1 AIT Asian Institute of Technology

Urban geology and land use of Yangon city, Myanmar

AuthorSan San Win
Call NumberAIT Thesis no. GT-91-27
Subject(s)Urban geology--Myanmar--Yangon
Land use, Urban--Myanmar--Yangon

NoteA thesis submitted in partial fulfillment of the requirements for the degree of Master of Science, School of Engineering and Technology
PublisherAsian Institute of Technology
Series StatementThesis ; no. GT-91-27
AbstractYangon is located on the Yangon Ridge which is the southern extremity of a long narrow spur of the Bago (Pegu) Yomas . Physiographically, the a1·ea consists of NNW-SSE trending hill with elevation ranging from 24 to 40 m above mean sea level, marine terrace II, marine terrace I and lowland tidal flat. The Quaternary s urficial deposits, which overlies Tertiary rocl< units consist of alluvial and estuarine deposits, tidal fl at deposits, marine terrace deposits and residual soil. The season al flooded area li es along the Hlaing-Yangon River and PazundaungNgemoyeil< Creel<. Flooding occurs clue to heavy rainfall , tidal effects, river discharge and fluctuation of 1·iver level a ncl improper drainage system. Landslides occur particularly at elevation more than 24 m above mean sea level along the ridge and slope-cu t alongside the rail and motor roads. The types of landslide are generally earthflow, slump, creep a nd combination of them . The Yangon area lies in a fairly active seismic and seis micity is found to range between VI to IX grades of Modified Mercalli Intensity Scale.
Year1991
Corresponding Series Added EntryAsian Institute of Technology. Thesis ; no. GT-91-27
TypeThesis
SchoolSchool of Engineering and Technology (SET)
DepartmentDepartment of Civil and Infrastucture Engineering (DCIE)
Academic Program/FoSGeotechnical and Transportation Engineering (GT)
Chairperson(s)Prinya Nutalaya;
Examination Committee(s)Balasubramaniam, A. S.;Honjo, Yusuke;Noppadol Phien- weja;
Scholarship Donor(s)Government of Finland;
DegreeThesis (M.Sc.) - Asian Institute of Technology


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