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By Alexander J. W.

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Geomorphic transport laws for predicting landscape form and dynamics. In: W ILCOCK , P. R. & I VERSON , R. M. (eds) Prediction in Geomorphology. American Geophysical Union, Geophysical Monograph, 135, 103–132. , D ENSMORE , A. , A LLEN , P. A. & K UBIK , P. W. 2005. Timing and controls on debris-flow fan deposition and abandonment on alluvial fans in Owens Valley, California. Geophysical Research Abstracts, 7, 03158, European Geosciences Union, 2005. E LLIS , M. , D ENSMORE , A. L. & A NDERSON , R.

2007a. Transient landscapes at fault tips. 1029/2006JF000560. D ENSMORE , A. , A LLEN , P. A. & S IMPSON , G. 2007b. Development and response of a coupled catchment– fan system under changing tectonic and climatic forcing. 1029/2006JF000474. D IETRICH , W. , B ELLUGI , D. , S KLAR , L. , S TOCK , J. , H EIMSATH , A. M. & R OERING , J. J. 2003. Geomorphic transport laws for predicting landscape form and dynamics. In: W ILCOCK , P. R. & I VERSON , R. M. (eds) Prediction in Geomorphology. American Geophysical Union, Geophysical Monograph, 135, 103–132.

For a similar concept see Carretier & Lucazeau (2005). A survey of the landscapes and sediment routing systems in regions of growing extensional fault arrays, such as the Basin and Range province of western USA, exemplifies some of the issues that need to be considered in understanding such polychromatic systems. The landscape responds to a tectonic displacement field that includes the elastic deformation around a range-bounding fault undergoing cumulative coseismic slip, the lateral growth of the fault segment by tip propagation, the interference and linkage with other fault segments, and secular changes in long-term slip rate on the main border fault.

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A Matrix Knot Invariant by Alexander J. W.


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