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The caron can be placed over the vowels: ǎ, ě, ǐ, ǒ, ǔ, ǚ. The alternative to a caron is a number 3 after the syllable: hǎo = hao3, as the "falling-rising" tone is the third tone in Mandarin. The caron is used in the New Transliteration System of D'ni in the symbol š to represent the sound (English "sh").
Halwaxiida or halwaxiids is a proposed clade equivalent to the older orders Sachitida He 1980 [2] and Thambetolepidea Jell 1981, [3] loosely uniting scale-bearing Cambrian animals, which may lie in the stem group to molluscs or lophotrochozoa.
Ǧ (miniscule: ǧ ), called "G with caron", is a letter used in several Latin orthographies. [1] In the Romany and Skolt Sami languages, ...
Simply Jigsaw. Piece together a new jigsaw puzzle every day, complete with themes that follow the seasons and a super useful edges-only tool. By Masque Publishing
Ancient Greek phonology is the reconstructed phonology or pronunciation of Ancient Greek.This article mostly deals with the pronunciation of the standard Attic dialect of the fifth century BC, used by Plato and other Classical Greek writers, and touches on other dialects spoken at the same time or earlier.
These terms are useful in describing some inflection patterns and other morphological processes, but exact definitions of "soft" and "hard" may differ somewhat. "Soft" generally refers to the palatal nature of a consonant. The alveolo-palatal sounds ń, ś, ź, ć, dź are considered soft, as normally is the palatal j .
The caron on a vowel represents palatalisation; ǒ and ǎ are pronounced /o/ and /a/ in Lovaricka, but /jo/ and /ja/ in Kalderash. [ 4 ] The three "morpho-graphs" are ç , q . and θ , which represent the initial phonemes of a number of case suffixes, which are realised /s/ , /k/ and /t/ after a vowel and /ts/ , /ɡ/ and /d/ after a nasal ...
The Burgess Shale is a series of sediment deposits spread over a vertical distance of hundreds of metres, extending laterally for at least 50 kilometres (30 mi). [18] The deposits were originally laid down on the floor of a shallow sea; during the Late Cretaceous Laramide orogeny, mountain-building processes squeezed the sediments upwards to their current position at around 2,500 metres (8,000 ...