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Terrain Work — Hudson Commons

18,000 years ago Manhattan was covered by two miles thick of glacial ice – taller than any building currently in Manhattan. As the glacier retreated it created the defining geological features and topography of Manhattan and deposited boulders and glacial debris that originated hundreds of miles away. The landscapes for the Manhattanville Factory District reveal this rich and varied geological history through the use of stone and topography. The landscapes also connect various…

Site Analysis

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