Bedrock geologic map of the Seattle 30' by 60' quadrangle, Washington

Yount, James C.; Gower, H.D.

doi:10.3133/ofr91147

Cited by 31 publications

(57 citation statements)

References 8 publications

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“…The nearest exposures of Miocene sedimentary rocks are about 31 mi (50 km) to the south on the south flank of the Seattle basin and include nonmarine rocks of the Blakely Harbor Formation (fig. 4;Fulmer, 1975;Johnson and others, 1994) and unnamed nonmarine sedimentary rocks described by Yount and Gower ( 1991 ). Pliocene strata have not been described in this part of the Puget Lowland.…”

Section: Standard Oil Company Of California Engstrom Community Noimentioning

confidence: 95%

Well stratigraphy and correlations, western Washington and northwestern Oregon

Rau¹,

Johnson²

1999

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Section: Standard Oil Company Of California Engstrom Community Noimentioning

confidence: 95%

Well stratigraphy and correlations, western Washington and northwestern Oregon

Rau¹,

Johnson²

1999

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“…1; scale 1:80,000) was produced by merging available digital surficial geologic and hydrogeologic maps (Yount and Gower, 1991, Survey, unpub. data, 2014).…”

Section: Hydrogeologymentioning

confidence: 99%

Hydrogeologic framework, groundwater movement, and water budget of the Kitsap Peninsula, west-central Washington

Welch¹,

Frans²,

Olsen³

2014

Scientific Investigations Report

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For more information on the USGS-the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprodTo order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. (15) within the township; the letter (Q) following the section gives the 40-acre tract of the section. The two-digit sequence number (01) following the letter indicates that the well was the first one inventoried by U.S. Geological Survey personnel in that 40-acre tract. An "S," "D," or "P" following the sequence number indicates that the site is a spring, deepened well, or piezometer in a well, respectively. In the figures of this report, wells and springs are identified individually by only the section and 40-acre tract, such as 15Q01; township and range are shown on the map borders. AbstractThis report presents information used to characterize the groundwater-flow system on the Kitsap Peninsula, and includes descriptions of the geology and hydrogeologic framework, groundwater recharge and discharge, groundwater levels and flow directions, seasonal groundwater-level fluctuations, interactions between aquifers and the surface-water system, and a water budget.

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“…Sceva (1957), Garling and others (1965), and Deeter (1979) have produced geologic maps of all or part of Suquamish quadrangle. Yount and Gower (1991) and Yount and others (1993) compiled and, in part, reinterpreted these maps at 1:100,000 scale.…”

Section: Introductionmentioning

confidence: 99%