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Most sediments are clayey silt, and six samples are silty clay. C-M pattern diagram of these sediments indicates that the most sediments are pelagic or hemipelagic, transported by suspension. Silty clay sediments whose median grain-size are larger than 8.0 phi, are distributed in a small elongated area off the Momigasaki. The locality is not the center of the lake but also not the deepest part of the lake. Such a distribution pattern seems to be related to some flow mechanisms such as a circulation current. Sediment of ST-3 off the mouth of the River Sugakawa is sandy silt. It probably results from the pour of the river. Sample of ST-31 taken from the subsurface terrace at 20 meters deep is ill-sorted gravelly sand. It seems to be relict sediment or old debris flow deposit. Sediment of ST-35 is muddy sand. It is near the southern margin of the basin plain of 36 to 38 meters in depth. 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