Water of Tanar

Water of Tanar is 32 km long, and has a stream level of 1.

Map of Water of Tanar

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Distributaries / Outflows

It has 1 side channels.

Water of Tanar flows into River Dee , which it joins at N 57° 3′ 58″, W 2° 48′ 10″ at OSM node n835145997, and there 1,456 km of total upstream flows in.

Tributaries

Water of Tanar has 14 tributaries.

Water of Gairney, which joins it at N 57° 2′ 8″, W 2° 52′ 43″ at OSM node n835146853, and 21 km of total upstream flows in.

Burn of Glendui, which joins it at N 57° 1′ 30″, W 2° 55′ 42″ at OSM node n835212355, and 5 km of total upstream flows in.

Allt Roy, which joins it at N 57° 3′ 41″, W 2° 49′ 22″ at OSM node n10035258725, and 5 km of total upstream flows in.

Burn of Skinna, which joins it at N 57° 2′ 20″, W 2° 52′ 1″ at OSM node n11243598947, and 4 km of total upstream flows in.

(unnamed), which joins it at N 57° 0′ 32″, W 2° 57′ 49″ at OSM node n11371987339, and 3 km of total upstream flows in.

(unnamed), which joins it at N 56° 59′ 29″, W 2° 59′ 24″ at OSM node n10879839720, and 3 km of total upstream flows in.

Allt na Cloch, which joins it at N 57° 1′ 28″, W 2° 55′ 47″ at OSM node n8861024206, and 3 km of total upstream flows in.

Cowie Burn, which joins it at N 56° 59′ 38″, W 2° 58′ 38″ at OSM node n8863274480, and 3 km of total upstream flows in.

Allt Deas, which joins it at N 56° 59′ 17″, W 3° 0′ 34″ at OSM node n10879839821, and 2 km of total upstream flows in.

(unnamed), which joins it at N 57° 0′ 38″, W 2° 57′ 43″ at OSM node n9461232284, and 2 km of total upstream flows in.

(unnamed), which joins it at N 56° 59′ 49″, W 2° 58′ 28″ at OSM node n9646593994, and 1 km of total upstream flows in.

(unnamed), which joins it at N 56° 59′ 13″, W 3° 1′ 12″ at OSM node n8861024424, and 1 km of total upstream flows in.

Red Stripe, which joins it at N 56° 59′ 30″, W 2° 58′ 50″ at OSM node n8863295746, and 571 m of total upstream flows in.

(unnamed), which joins it at N 56° 59′ 21″, W 3° 0′ 20″ at OSM node n10879839764, and 285 m of total upstream flows in.