Hydrogeologic Framework of Onslow County, North Carolina, 2008

Jason M. Fine

doi:10.3133/sim3055

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Hydrogeologic Framework of Onslow County, North Carolina, 2008

Jason M. Fine

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Abstract

The unconsolidated sediments that underlie the Onslow County area are composed of interlayered permeable and impermeable beds, which overlie the crystalline basement rocks. The aquifers, composed mostly of sand and limestone, are separated by confining units composed mostly of clay and silt. The aquifers from top to bottom are the surficial, Castle Hayne, Beaufort, Peedee, Black Creek, and Upper and Lower Cape Fear aquifers. For this study, the Castle Hayne aquifer is informally divided into the upper and lower Castle Hayne aquifers. The eight aquifers and seven confining units of the Tertiary and Cretaceous strata beneath Onslow County are presented in seven hydrogeologic sections. The hydrogeologic framework was refined from existing interpretations by using geophysical logs, driller's logs, and other available data from 123 wells and boreholes.

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Source-reported bounding extent: 34.333333333333336° to 35.166666666666664° latitude; -77.91666666666667° to -77° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Jason M. Fine. 2008. Hydrogeologic Framework of Onslow County, North Carolina, 2008. https://doi.org/10.3133/sim3055

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