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Airborne electromagnetic and magnetic survey data, Silverton, Colorado, 2019

Dates

Publication Date
Start Date
2019-04-14
End Date
2019-05-19

Citation

Hoogenboom, B.E., Deszcz-Pan, M., Anderson, E.D., Rodriguez, B.D., Smith, B.D., and Yager, D.B., 2022, Airborne electromagnetic and magnetic survey data, Silverton, Colorado, 2019: U.S. Geological Survey data release, https://doi.org/10.5066/P92IADBP.

Summary

Airborne electromagnetic (AEM) and magnetic survey data were collected during April and May 2019 along 1,467 line-kilometers in the San Juan-Silverton Caldera complex, Colorado, in the Southern Rocky Mountain Volcanic Field. Data were acquired by Geotech, Ltd. with the versatile time-domain electromagnetic (VTEM-ET) system together with a Geometrics optically pumped cesium vapor magnetometer. The survey was flown at a mean flight height of 140 meters (m) above terrain in various line directions and line spacings ranging from 150 m to 600 m. Multiple variable-spaced lines were flown along rivers and streams in the survey area. USGS provided the contractor with the San Juan National Forest Lidar Point Cloud elevation dataset imported [...]

Contacts

Attached Files

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4.42 GB application/zip
Silverton_2019_Geotech_ContractorReport.pdf 20.86 MB application/pdf
Silverton_AEM_2019.ncml 52.32 KB text/plain
revision_history.txt 312 Bytes text/plain
Shapefile: Silverton_2019_FlightLines.zip
Silverton_2019_FlightLines.cpg 5 Bytes
Silverton_2019_FlightLines.dbf 7.39 KB
Silverton_2019_FlightLines.prj 403 Bytes
Silverton_2019_FlightLines.sbn 3.84 KB
Silverton_2019_FlightLines.sbx 444 Bytes
Silverton_2019_FlightLines.shp 21.78 MB
Silverton_2019_FlightLines.shx 3.03 KB

Purpose

The purpose of this data release is to provide airborne electromagnetic (AEM) data to the public. The survey was conducted as part of a study of the hydrogeologic framework of the San Juan-Silverton caldera complex. The survey was designed to help characterize subsurface rock properties important for understanding surface water and groundwater quality issues, and to improve knowledge of shallow to deep faults and vein-structures that were conduits for hydrothermal fluids that formed mineral deposits. The study also has general applications to mineral resource assessments in other areas of the world, and in identifying possible groundwater flow paths and associated geochemistry important in abandoned mine lands cleanup.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P92IADBP

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