document_title: Deep Impact (film)

question_text: who played sarah in the movie deep impact

text: Deep Impact (film)

text: Plot[edit]

text: On May 10, 1998, teenaged amateur astronomer Leo Biederman (Elijah Wood) discovers an unusual object near the stars Mizar and Alcor at a star party. His teacher has Leo take a picture and then sends it to astronomer Dr. Marcus Wolf. Wolf realizes that the object is a comet on a collision course with Earth. Unfortunately, Wolf dies in a car accident on his way to alert the authorities.

text: One year later, MSNBC journalist Jenny Lerner investigates the sudden resignation of Secretary of the Treasury Alan Rittenhouse and his connection to "Ellie", supposedly a mistress. After interviewing Rittenhouse, she is taken by the FBI to see President Tom Beck. Lerner realizes that Ellie is really an acronym: "E.L.E." ("extinction-level event"). Due to Lerner's investigation, President Beck makes an announcement earlier than planned: the comet, named Wolf-Biederman, is headed for Earth. It is 7 miles (11 km) long, large enough to cause a mass extinction, and possibly wipe out humanity. He also reveals that the United States and Russia have been constructing an Orion spacecraft called Messiah in orbit that will transport a team, led by Oren Monash and including veteran astronaut Spurgeon "Fish" Tanner, to the comet, hoping to alter its path with nuclear weapons.

text: After landing on the comet, the crew plant nuclear bombs beneath the surface, but are caught in outgassing explosions when sunlight heats up the comet. Monash is blinded by unfiltered sunlight and suffers severe facial burns, while Gus Partenza is flung into space by an outflow of gas. When the bombs detonate, the ship is damaged by the blast and the team loses contact with Earth. President Beck announces that the bombs only split the comet into two smaller pieces, nicknamed "Biederman" (1.5 miles (2.4 km) long) and "Wolf" (6 miles (9.7 km) long), both still heading for Earth.

text: Beck then imposes martial law and reveals that governments worldwide have been building underground shelters. The United States' shelter is in the limestone caves of Missouri. A lottery selects 800,000 Americans under age 50 to join 200,000 selected individuals, as well as a massive supply of food, genetically viable populations of significant animals, and the seeds of every plant species. Lerner and the Biederman family are chosen, but Leo's girlfriend Sarah Hotchner and her family are not. Leo marries Sarah to try to save her family, but it does not work. Sarah refuses to leave without her parents.

text: A last-ditch effort to use ICBMs to deflect the comets fails. Biederman will strike the Atlantic Ocean off Cape Hatteras and generate megatsunamis up to 3,500 ft (1,067 m) high. Wolf will hit western Canada, creating a huge cloud of dust and molten particles that will block out the Sun for two years, killing all life on the surface in a matter of weeks. Leo returns home looking for Sarah, but her family has left for the Appalachian Mountains and is caught in a massive traffic jam. Leo catches up to them on a motorcycle. Sarah's parents tell Leo to take Sarah and her baby brother to high ground.

text: Meanwhile, Lerner gives up her seat in the last evacuation helicopter to her friend Beth and Beth's young daughter. She joins her estranged father Jason at his beach house, where they reconcile. Biederman hits the water, creating a megatsunami that kills many, including Lerner and her father.

text: Unable to safely attempt a second landing, the crew of Messiah decide to undertake a suicide mission, using their remaining nuclear warheads to try to obliterate Wolf. After they say goodbye to their loved ones by video conference, they manage to blow Wolf into smaller pieces that burn up harmlessly in Earth's atmosphere. Leo, Sarah, and her baby brother make it to safety.

text: After the waters recede, President Beck speaks to a large crowd, encouraging them to remember and honor the heroes for their sacrifice.

text: Cast[edit]

text:
Elijah Wood as Leo Biederman
Téa Leoni as Jenny Lerner
Robert Duvall as Captain Spurgeon "Fish" Tanner
Morgan Freeman as President Tom Beck
Maximilian Schell as Jason Lerner
Vanessa Redgrave as Robin Lerner
Leelee Sobieski as Sarah Hotchner
James Cromwell as Former Secretary of the Treasury Alan Rittenhouse
Ron Eldard as Commander Oren Monash
Mary McCormack as Andrea "Andy" Baker
Aleksandr Baluev as Colonel Michail Tulchinsky
Blair Underwood as Mark Simon
Jon Favreau as Gus Partenza
Laura Innes as Beth Stanley
Richard Schiff as Don Biederman
Betsy Brantley as Ellen Biederman
Mike O'Malley as Mike Perry
Rya Kihlstedt as Chloe
Charles Martin Smith as Dr. Marcus Wolf
Dougray Scott as Eric Vennekor
Francis X. McCarthy as General Scott
Kurtwood Smith as Otis Hefter
Denise Crosby as Vicky Hotchner
Jason Dohring as Jason
Christopher Darga as Section Leader

text: Production[edit]

text: The origins of Deep Impact started in the late 1970s when producers Richard Zanuck and David Brown approached Paramount Studios proposing a remake of the 1951 film When Worlds Collide.[1] Although several screenplay drafts were completed, the producers were not completely happy with any of them and the project remained in "development hell" for many years. In the mid 1990s, they approached director Steven Spielberg, with whom they had made the 1975 blockbuster Jaws, to discuss their long-planned project.[1] However, Spielberg had already bought the film rights to the 1993 novel The Hammer of God by Arthur C. Clarke, which dealt with a similar theme of an asteroid on a collision course for Earth and humanity's attempts to prevent its own extinction. Spielberg planned to produce and direct The Hammer of God himself for his then-fledgling DreamWorks studio, but opted to merge the two projects with Zanuck and Brown, and they commissioned a screenplay for what would become Deep Impact.[1] In 1995, the forthcoming film was announced in industry publications as "Screenplay by Bruce Joel Rubin, based on the film When Worlds Collide and The Hammer of God by Arthur C Clarke"[8] though ultimately, following a subsequent redraft by Michael Tolkin, neither source work would be credited in the final film. Spielberg still planned to direct Deep Impact himself, but commitments to his 1997 film Amistad prevented him from doing so in time, particularly as Touchstone Pictures had just announced their own similarly-themed film Armageddon, also to be released in summer 1998.[1] Not wanting to wait, the producers opted to hire Mimi Leder to direct Deep Impact, with Spielberg acting as Executive Producer.[1] Although publicised as an adaptation of his novel both before and after the film's release,[9][10][11][12] Clarke was disgruntled about not being credited on the film.[13][14]

