Oak Ridge Earthflow Observatory Data

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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.
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Sharing Status: Public
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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



Coordinate System/Geographic Projection:
WGS84 EPSG:4326
Coordinate Units:
['Decimal degrees']
North Latitude
East Longitude
South Latitude
West Longitude


Start Date:
End Date:

Collection Contents

Add Title Type Owners Sharing Status Remove
Snap Piezometer Resource Noah Finnegan Public
Crackle Piezometer Resource Noah Finnegan Public
Pop Piezometer Resource Noah Finnegan Public
Fizz Piezometer Resource Noah Finnegan Public
Met Station Resource Noah Finnegan Public
Extensometers Resource Noah Finnegan Public
OREO ERT Resource Colleen Murphy Public
OREO Hydraulic Conductivity Resource Colleen Murphy Public
OREO_spring_discharge Resource Colleen Murphy Public

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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.



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