Jump to content

Celilo Falls: Difference between revisions

From Wikipedia, the free encyclopedia
Browse history interactively
← Previous editNext edit →
Content deleted Content added
VisualWikitext
pronoun clarity, sentence flow
combine geology + description sections, add subsection for a cleaner line through the narrative, other minor changes
Line 1: Line 1:
[[Image:celilofalls-small.ogg|thumb|right|300px|Newsreel footage of [[Native Americans in the United States|native]] fishers at Celilo Falls in 1956, shortly before the site was submerged by [[The Dalles Dam]] (35 sec.) <small>([[Wikipedia:Media help|media help]])''</small>]]
[[Image:celilofalls-small.ogg|thumb|right|300px|Newsreel footage of [[Native Americans in the United States|native]] fishers at Celilo Falls in 1956, shortly before the site was submerged by [[The Dalles Dam]] (35 sec.) <small>([[Wikipedia:Media help|media help]])''</small>]]


'''Celilo Falls''' ('''''Wyam''''', meaning "echo of falling water" or "sound of water upon the rocks," in several native languages; also known as '''The Chutes''', '''Great Falls''', and '''Columbia Falls'''<ref name=gibson>{{cite book |last= Gibson |first= James R. | title= The Lifeline of the Oregon Country: The Fraser-Columbia Brigade System, 1811-47 |date= 1997 |publisher= University of British Columbia (UBC) Press |isbn= 0774806435 |pages= pp.125-128}} online at [http://books.google.com/books?id=4imt4oeWrr0C Google Books]</ref>) was a tribal [[fishing]] area on the [[Columbia River]], just east of the [[Cascade Range|Cascade Mountains]], on what is today the border between the [[U.S. states]] of [[Oregon]] and [[Washington]]. It was the first drop in a long series of rapids that culminated in the '''Big Dalles'''. The area was the location of the oldest continuously inhabited community on the [[North America]]n continent until 1957, when the falls and the nearby settlement were submerged by the construction of [[The Dalles Dam]].<ref>{{cite book | last = Dietrich | first = William | title = Northwest Passage: The Great Columbia River | publisher = University of Washington Press | place = Seattle, WA | date = 1995 | page = 52}}</ref>
'''Celilo Falls''' ('''''Wyam''''', meaning "echo of falling water" or "sound of water upon the rocks," in several native languages; also known as '''The Chutes''', '''Great Falls''', and '''Columbia Falls'''<ref name=gibson>{{cite book |last= Gibson |first= James R. | title= The Lifeline of the Oregon Country: The Fraser-Columbia Brigade System, 1811-47 |date= 1997 |publisher= University of British Columbia (UBC) Press |isbn= 0774806435 |pages= pp.125-128}} online at [http://books.google.com/books?id=4imt4oeWrr0C Google Books]</ref>) was a tribal [[fishing]] area on the [[Columbia River]], just east of the [[Cascade Range|Cascade Mountains]], on what is today the border between the [[U.S. states]] of [[Oregon]] and [[Washington]]. It was the first drop in a long series of rapids that culminated in the '''Big Dalles'''. Celilo Falls was the oldest continuously inhabited community on the [[North America]]n continent until 1957, when the falls and the nearby settlement were submerged by the construction of [[The Dalles Dam]].<ref>{{cite book | last = Dietrich | first = William | title = Northwest Passage: The Great Columbia River | publisher = University of Washington Press | place = Seattle, WA | date = 1995 | page = 52}}</ref>


