= Mohawk–Hudson convergence
{wiki=Mohawk–Hudson_convergence}
The Mohawk–Hudson convergence refers to a geological and tectonic interaction in the region where the Mohawk River and the Hudson River converge in New York State, USA. This area is characterized by complex geological formations and a history of geological events that have shaped its landscape. The term is often associated with the interaction of different tectonic plates and the resulting geological features, such as the formation of valleys, mountains, and faults.
Back to article page