Results Summary GIS-based topographic analysis of folded topography within the Camarillo fold belt suggests fold complexes young toward the west. Discrete changes in the relative age of tectonic topography and structural style occur at orthogonal cross faults.

Methods

1) One hundred and fifty-three catchments were constructed using ESRI ArcGIS

2) Drainage density and mean catchment erosion were calculated for each watershed and compared to the structure of the area   

Figure showing all watersheds analyzed within the CFB.