==Description==
==Geology==
Celilo Falls consisted of three main sections &mdash; a [[waterfall|cataract]] known as Horseshoe Falls or Tumwater Falls, a deep eddy known as Cul-de-Sac, and the main channel.<ref name="database"/> The seasonal flow of the Columbia River changed the height of the Celilo Falls over the course of a year. At low water the drop could reach about {{convert|20|ft|m}}. During the spring freshnet the falls could be completely submerged. Celilo Falls was the first of a series of cascades and [[rapids]] known collectively as '''The Narrows''' and '''The Dalles''', stretching for {{convert|30|mi|km}} and dropping a total of {{convert|82|ft|m}} at high water and {{convert|63|ft|m}} at low water.<ref name=gibson/>
Celilo Falls consisted of three main sections &mdash; a [[waterfall|cataract]] known as Horseshoe Falls or Tumwater Falls, a deep eddy known as Cul-de-Sac, and the main channel.<ref name="database"/> They were formed by the Columbia River's relentless push through [[basalt]] [[narrows]] on the final leg of its journey to the [[Pacific Ocean]]. Frequently more than a mile (1.6 km) in width, the river was squeezed here into a width of only 140 feet (43 m).<ref>{{cite book | last = Dietrich | first = William | title = Northwest Passage: The Great Columbia River | publisher = University of Washington Press | place = Seattle, WA | date = 1995 | page = 80}}</ref> The seasonal flow of the Columbia changed the height of the falls over the course of a year. At low water the drop was about {{convert|20|ft|m}}. During the spring [[freshet]] in June and July, the falls could be completely submerged. The falls were the sixth-largest by volume in the world and were among the largest in [[North America]].<ref>[http://www.worldwaterfalldatabase.com/database.php?s=N&t=W&orderby=avevolume&sortLimit=5000 World Waterfall Database]</ref> Average volume was 190,000 ft³/sec (5400 m³/s), and during periods of high water or [[flood]], nearly a million ft³/sec (28,000 m³/s) passed over the falls, creating a tremendous roar that could be heard many miles away.<ref name="database">{{cite web | title = World Waterfall database | url = http://www.worldwaterfalldatabase.com/waterfall.php?num=161 | accessdate=2008-02-01}}</ref>


===The Narrows and The Dalles===
About {{convert|3|mi|km}} below Celilo Falls was a stretch of rapids known variously as the Short Narrows, Ten Mile Rapids, the Little (or Upper) Dalles, and Les Petites Dalles. These rapids were about {{convert|1|mi|km}} long and {{convert|250|ft|m}} wide. About {{convert|10|mi|km}} below Celilo Falls was another stretch of rapids known by names including the Long Narrows, Five Mile Rapids, the Big (or Lower) Dalles, Les Grandes Dalles, and Grand Dalles. In this stretch of rapids was about {{convert|3|mi|km}} long and the river channel narrowed to {{convert|75|ft|m}}. Immediately below was the Dalles Rapids (or Wascopam to the local natives), about {{convert|1.5|mi|km}} long, through which the river dropped about {{convert|15|ft|m}} in a tumult much commented on by early explorers. The Long Narrows and the Dalles Rapids are sometimes described together under names such as Grand Dalles, Les Dalles, Big Dalles, and The Dalles. One early observer, Ross Cox, described the Big Dalles as a three mile "succession of boiling whirlpools". [[Alexander Ross (fur trader)|Alexander Ross]] wrote of it, "[The water] rushes with great impetuosity; the foaming surges dash through the rocks with terrific violence; no craft, either large or small, can venture there safely. During floods, this obstruction, or ledge of rocks, is covered with water, yet the passage of the narrows is not thereby improved." [[Charles Wilkes]] described the Big Dalles as "one of the most remarkable places upon the Columbia". He calculated that the river dropped about {{convert|50|ft|m}} over {{convert|2|mi|km}} at this point. Wilkes and others wrote that during the spring freshnet in June and July the river rose as much as {{convert|62|ft|m}}, radically altering the nature of the rapids.<ref name=gibson/>
Celilo Falls was the first in a series of cascades and [[rapids]] known collectively as '''The Narrows''' and '''The Dalles''', stretching for {{convert|30|mi|km}} downstream. Over that length, the river dropped {{convert|82|ft|m}} at high water and {{convert|63|ft|m}} at low water.<ref name=gibson/>


Three&nbsp;miles (4.8&nbsp;km) below Celilo Falls was a stretch of rapids known variously as the Short Narrows, Ten Mile Rapids, the Little (or Upper) Dalles, or Les Petites Dalles. These rapids were about {{convert|1|mi|km}} long and {{convert|250|ft|m}} wide. Ten&nbsp;miles (16&nbsp;km) below Celilo Falls was another stretch of rapids, this one known as the Long Narrows, Five Mile Rapids, the Big (or Lower) Dalles, Les Grandes Dalles, or Grand Dalles. This stretch of rapids was about {{convert|3|mi|km}} long, and the river channel narrowed to {{convert|75|ft|m}}. Immediately downstream were the Dalles Rapids (or Wascopam to the local natives), about {{convert|1.5|mi|km}} long. Here the river dropped {{convert|15|ft|m}} in a tumult much commented on by early explorers.
==Geology==

