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Glacial landforms
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71	(Nanophanerophytic Montane Tundra) up near the treeline in this zone, where the climate is cold, wet, and windy, and soils are thin. Vegetation is confined to protected areas and thus covers less than 30 percent of the s Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 17:59:58 Antarctic ecozone Tundra Glacial landforms Antarctica Ice core Transantarctic Mountains Micropaleontology Greenland ice sheet West Antarctic Ice Sheet Physical geography Glaciology Ice sheets
72	The origin of the moraines between Griffin Nunatak and Brimstone Peak, southern Victoria Land TERESA M. MENSING, GUNTER FAURE, MATTHEW C. PLACE, and DAVID B. REED, Byrd Polar Research Center and Department of Geological Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 18:52:40 Physical geography Geology Elephant Moraine Reckling Moraine Glacial landforms Moraine Glacier Till Outpost Nunataks Glaciology Geography of Antarctica Sediments
73	pie rift basin to a marginal basin displaying the characteristics of the early stages of seafloor spreading (Jeffers, Anderson, and Lawyer in press). The scientific party of cruise VIII-86 included J.B. Anderson (chief s Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 07:41:27 Glacial landforms Earth Sediments Petrology Glacier Meltwater West Antarctic Ice Sheet Fjord Sea level Glaciology Geology Physical geography
74	anisotropically distributed about a nonvertical axis. Most experiments, except the long-refraction shooting, were carried out along three separate azimuths. Good receiver coverage on the long-refraction profile made it p Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 04:10:14 Glacial landforms Ice sheets Geochronology Bindschadler Ice Stream Whillans Ice Stream Glacier Dye 3 West Antarctic Ice Sheet Crevasse Physical geography Geography of Antarctica Glaciology
75	Study of grounding-line sedimentation processes at the Mackay Glacier tongue using a remotely operated vehicle Observations on the seafloor epibenthic community MICHAEL DAwBER and Ross D. POwELL, Department of Geology, Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 17:41:00 Glacial landforms Physical geography Scott Coast Glacier McMurdo Sound Transantarctic Mountains Anchor ice Sediment Geography of Antarctica Petrology Geology
76	Specific targets, especially those related to the sediments that lie immediately above the Kukri erosion surface, were examined in detail. Several areas were found where sedimentary beds in the lower Beacon Group showed Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 06:13:47 McMurdo Dry Valleys Climate history Ice ages Glacial landforms Transantarctic Mountains Glacier Antarctica Ice sheet Coral Ridge Physical geography Geography of Antarctica Glaciology
77	ships attempting passage to and from the southern Ross Sea. The Pennell and Ross Passage polynyas are best developed in spring and autumn, but also display intermittently lower ice concentrations during winter. They appe Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 16:30:37 Fjord Glaciology Lakes Continental shelf Antarctica McMurdo Sound Glacier Ross Sea Physical geography Glacial landforms Antarctic region
78	(figure 3). This unusual reversed temperature dependence with altitude clearly leads to the absence of colder ice below the surface. This absence and the basal heat generation create the peculiar situation that ice strea Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 18:57:16 Geochronology Ice core Incremental dating Water ice Antarctica Crevasse Bindschadler Ice Stream Whillans Ice Stream Glacier Physical geography Glaciology Glacial landforms
79 $Optical materials / Glacial landforms / Physical geography / Petroleum / Reflection seismology / Crevasse / Seismic refraction / Seismic wave / Ice / Geology / Geophysics / Glaciology$	fast ice-stream movement across the ice plain. Analysis of the character of the diffraction shows that the diffractor roughness must be on the order of a few meters vertically with slopes on the order of 10 percent and t Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 20:44:25 Optical materials Glacial landforms Physical geography Petroleum Reflection seismology Crevasse Seismic refraction Seismic wave Ice Geology Geophysics Glaciology
80	be located or acquired, the average velocities of many more glaciers could be calculated. The measured average glacier velocities compare closely, in most instances, with field measurements made of the same glaciers. In Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 16:28:51 Glacier Surge Ice sheet Antarctica Crevasse Retreat of glaciers since Physical geography Glaciology Glacial landforms

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