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Brebes Sundanese (Sundanese: Basa Sunda Brebes, Sundanese pronunciation: [basa sʊnda brəbəs], in Sundanese script: ᮘᮞ ᮞᮥᮔ᮪ᮓ ᮘᮢᮨᮘᮨᮞ᮪) is the dialect of Sundanese language used by some people in Brebes Regency, Central Java, [3] [4] especially in the southern and southwestern parts of the region.
Until 1600 AD, Sundanese was the state language in the kingdoms of Salakanagara, Tarumanagara, Sunda, Galuh, Pajajaran, and Sumedang Larang. During this period, Sundanese was heavily influenced by the Sanskrit language as seen in the Batu Tapak Kaki Kiri Nyoreang inscription at the time of King Purnawarman , using the Pallava script .
Old Sundanese (Sundanese script: ᮘᮞ ᮞᮥᮔ᮪ᮓ ᮘᮥᮠᮥᮔ᮪, Old Sundanese script: , Buda script: , Roman script: Basa Sunda Buhun) is the earliest recorded stage of the Sundanese language which is spoken in the western part of Java, Indonesia.
The Sundanese (Indonesian: Orang Sunda; Sundanese: ᮅᮛᮀ ᮞᮥᮔ᮪ᮓ, romanized: Urang Sunda) are an Austronesian ethnic group native to western region of Java island in Indonesia, primarily West Java. They number approximately 42 million and form Indonesia's second most populous ethnic group.
A Bantenese diaspora in Taiwan speaking Bantenese.. Banten Sundanese or Bantenese (Basa Sunda Banten or Basa Wewengkon Banten) is one of the Sundanese dialects spoken predominantly by the Bantenese — an indigenous ethnic group native to Banten — in the westernmost region of the island of Java, and in the western Bogor Regency (especially in Jasinga, [2] the districts of Cigudeg, Tenjo ...
Tembang sunda, also called seni mamaos cianjuran, is a style of classical vocal music that originated in the Priangan highland of western Java. Unlike Sundanese gamelan music, tembang sunda was developed in the court of the regent Kabupaten Cianjur during the Dutch colonial period (mid-nineteenth century).
The Sahul Shelf and the Sunda Shelf today. The area in between is called "Wallacea"Sundaland [1] (also called Sundaica or the Sundaic region) is a biogeographical region of Southeast Asia corresponding to a larger landmass that was exposed throughout the last 2.6 million years during periods when sea levels were lower.
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