McNeile Glacier [SEP] continent
McNeile Glacier
McNeile Glacier () is a glacier flowing northward along the east slopes of Klokotnitsa Ridge to the southeast side of Almond Point where it enters Charcot Bay just east of Borovan Knoll, on the west side of Graham Land, Antarctica. It was charted in 1948 by the Falkland Islands Dependencies Survey (FIDS) and named for S.St.C. McNeile, a surveyor at the FIDS Hope Bay base in 1948–49.
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