The falls were formed by the Columbia River's relentless push through [[basalt]] [[narrows]] on the final leg of its journey to the [[Pacific Ocean]]. Frequently more than a mile (1.6 km) in width, the river was squeezed here into a width of only 140 feet (43 m).<ref>{{cite book | last = Dietrich | first = William | title = Northwest Passage: The Great Columbia River | publisher = University of Washington Press | place = Seattle, WA | date = 1995 | page = 80}}</ref> The falls were the sixth-largest by volume in the world and were among the largest in [[North America]].<ref>[http://www.worldwaterfalldatabase.com/database.php?s=N&t=W&orderby=avevolume&sortLimit=5000 World Waterfall Database]</ref> Average volume was 190,000 ft³/sec (5400 m³/s), and during periods of high water or [[flood]], nearly a million ft³/sec (28,000 m³/s) passed over the falls, creating a tremendous roar that could be heard many miles away.<ref name="database">{{cite web | title = World Waterfall database | url = http://www.worldwaterfalldatabase.com/waterfall.php?num=161 | accessdate=2008-02-01}}</ref>
The Long Narrows and the Dalles Rapids are sometimes grouped together under names such as Grand Dalles, Les Dalles, Big Dalles, or The Dalles. One early observer, Ross Cox, noted a three-mile "succession of boiling whirlpools".<ref name=gibson/> Explorer [[Charles Wilkes]] described it as "one of the most remarkable places upon the Columbia". He calculated that the river dropped about {{convert|50|ft|m}} over {{convert|2|mi|km}} here. During the spring freshet, the river rose as much as {{convert|62|ft|m}}, radically altering the nature of the rapids.<ref name=gibson/> Fur trader [[Alexander Ross (fur trader)|Alexander Ross]] wrote, "[The water] rushes with great impetuosity; the foaming surges dash through the rocks with terrific violence; no craft, either large or small, can venture there safely. During floods, this obstruction, or ledge of rocks, is covered with water, yet the passage of the narrows is not thereby improved."<ref name=gibson/>


== History ==
== History ==
Line 17: Line 19:
For 11,000 years, [[Native Americans in the United States|native peoples]] gathered at Wyam to fish and exchange goods.<ref>{{cite book | last = Barber | first = Katrine | coauthors=Ed. William G. Robbins | title=Narrative Fractures and Fractured Narratives: Celilo Falls in the Columbia Gorge Discovery Center and the Yakama Nation Cultural Heritage Center | work = The Great Northwest: The Search for Regional Identity | publisher = Oregon State University Press | place = Corvallis, Oregon | date 2001}}</ref> They built wooden platforms out over the water and caught [[salmon]] with dipnets and long spears on poles as the fish swam up through the rapids and jumped over the falls.<ref>{{cite book | last = Dietrich | first = William | title = Northwest Passage: The Great Columbia River | publisher = University of Washington Press | place = Seattle, WA | date = 1995 | page = 154}}</ref> Historically, an estimated fifteen to twenty million salmon passed through the falls every year, making it one of the greatest fishing sites in North America.<ref>{{cite news | last = Rohrbacher | first = George | title = Talk of the Past: The salmon fisheries of Celilo Falls | work = Common-Place | date = January 2006 | url=http://www.common-place.org/vol-06/no-02/talk/ | accessdate=2008-02-01}}</ref>
For 11,000 years, [[Native Americans in the United States|native peoples]] gathered at Wyam to fish and exchange goods.<ref>{{cite book | last = Barber | first = Katrine | coauthors=Ed. William G. Robbins | title=Narrative Fractures and Fractured Narratives: Celilo Falls in the Columbia Gorge Discovery Center and the Yakama Nation Cultural Heritage Center | work = The Great Northwest: The Search for Regional Identity | publisher = Oregon State University Press | place = Corvallis, Oregon | date 2001}}</ref> They built wooden platforms out over the water and caught [[salmon]] with dipnets and long spears on poles as the fish swam up through the rapids and jumped over the falls.<ref>{{cite book | last = Dietrich | first = William | title = Northwest Passage: The Great Columbia River | publisher = University of Washington Press | place = Seattle, WA | date = 1995 | page = 154}}</ref> Historically, an estimated fifteen to twenty million salmon passed through the falls every year, making it one of the greatest fishing sites in North America.<ref>{{cite news | last = Rohrbacher | first = George | title = Talk of the Past: The salmon fisheries of Celilo Falls | work = Common-Place | date = January 2006 | url=http://www.common-place.org/vol-06/no-02/talk/ | accessdate=2008-02-01}}</ref>


