WHAT DID HAPPEN ON TOP OF THAT ROCKY HILL? TERRAIN, GEOLOGY, AND HISTORICAL UNCERTAINTY AT THE BATTLE OF MINISINK (1779), NEW YORK-PENNSYLVANIA
The Minisink battleground is preserved as a county park near the top of a flat-topped hill 500 feet above an enclosing right-angle bend of the Delaware River opposite Lackawaxen, PA. Bedrock at the site consists of gently north-dipping, planar- and crossbedded sandstones of the Lackawaxen Member of the Late Devonian-age Catskill Formation. The upper east face of the hill, where most of the battle was apparently fought, consists of four topographic steps formed by sandstone ledges 10 to 20 ft high. The orientation of the ledges is controlled by subvertical north-south bedrock joints. The ledges step down to the valley of a small spring-fed stream that descends in a southeast direction to the Delaware.
Terrain and geological features that had an impact on the most probable battle scenario include the Minisink ford (localized the action at a strategic Delaware River crossing), the spring-fed ravine (allowed a party of BrantÂ’s men to come up behind the militia early in the fight), the bedrock ledges (controlled the later battle lines and gave shelter to the combatants), and "Sentinel Rock" (an isolated residual boulder that, according to tradition, marks the spot where the enemy broke through the militia's final hilltop position).