This form provides that any Party may propose that geoscience operations be conducted on the Contract Area lands. The Party wishing to conduct geoscience operations shall furnish the other Parties with an information notice which generally describes the proposed geoscience operation.
New York Geoscience Operations on the Contract Area
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US-OG-705
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Significant bedrock types and features include Fordham Gneiss (visible at Van Cortlandt Park, especially around Vault Hill north of the Parade Ground and an exposed section overlooking the Harlem River Ship Canal across from Inwood Hill Park, most notable for the giant ?C? painted by Columbia students), the Hartland ...
Several major rock units comprise the stratigraphic section beneath this portion of the city: the Middle Proterozoic Fordham Gneiss, the Cambrian Manhattan Formation, and of the Cambrian and Ordovician Inwood Marble. Outcrops of these formations disclose the complex, northeastward-trending structure of the region.
Central Park is home to innumerable rock outcrops, making it one of the few places in the City with visible evidence of the island's ancient bedrock. Known as Manhattan schist, this bedrock was formed around 500 million years ago and contains other minerals, including quartz, mica, and feldspar.
Manhattan's bedrock is composed primarily of two types of rock: Manhattan Schist and Fordham Gneiss. Manhattan Schist is a type of metamorphic rock that is strong, and durable, making it an ideal building material for many of New York City's famous skyscrapers.
New York City is primarily composed of sediments that were metamorphosed during the Taconic and Acadian orogenies roughly 500 - 400 million years ago. Garnets can be found in the rocks of the Hartland Formation and Manhattan Schist (view a NYC rock sample ).