Hinton Glacier [SEP] continent
Hinton Glacier
Hinton Glacier () is a tributary glacier in the Britannia Range of Antarctica, flowing north between Forbes Ridge and Dusky Ridge into Hatherton Glacier. It was named by the Advisory Committee on Antarctic Names for U.S. Navy chief construction mechanic Clarence C. Hinton, Jr., who wintered at McMurdo Station in 1963, and headed a team charged with the maintenance of mechanical equipment at the outlying U.S. stations.
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