The Great Vowel Shift was a series of changes in the pronunciation of the English language that took place primarily between 1400 and 1700, beginning in southern England and today having influenced effectively all dialects of English. Through this vowel shift, the pronunciation of all Middle English long vowels was changed. Some consonant sounds also changed, particularly those that became silent; the term Great Vowel Shift is sometimes used to include these consonantal changes.
A diphthong, also known as a gliding vowel, is a combination of two adjacent vowel sounds within the same syllable. Technically, a diphthong is a vowel with two different targets: that is, the tongue moves during the pronunciation of the vowel. In most varieties of English, the phrase "no highway cowboy" has five distinct diphthongs, one in every syllable.
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.
The phonology of the open back vowels of the English language has undergone changes both overall and with regional variations, through Old and Middle English to the present. The sounds heard in modern English were significantly influenced by the Great Vowel Shift, as well as more recent developments in some dialects such as the cot–caught merger.
In historical linguistics, a chain shift is a set of sound changes in which the change in pronunciation of one speech sound is linked to, and presumably causes, a change in pronunciation of other sounds. The sounds involved in a chain shift can be ordered into a "chain" in such a way that after the change is complete, each phoneme ends up sounding like what the phoneme before it in the chain sounded like before the change. The changes making up a chain shift, interpreted as rules of phonology, are in what is termed counterfeeding order.
This chart shows the most common applications of the International Phonetic Alphabet (IPA) to represent English language pronunciations.
California English collectively refers to varieties of American English native to California. As California became one of the most ethnically diverse U.S. states, English speakers from a wide variety of backgrounds began to pick up different linguistic elements from one another and also develop new ones; the result is both divergence and convergence within Californian English. However, linguists who studied English before and immediately after World War II tended to find few, if any, patterns unique to California, and even today most California English still largely aligns to a General or Western American accent. Still, certain newer varieties of California English have been gradually emerging since the late 20th century.
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.
Like many other languages, English has wide variation in pronunciation, both historically and from dialect to dialect. In general, however, the regional dialects of English share a largely similar phonological system. Among other things, most dialects have vowel reduction in unstressed syllables and a complex set of phonological features that distinguish fortis and lenis consonants.
High Tider, Hoi Toider, or High Tide English is an American English dialect, or family of dialects, spoken in very limited communities of the South Atlantic United States, particularly several small islands and coastal townships. The exact areas include the rural "Down East" region of North Carolina, which encompasses the Outer Banks and Pamlico Sound—specifically Atlantic, Davis, Sea Level, and Harkers Island in eastern Carteret County, the village of Wanchese, and also Ocracoke—plus the Chesapeake Bay, such as Smith Island in Maryland, as well as Guinea Neck and Tangier Island in Virginia. High Tider has been observed as far west as Bertie County, North Carolina; the term is also a local nickname for any native resident of these regions.
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.
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.
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.
English diphthongs have undergone many changes since the Old and Middle English periods. The sound changes discussed here involved at least one phoneme which historically was a diphthong.
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.
Monophthongization is a sound change by which a diphthong becomes a monophthong, a type of vowel shift. It is also known as ungliding, as diphthongs are also known as gliding vowels. In languages that have undergone monophthongization, digraphs that formerly represented diphthongs now represent monophthongs. The opposite of monophthongization is vowel breaking.
This article covers the phonological system of New Zealand English. While New Zealanders speak differently depending on their level of cultivation, this article covers the accent as it is spoken by educated speakers, unless otherwise noted. The IPA transcription is one designed by Bauer et al. (2007) specifically to faithfully represent a New Zealand accent, which this article follows in most aspects.
The Atlas of North American English: Phonetics, Phonology and Sound Change is a 2006 book that overviews the pronunciation patterns (accents) in all the major dialect regions of the English language as spoken in urban areas of the United States and Canada. It is the result of a large-scale survey by linguists William Labov, Sharon Ash, and Charles Boberg. Speech data was collected, mainly during the 1990s, by means of telephone interviews with individuals in metropolitan areas in all regions of the U.S. and Canada. Using acoustic analysis of speech from these interviews, ANAE traces sound changes in progress in North American English, and defines boundaries between dialect regions based on the different sound changes taking place in them.
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 Montréal, 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.
