Inhini River
The Inhini River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, in Cassiar Land District. From its source in the glaciers of Simma Mountain and Mount Rastus, the Inhini River flows north for about to the Iskut River just east of the Iskut's confluence with the Stikine River.
The Inhini River's watershed covers, and its mean annual discharge is an estimated. The river's watershed's land cover is classified as 26.2% shrubland, 23.7% barren, 20.7% snow/glacier, 16.2% conifer forest, and small amounts of other cover.
The mouth of the Inhini River is located about east-northeast of Wrangell, Alaska, about northwest of Stewart, British Columbia, and about south of Telegraph Creek, British Columbia.
The Inhini River is in the traditional territory of the Tlingit, specifically the Shtax'héen Ḵwáan, commonly known as the Stikine River people. It is also in the asserted traditional territory of the Tahltan First Nation and Iskut First Nation, of the Tahltan people.
Geography
The Inhini River originates in two forks near the border of Alaska. The longer eastern fork flows from the glacial meltwaters of Mount Rastus and Simma Mountain, close to the source of Simma Creek, a tributary of the Craig River. This fork flows for about before being joined by the west fork, which flows from the glacial meltwaters of Mount Fawcett, an Alaska–British Columbia boundary peak.The mainstem Inhini River flows north between Inhini Mountain and Mount Whipple, then between Fizzle Mountain and Snowy Mountain, collecting a number of unnamed tributary streams. It becomes a braided river after entering the floodplain of the Iskut River. The Inhini River empties into a side channel of the highly braided Iskut River about east of the mouth of the Iskut, where it joins the Stikine River a few kilometres upriver of the Alaska boundary.