| Breitenbush River | |
| Subdivision Type1: | Country |
| Subdivision Name1: | United States |
| Subdivision Type2: | State |
| Subdivision Name2: | Oregon |
| Subdivision Type3: | Region |
| Subdivision Name3: | Mount Jefferson Wilderness, Willamette National Forest |
| Length: | 18.1km (11.2miles) |
| Discharge1 Location: | above French Creek near Detroit Lake |
| Discharge1 Min: | 87cuft/s |
| Discharge1 Avg: | 569cuft/s |
| Discharge1 Max: | 16900cuft/s |
| Source1: | junction of North and South forks |
| Source1 Location: | Marion County, Mount Jefferson Wilderness, Oregon, United States |
| Source1 Coordinates: | 44.78°N -121.9647°W |
| Source1 Elevation: | 686m (2,251feet) |
| Mouth: | North Santiam River |
| Mouth Coordinates: | 44.7492°N -122.1339°W |
| Mouth Elevation: | 515m (1,690feet) |
| Basin Size: | 108sqmi |
The Breitenbush River is a tributary of the North Santiam River[1] in western Oregon in the United States. It drains a rugged, forested area of the Cascade Range east of Salem.
It descends from several short forks in the Mount Jefferson Wilderness in the high Cascades of eastern Marion County. The South Fork Breitenbush River begins at creeks flowing from Bays Lake and Russell Lake within Jefferson Park at approximately elevation 6000feet and flows west-northwest, joining with other forks. The North Fork Breitenbush River begins at Breitenbush Lake (mostly on the Warm Springs Reservation) and joins with another fork which passes by Pyramid Lake. It flows west-northwest and connects with a half dozen other forks and creeks then turns west-southwest abeam Bald Butte. Several more creeks and Mink Creek and Rapidam Creek join before another fork.
The North and South forks flow west, joining 0.25miles east of the small community of Breitenbush. The combined stream flows generally west-southwest through the Willamette National Forest. It joins the North Santiam at Detroit. The lower 2miles of the river cut what is now an arm of Detroit Lake, formed by the Detroit Dam on the North Santiam. During the winter draw down of the reservoir, the original bed of the river is visible in its natural course.