Triangles: 1.1M
Vertices: 558.7k
More model information藤六の海底地すべり跡(埼玉県秩父市下吉田)
新生代新第三紀の古秩父盆地に堆積した砂岩泥岩互層。当時の海底斜面において地滑りが発生し、半固結状態の地層が部分的に褶曲したスランプ構造が見られます。
Slump structure at Toroku (Shimoyoshida, Chichibu-shi, Saitama-ken)
Alternating beds of sandstone and mudstone deposited on the Paleo-Chichibu Basin in the Neogene Period, Cenozoic Era. Remarkable slump structures were formed by the sliding of the semi-consolidated sediments on the sea-floor slope.
36°01‘31”N, 139°02‘32”E
Comments