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The Jangdo high moor is an island and natural mountainous wetland in the Republic of Korea, which is located in the marine island ecosystem about 100 km from the Korean Peninsula. The Jangdo Island high moor is the only high moor on an island in Republic of Korea. The site is formed as a large piece on top of the island and also largest in unite area of high moor in ROK. This is unique as other high moor lands are composed of small separated pieces of moor lands. ==Formation== It was preliminarily considered that Jangdo wetland was a concave landform formed by the weathering of granite intruding Precambrian silicified metasedimentary rocks. Various granite-weathered topography was observed. The formation scenario of Jangdo wetland is as follows. By flood or slope mass movement of regolith, rock fragments were moved to form a low-relief slope landform. As a result, wetland was formed. By analyzing the slope soil and wetland sediment, we conjectured that Jangdo wetland depended on the influence of peripheral slope soil. In these concavelandform environment, the supply of water and organic materials was sustained for a long time to form an organicnondegradable wetland environment. In addition, the plants appropriate to this wetland environment were settled to thicken the wetland. This is how the present Jangdo wetland was thought to be formed. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Sinan Jangdo High Moor」の詳細全文を読む スポンサード リンク
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