Sentence examples for bedrock morphology from inspiring English sources

An exploratory analysis allowed us to describe surface and bedrock morphology and to detect discontinuities in the regolith in the immediate vicinity of the landslide.

The displacement, up to 1800 m, and the listric geometry were recognized by numerical modeling of the resulting hangingwall bedrock morphology and is responsible for the marked asymmetry that characterizes the corresponding scarp in the Concordia Subglacial Trench.

Slides in the area were affected by the bedrock morphology, location and sedimentation rate of the glaciomarine sediments, isostatic rebound, presence of gas/fluids in marine sediments and later, river incision, tides and groundwater flow.

The bedrock morphology was replicated through the activity of the listric Adventure Fault, characterized by a basal detachment at the base of the crust (34 km) and a vertical displacement of 2.5 km.

The combined results allowed us to outline the bedrock morphology of the tumulus foundations and identify areas of reduced soil strength in the embankment that we discuss with respect to the construction and usage of the tumulus.

The bedrock morphology was replicated through the activity of the listric Aurora Trench Fault, characterized by a basal detachment at 34 km (considered the base of the crust according to available geophysical interpretations) and vertical displacements ranging between 700 and 300 m.

Where dissolution processes of bedrock dominate peculiar morphologies develop and overrule all landforms controlled by other surface processes.

Flow hydraulics and channel morphology in bedrock rivers have much in common with coarse-bed alluvial rivers.

We use a comparative study of Fiordland and the western Southern Alps of New Zealand to examine how differences in rock type and bedrock fracturing influence landscape morphology and landslide response to rock uplift.

The area exhibits karst morphology, with bedrock largely consisting of limestones and comparatively small areas of dolomites and Quaternary sediments.

We investigate the relative importance of tectonic uplift, climate, and bedrock resistance as controls upon channel morphology in the active orogen of NE Sicily.