American English (AmE), sometimes called United States English or U.S. English, is the set of varieties of the English language native to the United States. English is the most widely spoken language in the United States; the de facto common language used in government, education and commerce; and an official language of most U.S. states. Since the late 20th century, American English has become the most influential form of English worldwide.
Canadian raising is an allophonic rule of phonology in many varieties of North American English that changes the pronunciation of diphthongs with open-vowel starting points. Most commonly, the shift affects or, or both, when they are pronounced before voiceless consonants. In North American English, and usually begin in an open vowel [~], but through raising they shift to, or. Canadian English often has raising in words with both and, while a number of American English varieties have this feature in but not. It is thought to have originated in Canada in the late 19th century.
General American English, known in linguistics simply as General American, is the umbrella accent of American English spoken by a majority of Americans, encompassing a continuum rather than a single unified accent. It is often perceived by Americans themselves as lacking any distinctly regional, ethnic, or socioeconomic characteristics, though the term was spread by the linguist John Samuel Kenyon, who hailed from Northeast Ohio and used speech forms there as the basis of his widely disseminated text American Pronunciation. Americans with high education, or from the North Midland, Western New England, and Western regions of the country are the most likely to be perceived as using General American speech. The precise definition and usefulness of the term continue to be debated, and the scholars who use it today admittedly do so as a convenient basis for comparison rather than for exactness. Other scholars prefer the term Standard American English.
Western Pennsylvania English, known more narrowly as Pittsburgh English or popularly as Pittsburghese, is a dialect of American English native primarily to the western half of Pennsylvania, centered on the city of Pittsburgh, but potentially appearing in some speakers as far north as Erie County, as far west as Youngstown, Ohio, and as far south as Clarksburg, West Virginia. Commonly associated with the working class of Pittsburgh, users of the dialect are colloquially known as "Yinzers".
Southern American English or Southern U.S. English is a regional dialect or collection of dialects of American English spoken throughout the Southern United States, though concentrated increasingly in more rural areas, and spoken primarily by White Southerners. In terms of accent, its most innovative forms include southern varieties of Appalachian English and certain varieties of Texan English. Popularly known in the United States as a Southern accent or simply Southern, Southern American English now comprises the largest American regional accent group by number of speakers. Formal, much more recent terms within American linguistics include "Southern White Vernacular English" and "Rural White Southern English".
Philadelphia English or Delaware Valley English is a variety or dialect of American English native to Philadelphia and extending into Philadelphia's metropolitan area throughout the Delaware Valley, including southeastern Pennsylvania, all of South Jersey, counties of northern Delaware, and the northern Eastern Shore of Maryland. Aside from Philadelphia and the surrounding counties and arguably Baltimore, the dialect is spoken in places such as Reading, Camden, Atlantic City, Wilmington, Vineland, and Dover. Philadelphia English is one of the best-studied types of English, as Philadelphia's University of Pennsylvania is the home institution of pioneering sociolinguist William Labov. Philadelphia English shares certain features with New York City English and Midland American English, although it remains a distinct dialect of its own. Philadelphia and Baltimore accents together fall under what Labov describes as a single Mid-Atlantic regional dialect.
North American English regional phonology is the study of variations in the pronunciation of spoken North American English —what are commonly known simply as "regional accents". Though studies of regional dialects can be based on multiple characteristics, often including characteristics that are phonemic, phonetic, lexical (vocabulary-based), and syntactic (grammar-based), this article focuses only on the former two items. North American English includes American English, which has several highly developed and distinct regional varieties, along with the closely related Canadian English, which is more homogeneous geographically. American English and Canadian English have more in common with each other than with varieties of English outside North America.
The cot–caught merger, also known as the LOT–THOUGHT merger or low back merger, is a sound change present in some dialects of English where speakers do not distinguish the vowel phonemes in words like cot versus caught. Cot and caught is an example of a minimal pair that is lost as a result of this sound change. The phonemes involved in the cot–caught merger, the low back vowels, are typically represented in the International Phonetic Alphabet as and or, in North America, as and. The merger is typical of most Indian, Canadian, and Scottish English dialects as well as some Irish and U.S. English dialects.
Pacific Northwest English is a variety of North American English spoken in the U.S. states of Washington and Oregon, sometimes also including Idaho and the Canadian province of British Columbia. Due to the internal diversity within Pacific Northwest English, current studies remain inconclusive about whether it is best regarded as a dialect of its own, separate from Western American English or even California English or Standard Canadian English, with which it shares its major phonological features. The dialect region contains a highly diverse and mobile population, which is reflected in the historical and continuing development of the variety.
New England English is, collectively, the various distinct dialects and varieties of American English originating in the New England area. Most of eastern and central New England once spoke the "Yankee dialect", some of whose accent features still remain in Eastern New England today, such as "R-dropping". Accordingly, one linguistic division of New England is into Eastern versus Western New England English, as defined in the 1939 Linguistic Atlas of New England and the 2006 Atlas of North American English (ANAE). The ANAE further argues for a division between Northern versus Southern New England English, especially on the basis of the cot–caught merger and fronting. The ANAE also categorizes the strongest differentiated New England accents into four combinations of the above dichotomies, simply defined as follows:
The Low-Back-Merger Shift is a chain shift of vowel sounds found in several dialects of North American English, beginning in the last quarter of the 20th century and most significantly involving the low back merger accompanied by the lowering and backing of the front lax vowels:, , and.
