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CSUniversity San Bernardino

QUALITATIVE COMPARISON OF OFFSET SURFACES BETWEEN THE CENTRAL AND EASTERN GARLOCK FAULT

Abstract

dc:description.abstract

<p>The Garlock Fault consists of three distinct segments, known as western, central, and eastern, together reaching approximately 260 km from the San Andreas Fault to the southern end of Death Valley. Although published slip rates are available along the western and central Garlock Fault segments, little is currently known of the Garlock Fault earthquake history or slip rate farther east. Using LiDAR and satellite imagery, the central and eastern Garlock Fault segments were analyzed for visibly offset, fault-adjacent, geomorphic surfaces that may potentially be used for estimating slip rate. Qualitative methods of assessing preserved alluvial surface maturity were adapted and used to establish unit age categories. Qualitative comparisons of late Pleistocene-Holocene surfaces reveal that the total offset at sites along the eastern Garlock Fault are less than half that of sites of comparable age along the central Garlock Fault, suggesting a significant reduction in slip rate across the intersection of the Brown Mountain, Owl Lake, and Garlock Faults. Digitally-measured offsets and their age groups were plotted in order to achieve preliminary slip-rate estimates. The resulting plot shows an eastward decrease in late Pleistocene-Holocene slip rate at sites along the central and eastern Garlock Fault segments. The central Garlock Fault slip-rate estimate taken from Slate Range West and Slate Range East sites in Pilot Knob Valley is approximately 4.2 mm/yr, within the error (but on the low side) of previously published rates. The slip-rate estimate from the Quail Mountains site, at the easternmost extent of the central Garlock Fault, is approximately 2.7 mm/yr. The slip-rate estimate from the Avawatz section of the eastern Garlock Fault is approximately 1.0 mm/yr.</p>

Degree

thesis:*
Name thesis:degree_name
Master of Science in Earth and Environmental Sciences
Level thesis:degree_level
Thesis
Discipline thesis:degree_discipline
Geological Sciences
Year dc:date.available
2014

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Crane, Thomas M
Contributors dc:contributor
  • McGill, Sally

Subjects

dc:subject × 8

Identifiers

dc:identifier.*
Repository record dc:identifier
https://scholarworks.lib.csusb.edu/etd/119
OAI identifier oai:identifier
oai:scholarworks.lib.csusb.edu:etd-1133

Chain of custody

source
Harvested from
CSUniversity San Bernardino
Base URL
scholarworks.lib.csusb.edu/do/oai/
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
citation

Crane, Thomas M. QUALITATIVE COMPARISON OF OFFSET SURFACES BETWEEN THE CENTRAL AND EASTERN GARLOCK FAULT. Thesis thesis, 2014. https://scholarworks.lib.csusb.edu/etd/119