Eastern New England English Eastern New England English Eastern New England English, historically known as the Yankee dialect since at least the nineteenth century, is the traditional regional dialect of Maine, New Hampshire, and the eastern half of Massachusetts. Features of this variety once spanned an even larger dialect area of New England, for example, including the eastern half of Vermont as recently as the mid-twentieth century. Studies vary as to whether the unique dialect of Rhode Island falls within the Eastern New England dialect region. Eastern New England English (here, including Rhode Island English) is classically associated with sound patterns such as non-rhoticity
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