This is a list of rapids of the Columbia River, listed in upriver order. The river flows through Canada and the United States. Almost all of these rapids are now submerged in the reservoirs of dams. The list is not exhaustive; there were numerous minor rapids and riffles, many of which were never named.
Map of the Columbia drainage Basin with the Columbia River highlighted and showing the major tributaries
Indian Rapids: Located at river mile 220, just above the mouth of the John Day River, at 45°44′34″N120°37′4″W / 45.74278°N 120.61778°W / 45.74278; -120.61778 (former Indian Rapids).[14] It was small and not a significant hazard. When David Thompson visited the rapids on August 2, 1811, he named it Muscle Rapids due to the many shells he found there.[15] The rapids were submerged in 1971 under Lake Umatilla, the reservoir of John Day Dam.
Squally Hook Rapids: Located at river mile 223, a few miles above the mouth of the John Day River, at 45°43′54″N120°33′19″W / 45.73167°N 120.55528°W / 45.73167; -120.55528 (former Squally Hook Rapids).[16] It was not a major hazard although one commentator described it as "short sharp and savage".[17] In 1912 the Army Corps of Engineers improved navigation by drilling and blasting rocks at the rapids.[13] The rapids were submerged in 1971 under Lake Umatilla, the reservoir of John Day Dam.
Rock Creek Rapids: Located near the mouth of Rock Creek,[17] approximately river mile 227 to 228. Described as "rough and rowdy" but not particularly hazardous.[17]
Blalock Rapids: A very minor rapid, probably located near the railway siding of Blalock at the mouth of Blalock Canyon, approximate river mile 233.[17][18][19] It was submerged in 1971 under Lake Umatilla, the reservoir of John Day Dam.
Umatilla Rapids: A significant rapid, located at what is now McNary Dam, river mile 292, 45°56′17″N119°18′9″W / 45.93806°N 119.30250°W / 45.93806; -119.30250 (former Umatilla Rapids).[22] There were at least three "riffles", with the third one downstream being the main one. The total length was somewhat over 1.5 miles (2.4 km).[17] During the low-water seasons, about November to March, Umatilla Rapids became a barrier to steamboat navigation in the late 19th century. The lesser rapids below Umatilla also became more hazardous; larger boats might not even be able to reach Umatilla Rapids during low-water. During high-water large boats could operate from Celilo Falls upriver as far as Lewiston, Idaho on the Snake River. The low-water season effectively suspended river navigation above Umatilla Rapids and on the Snake River.[23] In 1912 the Army Corps of Engineers described the Upper Umatilla Rapids as having two channels. The north channel, known as the low-water channel, was "narrow and tortuous at low water, but has been the only available channel". The south channel, known as the high-water channel, was used only during the high and medium stages of the river.[13] In 1891 rocks were blasted in Umatilla Rapids to create a passage for steamboats during low water.[24] Additional work to improve navigation was done in 1910 and 1911.[13] The rapids were submerged in 1954 under Lake Wallula, the reservoir of McNary Dam. Parts of the dam were built on top of the lower portion of the rapids. In 1805 the Lewis and Clark Expedition gave the name Musselshell Rapids due to the numerous mussels.[15]
Homley Rapids (Homly Rapids): A very minor rapid located about 7 miles (11 km) below Pasco, Washington.[17] In 1911 the Army Corps of Engineers described "Homly Rapids" as "the shoalest on the Columbia between Celilo and the mouth of the Snake River", and that the river was divided by numerous islands, with the main channel passing between "islands Nos. 4 and 5". The Corps made efforts to improve navigation by removing obstructions from the main channel and by building "wing dams" to force more water into the main channel.[13] The rapids were submerged in 1954 under Lake Wallula, the reservoir of McNary Dam.