text: Jenny Lerner, the character played by Téa Leoni, was originally intended to work for CNN. CNN rejected this because it would be "inappropriate". MSNBC agreed to be featured in the movie instead, seeing it as a way to gain exposure for the then newly created network.[15]

text: Director Mimi Leder later explained that she would have liked to travel to other countries to incorporate additional perspectives, but due to a strict filming schedule and a low budget, the idea was scratched.[16] Visual effects supervisor Scott Farrar felt that coverage of worldwide events would have distracted and detracted from the main characters' stories.[16]

text: Music[edit]

text:
Deep Impact – Music from the Motion Picture

Soundtrack album by James Horner

Released
May 5, 1998

Recorded
1997–1998

Genre
Film score

Length
77:12

Label
Sony Classical

James Horner chronology

Titanic
(1997)
Deep Impact – Music from the Motion Picture
(1998)
The Mask of Zorro
(1998)

text: The music for the film was composed and conducted by James Horner.

text: Reception[edit]

text: Box office[edit]

text: Deep Impact debuted at the North American box office with $41,000,000 in ticket sales. The movie grossed $140,000,000 in North America and an additional $209,000,000 worldwide for a total gross of $349,000,000. Despite competition in the summer of 1998 from the similar Armageddon, Deep Impact was still a box office hit and was the higher opener of the two.[17]

text: Critical reception[edit]

text: The film had a mixed critical reception. Based on 52 reviews collected by Rotten Tomatoes, 48% of critics enjoyed the film, with an average rating of 5.8/10.[18] Metacritic gave a score of 40 based on 20 reviews. Elvis Mitchell of The New York Times said that the film "has a more brooding, thoughtful tone than this genre usually calls for",[19] while Rita Kempley and Michael O'Sullivan of the Washington Post criticized what they saw as unemotional performances and a lack of tension.[20][21]


document_title: Peter Rabbit (film)

question_text: who does margot robbie voice in peter rabbit

root

text: Peter Rabbit (film)

text: Plot[edit]

text: In England's Lake District Peter Rabbit, his cousin Benjamin Bunny, and Peter's triplet sisters (who can be distinguished by the colour of jackets they each wear) Flopsy (red), Mopsy (yellow), and Cottontail (teal), spend most of their days picking on Mr. Joe McGregor and stealing vegetables from his garden. They are friends with a local woman named Bea who spends her time painting pictures of the rabbits as well as the surrounding nature. Bea takes on a mother-like relationship with the rabbits due to the death of their mother and father. One day Peter is forced to leave his jacket in McGregor's garden and goes back to retrieve it. McGregor spots and catches him, but suddenly dies of a heart attack, due to decades of unhealthy eating habits. Enthralled, Peter invites all of the woodland critters, and then takes over McGregor's manor.

tag: p

text: Meanwhile in London, McGregor's grandnephew Thomas McGregor, an uptight, controlling workaholic, works at the toy department of Harrods department store where he waits for a promotion to associate general manager. He indifferently accepts the news about his great-uncle's death, someone he was completely unaware of, but is infuriated over losing the promotion to a lazy nephew of the managing director and is fired for losing his temper. His now former manager encourages him to to get a hobby and spend some time in the country.

text: When Thomas learns that his great-uncle's manor is valuable and that he's inherited it, he decides to appraise and prepare it for resale in order to start his own toy store to rival Harrods. He kicks out Peter and his friends and begins to upgrade the security of the garden wall and gates, despite Bea's objections. When Peter and Benjamin sneak back into the garden, Thomas catches the latter and attempts to drown Benjamin. His cousins rescue him; Thomas instead accidentally drops the binoculars that Bea had given him earlier, forcing him into the river to retrieve it.

text: Thomas and Peter start a war with each other by setting up traps and other offensive nuisances. Thomas and Bea end up falling in love with each other, which causes Peter to become jealous and wanting to separate them more. Thomas framed Peter for ruining Bea's paintings and she sent Peter outside along with the other rabbits. Soon, Bea turns on Thomas when his violent tendencies begin to show. This all culminates when Thomas throws dynamite at Peter's burrow, and uses it to attack Peter in the garden, before telling him that his antics caused him to become aggressive. When Peter detonates the dynamite to prove to Bea that Thomas was using it, he ends up knocking down the tree on top of the burrow, which crushes Bea's art studio. Thinking that Thomas was responsible for the detonation, Bea breaks up with him, and he goes back to London to work at Harrods again.

text: Peter feels bad for what he has done, and upon learning that Bea intends to leave the neighborhood, he and Benjamin head to London to find Thomas at Harrods. Revealing they can talk, Peter apologizes for his part of the conflict and convinces Thomas to follow his heart. They rush back to the country where Peter reveals that he had activated the detonator, and he and Thomas apologize to Bea for their fighting. Thomas discovers that he cannot go home because a snobbish couple, whom Thomas had an ugly encounter with prior, had just bought the house. Peter and his friends use their tricks to force the couple out of the house, allowing Thomas to move back in.

text: In a mid-credits scene, Thomas sets up his own toy shop in the village, and Bea begins to write and illustrate books based on Peter and his friends.

