Earth and Planetary Sciences ETDs
Publication Date
5-1-2015
Abstract
The effects of large-scale landsliding on the continental-scale Colorado River system in Grand Canyon remain poorly understood. This paper describes deep-seated bedrock landslides in the Surprise Valley area by combining detailed mapping, volume-balanced cross-sections, strath terrace heights, and cosmogenic burial dating of river deposits buried by landslides. Mapping shows failures involving ~1000 m Paleozoic section localized within basal shale detachments, dammed and diverted the Colorado River and local tributaries, and forced the creation of epigenetic gorges. Restored cross-sections show pre-existing paleotopography in Surprise Valley possibly created by an older, through-flowing Colorado River. Two individual landslide segments dated to ~1 Ma with large errors via cosmogenic burial age dating. Detachment height, long-term bedrock incision rates, and structural relationships suggest major failures events occurred at 3 Ma, 1 Ma, <<1 Ma. Paleotopography, groundwater, and bedrock incision likely drove landsliding rather than lava-dammed lakes downstream based on geochronology.
Degree Name
Earth and Planetary Sciences
Level of Degree
Masters
Department Name
Department of Earth and Planetary Sciences
First Committee Member (Chair)
Huntoon, Peter
Second Committee Member
Crossey, Laura
Third Committee Member
Schmandt, Brandon
Project Sponsors
Geological Society of America, National Park Service, University of New Mexico Career Services, University of New Mexico Graduate and Professional Student Association
Language
English
Keywords
landsliding, Colorado River, Grand Canyon, cosmogenic burial age dating
Document Type
Thesis
Recommended Citation
Robertson, Jesse. "Deep-seated bedrock landsliding in Grand Canyon's Surprise Valley area." (2015). https://digitalrepository.unm.edu/eps_etds/72