Bull Run Rapids: A very minor rapid located a few miles below Wallula Gap.[17]
The 70 mile stretch between Priest Rapids and the mouth of the Snake River (the Hanford Reach) "has the slowest current of any part of the Columbia above The Dalles".[25]
Priest Rapids: A series of seven rapids located approximately between river mile 406 and 397 (an 1893 report says river miles 409.5 to 421[27]), near Mattawa, Desert Aire, and the Yakima Training Center. The USGS provides a single coordinate point, 46°45′17″N119°58′20″W / 46.75472°N 119.97222°W / 46.75472; -119.97222 (Priest Rapids).[28] The river dropped 72 feet (22 m) over the entire 9 miles (14 km) length, with a drop of 20 feet (6.1 m) occurring in one short section.[29] In 1888 two steamboats were built at Pasco specifically for the purpose of making it through Priest Rapids and Rock Island Rapids to Wenatchee. The first of the two failed. The second, smaller one, City of Ellensburg, under Captain William Polk Gray, succeeded in passing through Priest Rapids and the more difficult Rock Island Rapids. Later, the sister boat, Thomas L. Nixon, also succeeded in ascending both rapids and reaching Wenatchee.[30] In 1959 the rapids were submerged under Priest Rapids Lake, the reservoir of Priest Rapids Dam.
Rock Island Rapids: Located at approximately river mile 454, near Rock Island Dam and Rock Island, and a few miles upriver from Cabinet Rapids; 47°20′39″N120°5′52″W / 47.34417°N 120.09778°W / 47.34417; -120.09778 (former Rock Island Rapids).[34] The rapids were over 2 miles (3.2 km) long. Local native people called them Squah-ah-shee. They were given their present name in 1881 by Lieutenant Thomas W. Symons, who named them for Rock Island, a large rock in the river below Wenatchee, around which the water flowed swift and roughly.[15] The two channels around Rock Island were full of rocks and other obstructions, and there was a "great reef" a short distance above the head of the island, with large bars of gravel, "nearly choking the channel at low water". The river fell 10 feet (3.0 m) over a distance of 3,000 feet (910 m) at low-water.[32] In 1933 the rapids were submerged in Rock Island Pool, the reservoir of Rock Island Dam. At least two steamboats were wrecked at the rapids. The Selkirk wrecked at Rock Island Rapids on May 15, 1906 (see Shipwrecks of the inland Columbia River). In 1887 a steamboat tried and failed to ascend the Rock Island Rapids. In 1888 two steamboats were built at Pasco specifically for the purpose of making it through Priest Rapids and Rock Island Rapids to Wenatchee. The first of the two failed. The second, smaller one, City of Ellensburg, under Captain William Polk Gray, succeeded in passing through Priest Rapids and the more difficult Rock Island Rapids. Later, the sister boat, Thomas L. Nixon, also succeeded in ascending both rapids and reaching Wenatchee.[30]
The portion of the river between Monaghan Rapids and Foster Creek Rapids was regarded as particularly hazardous. An 1893 report by the Army Corps of Engineers described the river from Monaghan Rapids to the foot of Foster Creek Rapids as "very swift and studded with rocks, and taken all in all will be found an extremely hard and dangerous if not absolutely impassable portion of the river to navigate". Over the 45 miles (72 km) from Monaghan to Foster Creek the river fell 171 feet (52 m) at low-water. Over the 10 miles (16 km) between Mah-kin Rapids and a point three miles below Parson Rapids the river fell 41 feet (12 m) at low water. The portion from White Cap Rapids to Eagle Rapids was once known as "Nespilem Canyon". The Corps' 1893 report said that over the worst 3 miles (4.8 km) stretch the river fell 22 feet (6.7 m) at low-water and 24 feet (7.3 m) at high-water, and that the speed of the current at low-water was about 10 miles per hour (16 km/h). On the possibility of navigation the Corps was pessimistic: "The fall of the river here is so great that it is certain that no system of rock removal could make the river sufficiently navigable to justify the danger and risk necessarily incurred in running boats on it."[37]
