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The second article is a condensed and simplified version of Professor Ross’ "Linguistic Class-Indicators in Present-Day English", [10] which appeared in 1954 in the Finnish philological periodical Neuphilologische Mitteilungen. For him the English class-system was essentially tripartite — there exists an upper, a middle, and a lower class.
Ausable Chasm itself is a result of the conclusion of the last glacial period at the end of the Pleistocene, about 10,000 years ago. Prior to the formation of the gorge, the movement of the Laurentide ice sheet during the last glacial period carved deep cliffs along the Champlain Valley , which were subsequently covered in glacial till. [ 7 ]
The Ausable River (/ ɔː ˈ s eɪ b əl /), also known as AuSable River and originally written as "Au Sable", runs in the U.S. state of New York, from the Adirondack Mountains and past the village of Lake Placid and Au Sable Forks to empty into Lake Champlain (at ). It has an East and West branch that join at Au Sable Forks.
Au Sable, or Ausable (/ ɒ ˈ s eɪ b əl / oss-AY-bəl), is a town in Clinton County, New York, United States. The population was 3,146 at the 2010 census. [3] The name is from the Ausable River that flows through the town and means "of sand". The town is in the southeastern corner of the county, south of Plattsburgh.
Modern English, sometimes called New English (NE) [2] or present-day English (PDE) as opposed to Middle and Old English, is the form of the English language that has been spoken since the Great Vowel Shift in England, which began in the late 14th century and was completed by the 17th century.
Au Sable River (disambiguation) Topics referred to by the same term This disambiguation page lists articles about distinct geographical locations with the same name.
Au Sable (disambiguation) Topics referred to by the same term This disambiguation page lists articles about distinct geographical locations with the same name.
The Old Ausable Channel is a self-contained waterway in Lambton County, Ontario, Canada that runs through the Pinery Provincial Park and the community of Grand Bend. It is a 14 kilometre long river channel that was isolated from the Ausable River by the digging of canals for drainage in the late nineteenth century.