Geology of New England These settlers could have moved to recently formed dune fields, which were produced by wind erosion of glacial outwash deposits, such as those found in the Ohio Valley, in the Hudson and Connecticut River valleys, and in the Israel River valley. Early human settlers could have populated these river valleys in order to observe the caribou migrating northeast along the newly formed rivers. Geology of New England New England is a region in the North Eastern United States consisting of the states Rhode Island, Connecticut, Massachusetts, New Hampshire, Vermont, and Maine. Most of New England consists geologically of volcanic island
New England Penobscot River in Maine. The Narragansetts and smaller tribes under their sovereignty lived in Rhode Island, west of Narragansett Bay, including Block Island. The Wampanoag occupied southeastern Massachusetts, Rhode Island, and the islands of Martha's Vineyard and Nantucket. The Pocumtucks lived in Western Massachusetts, and the Mohegan and Pequot tribes lived in the Connecticut region. The Connecticut River Valley linked numerous tribes culturally, linguistically, and politically. As early as 1600, French, Dutch, and English traders began exploring the New World, trading metal, glass, and cloth for local beaver pelts. On April 10, 1606, King James I of England issued a