Oak Ridge Earthflow Observatory Data
| Authors: | |
|---|---|
| Owners: | Noah Finnegan |
| Type: | Collection |
| Storage: | The size of this collection is 1.4 KB |
| Created: | Jun 12, 2020 at 3:12 p.m. |
| Last updated: | Aug 31, 2021 at 4:56 p.m. |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
|---|---|
| Views: | 2525 |
| Downloads: | 77 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
Abstract
Oak Ridge earthflow is a seasonally active earthflow located in the northern Diablo Range, 20 km northeast of San Jose, California. Positioned on the south-facing flank of Oak Ridge, it extends 1.35 km in the horizontal direction from ridge top to near the valley bottom, spans about 400 m of vertical relief, and has an average slope of 15°. The landslide body is composed of Franciscan mélange, an assemblage of variably deformed and metamorphosed rock units formed in a subduction zone during the Mesozoic and early Cenozoic eras.
Subject Keywords
Coverage
Spatial
Coordinate System/Geographic Projection:
WGS84 EPSG:4326
Coordinate Units:
['Decimal degrees']
North Latitude
37.4609°
East Longitude
-121.7504°
South Latitude
37.4605°
West Longitude
-121.7517°
Temporal
| Start Date: | 06/01/2018 |
|---|---|
| End Date: | 11/02/2018 |
Leaflet Map data © OpenStreetMap contributors
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| National Science Foundation Geomorphology and Land-use Dynamics | RAPID: Exploiting El Nino to Test for Shear Dilation in a Slow Moving Landslide | 1613122 |
| National Science Foundation Geomorphology and Land-use Dynamics | Investigating Feedbacks Between Deformation and Groundwater Flow in a Slow Moving Landslide | 1658800 |
How to Cite
Finnegan, N., C. Murphy (2021). Oak Ridge Earthflow Observatory Data, HydroShare, http://www.hydroshare.org/resource/8e024d2aeb22489c92dbf0c2a1db4608
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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