Hydrology and Land Surface Studies
Isotopically-depleted late Pleistocene groundwater in Columbia River Basalt aquifers: Evidence for recharge of glacial Lake Missoula floodwaters?
Article first published online: 3 NOV 2010
Copyright 2010 by the American Geophysical Union.
Geophysical Research Letters
Volume 37, Issue 21, November 2010
How to Cite
2010), Isotopically-depleted late Pleistocene groundwater in Columbia River Basalt aquifers: Evidence for recharge of glacial Lake Missoula floodwaters? Geophys. Res. Lett., 37, L21402, doi:10.1029/2010GL044992., , , and (
- Issue published online: 3 NOV 2010
- Article first published online: 3 NOV 2010
- Manuscript Accepted: 14 SEP 2010
- Manuscript Revised: 9 SEP 2010
- Manuscript Received: 5 AUG 2010
Auxiliary material for this article contains a detailed description of the sample collection and analytical methods, a sample location map, and data tables.
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Additional file information is provided in the readme.txt.
|grl27484-sup-0001-readme.txt||plain text document||2K||readme.txt|
|grl27484-sup-0002-txts01.txt||plain text document||8K||Text S1. Detailed description of sample collection and analytical methods used in this study.|
|grl27484-sup-0003-fs01.eps||PS document||8911K||Figure S1. Location of groundwater samples collected and analyzed as part of this study in relation to the three Columbia River Basalt aquifers.|
|grl27484-sup-0004-ts01.xls||application/excel||30K||Table S1. Columbia River Basalt Aquifer (CRBA) groundwater sample locations, stable isotope composition, tritium content, and carbon-14 ages.|
|grl27484-sup-0005-ts02.xls||application/excel||16K||Table S2. Mean oxygen isotope values of groundwaters in the Columbia River Basalt Aquifers and Overburden deposits compared to local precipitation.|
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