text: Cast[edit]

text:
Domhnall Gleeson as Thomas McGregor / Mr. Jeremy Fisher (voice)
Rose Byrne as Bea / Jemima Puddle-Duck (voice)
Sam Neill as Mr. Joe McGregor / Tommy Brock (voice)
Marianne Jean-Baptiste as Harrods General Manager
Felix Williamson as Derek

tag: ul

text: Voice cast[edit]

text:
James Corden as Peter Rabbit
Daisy Ridley as Cottontail Rabbit
Margot Robbie as Flopsy Rabbit and the Narrator
Elizabeth Debicki as Mopsy Rabbit
Colin Moody as Benjamin Bunny
Sia as Mrs. Tiggy-Winkle
Fayssal Bazzi as Mr. Tod
Ewen Leslie as Pigling Bland
Christian Gazal as Felix D’eer
Rachel Ward as Josephine Rabbit
Bryan Brown as Mr. Rabbit
David Wenham as Johnny Town-Mouse
Alexandra Gluck and Taryn Gluck as London Street Rats
Will Reichelt as JW Rooster II
Jensen Karp as Rap Bird

text: The Singing Sparrows were voiced by Jessica Freedman, Shana Halligan, Katharine Hoye, Chris Mann, Chad Reisser, and Fletcher Sheridan

text: Production[edit]

text: The film was first revealed in April 2015 through email leaks as a result of the Sony Pictures hack.[8] The official announcement of the film came that December.[9]

text: On August 4, 2016, it was reported that Will Gluck would be directing the live-action/computer-animated film from a script by Gluck and Rob Lieber, with James Corden cast to voice Peter Rabbit and Rose Byrne to play one of the live-action roles.[10] The report also said Gluck would produce the film along with Zareh Nalbandian of Animal Logic, which will be providing the visual effects and animation for the film.[10]

text: On September 26, 2016, Daisy Ridley and Elizabeth Debicki had joined the cast, with the live action production scheduled to commence in Sydney, Australia in January 2017.[11][12][13] On October 18, Domhnall Gleeson was cast as Thomas McGregor, the descendent of the original Mr. McGregor, and on October 24, Margot Robbie joined the cast, expected to voice a bunny.[14][15] On November 7, Sia was cast to join the film as Mrs Tiggy-Winkle.[16]

text: Filming[edit]

text: On December 18, 2016, a first image of the title character, along with the movie's logo, had been revealed.[17] Production began in December 2016.[18][19] Live action scenes were filmed at Centennial Park in Sydney.[20] In March 2017, filming took place at Central railway station, Sydney, which was depicted as London Paddington station.[21]

text: In April 2017, a film crew were seen in Ambleside and Windermere in the Lake District. A local toy shop on Compston Road, Ambleside, was adapted to be Mr McGregor's.[citation needed]

text: Release[edit]

text: Peter Rabbit was originally scheduled to be released on March 23, 2018,[9] but it was moved up to February 9, 2018.[22]

text: Trailer criticism[edit]

text: The first trailer received negative feedback from critics and fans of the character, many of whom labelled the film as being too modern and insulting to Beatrix Potter's works. Collider slammed the trailer as "garbage" and a "low brow 'comedy' cringe fest."[23]

text: Stuart Heritage from The Guardian stated that "the Peter Rabbit film looks like the result of some blisteringly inept manhandling [...] there's something genuinely harrowing about the sight of Peter Rabbit – gentle, Edwardian Peter Rabbit – thoughtlessly injuring some birds, or grabbing a pile of lettuce leaves and making it rain like a banker in a strip club, or literally twerking" and argued "there is no way on Earth that [Beatrix Potter would] have ever given the green light to a slow motion car crash like this."[24]

text: Metro writer James Baldock found that the trailer was "so gut wrenchingly bad" and that "if the movie lives up to its two minute preview – [it] is set to be the greatest abomination to grace the big screen since The Emoji Movie." He finished by writing "Listen carefully, and you can just about hear the sound of Beatrix Potter, turning furiously in her grave."[25] On November 7, a new trailer for the United Kingdom was released.[26]

text: Home media[edit]

text: The film was released on digital platforms on April 20, 2018. A Blu-ray and DVD and 4K followed on May 1, 2018.[27]

text: Reception[edit]

text: Box office[edit]

text: As of May 28, 2018[update], Peter Rabbit has grossed $341.6 million worldwide, $115.1 million of that in the United States and Canada, against a production budget of $50 million.[7]

text: In the United States and Canada, the film was released alongside Fifty Shades Freed and The 15:17 to Paris, and was projected to gross around $16 million from 3,725 theaters in its opening weekend, with some estimates as high as $25 million.[28] It ended up making $25 million over the weekend, finishing second at the box office behind Fifty Shades ($38.8 million).[29]

text: In the UK, Peter Rabbit became the biggest family film of 2018, overtaking Pixar's Coco with $56.3 million.[30] Totals from other markets include China ($26.5 million), Australia ($20.2 million), France ($12.3 million) and Germany ($12.1 million).[31]

text: Critical response[edit]

text: On Rotten Tomatoes, the film has an approval rating of 62% based on 125 reviews and an average rating of 5.8/10. The site's critical consensus reads, "Peter Rabbit updates Beatrix Potter's classic characters with colorfully agreeable results that should entertain younger viewers while admittedly risking the wrath of purists."[32] On Metacritic, the film has a score of 51 out of 100 based on 26 critics, indicating "mixed or average reviews".[33] Audiences polled by CinemaScore gave the film an average grade of "A−" on an A+ to F scale.[34]

text: "Allergy bullying" controversy[edit]

text: In the first week after the film's release, groups in multiple countries criticized it for "allergy bullying" and called for an apology from Sony. The accusations focused on a scene where Thomas McGregor — whose character has a known severe allergy to blackberries — is pelted with the berries until one enters his mouth, causing him to enter anaphylactic shock and grab for his Epipen.[35][36][37] In response, Sony published a statement saying "We sincerely regret not being more aware and sensitive to this issue, and we truly apologise".[38]

text: Sequel[edit]

text: Sony Pictures Animation is developing a sequel set to be released on February 7, 2020, with Gluck returning to write and direct the film.[39]


document_title: List of costliest Atlantic hurricanes

question_text: what is the most costliest hurricane in us history

text: List of costliest Atlantic hurricanes

text: This is a list of costliest Atlantic hurricanes. Hurricanes, as defined by the National Oceanic and Atmospheric Administration (NOAA), are tropical cyclones—a warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters with organized deep convection and a closed surface wind circulation about a well-defined center—in the Atlantic, Caribbean Sea, Gulf of Mexico, or eastern Pacific, in which the maximum 1-minute sustained surface wind exceeds 64 knots (74 mph; 119 km/h) or greater. The hurricanes on the list below depict the severity of the damage the system has caused. Typically, if a hurricane has caused significant damage to a particular location, its name is retired so that it will not be re-used as a name for any future hurricanes. The costliest tropical cyclone ever recorded was Hurricane Harvey, which caused catastrophic flooding in southeastern Texas, in August 2017, causing $125 billion (2017 USD) in property damage. The costliest season on record was 2017, with damage estimated to around $300 billion.

