Evaluation of stability and Marine Hazards Coastal zoning in southern province of Sistan and Baluchistan using

Abstract:
The study area in the South East of Iran in geological zone Makran. The geographical location of the study area in orbit 25 degrees 13 minutes north latitude and 60 degrees to 25 degrees and 25 minutes and 35 minutes to the meridian of 60 degrees and 55 minutes east is located.This area covers part of the northern coast of Oman Sea. In addition to marine risks, different risks of coastal Makransubduction zone, especially during faults, sea water and its harmful effects on coasts and ports affected are southern province and Sometimes destroys all obstacles on your own.In this study, using hydrological studies, tectonics, using satellite images and aerial photographs using GIS, mapping areas of high risk, low risk and safe to reduce marine and coastal hazards have been identified. One application for this research review Lifeline residential areas for relief is taken when necessary. For example, invasion routes tsunami, mud flows, floods, landslides and loss development in the region, degradation of coastal, safe and risky areas on land and in the South East coast's topography is predicted. Accordingly,in the regionsLipar, Chabaharandtees, thedestructionis high.Greatseabeach resortarea, parkTajMahal(downhill), a beautifulcity, townGolshahrspringandwavepower, you must first gentleuphillandthendownhillthroughtheturns, With increasingwaveheight, thefloodareasand allvitalarterywillbe cutanddamagesmultiplier. In the regionsRaminandbracewitha positiveslope (uphill), damagesand injuriesless(lowrisk) will be.Free industrial and trade zone in Chabahar is one of the safe areas (Such as emergency rooms, hospitals, blood transfusion services, airports, fire departments) should all be transmitted vital artery to Safe areas. It is necessary, lines of communication and highways, to avoid traffic and appropriate relief work to be constructed in the event of coastal hazards.
Language:
Persian
Published:
Journal of Geotechnical Geology, Volume:12 Issue: 2, 2016
Page:
1
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