Answer: Ghareeb Nawaz, or reverently as a Shaykh Muʿīn al-Dīn or Muʿīn al-Dīn or Khwājā Muʿīn al-Dīn (Urdu: معین الدین چشتی) by Muslims of the Indian subcontinent, was a Persian Muslim[3] preacher,[6] ascetic, religious scholar, philosopher, and mystic from Sistan,[6] who eventually ended up settling in the Indian subcontinent in the early 13th-century, where he promulgated the famous Chishtiyya order of Sunni mysticism.[6][7] This particular tariqa (order) became the dominant Muslim spiritual group in medieval India and many of the most beloved and venerated Indian Sunni saints[4][8][9] were Chishti in their affiliation, including Nizamuddin Awliya (d. 1325) and Amir Khusrow (d. 1325).[6] As such, Muʿīn al-Dīn Chishtī's legacy rests primarily on his having been "one of the most outstanding figures in the annals of Islamic mysticism."[2] Additionally Muʿīn al-Dīn Chishtī is also notable, according to John Esposito, for having been one of the first major Islamic mystics to formally allow his followers to incorporate the "use of music" in their devotions, liturgies, and hymns to God, which he did in order to make the foreign Arab faith more relatable to the indigenous peoples who had recently entered the religion or whom he sought to convert.[10] Others contest that the Chisti order ever permitted musical instruments and a famous Chisti, Nizamuddin Auliya, is quoted as stating that musical instruments are prohibited.
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GLACIAL DEPOSITS
Today, glacial deposits formed during the Permo-Carboniferous glaciation (about 300 million years ago) are found in Antarctica, Africa, South America, India and Australia. If the continents haven’t moved, then this would suggest an ice sheet extended from the south pole to the equator at this time - which is unlikely as the UK at this time was also close to the equator and has extensive coal and limestone deposits. If the continents of the southern hemisphere are re-assembled near the south pole, then the Permo-Carboniferous ice sheet assumes a much more reasonable size.
More evidence comes from glacial striations – scratches on the bedrock made by blocks of rock embedded in the ice as the glacier moves. These show the direction of the glacier, and suggest the ice flowed from a single central point.