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Purapporul Venbamaalai (Tamil: புறப்பொருள் வெண்பாமாலை) is a medieval Tamil text on the grammar of the puram (lit. "external ...
A. H. Arden, A progressive grammar of the Tamil language, 5th edition, 1942. Schiffman, Harold F. (1998). A Reference Grammar of Spoken Tamil (PDF). Cambridge University Press. pp. 20– 21. ISBN 978-0-521-64074-9. Archived (PDF) from the original on 11 April 2024. Lehmann, Thomas. A Grammar of Modern Tamil. Pondicherry Institute of Linguistics ...
Tamil Lexicon (Tamil: தமிழ்ப் பேரகராதி Tamiḻ Pērakarāti) is a twelve-volume dictionary of the Tamil language. Published by the University of Madras , it is said to be the most comprehensive dictionary of the Tamil language to date.
The List of Tamil Proverbs consists of some of the commonly used by Tamil people and their diaspora all over the world. [1] There were thousands and thousands of proverbs were used by Tamil people, it is harder to list all in one single article, the list shows a few proverbs.
Naṉṉūl (Tamil: நன்னூல்) is a work on Tamil grammar written by a Jain ascetic [1] Pavananthi Munivar around 13th century CE. [2] It is the most significant work on Tamil grammar after Tolkāppiyam. [2] The work credits Western Ganga vassal king Seeya Gangan of Kolar with patronising it. [3] [4]
Venpa or Venba (வெண்பா in Tamil) is a form of classical Tamil poetry. Classical Tamil poetry has been classified based upon the rules of metric prosody. [1] Such rules form a context-free grammar. Every venba consists of between two and twelve lines.
Sculpture of Vishnu Measuring the Earth in Mahabalipuram Dating 7th Century CE.. The short poem mentions the Hindu god Vishnu through an elaborate simile. [7] [8] [9] The text mentions that The clouds resemble Vishnu in three points: (1) the clouds are black like the dark god, (2) they encompass the hills even as Vishnu encompasses the earth; (3) they pour rain as the water dripped from the ...
The band of precipitation that is associated with their warm front is often extensive, forced by weak upward vertical motion of air over the frontal boundary which condenses as it cools and produces precipitation within an elongated band, [63] which is wide and stratiform, meaning falling out of nimbostratus clouds.