往古川

往古川 is 8 km long, and has a stream level of 1.

Map of 往古川

This area: WaterwayMap main

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Distributaries / Outflows

往古川 flows into 船津川 , which it joins at N 34° 7′ 51″, E 136° 13′ 4″ at OSM node n734257345, and there 73 km of total upstream flows in.

Tributaries

往古川 has 15 tributaries.

真砂鬼丸谷, which joins it at N 34° 10′ 10″, E 136° 10′ 57″ at OSM node n734453319, and 5 km of total upstream flows in.

(unnamed), which joins it at N 34° 8′ 18″, E 136° 12′ 57″ at OSM node n734570300, and 2 km of total upstream flows in.

小木森谷, which joins it at N 34° 10′ 45″, E 136° 10′ 56″ at OSM node n734383892, and 2 km of total upstream flows in.

寺谷, which joins it at N 34° 9′ 14″, E 136° 11′ 25″ at OSM node n734296909, and 2 km of total upstream flows in.

久瀬谷, which joins it at N 34° 9′ 27″, E 136° 11′ 21″ at OSM node n734657159, and 2 km of total upstream flows in.

(unnamed), which joins it at N 34° 8′ 38″, E 136° 11′ 52″ at OSM node n734461970, and 1 km of total upstream flows in.

赤羽谷, which joins it at N 34° 8′ 30″, E 136° 12′ 25″ at OSM node n734695998, and 1 km of total upstream flows in.

湯谷, which joins it at N 34° 9′ 5″, E 136° 11′ 38″ at OSM node n734468046, and 826 m of total upstream flows in.

(unnamed), which joins it at N 34° 9′ 47″, E 136° 11′ 0″ at OSM node n734658404, and 771 m of total upstream flows in.

(unnamed), which joins it at N 34° 10′ 28″, E 136° 11′ 1″ at OSM node n734702941, and 644 m of total upstream flows in.

(unnamed), which joins it at N 34° 9′ 36″, E 136° 11′ 6″ at OSM node n734256657, and 639 m of total upstream flows in.

(unnamed), which joins it at N 34° 10′ 33″, E 136° 10′ 58″ at OSM node n734551088, and 529 m of total upstream flows in.

(unnamed), which joins it at N 34° 8′ 56″, E 136° 11′ 39″ at OSM node n734581527, and 431 m of total upstream flows in.

(unnamed), which joins it at N 34° 10′ 24″, E 136° 11′ 2″ at OSM node n734414536, and 254 m of total upstream flows in.

(unnamed), which joins it at N 34° 10′ 40″, E 136° 10′ 56″ at OSM node n734695752, and 126 m of total upstream flows in.