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The NW coast AB of the central island, together with the chain of volcanoes A'B', starting from theneighbourhood of fossa magna to Hokkaido, lie on two spirals, with the pole near the central depression, which for convenience sake may be called Yamato Basin in association with Yamato Bank on the main line of fissure2) M, that gave rise to fossa magna. AB has a branch ab, beginning from the great volcano Chokai, and crosses Iwakisan to Hokkaido. There is a third arc A'B', including many volcanoes, of which Asama and Bandaisan are the most remarkable. On the other side lies the arc CD along the coast of Kaga and Echizen, and a small one C'D' on the Wakasa coast nearly parallel to it. The arc AB has two small portions slightly projecting out of Echigo, and further north another near Hachirogata. These are often disturbed by weak earthquakes, showing that the non-osculating portion is somewhat unstable. The arcs AB, A'B' and CD end near the fissure line M, as is naturally to be expected. The Wakasa coast is characte rized by jagged appearance, indicating the formation of slip lines nearly parallel to CD ; such slip lines are usually found in test pieces. From the geological aspect, the slip lines ab, A'B' have many volcanoes in

Continental Margins as Slip Lines: Formation of Japanese Arcs and Deep Seated Earthquakes