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Progress in Earth and Planetary Science
Fig. 9 | Progress in Earth and Planetary Science

Fig. 9

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. 9

Occurrences of gravel beds at the bases of the post-LGM incised-valley fills. Black and white dots indicate presence and absence of a gravel bed, respectively, and are plotted on the elevation map of Fig. 7. Gravel beds are frequent along the Tama River. a–d Show × 2 enlargements of the undulating topography at the bases of the LGM incised valleys. Borehole logs are available for the bottoms and margins of pits in (a), (b), and (c), but are not available for the pits in (d)

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