Book Description

The ancient, boreal Eva forest forms the centerpiece in this evaluation of the time and nature of the enfironment during an interglaciation. This title brings together results of exmaination of hundreds of loess exposures, when loess faces were still frozen in gold-mining excavation, and data on the character and age of the deposits from fission-track dating of tphra, paleomagnetism of the loess, thermoluminescnece dating of loess, and radiocarbon dating by liquid scintillation. Dendrochronology studies of trees are compared to those from trees of the modern boreal forest.