@ARTICLE{Wiśniewski_Edward_Moraines_1981,
 author={Wiśniewski, Edward},
 volume={vol. 2},
 number={No 1-2},
 journal={Polish Polar Research},
 pages={17-28},
 howpublished={online},
 year={1981},
 publisher={Polish Academy of Sciences},
 publisher={Committee on Polar Research},
 abstract={Ice-cored moraines are the only accumulation forms of Antarctic ice-sheet in the contact zone with Bunger Hills. Their longiness ranges from 3.5 km to 250 m, they are from 300 m to 30 m wide and their elevation oscillates between 10 and 5 m. A thickness of moraimc cover which lags the ice-core is changeable in the limit of 1 m. A process of decay of ice-cores, leading to deformations of their moraines, plays a small part up to now. It is caused a dry climate, probably, which was not favorable for the release and the work of melted waters in a large scale. The weak separation of ice-cored moraines results from a small amount of morainic material transported to the front of ice-sheet, probably as the ice-sheet is almost motionless. The granulometric analysis of morainic sediments shows their bad segregation.},
 type={Article},
 title={Moraines forms and deposits of Antarctic ice-sheet at the contact with Bunger Hills},
 URL={http://ochroma.man.poznan.pl/Content/111554/PDF-MASTER/1981_1-2_017-028.pdf},
 keywords={Antarctic, Bunger Hills, glacial geomorphology},
}