text: A majority of the costliest Atlantic hurricanes in recorded history have peaked as major hurricanes. However, weaker tropical cyclones can still cause widespread damage. Both tropical storms Allison in 2001 and Lee in 2011 have caused over a billion in damage; the former of which accounted for a higher damage total. Due to their excessive damage, the names of tropical cyclones accruing at least $1 billion in damage are often retired by the World Meteorological Organization. However, this is not always the case. Hurricane Juan in 1985 was the first hurricane to cause at least a billion in damage and not be retired; its name was retired on a later usage in 2003 that did not cause over a billion in damage. Since Juan, seven tropical cyclones that caused at least a billion in damage were not retired, including Hurricane Emily in 2005, and the most recent of which being Hurricane Isaac in 2012. All other 46 Atlantic hurricanes to have caused as much damage have had their names retired, excluding recent hurricanes Harvey, Irma, and Maria of the 2017 season.

text: The first hurricane to cause at least $1 billion in damage was Hurricane Betsy in 1965, which caused much of its damage in southeastern Louisiana. Between two and four years later, Hurricanes Beulah and Camille both caused at least $1 billion in damage. After the 1960s, each decade saw an increase in tropical cyclones causing at least a billion in damage over the last, due to increasing urban development and population. In the 1970s, four hurricanes caused at least a billion in damage; the costliest of which was Hurricane Frederic, which caused $2.3 billion in damage, particularly in Mississippi and Alabama. The following decade featured seven hurricanes causing at least a billion in damage. In the 1989 season, Hurricane Hugo was the first storm to hit $10 billion U.S. dollars in cost. In the 1990s, nine tropical cyclones accrued at least a billion in damage. Hurricane Andrew in 1992 greatly exceeded the damage figure of any preceding tropical cyclone after causing $26.5 billion in damage, mostly in South Florida. Seventeen tropical cyclones in the 2000s caused at least $1 billion in damage. The 2005 season had six billion-dollar hurricanes, the most of any season on record. Hurricane Ivan caused at least $1 billion in damage in four separate countries, and according to estimates, Hurricane Irma caused at least $1 billion in damage in five separate countries. Thus far in the 2010s, eleven storms have caused at least $1 billion in damage, with the costliest so far being Hurricane Harvey which caused $125 billion in damage.

text: Overall costliest[edit]

text: This list ranks tropical cyclones within the Atlantic that have accrued at least US$1 billion in damage, based on their nominal USD damage totals. Because these numbers have not been adjusted for inflation, nor adjusted for changes in population and wealth in coastal counties, the costliness of recent hurricanes is artificially inflated compared to hurricanes of the past. This makes it hard to accurately compare the damage inflicted by hurricanes across time.

text:
Costliest Atlantic hurricanes[hide]

Name
Damage
(Billions USD)
Season
Storm classification
at peak intensity
Areas affected
References

Harvey
$125.0
2017
6 !Category 4 hurricane

Texas
Louisiana
South America
Central America
The Caribbean
Yucatan Peninsula

[1]

Katrina
$108.0
2005
7 !Category 5 hurricane

The Bahamas
Florida
United States Gulf Coast
Ohio Valley
Northeast
Eastern Canada

[2]

Maria
$99.45
2017
7 !Category 5 hurricane

Lesser Antilles
Greater Antilles
Caribbean Sea
Eastern United States

[1]

Sandy
$75.0
2012
5 !Category 3 hurricane

The Caribbean
United States East Coast
Eastern Canada

[3][4][5]

Irma
$66.7
2017
7 !Category 5 hurricane

Lesser Antilles
Greater Antilles
Caribbean Sea
Eastern United States

[1]

Ike
$37.5
2008
6 !Category 4 hurricane

Greater Antilles
Texas
Louisiana
Midwestern United States
Eastern Canada
Iceland

[6][7][8]

Wilma
$29.4
2005
7 !Category 5 hurricane

Greater Antilles
Central America
Florida

[9][10][11][12]

Andrew
$26.5
1992
7 !Category 5 hurricane

The Bahamas
Florida
United States Gulf Coast

[6][13]

Ivan
$23.3
2004
7 !Category 5 hurricane

The Caribbean
Venezuela
United States Gulf Coast

[6][14][15]

Irene
$16.6
2011
5 !Category 3 hurricane

The Caribbean
United States East Coast
Eastern Canada

[16][17][18]

Charley
$16.3
2004
6 !Category 4 hurricane

Jamaica
Cayman Islands
Cuba
Florida
The Carolinas

[19]

Matthew
$15.09
2016
7 !Category 5 hurricane

Colombia
Venezuela
The Caribbean
United States East Coast

[20][21]

Rita
$12.0
2005
7 !Category 5 hurricane

Cuba
United States Gulf Coast

[22]

Hugo
$10.0
1989
7 !Category 5 hurricane

The Caribbean
United States East Coast

[6][23]

Frances
$9.8
2004
6 !Category 4 hurricane

The Caribbean
Eastern United States
Ontario

[6][14][24][25]

Georges
$9.72
1998
6 !Category 4 hurricane

The Caribbean
United States Gulf Coast

[6][26][27][28][29][30]

Allison
$9.0
2001
2 !Tropical storm

Texas
Louisiana
Southern United States

[6][31]

Jeanne
$7.66
2004
5 !Category 3 hurricane

The Caribbean
Eastern United States

[6][14][32][33]

Gilbert
$7.1
1988
7 !Category 5 hurricane

Venezuela
Central America
Hispaniola
Mexico

[34]

Floyd
$6.9
1999
6 !Category 4 hurricane

The Bahamas
Eastern United States
Atlantic Canada

[6][35]

Gustav
$6.61
2008
6 !Category 4 hurricane

Hispaniola
Jamaica
Cuba
United States Gulf Coast

[6][7]

Mitch
$6.2
1998
7 !Category 5 hurricane

Central America
Yucatán Peninsula
South Florida

[36][37][38]

Isabel
$5.37
2003
7 !Category 5 hurricane

Greater Antilles
The Bahamas
Eastern United States
Ontario

[6][39]

Opal
$5.1
1995
6 !Category 4 hurricane

Guatemala
Yucatán Peninsula
Eastern United States

[6][40]

