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There are several lakes in Japan with permanently stagnated layers. Although in some of them stagnation is due either to sub lacustrine mineral springs or to entrance of sea-water (Yoshimura 1934), a few others, such as Lake Hangetu on the slope of Volcano Yotei (Ezohuzi) and probably Lake Ooike of the Tugaru Zyuniko Lake Group, Aomori Pref., come within the class mentioned by Findenegg 2' This paper deals with observations on two small ponds, Sindenmae Osikirenuma (abbrev. West Pond) and Gonzaemonura Osikirenuma (abbrev. East Pond), near Hatazaki, Miyagi Pref., 45 km NE of Sendai, ponds formed by water erosion following the collapse of the river bank during the great floods of 1875 and 1896. They are 5 m. above sea level, with areas only 1.1 (W. Pond) and 0.55 (E. Pond) ha, though fairly deep (11.5 and 9.1 m respectively). They are the second and third deepest lakes formed in this way in Japan. We visited these lakes three times during November, 19343' (Table

Kato- and Dichothermy during the Autumnal Circulation Period in Small Ponds of Miyagi Prefecture, Japan