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Magnetotelluric sounding locations, stations 1 to 22, Southern San Luis Valley, Colorado, 2006

Dates

Publication Date
Start Date
2006-07-31
End Date
2006-08-16

Citation

Brian D. Rodriguez, 2016, Magnetotelluric sounding locations, stations 1 to 22, Southern San Luis Valley, Colorado, 2006: U.S. Geological Survey, http://dx.doi.org/10.5066/F7SJ1HPT.

Summary

This dataset includes the locations of magnetotelluric (MT) stations collected in 2006 in the Southern San Luis Valley, Colorado. The U.S. Geological Survey conducted a series of multidisciplinary studies, including MT surveys, in the San Luis Valley to improve understanding of the hydrogeology of the Santa Fe Group and the nature of the sedimentary deposits comprising the principal groundwater aquifers of the Rio Grande rift. The shallow unconfined and the deeper confined Santa Fe Group aquifers in the San Luis Basin are the main sources of municipal water for the region. The population of the San Luis Valley region is growing rapidly and water shortfalls could have serious consequences. Future growth and land management in the region [...]

Child Items (22)

Contacts

Point of Contact :
Brian D. Rodriguez
Originator :
Brian D. Rodriguez
Metadata Contact :
Philip J Brown II
Publisher :
U.S. Geological Survey
Distributor :
U.S. Geological Survey - ScienceBase
USGS Mission Area :
Energy and Minerals
SDC Data Owner :
Geology, Geophysics, and Geochemistry Science Center

Attached Files

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USA_Colorado_Rio_Grande_Rift_San_Luis_Basin_2006_MT_stations.xml
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USA_Colorado_Rio_Grande_Rift_San_Luis_Basin_2006_MT_stations.shp 716 Bytes
USA_Colorado_Rio_Grande_Rift_San_Luis_Basin_2006_MT_stations.shx 276 Bytes

Purpose

The purpose of this data release is provide MT station locations and data to the public. Detailed geologic mapping, high-resolution airborne magnetic surveys, gravity surveys, an electromagnetic survey, called magnetotellurics (MT), and hydrologic and lithologic data are being used to better understand the aquifer systems. The primary goal of the MT survey is to map changes in electrical resistivity with depth that are related to differences in rock type. Aquifer properties can be characterized by these variations in rock types.

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The beginning and ending dates of data collection for this survey were changed from a single date (error) 20160731 to the actual range 20060731 to 20060816. This revision impacts only the metadata on the landing page. There were no changes to the data. December 13, 2016.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/F7SJ1HPT

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