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The Delaware Geological Survey is the primary source of information about Delaware geology and hydrogeology, such as surface and sub-surface geologic rock formations, extent and quality of aquifers, stream and groundwater monitoring, water supply, earthquakes, floods and droughts, coastal processes (tides, beach erosion), topographic mapping ...
A permanent state geological survey was established by the Delaware General Assembly in 1951 and is funded by direct state appropriation. The 1951 statute founding the Survey contains its fundamental charges: study the geology of Delaware, investigate mineral and water resources, advise state government, and provide the results of its studies ...
Pages in category "Geology of Delaware" The following 5 pages are in this category, out of 5 total. ... Iron Hill (Delaware) P. Piedmont (United States) S.
The Beaverdam Formation is an upper Pliocene geologic formation on the Delmarva Peninsula in southern Delaware and eastern Maryland. [2] [3] It is the largest major surficial layer on the Delmarva Peninsula and has a lower stream-deposited unit and an upper estuarine unit. These units may represent a cycle of regression and transgression. [4]
Delmar, Maryland, part of the Salisbury Urbanized Area, lies across the Maryland-Delaware border from its twin, Delmar, Delaware, on the Transpeninsular Line. Dover, Delaware, is the Delaware state capital and the peninsula's largest city in terms of population. It is also the county seat of Kent County, DE and is home to Delaware State University.
With a topographic prominence of 200 feet (61 m), it is the most prominent hill in Delaware. [2] However, its peak elevation of 328 feet (100 m) means that it is not the state's highest point, which is located in the Piedmont plateau region near Centreville where a peak elevation of 448 feet (137 m) is attained at Ebright Azimuth . [ 3 ]