Stan
$3.96
2005
3 !Category 1 hurricane

Mexico
Central America

[32][41]

Karl
$3.9
2010
5 !Category 3 hurricane

Mexico
Central America

[42]

Dennis
$3.71
2005
6 !Category 4 hurricane

Greater Antilles
Southeastern United States

[6][9][43]

Fran
$3.2
1996
5 !Category 3 hurricane

Eastern United States
Ontario

[6]

Luis
$3.0
1995
6 !Category 4 hurricane

Leeward Islands
Puerto Rico
Bermuda

[40]

Marilyn
$2.5
1995
5 !Category 3 hurricane

The Caribbean
Bermuda

[6][40]

Lee
$2.5
2011
2 !Tropical storm

United States East Coast

[1]

Isaac
$2.39
2012
3 !Category 1 hurricane

The Caribbean
Eastern United States

[44]

Frederic
$2.3
1979
6 !Category 4 hurricane

The Caribbean
Southeastern United States

[45]

Agnes
$2.1
1972
3 !Category 1 hurricane

Mexico
Cuba
Eastern United States

[6][46]

Joan
$2.0
1988
6 !Category 4 hurricane

Lesser Antilles
Colombia
Venezuela
Central America

[34]

Michelle
$2.0
2001
6 !Category 4 hurricane

Central America
Jamaica
Cuba
The Bahamas

[28][31]

Alex
$1.885
2010
4 !Category 2 hurricane

Central America
Greater Antilles
Texas

[47][48][49][50]

Fifi
$1.8
1974
4 !Category 2 hurricane

Jamaica
Central America
Mexico

[51][52]

Dean
$1.78
2007
7 !Category 5 hurricane

The Caribbean
Central America

[32][53]

Alicia
$1.7
1983
5 !Category 3 hurricane

East Texas
Louisiana

[54]

David
$1.54
1979
7 !Category 5 hurricane

The Caribbean
United States East Coast

[32][45]

Juan
$1.5
1985
3 !Category 1 hurricane

United States Gulf Coast

[6]

Bob
$1.5
1991
5 !Category 3 hurricane

United States East Coast
Canada

[55]

Roxanne
$1.5
1995
5 !Category 3 hurricane

Mexico

[40]

Ingrid
$1.5
2013
3 !Category 1 hurricane

Mexico

[6]

Betsy
$1.45
1965
6 !Category 4 hurricane

The Caribbean
Southeastern United States

[6]

Camille
$1.42
1969
7 !Category 5 hurricane

Cuba
United States Gulf Coast

[6]

Dolly
$1.35
2008
4 !Category 2 hurricane

Cayman Islands
Mexico
Southwestern United States

[7]

Elena
$1.3
1985
5 !Category 3 hurricane

Cuba
United States Gulf Coast

[56]

Isidore
$1.3
2002
5 !Category 3 hurricane

Cuba
Yucatán Peninsula
Louisiana

[57][58]

Allen
$1.24
1980
7 !Category 5 hurricane

The Caribbean
Yucatán Peninsula
Mexico
South Texas

[32][59][60]

Emily
$1.014
2005
7 !Category 5 hurricane

Guyana
Colombia
The Caribbean
Honduras
Belize
Mexico
Texas

[citation needed]

Beulah
$1.0
1967
7 !Category 5 hurricane

The Caribbean
Mexico
Texas

[61]

Alberto
$1.0
1994
2 !Tropical storm

Southeastern United States

[1]

tag: table


document_title: Snake River

question_text: where is the mouth of the snake river

question_tokens: where is the mouth of the snake river

text: Snake River

text: Course[edit]

text: Formed by the confluence of three tiny streams on the southwest flank of Two Oceans Plateau in Yellowstone National Park, western Wyoming, the Snake starts out flowing west and south into Jackson Lake. Its first 50 miles (80 km) run through Jackson Hole, a wide valley between the Teton Range and the Gros Ventre Range. Below the tourist town of Jackson, the river turns west and flows through Snake River Canyon, cutting through the Snake River Range and into eastern Idaho. It receives the Hoback and Greys Rivers before entering Palisades Reservoir, where the Salt River joins at the mouth of Star Valley. Below Palisades Dam, the Snake River flows through the Snake River Plain, a vast arid physiographic province extending through southern Idaho south-west of the Rocky Mountains and underlain by the Snake River Aquifer, one of the most productive aquifers in the United States.[10][11][12][13][14]

text: Southwest of Rexburg, Idaho, the Snake is joined from the north by Henrys Fork. The Henrys Fork is sometimes called the North Fork of the Snake River, with the main Snake above their confluence known as the "South Fork". From there it turns south, flowing through downtown Idaho Falls, then past the Fort Hall Indian Reservation and into American Falls Reservoir, where it is joined by the Portneuf River. The Portneuf River Valley is an overflow channel that in the last glacial period carried floodwaters from pluvial Lake Bonneville into the Snake River, significantly altering the landscape of the Snake River Plain through massive erosion. From there the Snake resumes its journey west, entering the Snake River Canyon of Idaho. It is interrupted by several major cataracts, the largest being 212-foot (65 m) Shoshone Falls, which historically marked the upriver limit of migrating salmon.[10][15] A short distance downstream it passes under the Perrine Bridge.[11][16] Near Twin Falls, the Snake approaches the southernmost point in its entire course, after which it starts to flow west-northwest.[10][11][13][14]

text: The Snake continues through its canyon, receiving the Malad River from the east near Bliss and then the Bruneau River from the south in C.J. Strike Reservoir. It passes through an agricultural valley about 30 miles (48 km) southwest of Boise and flows briefly west into Oregon, before turning north to define the Idaho–Oregon border. Here the Snake River almost doubles in size as it receives several major tributaries – the Owyhee from the southwest, then the Boise and Payette rivers from the east, and further downstream the Malheur River from the west and Weiser River from the east. North of Boise, the Snake enters Hells Canyon, a steep, spectacular, rapid-strewn gorge that cuts through the Salmon River Mountains and Blue Mountains of Idaho and Oregon. Hells Canyon is one of the most rugged and treacherous portions of the course of the Snake River, posing a major obstacle for 19th-century American explorers. Here the Snake is also impounded by Hells Canyon, Oxbow, and Brownlee Dams, which together make up the Hells Canyon Hydroelectric Project.[10][13][14][17]

