Science Fair Project Encyclopedia
Canaanite languages
The Canaanite languages are a subfamily of the Semitic languages, spoken by the ancient peoples of the Canaan region, including Canaanites, Hebrews, Phoenicians, and eventually Philistines. All of them became extinct as native languages in the early first millennium AD, although Hebrew remained in literary and religious use among Jews, and has been revived in the twentieth century. The Phoenician (and especially Carthaginian) expansion spread their Canaanite language to the Western Mediterranean for a time, but there too it died out, although it seems to have survived slightly longer than in Phoenicia itself.
- Ammonite language - extinct
- Moabite language - extinct
- Edomite language - extinct
- Hebrew language - live descendants
- Phoenician languages - extinct
- Punic language - extinct
The main sources for study of Canaanite languages are the Hebrew Bible (Tanakh), and inscriptions such as:
- in the Moabite language: Mesha Stele, El-Kerak Stela
- in the Biblical Hebrew language: Gezer Calendar
- in the Phoenician languages: Ahiram inscription ,sarcophagus of Eshmunazar[1], Kilamuwa inscription , the Byblos inscription
- in later Punic language: in Poenulus - by Plautus - beginning of 5th-Act.
The extra-biblical Canaanite inscriptions are gathered along with Aramaic inscriptions in editions of the book "Kanaanäische und Aramäische Inschriften ", from which they may be referenced as KAI n (for a number n); for example, the Mesha Stele is "KAI 181".
The Canaanite languages, together with the Aramaic languages, form the Northwest Semitic subgroup. Some distinctive features of Canaanite in relation to Aramaic are:
- The prefix 'h-' used as the definite article (whereas Aramaic has a postfixed -a). This seems to be an innovation of Canaanite.
- The first person pronoun being 'ʾnk' (אנכ - anok(i)) (versus Aramaic - ʾnʾ/ʾny) - which is similiar to Akkadian; this is a common retention from proto-Afro-Asiatic.
External links
The contents of this article is licensed from www.wikipedia.org under the GNU Free Documentation License. Click here to see the transparent copy and copyright details


