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dc.contributor.authorSummers, Thomasen
dc.date.accessioned2018-03-29T12:20:32Z
dc.date.available2018-03-29T12:20:32Z
dc.date.issued1901en
dc.identifier.urihttp://hdl.handle.net/1842/29386
dc.description.abstracten
dc.description.abstractThe Fuleli Canal, to which the Escape has just been completed, connecting it with the Sea, and turning it from an Inundation Canal, flowing for six months in the year, into a perennial canal, owes its origin to an old branch of the River Indus, which ran in a tortuous course, as shewn on Plan No.l. from A, along the line A C D F E, flowing eventually back into the main channel of the river at the point E. This outlet into the river was closed by a dam in the time of the Mirs, the water being sent forward to feed other canals to the South.en
dc.publisherThe University of Edinburghen
dc.relation.isreferencedbyen
dc.subjectAnnexe Thesis Digitisation Project 2018 Block 17en
dc.titleFuleli escapeen
dc.typeThesis or Dissertationen
dc.type.qualificationlevelDoctoralen
dc.type.qualificationnameDSc Doctor of Scienceen


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