Great Salt Lake Mineral Extraction Water Withdrawals
Authors: | |
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Owners: | David TarbotonMadeline Merck |
Type: | Resource |
Storage: | The size of this resource is 3.4 KB |
Created: | Mar 07, 2023 at 6:41 p.m. |
Last updated: | Dec 28, 2023 at 1:43 p.m. (Metadata update) |
Published date: | Dec 28, 2023 at 1:43 p.m. |
DOI: | 10.4211/hs.46b98820b7214850aadf6fa60c9bc1d1 |
Citation: | See how to cite this resource |
Sharing Status: | Published |
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Views: | 1329 |
Downloads: | 88 |
+1 Votes: | Be the first one to this. |
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Abstract
Great Salt Lake water withdrawals for use in mineral extraction evaporation ponds. This data is part of a study "The Salinity of the Great Salt Lake and its Deep Brine Layer." This study analyzes the lake’s historical salinity and level data record. Its purpose is to better understand the movement and changes of salt in time and space within the lake and evaluate the occurrence and extent of the deep brine layer. Mineral extraction water withdrawals contribute to changes in the salinity of the lake.
Subject Keywords
Coverage
Spatial
Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Great Salt Lake
Longitude
-112.5476°
Latitude
41.1028°
Temporal
Start Date: | 01/01/1976 |
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End Date: | 12/31/2021 |














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Related Resources
This resource is described by | Merck, M. F. and D. G. Tarboton, (2023), "The Salinity of the Great Salt Lake and Its Deep Brine Layer," Water, 15(8), http://doi.org/10.3390/w15081488 |
Title | Owners | Sharing Status | My Permission |
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Collection of Great Salt Lake Data | David Tarboton | Public & Shareable | Open Access |
Credits
Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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Utah Water Research Laboratory |
How to Cite
Merck, M., D. Tarboton (2023). Great Salt Lake Mineral Extraction Water Withdrawals, HydroShare, https://doi.org/10.4211/hs.46b98820b7214850aadf6fa60c9bc1d1
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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