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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.
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 .
Standard Sundanese script (Aksara Sunda Baku, ᮃᮊ᮪ᮞᮛ ᮞᮥᮔ᮪ᮓ ᮘᮊᮥ) is a traditional writing system used by Sundanese people to write Sundanese language. It is built based on Old Sundanese script ( Aksara Sunda Kuno ) which was used from the 14th to the 18th centuries.
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.
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.
Wawacan Sulanjana is a Sundanese manuscript containing Sundanese myths. The title means "The Tale of Sulanjana", derived from the name of the hero Sulanjana as the protector of rice plant against the attack of Sapi Gumarang cow, Kalabuat and Budug Basu boars symbolizing rice pestilence.
Old Sundanese script (Sundanese: ᮃᮊ᮪ᮞᮛ ᮞᮥᮔ᮪ᮓ ᮘᮥᮠᮥᮔ᮪, romanized: Aksara Sunda Buhun) is a script that developed in West Java in the 14th–18th centuries which was originally used to write Old Sundanese language.
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.