The Cascades Rapids (sometimes called Cascade Falls or Cascades of the Columbia) were an area of rapids along North America's Columbia River, between the U.S. states of Washington and Oregon.
We concluded to take our canoes first to the head of the rapids, hoping that by evening the rain would cease and afford us a fair afternoon to take our baggage over the portage. this portage is two thousand eight hundred yards along a narrow rough and slipery road. ... a few men were absolutely necessary at any rate to guard our baggage from the War-clel-lars who crowded about our camp in considerable numbers. these are the greates[t] thieves and scoundrels we have met with. ... the canoes were much damaged by being driven against the rocks in despite of every precaution which could be taken to prevent it. ... many of the natives crowded about the bank of the river where the men were engaged in taking up canoes; one of them had the insolence to cast stones down the bank at two of the men who happened to be a little detached from the party at the time. on the return of the party in the evening from the head of the rapids they met with many of the natives on the road, who seemed but illy disposed…
However, three forts, Fort Cascades, Fort Raines and Fort Lugenbeel were constructed between present day Stevenson, Washington and North Bonneville over 1855–6 to protect the portage road around the rapids. Natives burned Fort Cascades in 1856, but it was rebuilt. This attack prompted the construction of Fort Lugenbeel.
The Cascades were a significant barrier to river navigation. Steamboats could not go upriver through the rapids, and could be brought downriver only at great risk, although this was done a number of times by highly-skilled captains. A canal and lock around the rapids was completed in 1896 (see Cascade Locks, Oregon). But by 1938 the rapids were gone, submerged under the Bonneville Reservoir as it formed behind Bonneville Dam. Bonneville Lock at the dam, completed in 1937, replaced the old Cascade Locks around the rapids.