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Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Formation of undulating topography and gravel beds at the bases of incised valleys: Last Glacial Maximum examples beneath the lowlands facing Tokyo Bay

Fig. 2

Geological map of the area in and around the Tama River Lowland. Red squares indicate the locations of stratotype cores used in this study. Black dots indicate the locations of borehole logs used to reconstruct the morphology of the LGM incised valley. The blue lines and letters denote the cross sections shown on Fig. 6. Red lines indicate the position of the MIS 6 incised valley filled with the relatively soft Shimosa Group (Nakazawa et al. 2019). The MIS 6 incised valley flowed down in the direction of the red arrow. The geological map is based on Geological Survey of Japan, AIST (2019)

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