, northern Victoria Land.: Explanatory notes

被引:15
作者
Baroni, C
Frezzotti, M
Salvatore, MC
Meneghel, M
Tabacco, IE
Vittuari, L
Bondesan, A
Biasini, A
Cimbelli, A
Orombelli, G
机构
[1] Univ Pisa, Dipartimento Sci Terra, I-56126 Pisa, Italy
[2] CNR, Ist Geosci & Georisorse, I-56100 Pisa, Italy
[3] ENEA, Progetto Clima, CR Casaccia, I-00060 Rome, Italy
[4] Univ Roma La Sapienza, Dipartimento Sci Terra, I-00185 Rome, Italy
[5] Univ Padua, Dipartimento Geografia G Morandini, I-35127 Padua, Italy
[6] Univ Milan, Dipartimento Sci Terra, Sez Geofis, I-20129 Milan, Italy
[7] Univ Bologna, DISART, I-40136 Bologna, Italy
[8] Univ Milan, Dipartimento Sci Ambiente & Terr, I-20126 Milan, Italy
来源
ANNALS OF GLACIOLOGY, VOL 39, 2004 | 2004年 / 39卷
关键词
D O I
10.3189/172756404781814131
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Geomorphological and glaciological features are represented on a georeferenced satellite image mosaic of the Mount Murchison quadrangle, northern Victoria Land, Antarctica (73-74 degrees S, 162-166 degrees 30'E), at a scale of 1:250000. Landforms and deposits of glacial and periglacial environments, forms related to mass wasting, wind action, weathering and geological structures are identified and mapped. The chronological sequence of landforms and deposits, morphography and lithology is also indicated. Glacier velocities (up to 180 m a(-1)) and ice-front fluctuations (1964-99) were determined by analysis of aerial photography and satellite imagery. Airborne radar surveys reveal that the greatest ice thickness (about 1500 m) is located in the grounding zone of Aviator Glacier. Up to 1000 m of ice bury the subglacial relief of Deception Plateau, Hercules Neve and the Deep Freeze Range. Snow accumulation rates (average = 170 kg m(-2) a(-1)) exhibit an overall negative correlation with altitude and distance from the coast. The relationships among relict erosional landforms and volcanic activity provide chronological constraints for the palaeogeographic evolution of this sector of the Transantarctic Mountains.
引用
收藏
页码:256 / 264
页数:9
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