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  2. English prosody - Wikipedia

    en.wikipedia.org/wiki/English_prosody

    Overall the study of prosody has lagged other areas of linguistics. Within the study of English prosody, topics other than read speech and intonation have lagged. In any case, no comprehensive and complete description of English prosody is as yet available, [14] which makes prosody a challenge for both learners and teachers of English.

  3. Teaching prosody - Wikipedia

    en.wikipedia.org/wiki/Teaching_Prosody

    Prosody is an essential part of spoken language, and learners need often need help to perceive and produce the prosody of a new language. Prosody is, today, undertaught. [ 1 ] The improvement of prosody teaching is an active research area.

  4. Prosody (linguistics) - Wikipedia

    en.wikipedia.org/wiki/Prosody_(linguistics)

    In linguistics, prosody (/ ˈ p r ɒ s ə d i, ˈ p r ɒ z-/) [1] [2] is the study of elements of speech, including intonation, stress, rhythm and loudness, that occur simultaneously with individual phonetic segments: vowels and consonants.

  5. Metre (poetry) - Wikipedia

    en.wikipedia.org/wiki/Metre_(poetry)

    The study and the actual use of metres and forms of versification are both known as prosody. (Within linguistics , " prosody " is used in a more general sense that includes not only poetic metre but also the rhythmic aspects of prose , whether formal or informal, that vary from language to language, and sometimes between poetic traditions.)

  6. Isochrony - Wikipedia

    en.wikipedia.org/wiki/Isochrony

    Rhythm is an aspect of prosody, others being intonation, stress, and tempo of speech. [5] Isochrony refers to rhythmic division of time into equal portions by a language.The idea of was first expressed thus by Kenneth L. Pike in 1945, [6] though the concept of language naturally occurring in chronologically and rhythmically equal measures is found at least as early as 1775 (in Prosodia ...

  7. Stromatolite - Wikipedia

    en.wikipedia.org/wiki/Stromatolite

    Stromatolites are a major constituent of the fossil record of the first forms of life on Earth. [24] They peaked about 1.25 billion years ago (Ga) [ 22 ] and subsequently declined in abundance and diversity, [ 25 ] so that by the start of the Cambrian they had fallen to 20% of their peak.