تغییرات محیطی بعد از رخداد زمین لغزش کبیرکوه و تاثیر آن در شکل­گیری محوطه‌های باستانی محدودة دریاچة جایدر

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تغییرات محیطی بعد از رخداد زمین لغزش کبیرکوه و تاثیر آن در شکلگیری محوطه‌های باستانی محدودة دریاچة جایدر


نویسنده	مقصودی مهران ,شرفی سیامک ,یمانی مجتبی ,مقدم عباس ,زمانزاده محمد
منبع	كواترنري ايران - 1394 - دوره : 1 - شماره : 1 - صفحه:1 -14
چکیده	کوهستان زاگرس در بخش مرکزی با محیط جغرافیایی مساعد، مکان مناسبی برای شکل‌گیری استقرارها و جوامع انسانی است. وابستگی شدید جوامع انسانی این منطقه به محیط طبیعی سبب شده تا همواره تحت تاثیر شرایط محیطی و تغییرات ناشی از آن قرارگیرند. تغییر محیطی اوایل دورة هولوسن در نتیجة رخداد زمین‌لغزش کبیرکوه و متعاقب آن شکل‌گیری دریاچه‌های سیمره و جایدر، از جمله تغییرات محیطی است که طی هزاران سال الگوهای استقراری جوامع انسانی منطقه را تحت تاثیر قرار داده است. محدودة مورد مطالعه دریاچة جایدر و روش تحقیق توصیفی- تحلیلی و میدانی بود. از ابزارهایی مانند نقشه‌های توپوگرافی، زمین‌شناسی، تصاویر ماهواره‌ای، gps و نرم‌افزارهای arc gis و global mapper جهت بررسی تغییر الگوی استقرار محوطه‌های باستانی استفاده شده است. مطالعة 27 محوطة باستانی شناسایی شده در حوضة رسوب‌گذاری دریاچة جایدر از یک‌سو منجر به شناخت الگوهای استقراری متفاوتی طی دورة زمانی فراپارینه‌سنگی تا اواخر دوران اسلامی در این محدوده شد؛ و از سوی دیگر، شناخت الگوهای استقراری طی این دوران، باعث روشن شدن وضعیت تغییرات محیطی حوضة رسوب‌گذاری دریاچة جایدر شد. نتایج نشان داد که الگوی استقرار محوطه‌های باستانی بعد از رخداد زمین‌لغزش کبیرکوه و تشکیل دریاچة جایدر، از دورة فراپارینه‌سنگی تا اواخر دوران اسلامی به تبعیت از تغییرات سطح آب دریاچه و ضخامت رسوبات پادگانة دریاچه بوده است.
کلیدواژه	جبر محیطی ,دریاچة جایدر ,زمین‌باستان‌شناسی ,محوطه‌های باستانی
آدرس	دانشگاه تهران, دانشکده جغرافیا, ایران, دانشگاه تهران, ایران, دانشگاه تهران, دانشکده جغرافیا, ایران, پژوهشکده باستان شناسی کشور, ایران, دانشگاه تهران, دانشکده جغرافیا, ایران
پست الکترونیکی	maghsoud@ut.ac.ir



