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Information Journal Paper

Title

RECONSTRUCTION OF QUATERNARY PALEO LAKE LEVELS OF URMIA BY STUDYING LAKE TERRACES

Pages

 Start Page 1 | End Page 3

Abstract

 Introduction: LAKE TERRACEs are geomorphological evidence of climate change during QUATERNARY. Location of these terraces location in different elevation shows paleo water lake level fluctuations. Investigation about Urmia LAKE TERRACEs was conducted by Bobek (1973).He found those terraces in 45-55 meter above Urmia water level on that time. According to Bobek, development of lake area in paleo Pleistocene period and cold Pleistocene periods was caused by reduction of temperature about 5 centigrade and reduction of evaporation. It is important that we don’t have any comprehensive investigation on Urmia LAKE TERRACEs and many of these terraces and paleo shorelines remained unknown up to now. The aims of this research investigation of QUATERNARY terraces of URMIA LAKE represent their elevations and reconstruction of the areas affected by these fluctuations.

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