Inland Northern (American) English, also known in American linguistics as the Inland North or Great Lakes dialect, is an American English dialect spoken primarily by White Americans in a geographic band reaching from the major urban areas of Upstate New York westward along the Erie Canal and through much of the U.S. Great Lakes region. The most distinctive Inland Northern accents are spoken in Chicago, Milwaukee, Detroit, Cleveland, Buffalo, Rochester, and Syracuse. The dialect can be heard as far west as eastern Iowa and even among certain demographics in the Twin Cities, Minnesota. Some of its features have also infiltrated a geographic corridor from Chicago southwest along historic Route 66 into St. Louis, Missouri; today, the corridor shows a mixture of both Inland North and Midland American accents. Linguists often characterize the western Great Lakes region's dialect separately as North-Central American English.
Older Southern American English is a diverse set of American English dialects of the Southern United States spoken most widely up until the American Civil War of the 1860s, before gradually transforming among its White speakers, first, by the turn of the 20th century, and, again, following the Great Depression, World War II, and, finally, the Civil Rights Movement. By the mid-20th century, among White Southerners, these local dialects had largely consolidated into, or been replaced by, a more regionally unified Southern American English. Meanwhile, among Black Southerners, these dialects transformed into a fairly stable African-American Vernacular English, now spoken nationwide among Black people. Certain features unique to older Southern U.S. English persist today, like non-rhoticity, though typically only among Black speakers or among very localized White speakers.
Western American English is a variety of American English that largely unites the entire Western United States as a single dialect region, including the states of California, Nevada, Arizona, Utah, New Mexico, Colorado, and Wyoming. It also generally encompasses Washington, Oregon, Idaho, and Montana, some of whose speakers are classified additionally under Pacific Northwest English.
Midland American English is a regional dialect or super-dialect of American English, geographically lying between the traditionally-defined Northern and Southern United States. The boundaries of Midland American English are not entirely clear, being revised and reduced by linguists due to definitional changes and several Midland sub-regions undergoing rapid and diverging pronunciation shifts since the early-middle 20th century onwards.
Northern American English or Northern U.S. English is a class of historically related American English dialects, spoken by predominantly white Americans, in much of the Great Lakes region and some of the Northeast region within the United States. The North as a superdialect region is best documented by the 2006 Atlas of North American English (ANAE) in the greater metropolitan areas of Connecticut, Western Massachusetts, Western and Central New York, Northwestern New Jersey, Northeastern Pennsylvania, Northern Ohio, Northern Indiana, Northern Illinois, Northeastern Nebraska, and Eastern South Dakota, plus among certain demographics or areas within Michigan, Wisconsin, Minnesota, Vermont, and New York's Hudson Valley. The ANAE describes that the North, at its core, consists of the Inland Northern dialect and Southwestern New England dialect.
The sound system of New York City English is popularly known as a New York accent. The New York metropolitan accent is one of the most recognizable accents of the United States, largely due to its popular stereotypes and portrayal in radio, film, and television. Several other common names exist for the accent that associate it with more specific locations in the New York City area, such as Bronx accent, Brooklyn accent, Queens accent, Long Island accent, North Jersey accent, etc.; however, no research has demonstrated significant linguistic differences between these locations.
Standard Canadian English is the largely homogeneous variety of Canadian English that is spoken particularly across Ontario and Western Canada, as well as throughout Canada among urban middle-class speakers from English-speaking families, excluding the regional dialects of Atlantic Canadian English. Canadian English has a mostly uniform phonology and much less dialectal diversity than neighbouring American English. In particular, Standard Canadian English is defined by the cot–caught merger to and an accompanying chain shift of vowel sounds, which is called the Canadian Shift. A subset of the dialect geographically at its central core, excluding British Columbia to the west and everything east of Montreal, has been called Inland Canadian English. It is further defined by both of the phenomena that are known as Canadian raising : the production of and with back starting points in the mouth and the production of with a front starting point and very little glide that is almost in the Canadian Prairies.
Western New England English refers to the varieties of New England English native to Vermont, Connecticut, and the western half of Massachusetts; New York State's Hudson Valley also aligns to this classification. Sound patterns historically associated with Western New England English include the features of rhoticity, the horse–hoarse merger, and the father–bother merger, none of which are features traditionally shared in neighboring Eastern New England English. The status of the cot–caught merger in Western New England is inconsistent, being complete in the north of this dialect region (Vermont), but incomplete or absent in the south, with a "cot–caught approximation" in the middle area.
In the sociolinguistics of the English language, raising or short-a raising is a phenomenon by which the "short a" vowel, the TRAP/BATH vowel, is pronounced with a raising of the tongue. In most American and many Canadian English accents, raising is specifically tensing: a combination of greater raising, fronting, lengthening, and gliding that occurs only in certain phonological environments or certain words. The most common context for tensing throughout North American English, regardless of dialect, is when this vowel appears before a nasal consonant.
