ðə ɹˈæpɪdz ɪnðə hˈaɪ ɹˈaɪn ʃˌʊd biː vjˈuːd ɪnðə kˈɑːntɛkst ʌvðə ɹˈɛlətˌɪvli hˈaɪ slˈoʊp—fɹʌm əbˌʌv sˈiː lˈɛvəl ɪn dʒˈʌst —ænd ðə tʃˈeɪndʒ ʌvðə ɹˈɪvɚz kˈoːɹs dˈʊɹɹɪŋ ðə wˈuːəm ˈaɪs ˈeɪdʒ.
The rapids in the High Rhine should be viewed in the context of the relatively high slope—from  above sea level in just —and the change of the river's course during the Würm ice age.