![Displacement](KeeneValleyLandslide/IMG_0588a.jpg) |
![Scarp Face](KeeneValleyLandslide/IMG_0585a.jpg) |
![Scarp by GPR](KeeneValleyLandslide/IMG_0618a.jpg) |
Andrew Kozlowski (left) and Brian Bird
(right) measure the displacement based on
tree root separation. |
The scarp face is visible just 60m from
surface exposures of bedrock |
Jarred Swiontek pulls the GPR antenna
adjacent to a scarp face within the
landslide block. |
![](KeeneValleyLandslide/IMG_0614a.jpg) |
![Ken Resistivity](KeeneValleyLandslide/IMG_0647a.jpg) |
![Sherrod and Swiontek Survey](../Pictures/IMG_0658a.jpg) |
The force of the movement of 82 acres of
earth is enough to split trees unfortunate
enough to be located on a fissure.
|
Kenneth Schlosser takes notes as the
resistivity survey is performed at the base
of the slide. |
Dr. Sherrod and Jarred Swiontek lay out
the resistivity line on the active
landslide. |
![Data Processing](KeeneValleyLandslide/IMG_0649a.jpg) |
|
|
Late night data processing after a full
day of field work - Jarred Swiontek (left)
and Kenneth Schlosser (right) |
Jarred Swiontek (left) and Kenneth
Schlosser (right) at the scarp at the head
of the slide. |
KU research group at the toe of the
slide (note the trees leaning in the
direction of slide movement). |