The Watershed

The Takshanuk Watersheds

There are three drainages included in the Takshanuk Watershed Council’s area. These are the Chilkat, Chilkoot and Ferebee valleys. The name for the council comes from the Takshanuk Mountains, the high ridge which divides the Chilkoot and Chilkat valleys. Peaks like Mt. Ripinsky, 3920, and Tugahoe are part of the Takshanuk Mountain.

Within this vast area exists a wide variety of landscapes and habitat types- everything from glacial ice to dense forest to wide expanses of wetland and bog. For instance, a drop of rain landing high up on the southwest side of Mount Ripinsky will travel over rock, through forest, and the settled area of the Haines townsite before emptying into the Chilkat River via Sawmill Creek. Along the way it will help sustain living creatures dependent on water- not only aquatic plants and animals but landlubbers as well. It will absorb both natural and man-made compounds as it travels downhill before joining with the Chilkat near Jones Point.

Some of our watershed work focuses on restoration projects in "urban" streams like Holgate Creek and Sawmill Creek.

What is a watershed?

A watershed is the drainage basin of a river or stream. All the precipitation, whether rain or snow, that falls in the basin eventually drains downstream and collects in larger and larger watercourses. Tiny brooks join to form streams, these combine to become creeks and these drain together into rivers. A watershed is actually an area of land from which water drains into a single river. Water ties this tract of land together.

Takshanuk History

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