Our family is on a nature exploration kick lately, and no one is more surprised than me. It’s never really been our thing. Granted, we stick to “bunny slope” versions of hiking trails, and I don’t go anywhere without a backpack filled with antibacterial wipes and provisions for a potential week in the wild.
Earlier this fall we scrambled over a mossy rock embankment to reach the Old Stone Church in Dover Plains, a town park in the Hudson Valley. Most recently, we explored Rock City Park, home to the world’s largest exposure of quartz conglomerate, in Olean, New York. It’s a small city in the western part of the state, just north of the Pennsylvania border. And it was a little—okay, a lot—out of the way as we headed toward Niagara Falls, but we got to spend some time with Matt’s cousin, who told us about this “world’s largest.” We couldn’t resist!
This place makes you exclaim “wow” on a continuous loop. Rock formations, created 320 million years ago, surround and engulf you as you make your way through the 45-minute hiking trail. The rocks represent a combination of shale with exposed quartz veins, non-quartz sediment, and Olean conglomerate. Geologists believe the crevices and fractures formed 280 to 225 million years ago.
Your tour starts by descending down stairs into one of these crevices, called “Fat Man’s Squeeze.” There are endearing names like this for most points along the trail, as well as for many of the largest rocks.