Fracture density and grain size controls on the relief structure of bedrock landscapes-Reference-Cited by-同舟云学术

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Fracture density and grain size controls on the relief structure of bedrock landscapes

Published:2018-02-23 Issue:5 Volume:46 Page:399-402
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:

Author:

DiBiase Roman A.¹²,Rossi Matthew W.³,Neely Alexander B.¹

Affiliation:

1. Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA

2. Earth and Environmental Systems Institute, Pennsylvania State University, University Park, Pennsylvania 16802, USA

3. Earth Lab, University of Colorado, Boulder, Colorado 80309, USA

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/geology/article-pdf/46/5/399/4134047/399.pdf

Reference32 articles.

1. Functional relationships between denudation, relief, and uplift in large, mid-latitude drainage basins;Ahnert;American Journal of Science,1970

2. Attal, M., Mudd, S.M., Hurst, M.D., Weinman, B., Yoo, K., and Naylor, M., 2015, Impact of change in erosion rate and landscape steepness on hillslope and fluvial sediments grain size in the Feather River basin (Sierra Nevada, California): Earth Surface Dynamics, v. 3, p. 201–222, https://doi.org/10.5194/esurf-3-201-2015.

3. Clarke, B.A., and Burbank, D.W., 2011, Quantifying bedrock-fracture patterns within the shallow subsurface: Implications for rock mass strength, bedrock landslides, and erodibility: Journal of Geophysical Research: Earth Surface, v. 116, F04009,https://doi.org/10.1029/2011JF001987.

4. Geologic map of the San Jacinto Peak quadrangle, Riverside County, California;Dibblee,2007

5. Hillslope response to tectonic forcing in threshold landscapes;DiBiase;Earth Surface Processes and Landforms,2012

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