All the rock debris shown in the foreground of this photo constitutes ground moraine. The material was formerly beneath Grinnell Glacier. Debris in moraines ranges in size from fine silt, which we cannot see in this photo, to large boulders;
www.uwsp.edu/geo/faculty/lemke/alpine_glacial_glossary/... www.uwsp.edu/geo/faculty/lemke/alpine_glacial_glossary/landforms/groundmoraine.html
The Physical Environment ... Bouldery ground moraine, Canada; ... Ground moraine is glacial till deposited beneath a melting glacier.
www.uwsp.edu/geo/faculty/ritter/glossary/E_G/ground_mor... www.uwsp.edu/geo/faculty/ritter/glossary/E_G/ground_moraine.html
Moraine - Wikipedia, the free encyclopedia
A moraine is any glacially formed accumulation of unconsolidated glacial debris (soil and rock) which can occur in currently glaciated and formerly glaciated regions, such as those areas acted upon ...
en.wikipedia.org/wiki/Moraine
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Ground moraine is usually in the form of undulating plains having gently sloping swells, sags, and enclosed depressions. ... moraine de fond Source: Research Branch, 1976; Contact: Peter Schut...
sis.agr.gc.ca/cansis/glossary/ground_moraine.html sis.agr.gc.ca/cansis/glossary/ground_moraine.html
A post-glacial surficial sediment 0.3 to 3.6 m or more thick overlies the Cary till in central Iowa, and is usually separated from the till by a discontinuous, often weakly-expressed stone line. ... Title : SURFICIAL SEDIMENTS ON UNDULATING CARY GROUND MORAINE IN CENTRAL IOWA.
stinet.dtic.mil/oai/oai?verb=getRecord&metadataPrefix=h... stinet.dtic.mil/oai/oai?verb=getRecord&metadataPrefix=html&identifier=AD0666977
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They usually occur in areas once occupied by the ground moraine of a continental glacier. In length, they may extend up to 500 miles (800 km). However, they are seldom more tha 1,000 feet (303 meters) in width and 150 feet (45 meters) in height.
www.innvista.com/science/earth/geology/glacial.htm
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