text: At the halfway point in Hells Canyon, in one of the most remote and inaccessible sections of its course, the Snake River is joined from the east by its largest tributary, the Salmon River. From there, the Snake begins to form the Washington–Idaho border, receiving the Grande Ronde River from the west before receiving the Clearwater River from the east at Lewiston, which marks the head of navigation on the Snake. The river leaves Hells Canyon and turns west, winding through the Palouse Hills of eastern Washington. The Lower Snake River Project's four dams and navigation locks have transformed this part of the Snake River into a series of reservoirs. The confluence of the Snake and Columbia rivers at Burbank, Washington is part of Lake Wallula, the reservoir of McNary Dam. The Columbia River flows about 325 miles (523 km) further west to the Pacific Ocean near Astoria, Oregon.[10][13][14]

text: Geology[edit]

text: As recently as 165 million years ago, most of western North America was still part of the Pacific Ocean. The nearly complete subduction of the Farallon Plate underneath the westward-moving North American Plate created the Rocky Mountains, which were pushed up by rising magma trapped between the sinking Farallon plate and the North American plate. As the North American Plate moved westwards over a stationary hotspot beneath the crust, a series of tremendous lava flows and volcanic eruptions carved out the Snake River Plain beginning about 12 million years ago, west of the Continental Divide.[18]  Even larger lava flows of Columbia River basalts issued over eastern Washington, forming the Columbia Plateau southeast of the Columbia River and the Palouse Hills in the lower Snake.[19] Separate volcanic activity formed the northwestern portion of the plain, an area far from the path of the hotspot which now lies beneath Yellowstone National Park.[18] At this point, the Snake River watershed was beginning to take shape.

text: The Snake River Plain and the gap between the Sierra Nevada and Cascade Range together formed a "moisture channel," opening the way for Pacific storms to travel more than 1,000 miles (1,600 km) inland to the headwaters of the Snake River. When the Teton Range uplifted about 9 million years ago along a detachment fault running north–south through the central Rockies,[20] the river maintained its original course and cut through the southern end of the mountains, forming the Snake River Canyon of Wyoming. About 6 million years ago, the Salmon River Mountains and Blue Mountains at the far end of the plain began to rise; the river cut through these mountains as well, forming Hells Canyon was. Lake Idaho, formed during the Miocene, covered a large portion of the Snake River Plain between Twin Falls and Hells Canyon, and its lava dam was finally breached about 2 million years ago.[21]

text: Lava flowing from Cedar Butte in present southeast Idaho blocked the Snake River at Eagle Rock about 42,000 years ago, near the present-day site of American Falls Dam. A 40-mile-long (64 km) lake, known as American Falls Lake, formed behind the barrier. The lake was stable and survived for nearly 30,000 years. About 14,500 years ago, pluvial Lake Bonneville in the Great Salt Lake area, formed in the last glacial period, spilled catastrophically down the Portneuf River into the Snake in an event known as the Bonneville Flood.[22] This was one of the first in a series of catastrophic flooding events in the Northwest known as the Ice Age Floods.

text: The deluge caused American Falls Lake to breach its natural lava dam, which was rapidly eroded with only the 50-foot-high (15 m) American Falls left in the end. The flood waters of Lake Bonneville, approximately twenty times the flow of the Columbia River or 5 million ft3/s (140,000 m3/s), swept down the Snake River and across the entirety of southern Idaho. For miles on either side of the river, flood waters stripped away soils and scoured the underlying basalt bedrock, forming the Snake River Canyon and creating Shoshone Falls, Twin Falls, Crane Falls, Swan Falls and other waterfalls along the Idaho section of the river.[23] The Bonneville flood waters continued through Hells Canyon and eventually reached the Columbia River. The flood widened Hells Canyon but did not deepen it.[24][25]

text: As the Bonneville Floods rushed down the Snake River, the Missoula Floods occurred in the same period, but originating farther north. The Missoula Floods, which occurred more than 40 times between 15,000 and 13,000 years ago, were caused by Glacial Lake Missoula on the Clark Fork repeatedly being impounded by ice dams then breaking through, with the lake's water rushing over much of eastern Washington in massive surges far larger than the Lake Bonneville Flood. These floods pooled behind the Cascade Range into enormous lakes and spilled over the northern drainage divide of the Snake River watershed, carving deep canyons through the Palouse Hills including the Palouse River canyon and Palouse Falls. The Lake Bonneville Floods and the Missoula Floods helped widen and deepen the Columbia River Gorge, a giant water gap which allows water from the Columbia and Snake rivers to take a direct route through the Cascade Range to the Pacific.[24][26][27]

text: The massive amounts of sediment deposited by the Lake Bonneville Floods in the Snake River Plain also had a lasting effect on most of the middle Snake River. The high hydraulic conductivity of the mostly-basalt rocks in the plain led to the formation of the Snake River Aquifer, one of the most productive aquifers in North America. Many rivers and streams flowing from the north side of the plain sink into the aquifer instead of flowing into the Snake River, a group of watersheds called the lost streams of Idaho.[28] The aquifer filled to hold nearly 100,000,000 acre feet (120 km3) of water, underlying about 10,000 square miles (26,000 km2) in a plume 1,300 feet (400 m) thick.[29] In places, water exits from rivers at rates of nearly 600 cubic feet per second (17 m3/s).[23] Much of the water lost by the Snake River as it transects the plain issues back into the river at its western end, by way of many artesian springs.[12][30][31]

text: Watershed[edit]

text: The Snake River is the thirteenth longest river in the United States.[9] Its watershed is the 10th largest among North American rivers, and covers almost 108,000 square miles (280,000 km2) in portions of six U.S. states: Wyoming, Idaho, Nevada, Utah, Oregon, and Washington, with the largest portion in Idaho. Most of the Snake River watershed lies between the Rocky Mountains on the east and the Columbia Plateau on the northwest. The largest tributary of the Columbia River, the Snake River watershed makes up about 41% of the entire Columbia River Basin. Its average discharge at the mouth constitutes 31% of the Columbia's flow at that point.[32][33] Above the confluence, the Snake is slightly longer than the Columbia—1,078 miles (1,735 km)[5] compared to 928 miles (1,493 km)[34]—and its drainage basin is slightly larger—4% bigger than the upstream Columbia River watershed.[6][35]