The falls were strategically located at the border between [[Chinook|Chinookan]] and [[Sahaptian]] speaking peoples and served as the center of an extensive trading network across the Pacific Plateau.<ref name="Ronda">{{cite book | last = Ronda | first = James P. | title=Lewis & Clark among the Indians | work=Down the Columbia | publisher=University of Nebraska Press | place=Lincoln, Nebraska | date = 1984 | url = http://209.85.173.104/search?q=cache:0kyIwDqLbCcJ:lewisandclarkjournals.unl.edu/hilight.php%3Fid%3D1221%26keyword%3Dportaging%26keyword2%3D%26keyword3%3D+emporium+site:lewisandclarkjournals.unl.edu/&hl=en&ct=clnk&cd=1&gl=us&client=safari | accessdate=2008-02-01}}</ref> Artifacts from the original village site suggest that tribes came from as far away as the [[Great Plains]], [[Southwestern United States]], and [[Alaska]].<ref>{{cite web | last = Center for Columbia River History | title=Oregon's Oldest Town: 11,000 Years of Occupation | url = http://www.ccrh.org/comm/river/celilo.htm | accessdate=2008-02-01}}</ref> When the [[Lewis and Clark expedition]] passed through the area in 1805, the explorers found a "great emporium…where all the neighboring nations assemble," and a population density unlike anything they had seen on their journey.<ref>{{cite journal | last = Cressman | first = L.S. | coauthors = et al. | title = Cultural Sequences at the Dalles, Oregon: A Contribution to Pacific Northwest Prehistory | journal = Transactions of the American Philosophical Society | volume = 50| issue = 10| pages = 1-108 | 1960 | doi = 10.2307/1005853}}</ref> Accordingly, historians have likened the Celilo area to the “[[Wall Street]] of the West."<ref>{{cite news | last = Alpert | first = Emily | title = Remembering Celilo Falls | work = The Dalles Chronicle | date = 10 July 2006 | url=http://www.bluefish.org/celilofa.htm | accessdate=2008-02-01}}</ref> The [[Wishram]] people lived on the north bank, while the [[Wasco]] lived on the south bank, with the most intense bargaining occurring at the Wishram village of Nix-luidix.<ref name="Ronda"/>
Celilo Falls and the Big Dalles were strategically located at the border between [[Chinook|Chinookan]] and [[Sahaptian]] speaking peoples and served as the center of an extensive trading network across the Pacific Plateau.<ref name="Ronda">{{cite book | last = Ronda | first = James P. | title=Lewis & Clark among the Indians | work=Down the Columbia | publisher=University of Nebraska Press | place=Lincoln, Nebraska | date = 1984 | url = http://209.85.173.104/search?q=cache:0kyIwDqLbCcJ:lewisandclarkjournals.unl.edu/hilight.php%3Fid%3D1221%26keyword%3Dportaging%26keyword2%3D%26keyword3%3D+emporium+site:lewisandclarkjournals.unl.edu/&hl=en&ct=clnk&cd=1&gl=us&client=safari | accessdate=2008-02-01}}</ref> Artifacts from the original village site at Celilo suggest that tribes came from as far away as the [[Great Plains]], [[Southwestern United States]], and [[Alaska]].<ref>{{cite web | last = Center for Columbia River History | title=Oregon's Oldest Town: 11,000 Years of Occupation | url = http://www.ccrh.org/comm/river/celilo.htm | accessdate=2008-02-01}}</ref> When the [[Lewis and Clark expedition]] passed through the area in 1805, the explorers found a "great emporium…where all the neighboring nations assemble," and a population density unlike anything they had seen on their journey.<ref>{{cite journal | last = Cressman | first = L.S. | coauthors = et al. | title = Cultural Sequences at the Dalles, Oregon: A Contribution to Pacific Northwest Prehistory | journal = Transactions of the American Philosophical Society | volume = 50| issue = 10| pages = 1-108 | 1960 | doi = 10.2307/1005853}}</ref> Accordingly, historians have likened the Celilo area to the “[[Wall Street]] of the West."<ref>{{cite news | last = Alpert | first = Emily | title = Remembering Celilo Falls | work = The Dalles Chronicle | date = 10 July 2006 | url=http://www.bluefish.org/celilofa.htm | accessdate=2008-02-01}}</ref> The [[Wishram]] people lived on the north bank, while the [[Wasco]] lived on the south bank, with the most intense bargaining occurring at the Wishram village of Nix-luidix.<ref name="Ronda"/> Charles Wilkes reported finding three major native fishing sites on the lower Columbia &mdash; Celilo Falls, the Big Dalles, and [[Cascades Rapids]], with the Big Dalles being the largest. Alexander Ross described it as the "great rendezvous" of native traders, as "the great emporium or mart of the Columbia."<ref name=gibson/>

