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Created: | Nov 19, 2019 at 8:10 a.m. | |
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Abstract
Seismic refraction surveys consisted of 24 channel Geometrics Geode system and 14 Hz vertical component geophones. Seismic source was by using a sledgehammer striking a steel plate.
Date Range Comments: Campaign
Subject Keywords
Coverage
Spatial
Temporal
Start Date: | |
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End Date: |
Content
ReadMe.md
SSHCZO -- Seismic Refraction, Geophysics -- Cole Farm -- (2018)
OVERVIEW
Description/Abstract
Seismic refraction surveys consisted of 24 channel Geometrics Geode system and 14 Hz vertical component geophones. Seismic source was by using a sledgehammer striking a steel plate.
Creator/Author
Hayes, Jorden
CZOs
Shale Hills
Contact
Jorden Hayes, Assistant Professor of Earth Scienes, (717)254-8303, hayesjo@dickinson.edu
Subtitle
Seismic Refraction Data
SUBJECTS
Disciplines
Geophysics|Geomorphology
Topics
Seismic Refraction|Geophysics
Keywords
Seismic refraction|geophysics
Variables
Seismic refraction|surface wave analyses
Variables ODM2
Groundwater Depth|surface wave analyses
TEMPORAL
Date Start
2018-04-13
Date End
2018-04-13
Date Range Comments
Campaign
SPATIAL
Field Areas
Cole Farm (Agricultural Site)
Location
Cole Farm
North latitude
40.640115
South latitude
40.629135
West longitude
-77.946281
East longitude
-77.934399
REFERENCE
Citation
The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Susquehanna Shale Hills Critical Zone Observatory.
CZO ID
7214
Additional Metadata
Name | Value |
---|---|
czos | Shale Hills |
czo_id | 7214 |
citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Susquehanna Shale Hills Critical Zone Observatory. |
keywords | Seismic refraction, geophysics |
subtitle | Seismic Refraction Data |
variables | Seismic refraction, surface wave analyses |
disciplines | Geophysics, Geomorphology |
date_range_comments | Campaign |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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