text: The mostly semi-arid, even desert climate of the Snake River watershed on average, receives less than 12 inches (300 mm) of precipitation per year. However, precipitation in the Snake River watershed varies widely. At Twin Falls, in the center of the Snake River Plain, the climate is nearly desert, with an annual rainfall of just 9.24 inches (235 mm), although the average snowfall is 13.1 inches (330 mm).[36] This desert climate occupies the majority of the basin of the Snake River, so although it is longer than the Columbia River above the Tri-Cities, its discharge is on average significantly less. However, in the high Rockies of Wyoming, in the upper Jackson Hole area, the average precipitation is over 30 inches (760 mm), and snowfall averages 252 inches (6,400 mm).[37] Most of the Snake River basin consists of wide, arid plains and rolling hills, bordered by high mountains. In the upper parts of the watershed, however, the river flows through an area with a distinct alpine climate. There are also stretches where the river and its tributaries have incised themselves into tight gorges. The Snake River watershed includes parts of Yellowstone National Park, Grand Teton National Park, Hells Canyon National Recreation Area, and many other national and state parks.

text: Much of the area along the river, within a few miles of its banks, is irrigated farmland, especially in its middle and lower course. Irrigation dams include American Falls Dam, Minidoka Dam, and C.J. Strike Dam. Aside from water from the river, water is also pulled from the Snake River Aquifer for irrigation. Major cities along the river include Jackson in Wyoming, Twin Falls, Idaho Falls, Boise, and Lewiston in Idaho, and the Tri-Cities in Washington (Kennewick, Pasco and Richland). There are fifteen dams in total along the Snake River, which aside from irrigation, also produce electricity, maintain a navigation channel along part of the river's route, and provide flood control.[38] However, fish passage is limited to the stretch below Hells Canyon.[39]

text:
The Snake River watershed is bounded by several other major North American watersheds, which drain both to the Atlantic or the Pacific, or into endorheic basins. On the southwest side a divide separates the Snake watershed from Oregon's Harney Basin, which is endorheic. On the south, the Snake watershed borders that of the Humboldt River in Nevada, and the watershed of the Great Salt Lake (the Bear, Jordan and Weber rivers) on the south.[40]
The Snake River also shares a boundary with the Green River to the southeast; the Green River drains parts of Wyoming and Utah and is the largest tributary of the Colorado River. On the western extremity for a short stretch the Continental Divide separates the Snake watershed from the Bighorn River, a tributary of the Yellowstone River, which the Snake begins near. On the north the Snake River watershed is bounded by the Red Rock River, a tributary of the Beaverhead River, which flows into the Jefferson River and into the Missouri River, part of the Gulf of Mexico drainage basin.[40]

text: The rest of the Snake River watershed borders on several other major Columbia River tributaries - mostly the Spokane River to the north, but also Clark Fork in Montana to the northeast and the John Day River to the west. Of these, the Clark Fork (via the Pend Oreille River) and the Spokane join the Columbia above the Snake, while the John Day joins downstream of the Snake, in the Columbia River Gorge. It is of note that the northeastern divide of the Snake River watershed forms the Idaho-Montana boundary, so the Snake River watershed does not extend into Montana.[40]

text: Mountain ranges in the Snake watershed include the Teton Range, Bitterroot Range, Clearwater Mountains, Seven Devils Mountains, and the extreme northwestern end of the Wind River Range. Grand Teton is the highest point in the Snake River watershed, reaching 13,775 feet (4,199 m) in elevation. The elevation of the Snake River is 358 feet (109 m) when it joins the Columbia River.[2]

text: Pollution[edit]

text: Agricultural runoff from farms and ranches in the Snake River Plain and many other areas has severely damaged the ecology of the river throughout the 20th century. After the first irrigation dams on the river began operation in the first decade of the 20th century, much of the arable land in a strip a few miles wide along the Snake River was cultivated or turned to pasture, and agricultural return flows began to pollute the Snake. Runoff from several feedlots was dumped into the river until laws made the practice illegal.[41] Fertilizer, manure and other chemicals and pollutants washed into the river greatly increase the nutrient load, especially of phosphorus, fecal coliforms and nitrogen. During low water, algae blooms occur throughout the calm stretches of the river, depleting its oxygen supply.[42]

text: Much of the return flows do not issue directly back into the Snake River, but rather feed the Snake River Aquifer underneath the Snake River Plain. Water diverted from the river for irrigation, after absorbing any surface pollutants, re-enters the ground and feeds the aquifer. Although the aquifer has maintained its level, it has become increasingly laced with contaminants. Water in the aquifer eventually travels to the west side of the Snake River Plain and re-enters the river as springs.[43] Throughout much of the Snake River Plain and Hells Canyon, excessive sediment is also a recurring problem.[44] In December 2007, the U.S. Environmental Protection Agency (EPA) issued a permit requiring owners of fish farms along the Snake River to reduce their phosphorus discharge by 40%. Pollutant levels in Hells Canyon upstream of the Salmon River confluence, including that of water temperature, dissolved nutrients, and sediment, are required to meet certain levels.[45]

text: Discharge[edit]

text: The Snake River's average flow is 54,830 cubic feet per second (1,553 m3/s). The United States Geological Survey recorded the river's discharge from a period of 1963–2000 at a stream gauge below Ice Harbor Dam. In that period, the largest average annual flow recorded was 84,190 cu ft/s (2,384 m3/s) in 1997, and the lowest was 27,100 cu ft/s (770 m3/s) in 1992.[7] The lowest recorded daily mean flow was 2,700 cu ft/s (76 m3/s) on February 4, 1979. On August 27, 1965, there was temporarily no flow as a result of testing at Ice Harbor Dam. The highest recorded flow was 312,000 cu ft/s (8,800 m3/s) on June 19, 1974.[7] The highest flow ever recorded on the Snake River was at a different USGS stream gauge near Clarkston, which operated from 1915 to 1972. This gauge recorded a maximum flow of 369,000 cu ft/s (10,400 m3/s)—more than the Columbia's average discharge—on May 29, 1948. An even larger peak discharge, estimated at 409,000 cu ft/s (11,600 m3/s), occurred during the flood of June 1894.[8]