[[Charles Wilkes]] wrote that there were three major native fishing sites on the lower Columbia &mdash; Celilo Falls, the Big Dalles, and [[Cascades Rapids]], with the Big Dalles being the largest. Alexander Ross described the Big Dalles as the "great rendezvous" of native traders, as "the great emporium or mart of the Columbia."<ref name=gibson/>


The seasonal changes in the Columbia's flow, high in summer and low in winter, affected Celilo Falls dramatically. Lewis and Clark reached Celilo Falls in the late autumn when the water was relatively low, making the falls into a major barrier. In contrast, when [[David Thompson (explorer)|David Thompson]] passed Celilo Falls in July of 1811 the high water obscured the falls and made his passage through the Columbia Gorge relatively easy.<ref>{{cite book |last= Meinig |first= D.W. |authorlink= D.W. Meinig |title= The Great Columbia Plain |origyear= 1968 |edition= Weyerhaeuser Environmental Classic edition |year= 1995 |publisher= University of Washington Press |isbn= 0-295-97485-0 |pages= pp. 37-38, 50}}</ref>
The seasonal changes in the Columbia's flow, high in summer and low in winter, affected Celilo Falls dramatically. Lewis and Clark reached Celilo Falls in the late autumn when the water was relatively low, making the falls into a major barrier. In contrast, when [[David Thompson (explorer)|David Thompson]] passed Celilo Falls in July of 1811 the high water obscured the falls and made his passage through the Columbia Gorge relatively easy.<ref>{{cite book |last= Meinig |first= D.W. |authorlink= D.W. Meinig |title= The Great Columbia Plain |origyear= 1968 |edition= Weyerhaeuser Environmental Classic edition |year= 1995 |publisher= University of Washington Press |isbn= 0-295-97485-0 |pages= pp. 37-38, 50}}</ref>
Line 37: Line 37:


Artist and architect [[Maya Lin]] is working on interpretive artwork at Celilo for the [[Confluence Project]], scheduled for completion in 2009.<ref>{{cite news | last = Egan | first = Timothy | title = Looking Backward and Ahead at Continent's End | work = New York Times | url = http://query.nytimes.com/gst/fullpage.html?res=9C03E3DA113EF937A3575BC0A9659C8B63 | date = 4 August 2003 | accessdate = 2008-02-01}}</ref><ref>{{cite web | title=Confluence Project: Celilo Park| url=http://www.confluenceproject.org/project_sites/celilo_park/ | accessdate=2008-02-01}}</ref>
Artist and architect [[Maya Lin]] is working on interpretive artwork at Celilo for the [[Confluence Project]], scheduled for completion in 2009.<ref>{{cite news | last = Egan | first = Timothy | title = Looking Backward and Ahead at Continent's End | work = New York Times | url = http://query.nytimes.com/gst/fullpage.html?res=9C03E3DA113EF937A3575BC0A9659C8B63 | date = 4 August 2003 | accessdate = 2008-02-01}}</ref><ref>{{cite web | title=Confluence Project: Celilo Park| url=http://www.confluenceproject.org/project_sites/celilo_park/ | accessdate=2008-02-01}}</ref>

