New England town left over when a particular region was carved into towns, not large enough to be a town on their own. Some appear to have simply been granted outside the usual town structure, sometimes in areas where it was probably not contemplated that towns would ever develop. Over time, those located in more populated areas were, in general, annexed to neighboring towns, or incorporated as towns in their own right. No such areas exist today in Massachusetts, Connecticut or Rhode Island, but some remain in New Hampshire, Vermont and Maine. All three of the northern New England states contain some town-sized
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