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The products of chalk weathering are dissolved in rainwater and are transported in stream flow. Chalk streams transport little suspended material (unlike most rivers), but are considered "mineral-rich" due to the dissolved calcium and carbonate ions. The surface water of chalk streams is commonly described as "gin clear".
The Weiser River is a 103-mile-long (166 km) [3] tributary of the Snake River in western Idaho in the United States. It drains a mountainous area of 1,660 square miles (4,300 km 2) consisting primarily of low rolling foothills intersected by small streams south and east of Hells Canyon along the Idaho-Oregon border.
Bad Luck Creek (Idaho County, Idaho) Badger Creek; Bannock Creek; Battle Creek; Bear River (Boise River tributary) – Bear River tributary of the Boise River, Idaho; Bear River (Great Salt Lake) – Bear River in SE Idaho, SW Wyoming, and NE Utah corner; Beaver dam; Beaver Creek; Big Dick Creek; Big Lost River; Big Canyon Creek; Big Creek; Big ...
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Logan River (Utah-Idaho) Lost streams of Idaho; M. Malad River (Gooding County, Idaho) Malad River (Idaho-Utah) Marsh Creek (Portneuf River tributary)
It begins in Wyoming and flows through Idaho for 769 miles (1,238 km), and then through Oregon and Washington. Some of the other streams also cross borders between Idaho and Montana, Nevada, Oregon, Utah, Washington, or Wyoming, but the majority flow entirely within Idaho, the longest of which is the Salmon River at 425 miles (684 km).
Image map of all Idaho streams more than 50 miles (80 kilometers) long. Each label is wikilinked to an article. Click on the small rectangles to the right of the caption for a larger map.
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