Fig. 6From: Formation of undulating topography and gravel beds at the bases of incised valleys: Last Glacial Maximum examples beneath the lowlands facing Tokyo BayCross sections of lithology (upper section in each figure part) and N value (lower section in each figure part) in the Tama River Lowland (sections AA’, BB’, and CC’), the Tsurumi River Lowland (section DD’), the Owoka and Katabira river lowlands (section EE’), and the Tokyo Lowland (section FF’). The traces of cross sections are reported on Fig. 2. Drilling of most borehole logs ceased at the firm surface of the Kazusa and Shimosa groups; therefore, the lithology and N value of the pre-LGM deposits are not known for most areasBack to article page