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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 ...
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 ...
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]
Geoscientist in Training, or GIT is a professional designation from the National Association of State Boards of Geology (ASBOG) and other organizations, used in U.S. States which regulate the practice of Geology and related earth science fields. [1] Requirements for GIT certification are generally as follows: [2]
^ Florida's state gem, moonstone, was adopted to highlight Florida's role in the United States' Lunar program, which landed the first astronauts on the Moon. [81] ^ Since 1983, Massachusetts has had 3 other official state rocks: State Historical Rock (Plymouth Rock), State Explorer Rock (Dighton Rock), and State Building and Monument Stone . In ...
Pages in category "Geology of Delaware" The following 5 pages are in this category, out of 5 total. This list may not reflect recent changes. ...
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 ]
"The Gap" as seen from the Delaware River Viaduct. The namesake feature of the recreation area is the prominent Delaware Water Gap, located at the area's southern end.The Delaware River runs through the gap, separating Pennsylvania's Mount Minsi on Blue Mountain, elevation 1,461 feet (445 m), from New Jersey's Mount Tammany on Kittatinny Mountain, elevation 1,527 feet (465 m).