경남 함안 조남산 동쪽사면의 사면물질이동 발생사 - 함안 성산산성을 사례로 -
The History of Mass-Movement on the Eastern Slope of Mt. Jonam in Haman, Gyeongnam Province - A Case of the Seongsan Sanseong Fortress in Haman -
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초록
This study is to restore the history of movement mass material (hereinafter called ‘mass movement’) on the eastern slope of Mt. Jonam(139.4m a.s.l.) in Haman, Gyeongnam province. For this purpose, grain size analysis, stratiform interpretation and stratigraphic interpretation were carried out and the previous archaeological data were reviewed for the valley deposits of Seongsan Sanseong Fortress(hereinafter mountain fortress) in Haman. The results are as follows. Various inorganic layers(12 layers, 6 sublayers) and organic layers (4 layers) were observed in the valley deposits of the mountain fortress. The inorganic layer was found to have been transported and deposited to the valley by erosion (or denudation) from the back slope surrounding the mountain fortress during ‘the instability period of hillslope’ where mass movement of the slope occurred. Also, it is thought that most of the organic layer was formed on the valley surface at the time when the hillslope was stable because the mass movement was inactive. From the above results, it was found that the eastern slope of Mt. Jonam has at least 12 times of mass movement during the instability period of the slope.
Abstract
This study is to restore the history of movement mass material (hereinafter called ‘mass movement’) on the eastern slope of Mt. Jonam(139.4m a.s.l.) in Haman, Gyeongnam province. For this purpose, grain size analysis, stratiform interpretation and stratigraphic interpretation were carried out and the previous archaeological data were reviewed for the valley deposits of Seongsan Sanseong Fortress(hereinafter mountain fortress) in Haman. The results are as follows. Various inorganic layers(12 layers, 6 sublayers) and organic layers (4 layers) were observed in the valley deposits of the mountain fortress. The inorganic layer was found to have been transported and deposited to the valley by erosion (or denudation) from the back slope surrounding the mountain fortress during ‘the instability period of hillslope’ where mass movement of the slope occurred. Also, it is thought that most of the organic layer was formed on the valley surface at the time when the hillslope was stable because the mass movement was inactive. From the above results, it was found that the eastern slope of Mt. Jonam has at least 12 times of mass movement during the instability period of the slope.
참고문헌 (16)
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