Miller Glacier [SEP] continent
Miller Glacier
Miller Glacier is a glacier about wide, described by Griffith Taylor as a transection glacier lying in a transverse trough and connecting Cotton Glacier and Debenham Glacier in Victoria Land, Antarctica. It was discovered by the Western Geological Party, led by Taylor, of the British Antarctic Expedition, 1910–13, and was named by Taylor for M.J. Miller, Mayor of Lyttelton, and the shipwright who repaired the expedition vessel, "Terra Nova", prior to its voyage from New Zealand.
Eocene–Oligocene extinction event). The term Late Cenozoic Ice Age is used to include this early phase.
During this last glacial period there were alternating episodes of glacier advance and retreat. Within the last glacial period the Last Glacial Maximum was approximately 22,000 years ago. While the general pattern of global cooling and glacier advance was similar, local differences in the development of glacier advance and retreat make it difficult to compare the details from continent to continent (see picture of ice core data below for differences). Approximately 13,000