"The Geological History of the Hudson River"

The geological history of the Hudson River spans millions of years, shaped by glacial activity and tectonic movements. Originally a valley, it was carved by glaciers during the last Ice Age, which created its current deep channel. As glaciers retreated, rising sea levels further influenced the river's shape and flow. The Hudson's surrounding landscape features diverse rock formations, showcasing ancient sediments and volcanic activity. This river has played a crucial role in trade and transportation, reflecting not just the natural processes that formed it but also its ongoing importance to human civilization.