At collisional mountain ranges the tectonic history of crustal shortening and
subsequent post-collisional erosion is preserved in the form of the presently observed
gravity anomalies. In this study, models of erosion and isostatic rebound at various stages
of collision illustrate the evolution of crustal structure, topography, and resulting gravity
anomalies....
The catchment-filter, soil erosion gage, macroprofile, and
spike and washer techniques for erosion measurement were compared
on six plots along a newly constructed logging road in the Oregon
Coast Range during the winter of 1965-66. Three plots were located
on a cut slope; three plots were on a fill slope....