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Saturated Thickness in the Alluvium of the Lower Arkansas Valley, Southeast Colorado, Fall 2015

Dates

Publication Date
Start Date
2015-06-01
End Date
2015-11-30

Citation

Holmberg, M.J., 2017, Data Release — Hydrogeologic Characteristics and Geospatial Analysis of Water-Table Changes in the Alluvium of the Lower Arkansas River Valley, Southeastern Colorado, 2002, 2008, and 2015: U.S. Geological Survey data release, https://doi.org/10.5066/F71G0JF6.

Summary

Raster dataset showing saturated thickness (in feet) of the alluvium in the Lower Arkansas River Valley, Southeast Colorado, June 1 - November 30, 2015 (hereafter defined as "fall"). Saturated thickness values based on water levels measured in the study area and median lake level at John Martin Reservoir during this time period. Surface interpolations for water-table altitude were done using Inverse Distance Weighting using coordinate and altitude data from "Wells and water-level altitude in the alluvium in the Lower Arkansas River Valley, Southeast Colorado, Spring and Fall 2002, 2008, and 2015" (see cross reference section in metadata), and surface interpolation of bedrock was done using Topo to Raster using elevation (20-ft contours) [...]

Contacts

Point of Contact :
Michael J. Holmberg
Originator :
Michael J. Holmberg
Metadata Contact :
Michael J. Holmberg
Publisher :
U.S. Geological Survey
Distributor :
Science Base

Attached Files

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Extension: SaturatedThickness_Fall2015.zip
SaturatedThickness_Fall2015.tfw 94 Bytes
SaturatedThickness_Fall2015.tif 269.99 KB
SaturatedThickness_Fall2015.tif.aux.xml 1.8 KB
SaturatedThickness_Fall2015.tif.ovr 70.46 KB
SaturatedThickness_Fall2015.tif-ColorRamp.SLD 2.09 KB

Purpose

These data were collected to show changes in hydrogeologic conditions over a 15-year study period. See larger work citation

Map

Spatial Services

ScienceBase WMS

ScienceBase WCS

Communities

  • USGS Colorado Water Science Center

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Provenance

Data source
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Additional Information

Raster Extension

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maxY38.37568441398533
maxX-102.03050891094045
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