Authors	maghsoudi Mehran ,sharafi Siyamack ,Yamani Mojtaba ,moghadam Abbas ,zamanzadeh mohammad
Abstract	Abstract:Central Zagros Mountains regarding to their proper geographical location, have provided suitable locations for establishment and development of human societies. High dependence of the societies of this region on the natural environment has caused these communities to be affected by environmental conditions and changes. Environmental changes during the early Holocene period as results of the occurrence of landslides mountain Kabir kuh and the subsequent formation of the Jaydar and Seymareh lakes are among the environmental changes that affect the settlement patterns of the inhabitants of this region over thousands of years. The Jaydar Lake is considered to be studied field and descriptive analytical research methods along with tools such as topographic maps, geologic, satellite images, GPS and other software like Arc GIS and Global Mapper are used to assess the changing process of the settlement patterns of archaeological sites. The study of 27 identified archaeological sites in basin sedimentation of the Jaydr lake in one hand, has led to the identification of different settlement patterns during the late Paleolithic period to the Late Islamic period in this region, and in other hand there cognition of settlement patterns during this periods have clarified the status of environmental changes of sedimentation basin of the Jaydr lake.1 IntroductionGeographical and natural potentials of Zagros and archaeological findings from the studies suggest that this cultural area has been used for human societies from pre history to the present days. Many devastating earthquakes (The earthquake of 872 AD Saymareh) and a lot of landslides in the Zagros, caused severe environmental changes in this region. Landslide occurrence in Kabir Kuh,blocking the Kashkan and Seymareh river and subsequently formation of the Jaydar and Saymareh lake are among the most important environmental changes in this region.Kashkan River is one of the environments that provides a suitable environment to settlement in this area from past to the present. But environmental changes, especially Kashkan river redirections and formation of the Jaydar Lake, had significant effects on the settlement pattern of archaeological environments in the past. Therefore, the aim of this study is to investigate changes in settlement patterns of archaeological sites in the area of the jaydar lake after occurrence of kabir kuh landslide.2 Materials and methodsThe Jaydar Lake located in the western parts of Pole Dokhtar is considered as studied area. Field and descriptive analytical research methods along with tools such as topographic maps, geologic, satellite images, GPS and other software like Arc GIS and Global Mapper are used to assess the changing process of the settlement patterns of archaeological sites. Then, extensive field studies have been done in the area and with observing the lake deposits at several points on the periphery of Khorramabad Poldokhtar road and then recording their heights, Lakes area has been drawn based on 740 meter contour.In the next stage, the position and period of archaeological sites on the lake area have been overlapped and using investigation of the height and thickness changes of sediments in the lake, the settlement pattern changes of the archaeological sites after formation of Jaydar Lake during the different periods have been analyzed. Finally, at the end of this study the results are presented.3 Results and discussionkabirkuh Landslide, is the world's largest landslide and based on Thermoluminescence dating method on deep lake sediments les of Saymareh lake, Kabir Kuh landslide time has been determined equal to about 15700 ± 2500 years. After the occurrence of landslides and blocking Kashkan river, Jaydar lake has been formed behind apile of sediments slide. Jaydar lake formation has coincided with the formation of the first stage of Saymareh lake. Because only in the first step, landslides had the most volume and vastness so that it blocked the Kashkan river path. Based on field studies Jaydar Lake area is calculated around 88 square kilometers. Chronologically, 27 archaeological sites have been identified in the area Show that archaeological sites have been created in the prehistoric, historic and Islamice period.The distribution pattern of the identified 27 Archaeological sites show that all the ancients ites are located in adjacent too rat a distance of less than 1000 meters far from the Kashkan River. Proximity to the waterand flatness of its surface have been the most important factors that affect the formation and distribution of archaeological sites adjacent to the lake. Other factors such as topography and fertile land are important in the formation of archaeological sites, have been affected by the water level of the lake and then by the river. So that the rise in water level is directly related to the height of archaeological site and the fertile lands in the margin of river.Investigating changes in the height and thickness of the lake sediments show that in the Bronze period we can observe the formation of a permanent establishment(or perhaps semi permanent establishment) and adjacent cemetery for the first time. In addition, during this period we can see the formation of archaeological site on these dimentary terrace at the end of these dimentation basin of Jaydar lakes.4 ConclusionThe study of 27archaeological sites from the EpiPaleolithic period to the late of the Islamic period in the Jaydar lake sedimentation area showed that during this period, major changes in the settlement pattern of archaeological sites in the lake area have been occurred. All of these changes are directly related to the occurrence of kabir kuh landslides and the subsequent formation of Jaydar lake and its remaining sediments.Gradual risein water level, brought about loss of 6 human kind settlements in the late period of Epipaleolithic with average height of 695 meters from the open waters of in the lake margin and for cible migration to more elevated areas. It looks like that water in the Neolithic period reach to its highest level, 740 meters,and up to the end of this period remains at the same level. With beginning of the Chalcolithic period the height of the archaeological site areais reducedand areas that have already been buriedunder the water, in this period once they become residential. Formation of the first permanent settlement with in the Jaydar lake, coincides with the Bronze Age. In addition, residents of this area in this period of time for the first time build graveson lake and river sediments. Two periods of drought during the Iron Age cause the formation of Iron Age sites in the alluvium mountain path and near the river Kashkan. In the historical period(Achaemenid, Parthianand, Sasanian) much of the lake sediments(probably up to the entrance of Poldokhtar) have been dried. In historical period, archaeological sites to access the river have been formed in the closest parts to the river.The pattern of settlement in the early Islamic periodis not much different from the previous period. But at the end of the Islamic period and After over 5000 years, the basin sediments of Jaydar lake are dried and conditions for the formation of new settlements especially in the Jaydar plain area are provided.
Keywords	Environmental determinism ,Jaydar Lake ,Geoarchaeology ,Archaeological site