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From CSDMS
Yes  +
82  +
Boulder  +
No but possible  +
No but possible  +
Single Processor  +
United States  +
Creation date"Creation date" is a predefined property that corresponds to the date of the first revision of a subject and is provided by <a target="_blank" rel="nofollow noreferrer noopener" class="external text" href="https://www.semantic-mediawiki.org/wiki/Help:Special_properties">Semantic MediaWiki</a>.
22:09:48, 2 May 2011  +
https://csdms.colorado.edu/pub/models/doi-source-code/bedrock_fault_scarp-10.1594.IEDA.100097-0.1.tar.gz  +
10.1594/IEDA/100097  +
HILLSLOPE_LENGTH: length of hillslope, in HILLSLOPE_LENGTH: length of hillslope, in meters</br>NUMBER_OF_NODES: number of model nodes (initially)</br>EROSION_RATE: slope-normal erosion rate in m/yr</br>THRESHOLD_SLOPE: threshold slope angle (m/m)</br>THROW_RATE: fault throw rate, meters per year</br>FAULT_DIP: fault dip angle, degrees</br>SEISMIC_INTERVAL: Time interval between earthquakes, in years</br>RUN_DURATION: duration of run in years</br>DT: time step duration in years</br>OPT_ERO_VAR: option for time variation in erosion rate</br>AMPLITUDE: amplitude of sinusoidal variation (m/yr)</br>PERIOD: period of sinusoidal variation (yr)</br>PHASE: phase offset for sinusoidal variation (degrees)</br>DEL18O_FILENAME: name of file containing oxygen isotope curve</br>DEL18O_POWER: exponent</br>MIN_ERORATE:</br>OPT_PLOT: option for plotting</br>OPT_EPS_PLOT: option for output to .eps file</br>PLOT_INTERVAL: time interval for plotting, in yearsRVAL: time interval for plotting, in years  +
Resolution on order of one to a few meters. Domain length grows over time, reaching order tens to hundreds of meters long.  +
Simple ascii files containing x and z coordinates of points at end of run. Optional output of figure in .eps format.  +
Weathering and erosion of bedrock on a hillslope; vertical and horizontal displacement due to earthquakes.  +
Typical time scale of order tens to hundreds of thousands of years.  +
Active  +
2,010  +  and 2,011  +
The code computes the formation of a hillsThe code computes the formation of a hillslope profile above an active normal fault. It represents the hillslope as a set of points with vertical and horizontal (fault-perpendicular) coordinates. Points move due to a prescribed erosion rate (which may vary in time) and due to offset during earthquakes with a specified recurrence interval and slip rate.</br></br>The model is described and illustrated in the following journal article:</br></br>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.i: http://dx.doi.org/10.1029/2010JF001861.  +
+1 303 492 2606  +
Greg  +
1  +
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Cooperative Institute for Research in Environmental Sciences (CIRES)  +
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Tucker  +
0.07  +
Terrestrial  +  and Geodynamic  +
fault  +, two-dimensional  +, numerical  +, model  +, active normal fault  +, normal fault  +, code computes  +, computes the formation  +, active normal  +, hillslope profile  +, hillslope  +, points move due  +, prescribed erosion rate  +, vertical and horizontal  +, code  +, computes  +, formation  +, profile  +, fault, erosion, hillslope, facet, spur, scarp  +  and bedrock fault scarp  +
As code  +
fault, erosion, hillslope, facet, spur, scarp  +
Single  +
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02:19:38, 17 September 2020  +
2  +
This is a two-dimensional numerical model that computes the topographic evolution of the facet slope in the footwall of an active normal fault.  +
+1 303 492 6985  +
Campus Box 399  +
University of Colorado  +
80309  +
minutes  +
Through CSDMS repository  +
https://github.com/csdms-contrib/bedrock_fault_scarp  +
Watershed-Scale  +  and Reach-Scale  +
Colorado  +
Unix  +, Linux  +  and Mac OS  +
Model developer  +