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Rome Sand Plains is a 15,000-acre (61 km 2) pine barrens about five miles (8.0 km) west of the city center of Rome in Oneida County in central New York. It consists of a mosaic of sand dunes rising about 50 feet (15 m) above low peat bogs that lie between the dunes.
Clark Reservation State Park is a state park in Onondaga County, New York. The park is in Jamesville, NY, in the Town of DeWitt, south of Syracuse. It was the site of a large waterfall formed by melting glacial ice at the end of the last Ice Age; the plunge basin at the base of the old falls is now a small lake. James Macfarlane described the ...
Location of New York in the United States. New York is located in the northeastern United States, in the Mid-Atlantic Census Bureau division. New York covers an area of 54,556 square miles (141,299 km 2) making it the 27th largest state by total area (but 30th by land area). [4]
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Part of the "Eastern Lake Ontario Barrier Beach and Wetland Complex" New York Natural Heritage Area. [7] Bog Brook: Putnam: 132 acres (0.53 km 2) Braddock Bay: Monroe: 2,402 acres (9.72 km 2) Canadaway Creek: Chautauqua: 2,080 acres (8.4 km 2) Canoga Marsh: Seneca: 104 acres (0.42 km 2) [8] Protects marshland along the western shore of Cayuga ...
The greater Tug Hill region is defined in New York State law as encompassing the following 41 towns in four counties, with a total area of approximately 2,100 square miles (5,400 km 2): [3] Jefferson County
New Jersey's Pochuck Mountain looms just to the south of the region, and the ridge continues into the region as a small upland area called Pochuck Neck; there are two smaller hills within it known as Mounts Adam and Eve, rising to 900 and 1,060 feet (270 and 320 m) respectively. The area is also very noticeable on satellite imagery by the color ...
The two main types of lava field structures are defined as sheet flow lava and pillow lava. Sheet flow lava appears like a wrinkled or folded sheet, while pillow lava is bulbous, and often looks like a pile of pillows atop one another. [2] An important aspect of lava flow morphology is a phenomenon known as lava flow inflation.