== See also ==
* [[Cascades Rapids]], another deluged waterfall downstream of Celilo


== References ==
== References ==

Revision as of 08:53, 8 April 2008

Newsreel footage of native fishers at Celilo Falls in 1956, shortly before the site was submerged by The Dalles Dam (35 sec.) (media help)

Celilo Falls (Wyam, meaning "echo of falling water" or "sound of water upon the rocks," in several native languages; also known as The Chutes, Great Falls, and Columbia Falls[1]) was a tribal fishing area on the Columbia River, just east of the Cascade Mountains, on what is today the border between the U.S. states of Oregon and Washington. It was the first drop in a long series of rapids that culminated in the Big Dalles. Celilo Falls was the oldest continuously inhabited community on the North American continent until 1957, when the falls and the nearby settlement were submerged by the construction of The Dalles Dam.[2]

Geology

Celilo Falls consisted of three main sections — a cataract known as Horseshoe Falls or Tumwater Falls, a deep eddy known as Cul-de-Sac, and the main channel.[3] They were formed by the Columbia River's relentless push through basalt narrows on the final leg of its journey to the Pacific Ocean. Frequently more than a mile (1.6 km) in width, the river was squeezed here into a width of only 140 feet (43 m).[4] The seasonal flow of the Columbia changed the height of the falls over the course of a year. At low water the drop was about 20 feet (6.1 m). During the spring freshet in June and July, the falls could be completely submerged. The falls were the sixth-largest by volume in the world and were among the largest in North America.[5] Average volume was 190,000 ft³/sec (5400 m³/s), and during periods of high water or flood, nearly a million ft³/sec (28,000 m³/s) passed over the falls, creating a tremendous roar that could be heard many miles away.[3]

The Narrows and The Dalles

Celilo Falls was the first in a series of cascades and rapids known collectively as The Narrows and The Dalles, stretching for 30 miles (48 km) downstream. Over that length, the river dropped 82 feet (25 m) at high water and 63 feet (19 m) at low water.[1]

Three miles (4.8 km) below Celilo Falls was a stretch of rapids known variously as the Short Narrows, Ten Mile Rapids, the Little (or Upper) Dalles, or Les Petites Dalles. These rapids were about 1 mile (1.6 km) long and 250 feet (76 m) wide. Ten miles (16 km) below Celilo Falls was another stretch of rapids, this one known as the Long Narrows, Five Mile Rapids, the Big (or Lower) Dalles, Les Grandes Dalles, or Grand Dalles. This stretch of rapids was about 3 miles (4.8 km) long, and the river channel narrowed to 75 feet (23 m). Immediately downstream were the Dalles Rapids (or Wascopam to the local natives), about 1.5 miles (2.4 km) long. Here the river dropped 15 feet (4.6 m) in a tumult much commented on by early explorers.

The Long Narrows and the Dalles Rapids are sometimes grouped together under names such as Grand Dalles, Les Dalles, Big Dalles, or The Dalles. One early observer, Ross Cox, noted a three-mile "succession of boiling whirlpools".[1] Explorer Charles Wilkes described it as "one of the most remarkable places upon the Columbia". He calculated that the river dropped about 50 feet (15 m) over 2 miles (3.2 km) here. During the spring freshet, the river rose as much as 62 feet (19 m), radically altering the nature of the rapids.[1] Fur trader Alexander Ross wrote, "[The water] rushes with great impetuosity; the foaming surges dash through the rocks with terrific violence; no craft, either large or small, can venture there safely. During floods, this obstruction, or ledge of rocks, is covered with water, yet the passage of the narrows is not thereby improved."[1]

History

Lewis and Clark's arrival at Celilo Falls in 1805 (mural on the Oregon State Capitol rotunda).
Dipnet fishing at the Cul-De-Sac.

