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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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United States
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Connecticut (1)
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New York
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New York City New York
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Manhattan (1)
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elements, isotopes
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isotopes (1)
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metals
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rare earths
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neodymium (1)
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geologic age
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Mesozoic
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Cretaceous (1)
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Jurassic (1)
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Triassic (1)
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Paleozoic
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Devonian (1)
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Hartland Formation (3)
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Manhattan Formation (1)
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Ordovician (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic
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Fordham Gneiss (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites (1)
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pegmatite (1)
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metamorphic rocks
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metamorphic rocks
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metaigneous rocks
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serpentinite (1)
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metasedimentary rocks (1)
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metasomatic rocks
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serpentinite (1)
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minerals
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silicates
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orthosilicates
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nesosilicates
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garnet group (1)
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zircon group
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zircon (1)
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Primary terms
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deformation (1)
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earthquakes (1)
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education (1)
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faults (2)
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foundations (1)
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fractures (1)
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geochemistry (1)
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geomorphology (1)
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igneous rocks
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plutonic rocks
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granites (1)
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pegmatite (1)
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intrusions (1)
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isotopes (1)
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Mesozoic
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Cretaceous (1)
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Jurassic (1)
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Triassic (1)
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metals
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rare earths
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neodymium (1)
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metamorphic rocks
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metaigneous rocks
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serpentinite (1)
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metasedimentary rocks (1)
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metasomatic rocks
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serpentinite (1)
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Paleozoic
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Devonian (1)
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Hartland Formation (3)
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Manhattan Formation (1)
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Ordovician (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic
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Fordham Gneiss (1)
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slope stability (1)
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soils (1)
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tectonics (3)
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United States
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Connecticut (1)
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New York
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New York City New York
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Manhattan (1)
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soils
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soils (1)
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Hartland Formation
ABSTRACT Here we present an overview of the geology of the Manhattan Prong and a specific guide for field stops in northern Central Park. This guide is intended to provide a brief introduction to these complex rocks for researchers, undergraduate students, and teachers. Given the easy access to Central Park and numerous schools and institutions nearby, these outcrops provide ideal teaching outcrops for students of all levels. We also present new geochemical and isotopic results for the Manhattan and Hartland Schists. Previous work has focused primarily on field mapping, structural relationships, or infrastructure-related mapping, whereas our new geochemistry data allow for more detailed discussions of provenance and overall tectonic history of these rocks. Our results suggest that all of the rocks in northern Central Park (regardless of mapped unit) are derived from Laurentia.