Watershed Drainage Pattern Title Image



McKenzie Watershed Drainage Pattern Map

 

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excerpt from: Technical Report for Water Quality and Fish and Wildlife Habitat,  
McKenzie Watershed Council, February 1996, pp. 5

 

"The main stem of the McKenzie River originates in the northeast portion of the watershed at Clear Lake, which lies at an elevation of 3000 feet just outside the northwest corner of the Mount Washington Wilderness Area.  From Clear Lake, the river flows southward for 15 miles to Belknap Springs and then turns sharply westward for 75 miles before emptying into the Willamette River just south of the community of Coburg.

Several principal tributaries drain into the McKenzie River. Lost Creek, Horse Creek, South Fork  McKenzie River and Quartz Creek join the McKenzie River from the south.  Of these, all except Quartz Creek  originate in the High Cascades with Lost and Horse Creek being fed from glaciers on the west flank of the Three Sisters mountains.  Smith River, Blue River, Gate Creek, Camp Creek and the Mohawk River are the principal tributaries joining from the north.  In all, there are about 1,780 stream miles, of which approximately 1,040 miles flow year round (Water Resources Department, 1991)."

 

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