For 11,000 years, native peoples gathered at Wyam to fish and exchange goods.[6] They built wooden platforms out over the water and caught salmon with dipnets and long spears on poles as the fish swam up through the rapids and jumped over the falls.[7] Historically, an estimated fifteen to twenty million salmon passed through the falls every year, making it one of the greatest fishing sites in North America.[8]

Celilo Falls and the Big Dalles were strategically located at the border between Chinookan and Sahaptian speaking peoples and served as the center of an extensive trading network across the Pacific Plateau.[9] Artifacts from the original village site at Celilo suggest that tribes came from as far away as the Great Plains, Southwestern United States, and Alaska.[10] When the Lewis and Clark expedition passed through the area in 1805, the explorers found a "great emporium…where all the neighboring nations assemble," and a population density unlike anything they had seen on their journey.[11] Accordingly, historians have likened the Celilo area to the “Wall Street of the West."[12] The Wishram people lived on the north bank, while the Wasco lived on the south bank, with the most intense bargaining occurring at the Wishram village of Nix-luidix.[9] Charles Wilkes reported finding three major native fishing sites on the lower Columbia — Celilo Falls, the Big Dalles, and Cascades Rapids, with the Big Dalles being the largest. Alexander Ross described it as the "great rendezvous" of native traders, as "the great emporium or mart of the Columbia."[1]

The seasonal changes in the Columbia's flow, high in summer and low in winter, affected Celilo Falls dramatically. Lewis and Clark reached Celilo Falls in the late autumn when the water was relatively low, making the falls into a major barrier. In contrast, when David Thompson passed Celilo Falls in July of 1811 the high water obscured the falls and made his passage through the Columbia Gorge relatively easy.[13]

In the 1840s and 1850s, American pioneers began arriving in the area, traveling down the Columbia on wooden barges loaded with wagons. Many lost their lives in the violent currents near Celilo.[14] In the 1870s, the Army Corps of Engineers embarked on a plan to improve navigation on the river. In 1915, they completed the 14-mile Celilo Canal, a portage allowing steamboats to circumvent the turbulent falls. At the dedication of the canal, Portland investor and civic leader Joseph Nathan Teal gave voice to a common sentiment that endured for decades: “Our waters shall be free: free to serve the uses and purposes of their creation by a Divine Providence.”[15] However, the canal was scarcely used and was completely idle by 1919.[16]

As more settlers arrived in the Pacific Northwest in the 1930s and 1940s, civic leaders advocated for a system of hydroelectric dams on the Columbia River. They argued that the dams would improve navigation for barge traffic from interior regions to the ocean; provide a reliable source of irrigation for agricultural production; provide electricity for the World War II defense industry; and alleviate the flooding of downriver cities, as occurred in the 1948 destruction of Vanport, Oregon.

Aluminum production, shipbuilding, and nuclear production at the Hanford site contributed to a rapid increase in regional demand for electricity. By 1943, fully 96 percent of Columbia River electricity was being used for war manufacturing.[17] The volume of water at Celilo Falls made The Dalles an attractive site for a new dam in the eyes of the Corps of Engineers.

Throughout this period, native people continued to fish at Celilo, under the provisions of the 1855 Treaties signed with the Yakama Nation,[18] the Confederated Tribes of Warm Springs,[19] and the Walla Walla, Umatilla, and Cayuse,[20] which granted "the right of taking fish at all usual and accustomed stations." In 1947, the federal government convened Congressional hearings and concluded that the proposed dam at The Dalles would not violate tribal fishing rights under the treaties.[21] Subsequently, the government reached a monetary settlement with the affected tribes, paying $26.8 million for the loss of Celilo and other fishing sites on the Columbia.[22]

The Army Corps of Engineers commenced work on the Dalles Dam in 1952 and completed it five years later. On March 10, 1957, hundreds of observers looked on as a rising Lake Celilo rapidly silenced the falls, submerged fishing platforms, and consumed the village of Celilo, ending an age-old existence for those who lived there. A small Native American community exists today at nearby Celilo Village, on a bluff overlooking the former location of the falls.

