IntroductionForest fires are one of the most important natural or anthropogenic events for grazing and forestry in dry lands. Extreme weather or climate change, usually characterized by hot and dry summers, is associated with high levels of forest fires. Another important issue is strong summer winds causing fires to spread at high speeds. Bassi and Kettunen ( 2008) stated that research on climate change indicated that increased fire hazards were likely to arise from global warming. Moreover, a combination of livestock grazing, fire exclusion, and logging disturbances has resulted in increases in tree density, canopy closure, vertical diversity, aerial fuel continuity, and surface fuel loads (Covington and Moore, 1994). As a consequence of these events and increasing human impact, the history of fire within a region and how these fires impact forests has become important information.Tree rings are one of the most comprehensive tools to find the years of past wildfires, their frequency, and their areas (Swetnam and Dieterich, 1983). In recent decades, fire events, their statistics, and magnitudes have been recorded throughout the world. Using tree rings the histories of many fires were determined in some dry lands in the United States and Europe (