Snyder Estate Natural Cement Historic District - Geography

Geography

The district is shaped like a letter "r", solidly bounded by the roads and creek on three of its sides, but with its eastern boundary mostly following old roads between Route 213, Binnewater and Sawdust. Physically, it is dominated by two large hills, foothills of the Shawangunk Ridge to the south, which rise to over 300 feet (91 m) in elevation, more than 200 feet (61 m) above the creek's waters to the south.

Between them in a narrow valley sit the remains of one the largest cement plants in it. An old Wallkill Valley Railroad siding runs from there to the northeast corner near where it once joined the main line at today's Binnewater Historic District. Old mines and quarries are tunneled into the sides of both hills.

The property is mostly wooded save for the developed areas. Some of the areas along the road are old fields, today meadows.

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