As mentioned in the last post, steamboats plied the
Willamette to Corvallis from 1851 to 1918.
Water levels so low that the boats scraped bottom were a common
problems, especially in the summer months. Winter's high water also created
problems because there were no flood-control dams on the river prior to the
1940s. In years with especially heavy rains or rapidly melting snow cover, the
volume of water increased and the river would overflow its banks as it did in
1916 and 1923.
In recent years, the peak flow of the Willamette River at
Corvallis has been between 56,400 cubic feet per second (cfs) in 2010 and 77,100 cfs in 2016. Anything more than 83,000 cfs is considered a
flood and anything over 142,000 cfs would result in a “major flood.” In 1916, the peak flow in February was
165,000 cfs. The river flooded a section of the Oregon Electric Line near
Corvallis. This photo shows the extent
of flooding looking east from the Van Buren bridge.
1923 flood |
The flood waters carried many downed trees into the
river. These snags could catch in the
paddle wheel or puncture a hole in the bottom. Also, as the Army Corps of
Engineers noted, “The water was so thick with mud as to render it impossible to
discern the positions of snags below the surface.” Floods also changed the
location of sandbars and relocated the main channel, causing difficulties for
even the most experienced pilots. Beginning in 1870, the Army Corps of
Engineers began removing these snags.
By
Martha Fraundorf, Volunteer for Benton County Historical Society, Philomath,
Oregon