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Date Permissions Signed
2-27-2017
Date of Award
Winter 2017
Document Type
Masters Thesis
Degree Name
Master of Science (MS)
Department
Geology
First Advisor
Schermer, Elizabeth, 1959-
Second Advisor
Amos, Colin B.
Third Advisor
Sherrod, Brian Louis
Abstract
Significant uncertainty remains in how and where modest, distributed shortening is accommodated throughout the eastern Cascade Range in Washington State. Using lidar imagery, I identified a ~5 km long lineament in Swakane Canyon near Wenatchee, roughly coincident with a strand of the Entiat fault. Topographic profiles show the lineament is formed by a southwest-side-up break in slope with between 2 and 42 m of vertical separation of the ground surface. Trenching reveals deformed saprolite and colluvium consistent with southwest-side-up folding caused by blind reverse faulting at depth. Radiocarbon and luminescence dating combined with stratigraphic constraints suggest up to three Holocene earthquakes on the southern Entiat fault with an average vertical separation of ~0.7 m per event. A ground penetrating radar survey reveals up to 3.8 m of cumulative vertical separation of the basal trench unit, consistent with up to six earthquakes on this structure. Rupture of the 5 km fault segment in Swakane Canyon could produce an earthquake of M5.9 or M6.8 based on rupture length or average slip, respectively. Holocene earthquakes on the southern Entiat fault could suggest reactivation of the entire Entiat fault as well as other bedrock faults in the eastern Cascades. Low rates of strain accumulation, as indicated by GPS surface velocities, likely result in long earthquake recurrence intervals. Although active erosion and slow strain rates lead to a subdued geomorphic expression of recent deformation, this study shows that the Entiat fault is an active, seismogenic structure that should be considered in regional seismic hazard analyses.
Type
Text
DOI
https://doi.org/10.25710/as5f-hq18
Publisher
Western Washington University
OCLC Number
974917418
Subject – LCSH
Faults (Geology)--Washington (State), Eastern; Geology, Structural--Washington (State), Eastern; Plate tectonics--Washington (State), Eastern; Earthquake hazard analysis--Washington (State), Eastern
Geographic Coverage
Washington (State), Eastern
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.
Creative Commons License
This work is licensed under a Creative Commons Attribution-No Derivative Works 4.0 License.
Recommended Citation
Carlson, Benjamin M., "Holocene Fault Reactivation and Landscape Evolution in the Eastern Cascades, WA" (2017). WWU Graduate School Collection. 555.
https://cedar.wwu.edu/wwuet/555