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The Southern Shift and Southern Drawl: A vowel shift known as the Southern Shift, which largely defines the speech of most of the Southern United States, is the most developed both in Texas English and here in Appalachian English (located in a dialect region which The Atlas of North American English identifies as the "Inland South"). [11]
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One such example accent feature is the "r-dropping" (or non-rhoticity) of the late 18th and early 19th century, resulting in the similar r-dropping found in these American areas during the cultural "Old South". Contrarily, in Southern areas away from the major coasts and plantations (like Appalachia), on certain isolated islands, and variously ...
A diversity of earlier Southern dialects once existed: a consequence of the mix of English speakers from the British Isles (including largely English and Scots-Irish immigrants) who migrated to the American South in the 17th and 18th centuries, with particular 19th-century elements also borrowed from the London upper class and enslaved African-Americans.
For example, the Appalachian and Ozark mountain region landforms differing in settlement from that of low-lying areas such as the Virginia Tidewater, Gulf Coast, South Carolina Lowcountry, and the Mississippi Delta. By contrast, farmers in the Upland South cultivated land for subsistence, and few held slaves.
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Regional dialects in North America are historically the most strongly differentiated along the Eastern seaboard, due to distinctive speech patterns of urban centers of the American East Coast like Boston, New York City, and certain Southern cities, all of these accents historically noted by their London-like r-dropping (called non-rhoticity), a feature gradually receding among younger ...