ænd ɐ wˈaɪd ɹˈeɪndʒ ʌv ˈʌðɚ fˈeɪzᵻz, ɪz wˌaɪ ðə pɹˈɛzənt ˈaʊtkɹɑːp ʌvðə sənt ˈɔːstɛl ɡɹˈænɪt ɪz kənsˈɪdɚd tə hɐvbɪn klˈoʊs tə ðə ɹˈuːf ʌvðɪ ɪntɹˈuːʒən.
and a wide range of other phases, is why the present outcrop of the St Austell granite is considered to have been close to the roof of the intrusion.