Hillslope Geomorphology Experiment: Determining Geomorphic Processes in Coastal Range - Pr, Papers of Environmental Science

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.
1. Use the real-time differential-correction GPS to map the {x,y,z} coordinates of the
hill.
2. Be sure to make a point measurement once every 2 m (6’). Each point measurement
should last for 15 seconds.
Equipment Needs: Trimble Pathfinder Pro XRS
B. Slope mantle characterization
1. While taking point measurements with the GPS, record the type of surface as
“bedrock”, “fine colluvium”, or “coarse rubble” using the data dictionary function.
C. Channels
1. Make a field sketch of the channel network.
2. Use field indicators to guesstimate where the channel begins, and be sure to GPS that
point.
D. Landslides
1. Make a field sketch showing the locations of any landslide scars.
Data Analyses:
1. Make an x,y plot showing the locations of all GPS points.
2. Use MS Excel to make a table of the basic statistics (including mean, standard deviation,
minimum, maximum, etc) of elevation and slope mantle data.
3. Use the program Surfer 7.0 to make a topographic map from your GPS data. Be sure to
print out both a surface “mesh” map as well as a standard “contour” map.
4. Plot a longitudinal profile of a hillslope nose and a valley. Make sure the nose is actually
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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.

  1. Use the real-time differential-correction GPS to map the {x,y,z} coordinates of the hill.
  2. Be sure to make a point measurement once every 2 m (6’). Each point measurement should last for 15 seconds. Equipment Needs: Trimble Pathfinder Pro XRS

B. Slope mantle characterization

  1. While taking point measurements with the GPS, record the type of surface as “bedrock”, “fine colluvium”, or “coarse rubble” using the data dictionary function.

C. Channels

  1. Make a field sketch of the channel network.
  2. Use field indicators to guesstimate where the channel begins, and be sure to GPS that point.

D. Landslides

  1. Make a field sketch showing the locations of any landslide scars.

Data Analyses:

  1. Make an x,y plot showing the locations of all GPS points.
  2. Use MS Excel to make a table of the basic statistics (including mean, standard deviation, minimum, maximum, etc) of elevation and slope mantle data.
  3. Use the program Surfer 7.0 to make a topographic map from your GPS data. Be sure to print out both a surface “mesh” map as well as a standard “contour” map.
  4. Plot a longitudinal profile of a hillslope nose and a valley. Make sure the nose is actually

in the basin, and not in the interpolated zone that is actually outside the basin boundary.

  1. Plot a longitudinal slope profile of a hillslope nose and one of the valley.
  2. Use Surfer to delineate divergent, planar, and convergent regions on the hillslope.
  3. Use Surfer to make a vector map showing the steepest descent path throughout the basin.
  4. Determine the topographic characteristics of 20 points distributed over the hillslope. Be sure to include points from the channel, the nose, the hollow, and landslide areas. a. Use the vector map to help delineating upslope area for each point. Calculate area using a planimeter, the square-counting method, or the paper-weighing method. b. Calculate the local slope in the vicinity of each point by taking the difference in elevation between the 2 contours on either side of a point and dividing that difference by the distance between the contour lines. c. Plot Upslope Area versus Slope on a graph, using a different symbol for convergent, divergent, and planar sites. d. Using the steady state landscape model discussed in class, determine which points experience SOF and which SSSF. Then determine which are dominated by soil creep, SOF surface wash erosion, SOF channelization, or landsliding. e. Make an Excel table reporting {x,y,z} coordinates, local slope, upslope area, wetness index, convergent/divergent/planar, flow pathway, sediment transport mechanism. f. Plot the points onto the landscape model graph, using a different symbol for convergent, divergent, and planar sites.

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?