Abstract
The Mukogawa River, one of major rivers in Hyogo Prefecture, west Japan, flows from the
southwestern part of the Sasayama Basin to the Osaka Bay through the Sanda Basin and more
downward mountaineous areas of the Rokko Uprift Zone. The intrabasinal watershed between
river systems of the Mukogawa River and its westward Kakogawa River has been poorly
known in the western part of the Sanda Basin. In the part, the 4.9 km long Ainogawa River
flowing eastwards into the Mukogawa River is close to the 4.3 km long unnamed river, a
tributary of the Tojyogawa River flowing southwards into the Kakogawa River. The exact
boundary between these two river systems in the Sanda Basin has been traced through detailed
field observation and the decipherment of topographic maps and an aerial photo. This
intrabasinal watershed is described and discussed topographically in this paper. It is inferred to
have migrated gradually eastwards mainly by a marked difference of the floor gradient between
these two small rivers as well as between the Mukogawa River in the Sanda Basin and the
Tojyogawa River. The degree and rate of the migration in the near future depend more largely
on artifici aclontrols than on natural environmental factors including tectoni cmovements.