Foster Creek Rapids: Located at river mile 547-546, just above Chief Joseph Dam and Bridgeport.[39] About a mile long,[40] the rapids are submerged in Rufus Woods Lake, the reservoir of Chief Joseph Dam. An 1893 report by the United States War Department described Foster Creek Rapids as "among the worst rapids on the river", and being about 3 miles (4.8 km) long, including Reef Rapids. Over this length the river fell 21 feet (6.4 m) during low water and 24 feet (7.3 m) at high water.[41] In 1911 and 1912 efforts were made by the Army Corps of Engineers to improve navigation by blasting submerged rocks and reefs from Reef Rapids through Foster Creek Rapids and upriver to "Kalichen Rock" (Eagle Rapids).[13]
White Cap Rapids: Located at river mile 558.5, between Gaviota Bend and Box Canyon; 48°3′50″N119°25′29″W / 48.06389°N 119.42472°W / 48.06389; -119.42472 (former White Cap Rapids).[44] Submerged in Rufus Woods Lake, the reservoir of Chief Joseph Dam. Lewis R. Freeman described White Cap Rapids as a narrow, straight, and steep channel "heavily littered with boulders and fanged with outcropping bedrock", with a "mad tumble of wallowing waters", somewhat similar to Gordon Rapids in the Big Bend region, but rougher.[45]
Monaghan Rapids (Moneghan's Rapids, Buckley's Rapids[50]): Located at river mile 587, just below an island called Buckley Bar.; 48°4′0″N119°0′55″W / 48.06667°N 119.01528°W / 48.06667; -119.01528 (former Monaghan Rapids).[52] The name was given in 1881 by Lieutenant Thomas W. Symons, in honor of James Monaghan, who had encountered difficulties at the rapids in 1879-1880 attempting to bring rafts of supplies downriver to a military camp on the Okanogan River.[15] Submerged in Rufus Woods Lake, the reservoir of Chief Joseph Dam.
Turtle Rapids: A minor rapid located approximately at river mile 670, near Bissell, above Stray Dog Canyon.[56] The name comes from a number of rock outcroppings that resembled turtle backs.[57]
Little Dalles: Located at river mile 729, six miles downriver of Northport; 48°52′18″N117°52′9″W / 48.87167°N 117.86917°W / 48.87167; -117.86917 (former Little Dalles).[60] The river narrowed to 130 feet (40 m) at the head of the Little Dalles, then widened somewhat over a length of at least 2,000 feet (610 m). Boat navigation through the Little Dalles was not difficult at low water, but during the high water season the drop increased to 20 feet (6.1 m), making it a major hazard.[61] The Little Dalles presented the primary obstacle to navigation on the upper river into Canada. The river was constricted between massive stone cliffs. The first official use of the name "Little Dalles" appears to come from the 1881 report of Lieutenant Symons, although it is likely the name was informally used long before.[15] In an 1893 report Symons described the Little Dalles at low-water as "placid", but at high-water as "a seething, whirling torrent, impelled forward by a 16-foot head". He recommended ways to improve navigation during low-water. To improve navigation during high-water would require extensive work and would still be hazardous. He wrote, "Trees and logs 60 or 70 feet in length disappear in Little Dalles at high water; they go right down on end and do not reappear".[37] In 1942 the rapids were submerged in Franklin D. Roosevelt Lake, the reservoir of Grand Coulee Dam.
