1923 Map of Livingston Manor

About this map

Livingston Manor serves as a central hub in this early 1920s survey, where the New York Ontario and Western RR follows the valleys of the Beaver Kill and Willowemoc Creek. The landscape is a dense network of upland agriculture and specialized chemical industry, evidenced by the Acid Plant near Rockland and a Creosote Plant downstream from the main settlement. Dozens of one-room schoolhouses, such as the Russell School and Fox Mountain School, are scattered across the townships of Callicoon and Rockland, marking the population distribution before the centralization of rural education. To the west, the topography rises toward Mandrake Hill and Baldy, sheltering numerous water bodies like Tennanah Lake and Shandelee Lake that would define the region's character as a destination for outdoor recreation and seasonal retreat. Local commerce and transit are anchored by smaller junctions like Roscoe, Cooks Falls, and Jeffersonville.