It is named for Captain Carl Anton Larsen, the master of the Norwegian whaling vessel " Jason ", who sailed along the ice front as far as 68?0'South during December 1893.
32.
After the winter settled, the ice front between Color Air and Braathens grew colder following Braathens'denying Color Air to use their deicing equipment at �lesund, resulting in the plane being stuck at the airport.
33.
Variables used in models include properties of the ice such as thickness, density, temperature, c-axis fabric, impurity loading, though'ice front normal spreading stress', is likely the most important variable, however it is usually not measured.
34.
Ross mapped the ice front eastward to 160�W . In 1947, the US Board on Geographic Names applied the name "'Ross Shelf Ice "'to this feature and published it in the original US Antarctic Gazetteer.
35.
In 2002 the long floating terminus of the glacier entered a phase of rapid retreat, with the ice front breaking up and the floating terminus disintegrating and accelerating to a retreat rate of over per day.
36.
It was believed initially that during the moments immediately following the nucleation of the ice crystals, particles were ejected from the growing planar ice front, leading to the formation of a constitutionally super-cooled zone directly ahead of the growing ice.
37.
As the Erie Lobe of the glacier continued to retreat its meltwater was temporarily trapped between the ice front to the east and the Fort Wayne Moraine to the west, and formed proglacial Lake Maumee, the ancestor of modern Lake Erie.
38.
"' Cape Vestkapp "'( ) is a prominent westward projection of the ice front of the Riiser-Larsen Ice Shelf located midway along the ice front and about 60 nautical miles ( 110 km ) west of the Kraul Mountains, Queen Maud Land.
39.
"' Cape Vestkapp "'( ) is a prominent westward projection of the ice front of the Riiser-Larsen Ice Shelf located midway along the ice front and about 60 nautical miles ( 110 km ) west of the Kraul Mountains, Queen Maud Land.
40.
From a photograph taken by Mendenhall in the latter part of April, 1898, it is evident that the rock ledges were exposed beneath the middle of the ice front and the eastern half exhibited " the rough pinnacled front of a still-advancing stream.
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