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Date Permissions Signed
5-14-2018
Date of Award
Winter 1980
Document Type
Masters Thesis
Degree Name
Master of Science (MS)
Department
Geology
First Advisor
Easterbrook, Don J., 1935-
Second Advisor
Pevear, David R.
Third Advisor
Pessl, Fred
Fourth Advisor
Christman, Robert A.
Abstract
The Neoglacial fluctuations of two of Mt. Baker's alpine glaciers were studied by tephrochronologic, dendrochronologic, and relative dating methods coupled with detailed geologic mapping. The earliest recognizable advance of the Deming Glacier occurred prior to deposition of Mazama tephra and after the Vashon Stade of Fraser Glaciation. The oldest recognizable Holocene advance of the Deming Glacier occurred >800 years B.P. and 16th, 17th, 18th(?), early 19th, late 19th, and 20th centuries. The Neoglacial record for the Rainbow Glacier is poorly preserved due to modification by two historic rock-debris avalanches, but the 20th century moraines of the Rainbow and Deming Glaciers disclose a close synchronism in their fluctuations. Glacier fluctuations on Mt. Baker during the past 500 years are broadly synchronous with those of glacier fluctuations elsewhere in the Pacific Northwest.
Type
Text
Keywords
Neoglacial records, Neoglacial fluctuations, Demin Glacier, Rainbow Glacier
Publisher
Western Washington University
OCLC Number
1061314518
Subject – LCSH
Glaciers--Washington (State)--Baker, Mount; Moraines--Washington (State)--Baker, Mount
Geographic Coverage
Baker, Mount (Wash.)
Format
application/pdf
Genre/Form
masters theses
Language
English
Rights
Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without the author's written permission.
Recommended Citation
Fuller, Steven Richard, "Neoglaciation of Avalanche Gorge and the Middle Fork Nooksack River Valley Mt. Baker, Washington" (1980). WWU Graduate School Collection. 793.
https://cedar.wwu.edu/wwuet/793