It is difficult to imagine that 480-50 million years ago Vermont and New York States were a marine environment in a shallow tropical sea, far to the east and straddling the equator. At that time earth was a strange and barren place. There was no life on dry land except for a few primitive plants such as mosses and algae. Almost all of life was in the oceans.
Carbon dioxide levels were 14-16 times higher than today with high sea levels covering much of the continents. The continents themselves were mostly located south of the equator.
Along the continental shelf of what was to become North America, strange animals with hard exoskeletons had begun to build the first great reef community in the history of life on earth.
Over hundreds of millions of years, tectonic plate motion at a rate of less than an inch a year resulted in the movement of the landmass now called North America from the equator to its present location. Hence we now find fossil reefs in the unlikely locations of northern Vermont and New York.