
Originally, the island was a narrow and long piece of land called Majoli (land in the middle of two parallel rivers) that had Brahmaputra flowing in the north and the Burhidihing flowing in the south, till they met at Lakhu. Frequent earthquakes in the period 1661–1696 set the stage for a catastrophic flood in 1750 that continued for 15 days, which is mentioned in historical texts and reflected in folklore. As a result of this flood, the Brahmaputra split into two anabranches—one flowing along the original channel and the other flowing along the Burhidihing channel and the MÄjuli island was formed. The Burhidihing's point of confluence moved 190 km east and the southern channel which was the Burhidihing became the Burhi Xuti. The northern channel, which was previously the Brahmaputra, became the Luit Xuti. In due course, the flow in the Luit Xuti decreased, and it came to be known as the Kherkutia Xuti; and the Burhi Xuti expanded via erosion to become the main Brahmaputra river.