SSHCZO -- Groundwater Depth, Groundwater Temperatures, Barometric Pressure, Groundwater Chemistry -- Shale Hills Groundwater Depth and Groundwater Temp -- Shale Hills -- (2013-2019)
Authors: | |
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Owners: | CZO Shale-HillsCZO National |
Type: | Resource |
Storage: | The size of this resource is 988.8 KB |
Created: | Nov 19, 2019 at 7:11 a.m. |
Last updated: | Feb 28, 2020 at 7:51 p.m. |
Citation: | See how to cite this resource |
Content types: | Single File Content |
Sharing Status: | Public |
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Views: | 2012 |
Downloads: | 44 |
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Abstract
Groundwater water level data and water temperature for wells in Shale Hills. Wells include:
* CZMW 5
* CZMW 8
* CZMW 10
* CZMW 11
* Well 3
* Well 5
* Well 7
* Well 9
* Well 11
* Well 12
Date Range Comments: data are continuous and will be updated quarterly
Subject Keywords
Coverage
Spatial
Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Susquehanna Shale Hills Critical Zone Observatory, Shale Hills
North Latitude
40.6646°
East Longitude
-77.9053°
South Latitude
40.6645°
West Longitude
-77.9056°
Temporal
Start Date: | 08/07/2013 |
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End Date: | 02/01/2019 |


















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Additional Metadata
Credits
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
Name | Organization | Address | Phone | Author Identifiers |
---|---|---|---|---|
Brandon Forsythe | Pennsylvania State University;Susquehanna Shale Hills Critical Zone Observatory | PA, US | 814-865-0294 | ORCID |
How to Cite
Brantley, S. L., B. Forsythe, H. Kim (2020). SSHCZO -- Groundwater Depth, Groundwater Temperatures, Barometric Pressure, Groundwater Chemistry -- Shale Hills Groundwater Depth and Groundwater Temp -- Shale Hills -- (2013-2019), HydroShare, http://www.hydroshare.org/resource/6dd3a7e69375411389cc7a587ed6cdf9
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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