Glacial deposits

thumb|right|Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as matrix support, is diagnostic of till. thumb|right|Glacial till with tufts of grass thumb|Till after avalanche, Norway Till, or glacial till, is unsorted glacial sediment.

material of glacial origin

type of glaciomarine clay

thumb|300px|A dropstone of quartzite in layered [[rhythmite at Itu, Brazil]] Dropstones are isolated fragments of rock found within finer-grained water-deposited sedimentary rocks or pyroclastic beds. They range in size from small pebbles to boulders. The critical distinguishing feature is that there is evidence that they were not transported by normal water currents, but rather dropped in vertically through the air or water column, such as during a volcanic eruption.

geological formation