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Peary, Robert (1898). Northward over the great ice : a narrative of life and work along the shores and upon the interior ice-cap of northern Greenland in the years 1886 and 1891-1897, with a description of the little tribe of Smith Sound Eskimos, the most northerly human beings in the world, and an account of the discovery and bringing home of the Saviksue or great Cape York meteorites.
Peary, Robert E. Northward Over the "Great Ice" A Narrative of Life and Work Along the Shores and Upon the Interior Ice-Cap of Northern Greenland in the Years 1886 and 1891-1897 : with a Description of the Little Tribe of Smith-Sound Eskimos, the Most Northerly Human Beings in the World, and an Account of the Discovery and Bringing Home of the ...
When the glacial ice receded northward, reaching the Olympia area, a low drainage was reached in the eastern Black Hills. Using the Black River as its primary drainage, Lake Russell came into existence was continued after the edge of the ice had withdrawn from the region.
This new storm will take a much more southern route across the Central states but could turn northward, ... snow and ice over portions of the southern Appalachians and an icy mix for the Piedmont ...
This occurred while the Laurentian Ice Sheet was at or south of the current Canada–US border. [1] As the ice sheet melted northward, an early Lake Agassiz covered southern Manitoba, the Minnesota and Ontario boundary country, and along the Red River south of Fargo, North Dakota. The Lockhart Phase is associated with the Herman lake stage (335 ...
Whenever mild and moist air flows over a zone of cold and dry air, dense fog can form and where the air remains cold enough, there will be some ice and snow concerns for travelers from the Great ...
Academy Glacier (Danish: Academy Gletscher or Academy Brae), is one of the major glaciers in northern Greenland. [1]It was named in 1892 after the Academy of Natural Sciences in Philadelphia by Robert Peary [2] during his expedition to north Greenland.
The Laurentide ice sheet (LIS) was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glaciation epochs, from 2.58 million years ago to the present.