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The Apennines [2] or Apennine Mountains (/ ˈ æ p ə n aɪ n / AP-ə-nyne; Ancient Greek: Ἀπέννινα ὄρη or Ἀπέννινον ὄρος; [3] Latin: Appenninus or Apenninus Mons – a singular with plural meaning; [4] Italian: Appennini [appenˈniːni]) [note 1] are a mountain range consisting of parallel smaller chains extending c. 1,200 km (750 mi) the length of peninsular Italy.
In Italian phonemic distinction between long and short vowels is rare and limited to a few words and one morphological class, namely the pair composed by the first and third person of the historic past in verbs of the third conjugation—compare sentii (/senˈtiː/, "I felt/heard'), and sentì (/senˈti/, "he felt/heard").
This is the pronunciation key for IPA transcriptions of Italian on Wikipedia. It provides a set of symbols to represent the pronunciation of Italian in Wikipedia articles, and example words that illustrate the sounds that correspond to them.
The main watercourse in the valley is the Luretta river, 28 km long [5] and with a catchment area of 101.6 km². [6]The secondary network of tributaries of the Luretta consists of the Rio Tarone and the Rio Magnana on the orographic left and the Rio Canto, the Rio Sarturano and the Rio Frate on the orographic right.
Square brackets are used with phonetic notation, whether broad or narrow [17] – that is, for actual pronunciation, possibly including details of the pronunciation that may not be used for distinguishing words in the language being transcribed, but which the author nonetheless wishes to document. Such phonetic notation is the primary function ...
Satellite view of the peninsula in March 2003. The Italian peninsula (Italian: penisola italica or penisola italiana), also known as the Italic Peninsula, Apennine Peninsula, Italian Boot, or Mainland Italy, is a peninsula, within the Italian geographical region, extending from the southern Alps in the north to the central Mediterranean Sea in the south which comprises much of the country of ...
Around the Apennines and Sicily, late Miocene evaporites were left by the Messinian salinity crisis (for example, Gessosso-Solfifera Formation). [9] The opening of backarc basins like the Thyrrenian Sea caused the Calabro-Peloritan block to be separated from Sardinia, moving further south-east and finally included in the southern apenninic arc.
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