Lithologic, Hydrologic And Petrophysical Characterization Of An Unconsolidated Cobble-And-Sand Aquifer Capital Station Site, Boise, Idaho
Abstract
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.
Document Details
- Document Type
- Technical Report
- Publication Date
- Mar 01, 1997
- Accession Number
- ADA639997
Entities
People
- Dora M. Gallegos
- Roger H. Morin
- Warren Barrash