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Hawaiian Pidgin (alternately, Hawaiʻi Creole English or HCE, known locally as Pidgin) is an English-based creole language spoken in Hawaiʻi.An estimated 600,000 residents of Hawaiʻi speak Hawaiian Pidgin natively and 400,000 speak it as a second language.
Niʻihau dialect (Standard Hawaiian: ʻŌlelo Niʻihau, Niʻihau: Olelo Matuahine, lit. 'mother tongue') is a dialect of the Hawaiian language spoken on the island of Niʻihau , more specifically in its only settlement Puʻuwai , and on the island of Kauaʻi , specifically near Kekaha , where descendants of families from Niʻihau now live.
Hawaiian (ʻōlelo Hawaiʻi, pronounced [ʔoːˈlɛlo həˈvɐjʔi]) [7] is a Polynesian language and critically endangered language of the Austronesian language family that takes its name from Hawaiʻi, the largest island in the tropical North Pacific archipelago where it developed.
Pidgin Hawaiian (or Hawaii Plantation Pidgin [1]) is a pidgin spoken in Hawaii, which draws most of its vocabulary from the Hawaiian language and could have been influenced by other pidgins of the Pacific Ocean region, such as Maritime Polynesian Pidgin.
Schütz [15] conjectured that a t-dialect existed in the northwestern islands, and a k-dialect in the southeastern islands. As of the 1820s, the [k] variant was becoming dominant on Oʻahu. [ 9 ] Helen Heffron Roberts documented a sound between that of English th , [ θ ] or [ ð ] , and [ z ] in free variation with [ k ] among elders from ...
The term is applied most often to regional speech patterns, but a dialect may also be defined by other factors, such as social class or ethnicity. [3] A dialect associated with a particular social class is called a sociolect ; one associated with a particular ethnic group is an ethnolect ; and a geographical or regional dialect is a regiolect ...
Nov. 30—Like many parts of the state socked by extra-wet weather Wednesday, the chamber level of the state Capitol got pretty drenched. Like many parts of the state socked by extra-wet weather ...
Trade winds blow from right to left in the image. The bottom image shows the ocean current formed by the islands’ wake. Arrows indicate current direction and speed, while white contours show ocean temperatures. The warm water of the current generates winds that sustain the current for thousands of miles. [13]