Lithologic, Hydrologic And Petrophysical Characterization Of An Unconsolidated Cobble-And-Sand Aquifer Capital Station Site, Boise, Idaho
GEOLOGICAL SURVEY DENVER CO
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The shallow unconfined aquifer in the Boise, Idaho area commonly consists of coarse, unconsolidated Quaternary braided-stream deposits Qal over unconsolidated late-Tertiary sands with clay or tight silt zone TGF forming a local base to the variability of the system is applicable to site investigations, modeling and remediation designs.
- Geology, Geochemistry and Mineralogy
- Hydrology, Limnology and Potamology