Survey of Glacial Processes Function Using of Statistical Analysis Wandering Rocks Diameter (Case Study: Eslamieh(Farashah) Village, Taft township)

Glacier impacts are the most important evidence that climate change Quaternary period. That Geomorphological phenomenon in the Earth's crust on the outer surface are left. Because they can be reconstructed past climate (Ramesht and Kazemi, 2008: 1). Central plateau of Iran, has dry to very dry conditions. Geomorphologic evidence shows significant changes in climate and natural conditions of the region occurred during the Quaternary. The situation today is very different from that sometimes. Evidence remains of the Quaternary period, such Syrkhay glacier, river and lake terraces, alluvial fans, and fossilized. .., show the Quaternary climatic changes. Glacialmorans geomorphologic effects, which are seen in the study area. However, results of studies on glacial forms, has had important results. Quantitative measure rarely used and ever the results classic approach is used in the formation of these forms. This study attempts to use quantitative and statistical models to answer the question whether the process has existed except glacial processes in creation of this landscape?