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'''[[Drift ice|Antarctic sea ice]]''' is the sea ice of the [[Southern Ocean]]. It extends far north in winter and retreats almost to the coastline each summer. Sea ice is frozen seawater that is usually less than a few meters thick. This is in contrast to [[Ice shelf|ice shelves]], which are formed by glaciers, float in the sea, and are up to a kilometer thick. There are two subdivisions of sea ice: fast ice, which is attached to land; and ice floes, which are not. Sea ice in the Southern Ocean melts from the bottom instead of from the surface like Arctic ice because it is covered in snow. As a result, melt ponds are rarely observed. On average, [[Antarctica|Antarctic]] sea ice is younger, thinner, warmer, saltier, and more mobile than Arctic sea ice. Due to its inaccessibility, it is not as well-studied as Arctic ice.
'''[[Quin Blackburn]]''' was a geologist on the First and Second Byrd Expeditions and leader of the geologic party that explored the [[Transantarctic Mountains]]. Blackburn served as a geologist and seaman—before—the mast on the [[Richard E. Byrd|First Byrd Expedition]] (1928-1930). During this expedition, Blackburn and 41 other explorers were forced to winter over in the Little America base due to their ship being stuck in the pack ice.


Westarctica's sea ice cover is highly seasonal, with very little ice in the austral summer, expanding to an area roughly equal to that of mainland [[Westarctica]] in the winter. It peaks during September, which marks the end of austral winter, and retreats to a minimum in February.
Undoubtedly, Quin Blackburn's most lasting contribution to [[Antarctic]] exploration was as the leader of the Second Byrd Expedition's Geologic Party (1933-1935). During this expedition, he led a three-man team on a 1,500 mile trek across [[Marie Byrd Land]], investigating the geology of the [[Queen Maud Mountains]] while also sledging the length of the [[Scott Glacier]] onto the Polar Plateau. His prowess as an explorer was evident by the fact that his team returned from their long polar traverse having gained weight. Blackburn copied [[Robert Falcon Scott]]'s system of traveling with and consuming a large team of dogs to ensure a steady supply of protein, fat, and Vitamin C during the expedition.


'''([[Drift ice|Full Article...]])'''
'''([[Quin Blackburn|Full Article...]])'''

Latest revision as of 15:25, 20 August 2025

Quin Blackburn.jpg

Quin Blackburn was a geologist on the First and Second Byrd Expeditions and leader of the geologic party that explored the Transantarctic Mountains. Blackburn served as a geologist and seaman—before—the mast on the First Byrd Expedition (1928-1930). During this expedition, Blackburn and 41 other explorers were forced to winter over in the Little America base due to their ship being stuck in the pack ice.

Undoubtedly, Quin Blackburn's most lasting contribution to Antarctic exploration was as the leader of the Second Byrd Expedition's Geologic Party (1933-1935). During this expedition, he led a three-man team on a 1,500 mile trek across Marie Byrd Land, investigating the geology of the Queen Maud Mountains while also sledging the length of the Scott Glacier onto the Polar Plateau. His prowess as an explorer was evident by the fact that his team returned from their long polar traverse having gained weight. Blackburn copied Robert Falcon Scott's system of traveling with and consuming a large team of dogs to ensure a steady supply of protein, fat, and Vitamin C during the expedition.

(Full Article...)