— — the rock that keeps winter into July.
“The high southern end of the Shawangunk Ridge, where the white quartz conglomerate splits into deep crevices that hold ice through the warm months. A loop trail leads from the parking area at Sam's Point past dwarf pitch pines to the caves and the cliff edge above Verkeerderkill Falls. Cooler by ten degrees than the valley below, even in August.
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Sam's Point sits at roughly 2,255 feet on the southern end of the Shawangunk Ridge, above the village of Cragsmoor in Ulster County, New York. The 4,600-acre Sam's Point area is the largest contiguous tract within Minnewaska State Park Preserve and is managed by the New York State Office of Parks. The bedrock is a hard quartz-pebble conglomerate called Shawangunk grit, which fractures into wide vertical crevices. A globally rare dwarf pine barrens covers the ridge top.
The conglomerate that forms the ridge is roughly 420 million years old, deposited in a Silurian river system and uplifted as the Appalachians rose. The wide tectonic crevices in the cliff face are deep and narrow enough to trap cold air and snow through the warm months, true ice caves rather than seasonal ones. Ice persists into late June or early July in cooler years. The same rock forms the climbing crags at the Trapps, ten miles north along the ridge.
The preserve is open year-round but the ice caves are at their strangest in May and June, when the surrounding woods are leafed out at eighty degrees and the cave floors still hold winter ice. The high blueberry barrens on the ridge ripen in late July. Fall color peaks across the dwarf pines and oaks in mid-October. Winter access is limited; the gate road closes when conditions warrant, and the upper loop is exposed to wind off the Catskills to the north.