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  1. Geology | The New York State Museum
    The mission of the Geology Department and New York State Geological Survey (NYSGS) is to conduct geologic research, evaluate mineral resources and geologic ...
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  2. Geology of the New York Region | U.S. Geological Survey
    Laurentia collided with another continental plate in what is now called the Grenville Orogeny. The collision created a large mountain range along Laurentia's ...
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  3. Geology of New York State
    Jun 17, 2013 ... Buehler, E.J., Geology of Western New York, Guidebook, New York State Geological. Association, 38 th. Annual Meeting, Department of Geological ...
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  4. Geology of New York: a Simplified Account (second edition)
    Page 1. GEOLOGY OF NEW YORK. A Simplified Account. Y. W. Isachsen, E. Landing, J. M. Lauber, L. V. Rickard, W. B. Rogers, editors. GEO. 050-4. GEONY. 90-55542.
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  5. Explore New York's Geological Features – A Journey Through Time
    During the Taconic Orogeny, the granite bedrock was overthrust and interlayered with the schist and marble strata, forming the so-called Manhattan Prong. It ...
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  6. AMNH | Geology of NYC| Manhattan Prong | Geology of Central Park
    Generally, earthquakes are located at the boundaries between plates where they collide, or grind past each other, or spread apart. New York City lies within the ...
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  7. NYSCPG - Home
    NYSCPG is the principal organization of professional geologists responsible for the advancement of the competent and ethical practice of geology in New York ...
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  8. Geology of New York (state) - Wikipedia
    Fewer rocks have deposited since the Mesozoic as several kilometers of rock have eroded into the continental shelf and Atlantic coastal plain, although volcanic ...
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  9. NYSGA Online – Official Website of the New York State Geological ...
    2024 Annual Conference Saturday, September 13-15. This year's NYSGA field conference will be a single field trip focusing on the Structure, Petrology, ...
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  10. Geological History of NYC Parks : NYC Parks
    The bedrock in the city ranges in age from 1.1 billion to 190 million years old, and the rocks we see at the surface are the roots of an ancient mountain chain ...
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