Model:Bedrock Fault Scarp: Difference between revisions
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The model is described and illustrated in the following journal article: | The model is described and illustrated in the following journal article: | ||
Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:10.1029/2010JF001861. | Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:[http://dx.doi.org/10.1029/2010JF001861 10.1029/2010JF001861]. | ||
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{{Start model keyword table}} | {{Start model keyword table}} | ||
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|Describe processes represented by the model=Weathering and erosion of bedrock on a hillslope; vertical and horizontal displacement due to earthquakes. | |Describe processes represented by the model=Weathering and erosion of bedrock on a hillslope; vertical and horizontal displacement due to earthquakes. | ||
|Describe key physical parameters and equations=See: | |Describe key physical parameters and equations=See: | ||
Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:10.1029/2010JF001861. | Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:[http://dx.doi.org/10.1029/2010JF001861 10.1029/2010JF001861]. | ||
|Describe length scale and resolution constraints=Resolution on order of one to a few meters. Domain length grows over time, reaching order tens to hundreds of meters long. | |Describe length scale and resolution constraints=Resolution on order of one to a few meters. Domain length grows over time, reaching order tens to hundreds of meters long. | ||
|Describe time scale and resolution constraints=Typical time scale of order tens to hundreds of thousands of years. | |Describe time scale and resolution constraints=Typical time scale of order tens to hundreds of thousands of years. | ||
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{{Users groups model}} | {{Users groups model}} | ||
{{Documentation model | {{Documentation model | ||
|Provide key papers on model if any=Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:10.1029/2010JF001861. | |Provide key papers on model if any=Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:[http://dx.doi.org/10.1029/2010JF001861 10.1029/2010JF001861]. | ||
|Manual model available=No | |Manual model available=No | ||
}} | }} |
Revision as of 09:52, 24 August 2011
Bedrock Fault Scarp
Metadata
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Download statistics
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