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During our fieldwork in 1979 we have focused our investigations on the area between Murodo-Terminal, Ryuo-bake, Yamasaki-Cirque, Tsurugi-Gozengoya and the New Fusaj i Hotel close to the JigokudaniSolfataras to the west and on the Kurobe-Daira to the east of Mt. Tateyama. There are four major localities where new stratigraphic observations have been possible: (1) A cliff-section to the east of Raicho-so exposes the strata of the plateau towards the ShomyoValley (Fig. 1, G, cf. map in Ono 1980). It is a 50-60 m high exposure containing a complex partially glacigenic stratigraphy. (2) The Yaeijo-Kanrisho-section is about 400 m to the north of the Raicho-so cliff (Fig. 1, H). The exposure is a 10-12 m high cliff containing a complex stratigraphy. (3) To the west of the New Fusaj i Hotel we reach the area of Jigokudani-Solf ataras, south of the ridge around Tateyama-renpo Lodge. This ridge (Fig. 1, I) is built of a till complex and is in close connection with volcanogenic stratae. The basin with the active solfataras in the upper and western part is partially filled with lake deposits. These lake sediments are dissected by the recent river erosion. The paleogeographically important unit of the lake sediments are bottom set deposits of well developed rhythmites. These laminated silts and clays (1 couplet is up to 2 cm) contain fossil leaves and needles of Pinus and volcanic bombs as dropstones. The lake sediment sequence is covered by the recent peat. (4) There is one outcrop in the area east of Mt. Tateyama which has to be mentioned here: It is a small cut directly behind the station of the Tateyama-Kurobe-Ropeway at Kurobe-Daira at the elevation of 1,830 m with two basal tills separated by a paleosoil. Morphology. (1) Most important was the observation of till of two different glaciations at Kurobe-Daira. That means that the wide

New evidence for multiglaciation in the high mountains of Japan. II. New observations in Tateyama.