A guide to the rocks of Red Clay ValleyThe Red Clay Creek Valley traverses geologic features that have long been recognized as important to science, industry, and history. The reader will note that within the text “Piedmont,” and “Atlantic Coastal Plain” are capitalized. This is because these are formal geologic provinces. The “Fall Line” or “fall zone” is also an important geologic area. The Fall Line is the contact where the hard crystalline rocks of the Piedmont dip under and disappear beneath the sediments of the Coastal Plain. The fall zone is a narrow zone that parallels the Fall Line where rapids and waterfalls are common. The landscape and rock types shown in northern Delaware are classical examples of the larger geologic features t...
This report describes the surface features, stratigraphy, and geologic structure and the sources and...
Rocks of Cretaceous age deposited in continental and marginal environments, and now found along the ...
This publication formally establishes the Old College Formation, a lithostratigraphic unit located a...
The complex geologic framework of the Fall Zone in Delaware is primarily caused by diverse structura...
Delaware’s oldest rocks are metamorphic crystalline rocks of the central Appalachian Piedmont Physio...
The stratigraphy of the Coastal Plain of Delaware is discussed with emphasis placed upon an appraisa...
This geologic map shows: (1) distribution of geologic units found at the land surface; (2) updip lim...
The Delaware Piedmont is underlain by metamorphosed sedimentary and igneous rocks of Middle Proteroz...
This Bulletin has 10 plates. Plate 1 appears on inside front cover. Plates 2-10 are listed separatel...
The Columbia sediments of Delaware cover almost all of the surface of the Coastal Plain portion of t...
The Columbia (Pleistocene) deposits of Delaware form a regional water-table aquifer, which supplies ...
The geological history of the surficial units of the Clayton, Smyrna, and the Delaware portion of th...
This report has 1 plate listed as a separate file.Ground water comprises nearly all of the water sup...
The Pennsylvania-Delaware Piedmont is thought to have been deformed and metamorphosed in the Early P...
This report includes 4 plates and 4 appendices as separate files.The geology and hydrology of the ar...
This report describes the surface features, stratigraphy, and geologic structure and the sources and...
Rocks of Cretaceous age deposited in continental and marginal environments, and now found along the ...
This publication formally establishes the Old College Formation, a lithostratigraphic unit located a...
The complex geologic framework of the Fall Zone in Delaware is primarily caused by diverse structura...
Delaware’s oldest rocks are metamorphic crystalline rocks of the central Appalachian Piedmont Physio...
The stratigraphy of the Coastal Plain of Delaware is discussed with emphasis placed upon an appraisa...
This geologic map shows: (1) distribution of geologic units found at the land surface; (2) updip lim...
The Delaware Piedmont is underlain by metamorphosed sedimentary and igneous rocks of Middle Proteroz...
This Bulletin has 10 plates. Plate 1 appears on inside front cover. Plates 2-10 are listed separatel...
The Columbia sediments of Delaware cover almost all of the surface of the Coastal Plain portion of t...
The Columbia (Pleistocene) deposits of Delaware form a regional water-table aquifer, which supplies ...
The geological history of the surficial units of the Clayton, Smyrna, and the Delaware portion of th...
This report has 1 plate listed as a separate file.Ground water comprises nearly all of the water sup...
The Pennsylvania-Delaware Piedmont is thought to have been deformed and metamorphosed in the Early P...
This report includes 4 plates and 4 appendices as separate files.The geology and hydrology of the ar...
This report describes the surface features, stratigraphy, and geologic structure and the sources and...
Rocks of Cretaceous age deposited in continental and marginal environments, and now found along the ...
This publication formally establishes the Old College Formation, a lithostratigraphic unit located a...