| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4686178 | Geomorphology | 2010 | 8 Pages |
Abstract
Isolated parts of the Rincon Mountain landslide are active in the La Conchita area, but no evidence exists that the entire slide mass is moving as a unit. Landslides from the 200-m high slope behind La Conchita will reoccur and future development on the proposed Rincon Mountain slide should be very carefully evaluated to avoid reducing slope stability and reactivation of the megaslide.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Larry D. Gurrola, Duane E. DeVecchio, Edward A. Keller,