Sezill Creek

Sezill Creek is a tributary of Taweh Creek, which in turn is a tributary of Mess Creek, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally northwest for roughly 12 km to join Taweh Creek about 5 km east of Taweh Creek's confluence with Mess Creek. Sezill means "it is hot" in the Tahltan language, referring to a group of hot springs that occur along the creek.

Sezill Creek's watershed covers 51.6 km2 and its mean annual discharge is estimated at 1.51 m3/s. The mouth of Sezill Creek is located about 28 km southeast of Telegraph Creek, about 56 km southwest of Iskut and about 98 km southwest of Dease Lake. Sezill Creek's watershed's land cover is classified as 36.2% barren, 24.7% shrubland, 15% conifer forest, 12.4% snow/glacier, 11.1% herbaceous, and small amounts of other cover.

Sezill Creek is in Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people.

Geography
Sezill Creek originates from the western slope of the massive, glaciated Mount Edziza stratovolcano in the middle of the Big Raven Plateau. From its source between Ornostay Bluff and Koosick Bluff, Sezill Creek flows generally northwest and through a vegetated canyon to Taweh Creek. The head of Sezill Creek flows around an unnamed, low-lying bluff attaining an elevation of 1872 m.

Geology
Sezill Creek contains a large group of hot springs about 7 km above its junction with Taweh Creek. These hot springs, known as the Sezill Hot Springs or the Taweh Hot Springs, extend along Sezill Creek for more than 500 m. They occur at an elevation of 1310 m and contain extensive tufa deposits. Their close association with the recently active Snowshoe Lava Field suggests that they may be discharging from a shallow hydrothermal system driven by residual magmatic heat. The main hot spring discharges water at a temperature of 46 C. A jet of 43 C water on the north side of Sezill Creek is enriched with carbon dioxide.

Thin tongues of unglaciated pillow lava originating from the Mount Edziza volcanic complex extend into the upper part of Sezill Creek canyon. The distal end of this pillow flow has been cut by Sezill Creek to form a narrow, 6 m box canyon. Tuff breccia consisting of blocks and irregular globules of vesicular basalt in a granular matrix commonly underlies the pillow flow.