-
Ongoing hillslope processes can
change the
topology of the
hillslope surface,
which in turn can
change the
rates of
those processes.
Hillslopes that steepen...
-
Hillslope evolution is the
changes in the
erosion rates,
erosion styles and form of
slopes of
hills and
mountains over time.
During most of the 20th century...
- ****ociated
hillslope areas are the
hillslopes that
slope directly into the channels.
Precipitation that
enters the
system on the
hillslopes areas and is...
- loose,
unconsolidated sediments that have been
deposited at the base of
hillslopes by
either rainwash, sheetwash, slow
continuous downslope creep, or a variable...
- due only to
gravity can
occur on
sloping surfaces in general,
including hillslopes, scarps, cliffs, and the
continental shelf—continental
slope boundary...
-
referred to as the
channel head and it
marks an
important boundary between hillslope processes and
fluvial processes. The
channel head is the most upslope...
-
event or
continuous basis at both
small (
hillslopes, roads,
small parcels) and
large (watershed) scales.
Hillslope applications of the
model can simulate...
- Cross-section of a
hillslope depicting the
vadose zone,
capillary fringe,
water table, and the
phreatic or
saturated zone. (Source:
United States Geological...
- Look up rill in Wiktionary, the free dictionary. In
hillslope geomorphology, a rill is a
shallow channel (no more than a few inches/centimeters deep)...
- Cross-section of a
hillslope depicting the
vadose zone,
capillary fringe,
water table, and
phreatic or
saturated zone. (Source:
United States Geological...
