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Moraines
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#	Item
1	http://www.progeo.org.se NOOld harbour area in the Kvarken area. Glasioisostatic uplift causes change in harbour location. De Geer moraines give complex and shallow waters to navigate. Photo: Lars Erikstad. Add to Reading List Source URL: www.progeo.se Language: English - Date: 2009-12-29 05:23:44 Geology Earth Planetary science Geoheritage UNESCO Science Geotourism Geopark Site of Special Scientific Interest Miass
2	LICHENOMETRIC DATING OF LITTLE ICE AGE GLACIER MORAINES USING EXPLICIT DEMOGRAPHIC MODELS OF LICHEN COLONIZATION, GROWTH, AND SURVIVAL MICHAEL G. LOSO1, DANIEL F. DOAK2 and ROBERT S. ANDERSON3 1 Add to Reading List Source URL: doaklab.org Language: English - Date: 2015-10-12 23:46:32 Lichens Biology Nature Tree of life biology) Lichenometry Lichen Crustose lichen Fruticose lichen Rhizocarpon Moraine
3	9 recessional moraine The photos show recessional moraines Add to Reading List Source URL: popefarmconservancy.org - Date: 2013-05-05 20:45:20
4	3 Most moraines are formed by a combination of processes. Some rock debris is carried at the base of the ice and stacked at the ice margin. Other debris accumulates on the ice surface and slumps off Add to Reading List Source URL: popefarmconservancy.org Language: English - Date: 2013-05-05 20:45:19 Glacial landforms Geology Alpinism Glacier Moraines Washboard moraine Glacial history of Minnesota Glaciology Sediments Physical geography
5	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
6	References Faure, C., M. L. Kalistrom, and T. M. MensingClassification and age of terrestrial boulders in the Elephant and Reckling moraines. Antarctic Journal of the U.S., 19(5):Faure, C. and K. S. Taylo Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 19:39:40 Ross Dependency Pennell Coast Transantarctic Mountains Antarctica Fowlie Glacier Lawrence Peaks Geography of Antarctica Physical geography Borchgrevink Coast
7	Classification and age of terrestrial boulders in the Elephant and Reckling Moraines C. FAURE, M. L. KALLSTROM, and T. M. MENSING Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 04:08:33 Elephant Moraine Glaciology Reckling Moraine Moraine Transantarctic Mountains Meteorite Allan Hills Glacier Antarctica Physical geography Geography of Antarctica Geography
8	ice, outlet glacier terminus, etc.), areas of bedrock and blue ice, and other glaciological features (medial moraines, crevasse areas, etc.) (Scientific Committee on Antarctic ResearchA more accurate delineation Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 05:01:48 Antarctica Continents Poles Plate tectonics Ice sheet Ice age Pole shift hypothesis Antarctic Physical geography Glaciology Antarctic region
9	High-titanium basalt and dolerite clasts from the Elephant and Reckling moraines 6 5 Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 20:38:42 Reckling Moraine Elephant Moraine Pennell Coast Diabase Basalt Transantarctic Mountains Pain Mesa Geography of Antarctica Petrology Igneous petrology
10	boulders beyond the Ross I and Alpine I drift limits but within the Taylor III drift limit of Denton et al, figure 3) are grussified, cavernously weathered, and wind faceted. Stones on moraines above (and thus old Add to Reading List Source URL: s3.amazonaws.com Language: English - Date: 2011-05-06 05:15:43 Geography Glacier Transantarctic Mountains Antarctica Ice age McMurdo Dry Valleys Ice sheet Valley Subglacial channel Physical geography Glaciology Geography of Antarctica

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