Kootenay Rapids (formerly called Tincup Rapids or Tin Cups): A minor rapid located 0.5 miles (0.80 km) below Tincup Rapids, near Castlegar, just below the mouth of the Kootenay River.[63] About 0.25 miles (0.40 km) long, the rapids are mild.[64]
Tincup Rapids (formerly called Kootenay Rapids): A pair of rapids, called Upper and Lower, or Big and Little Tincup Rapids, located at Castlegar, just above the mouth of the Kootenay River; 49°19′N117°39′W / 49.317°N 117.650°W / 49.317; -117.650 (former Tincup Rapids).[65] The river narrows to 201 metres (659 ft) at the foot of the lower rapid. For steamboats, the rapids were a navigation hazard during low water in autumn and winter. In the 1890s efforts were made to improve the channel by blasting rocks in the river. The rapids were noted as a "strong rapid" by David Thompson in his journal entry of September 6, 1811. During the 19th century Tincup Rapids was called Kootenay Rapids, and what is today called Kootenay Rapids was called Tincup Rapids. Sometime before 1916 the nomenclature was reversed.[63]
Priest Rapids: Located just south (downriver) from Dalles des Morts and about 5 kilometres (3.1 mi) north (upriver) of the mouth of Downie Creek; 51°29′43.5″N118°29′44.1″W / 51.495417°N 118.495583°W / 51.495417; -118.495583 (former Priest Rapids).[74] The rapids were submerged in Lake Revelstoke in 1984. The name comes from the drowning deaths of two French-Canadian priests at the rapids.[75] Priest Rapids was reputed to be the fastest rapids of the Columbia River, with a current reckoned to be over 20 miles per hour (32 km/h).[76]
Dalles des Morts (Death Rapids): One of the most hazardous rapids of the Columbia River, located just above Priest Rapids and about 6 kilometres (3.7 mi) north of the mouth of Downie Creek; 51°30′40.6″N118°30′34.3″W / 51.511278°N 118.509528°W / 51.511278; -118.509528 (former Dalles des Morts).[74] The name dates to 1817 when seven voyageurs wrecked at the rapids and tried to walk to Spokane House, over 300 miles (480 km) away. Only one survived. A number of other fatal accidents occurred at the rapids, including the drowning of twelve people in 1838.[77] Today the rapids are submerged in Lake Revelstoke, the reservoir of Revelstoke Dam.
Rock Slide Rapids: Located about 1 mile (1.6 km) downriver of the foot of Twelve Mile Rapids. Lewis Freeman described Rock Slide Rapids as the narrowest point of the entire Columbia River below Windermere Lake, with a channel width averaging 70 feet (21 m). The river rushed through the narrows and poured into a "cauldron-like eddy", then into another narrow chute to form the Dalles des Morts.[78] Today the rapids are submerged in Lake Revelstoke, the reservoir of Revelstoke Dam.
Twenty-One-Mile Rapids: Lewis Freeman used the name Twenty-One-Mile Rapids for the series of rapids between the outlet of Kinbasket Lake (before its enlargement by Mica Dam) to the mouth of the Canoe River, which was about 21 miles (34 km) in length. Twenty-One-Mile Rapids in this sense included Redrock Canyon Rapids, Yellow Creek Rapids, Weasel Rapids, Mink Rapids, and Boulder Rapids. He also speculated that Twenty-One-Mile Rapids was "one of the longest, if not the longest, successfion of practically unbroken riffles on any of the great rivers of the world. Over the first 16 miles (26 km) the tail of one rapids generally ran right into the head of the next. The final 5 miles (8.0 km) contained less white water but still had a rapid current with many swirls and whirlpools. Throughout the series of rapids the river was closely constrained by canyons with no camping places along the way, thus one was compelled to run through the whole series in a single day.[81] Lewis Freeman, in his 1921 account, reports a new, powerful rapid at the end of Twenty-One-Mile Rapids. His guide, Blackmore, claimed there had previously been no major rapid between Yellow Creek and Death Rapids, and that this new rapid had been created by a large landslide during the spring before their journey. Freeman describes this new rapids as located directly upriver from "Red Canyon".[82]
Surprise Rapids: Located just northwest of the Bush River, at the north end of a large island in a wide portion of Kinbasket Lake and just south of a narrow channel called The Elbow;[88] approximately 15 kilometres (9.3 mi) northeast of Mount Sir Sandford and 70 kilometres (43 mi) upriver from Mica Dam; 51°46′31.2″N117°41′8″W / 51.775333°N 117.68556°W / 51.775333; -117.68556 (former Surprise Rapids).[74][89] The river fell about 100 feet (30 m) over approximately 3.33 miles (5.36 km). Within that length there were at least three cascades. The first cascade was the largest, with a drop of 21 feet (6.4 m) over 750 feet (230 m). At the second cascade the river dropped 15 feet (4.6 m) over 1,200 feet (370 m). At the third the drop was 25 feet (7.6 m) over 2,500 feet (760 m).[90] In 1973 the rapids were submerged in Kinbasket Lake, the reservoir of Mica Dam.
^Meinig, D.W. (1995) [1968]. The Great Columbia Plain (Weyerhaeuser Environmental Classic ed.). University of Washington Press. pp. 214, 252–253. ISBN0-295-97485-0.
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