Petrological Characteristics and Procurement Route of the Rocks Used to Construct Munsusanseong, Gimpo
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This study aimed to identify and determine the source and procurement route of the rocks used to construct the western rampart castellation and west gate of the Munsusanseong Fortress in Gimpo. Granodiorite, quartzite, schist, and sandstone or pebbly sandstone, identified as the construction rocks, were characterized according to occurrence, magnetic susceptibility, constituent mineral types and textures, and geochemical characteristics. A geological survey of the Munsusan Formation in the vicinity of Munsusanseong and the southern Ganghwa region was undertaken. The sandstone or pebbly sandstone was probably sourced locally; however, the granodiorite is believed to have been sourced externally from southern Ganghwa in the vicinity of Bunori Dondae, another historic fortress, from petrologically and geomorphologically similar granodiorite. Many traces of rock quarrying were observed on a shore platform in this area, and it is believed that the procurement route was via the Yeomha River. This indicates that at the time of construction, during the late Joseon dynasty, economic power and labor mobilization were centered in Ganghwa and its surrounding areas.
Abstract
This study aimed to identify and determine the source and procurement route of the rocks used to construct the western rampart castellation and west gate of the Munsusanseong Fortress in Gimpo. Granodiorite, quartzite, schist, and sandstone or pebbly sandstone, identified as the construction rocks, were characterized according to occurrence, magnetic susceptibility, constituent mineral types and textures, and geochemical characteristics. A geological survey of the Munsusan Formation in the vicinity of Munsusanseong and the southern Ganghwa region was undertaken. The sandstone or pebbly sandstone was probably sourced locally; however, the granodiorite is believed to have been sourced externally from southern Ganghwa in the vicinity of Bunori Dondae, another historic fortress, from petrologically and geomorphologically similar granodiorite. Many traces of rock quarrying were observed on a shore platform in this area, and it is believed that the procurement route was via the Yeomha River. This indicates that at the time of construction, during the late Joseon dynasty, economic power and labor mobilization were centered in Ganghwa and its surrounding areas.
참고문헌 (12)
- Gimpo Munsusanseong Fortress, presumed Three Kingdoms period wall excavation investigation, "An, S. H.", Central Archeological Society, Site Investigation Presentation, 296~303 (2014)
- Tongjin geological survey report, "Choi, W. C.", Korea Institute of Mineral Resources, ~ (1997)
- Brief report on the excavation of the western wall section of Gimpo Munsusanseong Fortress, "Gukto Institute of Cultural Heritage", 40~ (2020)
- Geological report of the Ganghwa-Onsuri sheet (1: 50000), "Hwang, J. H.", Korea Institute of Geoscience and Mineral Resourvces, 1~20 (2005)
- Choi, G. J., "Petrological characteristics and deterioration aspect of the Goryeong Yangjeondong petroglyph", Journal of Conservation Science, 25, pp.131~145 (2009)
- Herron, M. M., "Geochemical classification of terrigenous sands and shales from core and log data", Journal of Sedimentary Petrology, 58, pp.820~829 (1988)
- Shin, H. K., "Review in terms of the earthen wall stamped technique in the Three Kingdoms period", MUNHWAJAE, 55, pp.38~53 (2022)
- Irvine, T. N., "A guide to the chemical classification of the common volcanic rocks", Canadian Journal of Earth Science, 8, pp.523~548 (1971)
- Pettijohn, F. J., "Sedimentary rocks", pp.628~ (1975), Harper & Row Publishers
- Lee, S. O., "Analysis of the mix ratio mortar used in Joseon Dynasty Seongnam Godeung-dong Barrier Tombs", MUNHWAJAE, 53, pp.34~51 (2020)
- Le Maitre, R. W., "The chemical variability of some common igneous rocks", Journal of Petrology, 17, pp.589~637 (1976)
- Park, J. A., "Sandstone composition and paleoclimate of Cretaceous Jinju and Iljig formations of the western Euiseong area in the northern part of Kyongsang Basin", Journal Petrological Society of Korea, 6, pp.111~122 (1997)
