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Apr. 2023: 
Dr. Kerrigan has been chosen to receive a Fulbright Scholar Award to study rocks in Portugal for the fall of 2023.

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Examining bentonite ash units and hydrothermal fluorite at the New Paris Limestone Quarry

     

The New Paris Limestone Quarry was formerly a New Enterprise Stone and Lime Co. quarry for economic use of the Helderberg limestones. This quarry sits along the northwest limb of the Chestnut Ridge anticline in the eastern part of the Allegheny Plateau, on the boundary between the upper Silurian (~423 Ma) and the lower Devonian (~410 Ma). The Helderberg limestones are the result of shallow marine and tidal sea environment present in western Pennsylvania during this time. Within the limestone units at New Paris lie three volcanic ash layers named: Bald Hill Bentonite A (BHB A), Bald Hill Bentonite B (BHB B), and Bald Hill Bentonite C (BHB C), collectively, the Bald Hill Bentonites (BHBs). Bald Hill Bentonite A has been age dated at 417.6 Ma (Hanson, 1995) and Bald Hill Bentonite C has been age dated at 417 Ma (Gold et al., 2003). These volcanic ash layers originated from regional magmatism and volcanic activity on the east coast of North America which was particularly diverse during this period and it is unclear which volcanic style was dominant and responsible for their deposition (Sinha et al., 2012). Determining which volcanic style is responsible for the volcanic ash layers will allow for a greater understanding of the tectonic processes occurring during this active period of the Appalachians.

Igneous rocks, such as volcanic ash layers, can contain unique geochemical signatures of immobile trace elements which, when plotted on geochemical discrimination diagrams, these geochemical signatures can reveal the magmatic source of the igneous material (Pearce et al., 1984). Recent studies have applied these methods to determine the magmatic origins of bentonite volcanic ash layers (Ge et al., 2018; Kiipli et al., 2008). Applying this practice to the New Paris locality will determine the magmatic source of these ash layers. In the future, it will be possible to repeat this process with other localities for further correlational studies. Funding will allow geochemical analyses of the BHBs to ascertain what the magmatic source was, as well as chemically “fingerprinting” these bentonites. Understanding the source of these ash layers will allow for a better understanding of regional tectonics and its influence in the creation of the Appalachian Mountains.

This is a new project, there should be more to come soon!


I'm always looking for interested students to take on more projects!!!

Future Projects on Alleghany Plateau Geology: Other Projects:
Top images (left to right): Geologic Map of the Youngsford Road ultramfic body; field work at Bells Mill Road with Ryan Kerrigan, Loring Simboli, and Sam Louderback; XPL image of orthopyroxene altering to anthophyllite; Secondary electron image of relict olivine altering to serpentine; field contact between the Bells Mill granodiorite and the Wissahickon schist; trace element chemical discrimination diagram for serpentinites. Copyright © 2023 Ryan Kerrigan (last updated Jun 2023)