Fluvial terraces have been typically developed in the Utsunomiya region at the northern Kanto plain, NE Japan, since Middle Pleistocene. There are the Kamikake, Hoshakuji, Kanuma,Shirasawa, Takaragi and Tawara terraces, in ascending order. In this study, the lithostratigraphy of the UT05 core and the tephrostratigraphic abandonment ages of the terraces are described to reveal erosion and deposition history of the Kinu River. The UT05 core has been bored 40 m in depth through the Hoshakuji terrace. The UT05 core consists of eolian veneer deposits from 0 to 15.40 m in depth, the Hoshakuji fluvial terrace deposit from 15.40 to 18.88 m and the Early Pleistocene Sakaibayashi Formation from 18.88 to 40.00 m. The eolian veneer deposits are made up mainly of brown-colored massive volcanic soil and are interbedded with many pyroclastic fall deposits as follows; the tephra group from Akagi volcano, Daisen-Kurayoshi tephra, Nikko-Mamiana tephra, Iiji-Moka tephra, KinunumaKurodahara tephra and Haruna-Miyazawa tephra. The fluvial terrace deposit is composed of unconsolidated gravels and sand. The top of the fluvial deposit is about 2 m higher than the present alluvial plain along the Kinu River, and the bottom of the fluvial deposit is about 1.5 m lower than one. The Sakaibayashi Formation consists of semi-consolidated conglomerate and sandstone. The tephrostratigraphy of the eolian veneers shows that the abandonment ages of the Kamikake, Hoshakuji, Kanuma, Shirasawa and Takaragi-Tawara terraces are MIS (marine isotope stage) 10, MIS 8, MIS 6, MIS 5.4 and MIS 4 to 2,respectively. Therefore, accumulation of the fluvial sediments has occurred at every glacial tracts forming climatic terraces due to an increase of the sediment load against the stream discharge. All the relative heights between the tops of the fluvial terrace deposits and the present alluvial plain along the Kinu River have been less than 6 m and independent to the abandonment ages of the terraces since 0.35 Ma. This suggests that the formation of the fluvial terraces in this region has been only controlled by the climatic change, and not effected by tectonic movement.
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