Geology, Hydrology, And Geophysics Of Columbia Sediments In The Middletown-Odessa Area, Delaware

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dc.contributor.authorSpoljaric, N.
dc.contributor.authorWoodruff, K.D.
dc.date.accessioned2008-01-14T20:53:29Z
dc.date.available2008-01-14T20:53:29Z
dc.date.issued1970-08
dc.description.abstractColumbia sediments in the Middletown-Odessa area are composed of boulders, gravels, sands, silts and clays. These sediments are exposed in four gravel pits where their structures and textures were studied. Subsurface geology was interpreted on the basis of the well-log data from 40 holes drilled in the area of study. Columbia sediments were laid upon a surface made up of the greensands of the Rancocas Formation (Paleocene – Eocene age). The contact between the Rancocas and Columbia Formations is an erosional unconformity.en_US
dc.identifier.urihttp://udspace.udel.edu/handle/19716/3051
dc.language.isoen_USen_US
dc.publisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
dc.relation.ispartofseriesBulletinsen_US
dc.relation.ispartofseries13en_US
dc.subjectGeologyen_US
dc.subjectHydrologyen_US
dc.subjectGeophysicsen_US
dc.subjectColumbia Sedimentsen_US
dc.subjectMiddletown-Odessa Area, Delawareen_US
dc.subjectgreensandsen_US
dc.subjectRancocas Formationen_US
dc.subjectPaleocene – Eocene ageen_US
dc.titleGeology, Hydrology, And Geophysics Of Columbia Sediments In The Middletown-Odessa Area, Delawareen_US
dc.typeTechnical Reporten_US

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