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An experiment conducted in professor pasternack's hyd252 class during spring 2001, focusing on hillslope geomorphology and sediment budgets. Students were tasked with determining the most significant geomorphic processes on a coastal range hillslope using gps topographic survey, slope mantle characterization, channel analysis, and landslide identification. Data analyses included creating maps, longitudinal profiles, and slope profiles using surfer 7.0. The report required standard report format with sections for background, objectives, procedure, results, discussion, and conclusion.
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Hillslope Geomorphology and Sediment Budgets Professor Pasternack HYD252 Spring 2001
EXPERIMENT 1: HILLSLOPE GEOMORPHOLOGY
Background: Hilly and mountainous landscapes are partially to completely covered with soil under a wide range of erosion and uplift rates, bedrock type, and climate. The major processes that occur on a hillslope include soil creep, erosion by surface overland flow, and landslide. Which of these dominates on any part of a hillslope depends primarily on topography, and is now predictable thanks to major advances in geomorphic theory. The significance of this prediction capability for reducing landslide damages is of particular value here in northern California.
Objective: Determine which geomorphic processes are most significant on a Coastal Range hillslope.
Procedure:
A. Topographic survey using GPS A high quality digital topographic map is required to assess hillslope dynamics.
B. Slope mantle characterization
C. Channels
D. Landslides
Data Analyses:
in the basin, and not in the interpolated zone that is actually outside the basin boundary.
Report Content:
Format: Standard report format with abstract, background, objectives, study site, procedure, results, discussion, conclusion. The report is a significant part of your grade.
The results section should present and describe all findings without any interpretation.
In the discussion section, address the following issues: Where does the channel begin, and what evidence supports your assertion? Put together the data anlyses and field observation to explain the relative roles of soil creep, SOF erosion, and landslides on the hillslope studied in the field? Is this a Hack/Gilbert type “steady-state” landscape? How does this hillslope compare to Tennessee Valley in Marin County (work of Dietrich et al.) well as those discussed by Hack and Goodlett?