Climate of New England Climate of New England The climate of New England varies greatly across its span from northern Maine to southern Connecticut: Maine, Vermont, New Hampshire, and most of Massachusetts have a humid continental climate (Dfb in Köppen climate classification). In this region, the winters are long, cold, and heavy snow is common (most locations receive of snow annually in this region). The summer's months are moderately warm, though summer is rather short and rainfall is spread through the year. Cities like Worcester, Massachusetts; Concord, New Hampshire; and Burlington, Vermont average of snow annually. In central and eastern Massachusetts, Rhode Island, and
Geology of Rhode Island Pleistocene glaciations. The state's geology is part of the broader geology of New England. Rhode Island is divided into two distinct physiographic regions. The Eastern Highlands occupy the northwestern interior of the state, near the state line with Connecticut while the majority of the state's land area is grouped with the larger Atlantic Coastal Plain that extends along the eastern seaboard of the US. Rhode Island is the only state in New England formed entirely atop basement rock from the microcontinent Avalonia. The bedrock of Rhode Island first took shape with the emergence of a volcanic arc near a subduction