The first study examines bedrock hillslopes in Fiordland and the Southern Alps of New Zealand. A new method for quantifying bedrock fracture densities within the shallow subsurface based on seismic refraction surveys is presented.
|Title||Hillslope erosion by bedrock landslides and diffusion of unconsolidated sediment|
|Author||Clarke, Brian Arden|
|Degree Level||Doctor of Philosophy|
|Degree Grantor||University of California Santa Barbara (USA)|
|Keywords||erosion; landslide; unconsolidated medium; sediment|
|Locality||Fiordland; Southern Alps; New Zealand|