Celilo Falls retains great cultural significance for native peoples. Ted Strong of the Intertribal Fish Commission told one historian, "If you are an Indian person and you think, you can still see all the characteristics of that waterfall. If you listen, you can still hear its roar. If you inhale, the fragrances of mist and fish and water come back again."[23] In 2007, three thousand people gathered at Celilo Village to commemorate the 50-year anniversary of the inundation of the falls.[24]

Artist and architect Maya Lin is working on interpretive artwork at Celilo for the Confluence Project, scheduled for completion in 2009.[25][26]

References

  1. ^ a b c d e f Gibson, James R. (1997). The Lifeline of the Oregon Country: The Fraser-Columbia Brigade System, 1811-47. University of British Columbia (UBC) Press. pp. pp.125-128. ISBN 0774806435. {{cite book}}: |pages= has extra text (help) online at Google Books
  2. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 52.
  3. ^ a b "World Waterfall database". Retrieved 2008-02-01.
  4. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 80.
  5. ^ World Waterfall Database
  6. ^ Barber, Katrine. Narrative Fractures and Fractured Narratives: Celilo Falls in the Columbia Gorge Discovery Center and the Yakama Nation Cultural Heritage Center. Corvallis, Oregon: Oregon State University Press. {{cite book}}: |work= ignored (help); Text "date 2001" ignored (help)
  7. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 154.
  8. ^ Rohrbacher, George (January 2006). "Talk of the Past: The salmon fisheries of Celilo Falls". Common-Place. Retrieved 2008-02-01.
  9. ^ a b Ronda, James P. (1984). Lewis & Clark among the Indians. Lincoln, Nebraska: University of Nebraska Press. Retrieved 2008-02-01. {{cite book}}: |work= ignored (help)
  10. ^ Center for Columbia River History. "Oregon's Oldest Town: 11,000 Years of Occupation". Retrieved 2008-02-01.
  11. ^ Cressman, L.S. "Cultural Sequences at the Dalles, Oregon: A Contribution to Pacific Northwest Prehistory". Transactions of the American Philosophical Society. 50 (10): 1–108. doi:10.2307/1005853. {{cite journal}}: Text "1960" ignored (help)
  12. ^ Alpert, Emily (10 July 2006). "Remembering Celilo Falls". The Dalles Chronicle. Retrieved 2008-02-01.
  13. ^ Meinig, D.W. (1995) [1968]. The Great Columbia Plain (Weyerhaeuser Environmental Classic edition ed.). University of Washington Press. pp. pp. 37-38, 50. ISBN 0-295-97485-0. {{cite book}}: |edition= has extra text (help); |pages= has extra text (help)
  14. ^ "Waiilatpu Mission Resource Education Guide". Whitman Mission National Historic Site. 14 November 2004. Retrieved 2008-02-01. {{cite journal}}: Cite journal requires |journal= (help)
  15. ^ J. B. Tyrell, ed., David Thompson: Narrative of his Explorations in Western America, 1784-1812 (Toronto, 1916, 496-97; "Address of Joseph Nathan Teal, The Dalles-Celilo Celebration, Big Eddy, Oregon (May 5, 1915," Oregon Historical quarterly, 16 (Fall 1916), 107-8. (As quoted in The Columbia River's fate in the twentieth century)
  16. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 204.
  17. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 284.
  18. ^ "Treaty with the Yakama, 1855". Retrieved 2008-02-01.
  19. ^ "Treaty of Wasco, Columbia River, Oregon Territory with the Taih, Wyam, Tenino, & Dock-Spus Bands of the Walla-Walla, and the Dalles, Ki-Gal-Twal-La, and the Dog River Bands of the Wasco". Retrieved 2008-02-01.
  20. ^ "Treaty with the Walla Walla, Cayuse and Umatilla, 1855". Retrieved 2008-02-01.
  21. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 378.
  22. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 376.
  23. ^ Dietrich, William (1995). Northwest Passage: The Great Columbia River. Seattle, WA: University of Washington Press. p. 378.
  24. ^ Modie, Jonathan. "The Celilo Legacy commemoration brought together the tribes of the lower Columbia River and others to remember Celilo Falls, bringing a mix of sadness and nostalgia". Wana Chinook Tymoo. Retrieved 2008-02-01.
  25. ^ Egan, Timothy (4 August 2003). "Looking Backward and Ahead at Continent's End". New York Times. Retrieved 2008-02-01.
  26. ^ "Confluence Project: Celilo Park". Retrieved 2008-02-01.

External links

Template:Mapit-US-cityscale

Retrieved from "https://en.wikipedia.org/w/index.php?title=Celilo_Falls&oldid=204175841"