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DGS Annual Report

DGS Annual Report of Programs and Activities.

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Site content related to keyword: "Bringhurst Gabbro"

William "Sandy" Schenck's photomicrograph was chosen for "The Art in Science" exhibit at UD Harker Lab

"Bringhurst Gabbro, Bringhurst Woods, Wilmington, Delaware" ~ W.S.Schenck

The Art in Science exhibit will be held from April 4 to April 16 in the University of Delaware Harker Lab. With a two week display of art culminating in a symposium on the 16th, Art in Science is geared toward highlighting cutting edge research at UD across all disciplines in order to educate and engage the local community and to spark interest in STEM activities in underrepresented student populations.

Outcrop Bd44-b: Bringhurst Gabbro boulders in Shellpot Creek

Rock Outcrop Bd44-b: Bringhurst Gabbro boulders in Shellpot Creek

Found in the creek bed and flood plain, the large boulders in Shellpot Creek are excellent examples of Bringhurst Gabbro. The gabbro is very coarse-grained with crystals up to 2" long; however, variations in the grain size exist over a scale of a few inches. While observing this rock closely, one can occasionally find grains of orthopyroxene (possibly bronzite) up to 4" long. Some of the boulders have grains of olivine surrounded by double coronas of orthopyroxene, spinel, and hornblende.

Bringhurst Gabbro

Sbg

Coarse- to very coarse-grained gabbronoite with subophitic textures. Primary minerals are plagioclase, olivine, clinopyroxene and orthopyroxene. Olivine, where present, is surrounded by an inner corona of orthopyroxene and an outer corona of pargasitic hornblende, both with spinel symplectites. The gabbronorites locally contain abundant xenoliths of mafic Brandywine Blue Gneiss.

GM13 Geologic Map of New Castle County, Delaware

GM13 Geologic Map of New Castle County, Delaware

This map shows the surficial geology of New Castle County, Delaware at a scale of 1:100,000. Maps at this scale are useful for viewing the general geologic framework on a county-wide basis, determining the geology of watersheds, and recognizing the relationship of geology to regional or county-wide environmental or land-use issues. This map, when combined with the subsurface geologic information, provides a basis for locating water supplies, mapping ground-water recharge areas, and protecting ground and surface water. Geologic maps are also used to identify geologic hazards, such as sinkholes and flood-prone areas, to identify sand and gravel resources, and for supporting state, county, and local land-use and planning decisions.

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