Add to ORKGThe Bethany Beach borehole (Qj32-27) provides a nearly continuous record of the Oligocene to Pleistocene formations of eastern Sussex County, Delaware. This 1470-ft-deep, continuously cored hole penetrated Oligocene, Miocene, and Pleistocene stratigraphic units that contain important water-bearing intervals. The resulting detailed data on lithology, ages, and environments make this site an important reference section for the subsurface geology of the region
Cape May County, a peninsular area at the southernmost tip of New Jersey, is part of the Coastal Pla...
Pleistocene channels along the margins of the Atlantic Coastal Plain are developed in crystalline an...
Onshore and offshore geological and geophysical data were used to investigate the lithostratigraphy,...
McLaughlin, PeterThe Marshy Hope borehole (Nb53-08) sediments encompass the Calvert, Choptank and St...
Analyses of drillers' and geophysical logs, cuttings, and 29 core samples from well Nc13-3 near Gree...
McLaughlin, Peter P., Jr.Martin, Ronald E.This study examines the stratigraphy and palynology of thr...
The geologic history of the surficial units of the Bethany Beach and Assawoman Bay Quadrangles is th...
The report has 3 sections: 1) Biostratigraphy And Chronostratigraphy Of Test Well Je32-04, by Richa...
The Cypress Swamp of Sussex County, Delaware, is underlain by a body of late Pleistocene- to Holocen...
Rising and highstands of sea level during the middle to late Pleistocene deposited swamp to nearshor...
Exploration for sand resources for beach nourishment has led to an increase in the amount of geologi...
The geologic history of the surficial geologic units of the Georgetown Quadrangle is primarily that ...
This report has 1 plate listed as a separate file.Ground water comprises nearly all of the water sup...
Madsen, John A.Throughout the Quaternary Period, the Delaware Estuary, which is located within the M...
The geological history of the surficial units of the Millsboro Quadrangle and Delaware portion of th...
Cape May County, a peninsular area at the southernmost tip of New Jersey, is part of the Coastal Pla...
Pleistocene channels along the margins of the Atlantic Coastal Plain are developed in crystalline an...
Onshore and offshore geological and geophysical data were used to investigate the lithostratigraphy,...
McLaughlin, PeterThe Marshy Hope borehole (Nb53-08) sediments encompass the Calvert, Choptank and St...
Analyses of drillers' and geophysical logs, cuttings, and 29 core samples from well Nc13-3 near Gree...
McLaughlin, Peter P., Jr.Martin, Ronald E.This study examines the stratigraphy and palynology of thr...
The geologic history of the surficial units of the Bethany Beach and Assawoman Bay Quadrangles is th...
The report has 3 sections: 1) Biostratigraphy And Chronostratigraphy Of Test Well Je32-04, by Richa...
The Cypress Swamp of Sussex County, Delaware, is underlain by a body of late Pleistocene- to Holocen...
Rising and highstands of sea level during the middle to late Pleistocene deposited swamp to nearshor...
Exploration for sand resources for beach nourishment has led to an increase in the amount of geologi...
The geologic history of the surficial geologic units of the Georgetown Quadrangle is primarily that ...
This report has 1 plate listed as a separate file.Ground water comprises nearly all of the water sup...
Madsen, John A.Throughout the Quaternary Period, the Delaware Estuary, which is located within the M...
The geological history of the surficial units of the Millsboro Quadrangle and Delaware portion of th...
Cape May County, a peninsular area at the southernmost tip of New Jersey, is part of the Coastal Pla...
Pleistocene channels along the margins of the Atlantic Coastal Plain are developed in crystalline an...
Onshore and offshore geological and geophysical data were used to investigate the lithostratigraphy,...