text: The river's flow is also measured at several other points in its course. Above Jackson Lake, Wyoming, the discharge is about 885 cu ft/s (25.1 m3/s) from a drainage area of 486 square miles (1,260 km2).[46] At Minidoka, Idaho, about halfway through the Snake River Plain, the river's discharge rises to 7,841 cu ft/s (222.0 m3/s).[47] However, at Buhl, Idaho, only about 50 miles (80 km) downstream, the river's flow decreases to 4,908 cu ft/s (139.0 m3/s) because of agricultural diversions and seepage.[48] But at the border of Idaho and Oregon, near Weiser at the beginning of Hells Canyon, the Snake's flow rises to 17,780 cu ft/s (503 m3/s) after receiving several major tributaries such as the Payette, Owyhee and Malheur.[49] The discharge further increases to 19,530 cu ft/s (553 m3/s) at Hells Canyon Dam on the border of Idaho and Oregon.[50] At Anatone, Washington, downstream of the confluence with the Salmon, one of the Snake's largest tributaries, the mean discharge is 34,560 cu ft/s (979 m3/s).[51]

text: History[edit]

text: Name[edit]

text:
Canadian explorer David Thompson first recorded the Native American name of the Snake River as Shawpatin when he arrived at its mouth by boat in 1800. When the Lewis and Clark Expedition crossed westwards into the Snake River watershed in 1805, they first gave it the name Lewis River, Lewis Fork or Lewis's Fork, as Meriwether Lewis was the first of their group to sight the river.[52]
They also made note of the "Snake Indians" who lived along the river, who were actually the Shoshone tribe, and learned that the Native Americans called the river Ki-moo-e-nim or Yam-pah-pa (for an herb that grew prolifically along its banks).[53]
Later American explorers, some of whom were originally part of the Lewis and Clark expedition, journeyed into the Snake River watershed and records show a variety of names have been associated with the river. The explorer Wilson Price Hunt of the Astor Expedition named the river as Mad River. Others gave the river names including Shoshone River (after the tribe) and Saptin River.[2] Eventually, the name Snake River was derived from an S-shaped gesture the Shoshone tribe made with their hands to represent swimming salmon. Explorers misinterpreted it to represent a snake, giving the river its present-day name.[54]

text: Early inhabitants[edit]

text: People have been living along the Snake River for at least 11,000 years. Historian Daniel S. Meatte divides the prehistory of the western Snake River Basin into three main phases or "adaptive systems". The first he calls "Broad Spectrum Foraging", dating from 11,500 to 4,200 years before present. During this period people drew upon a wide variety of food resources. The second period, "Semisedentary Foraging", dates from 4,200–250 years before present and is distinctive for an increased reliance upon fish, especially salmon, as well as food preservation and storage. The third phase, from 250 to 100 years before present, he calls "Equestrian Foragers". It is characterized by large horse-mounted tribes that spent long amounts of time away from their local foraging range hunting bison.[55] In the eastern Snake River Plain there is some evidence of Clovis, Folsom, and Plano cultures dating back over 10,000 years ago.

text: Early fur traders and explorers noted regional trading centers, and archaeological evidence has shown some to be of considerable antiquity. One such trading center in the Weiser area existed as early as 4,500 years ago. The Fremont culture may have contributed to the historic Shoshones, but it is not well understood. Another poorly understood early cultural component is called the Midvale Complex. The introduction of the horse to the Snake River Plain around 1700 helped in establishing the Shoshone and Northern Paiute cultures.[56][57]

text: On the Snake River in southeastern Washington there are several ancient sites. One of the oldest and most well-known is called the Marmes Rockshelter, which was used from over 11,000 years ago to relatively recent times. The Marmes Rockshelter was flooded in 1968 by Lake Herbert G. West, the Lower Monumental Dam's reservoir.[58]

text: Eventually, two large Native American groups controlled most of the Snake River: the Nez Perce, whose territory stretched from the southeastern Columbia Plateau into northern Oregon and western Idaho, and the Shoshone, who occupied the Snake River Plain both above and below Shoshone Falls. Lifestyles along the Snake River varied widely. Below Shoshone Falls, the economy centered on salmon, who often came up the river in enormous numbers. Salmon were the mainstay of the Nez Perce and most of the other tribes below Shoshone Falls. Above the falls, life was significantly different. The Snake River Plain forms one of the only relatively easy paths across the main Rocky Mountains for many hundreds of miles, allowing Native Americans both east and west of the mountains to interact. As a result, the Shoshone centered on a trading economy.

text: According to legend, the Nez Perce tribe was first founded in the valley of the Clearwater River, one of the Snake River's lowermost major tributaries. At its height, there were at least 27 Nez Perce settlements along the Clearwater River and 11 more on the Snake between the mouth of the Clearwater and Imnaha Rivers. There were also villages on the Salmon River, Grande Ronde River, Tucannon River, and the lower Hells Canyon area. The Snake River's annual salmon run, which was estimated at that time to exceed four million in good years, supported the Nez Perce, who lived in permanent, well-defined villages, unlike the nomadic southeastern tribes along the Snake River. The Nez Perce also were involved in trade with the Flathead tribe to the north and other middle Columbia River tribes. However, they were enemies to the Shoshone and the other upstream Snake River tribes.[59]

text: The Shoshone or Shoshoni were characterized by nomadic groups that took their culture from the earlier Bitterroot culture and Great Basin tribes that migrated north via the Owyhee River. They were the most powerful tribe in the Rocky Mountains area, and were known to many Great Plains tribes as the "Snakes". In the 18th century, Shoshone territory extended beyond the Snake River Plain, extending over the Continental Divide into the upper Missouri River watershed and even further north into Canada.[60] A smallpox epidemic brought by European explorers and fur trappers was responsible for wiping out much of the Shoshone east of the Rocky Mountains, but the Shoshone continued to occupy the Snake River Plain. Eventually, the Shoshone culture merged with that of the Paiute and Bannock tribes, which came from the Great Basin and the Hells Canyon area, respectively. The Bannock brought with them the skill of buffalo hunting and horses they had acquired from Europeans, changing the Shoshone way of life significantly.[61]

text: Exploration and settling[edit]

text: The Lewis and Clark Expedition (1804–06) was the first American group to cross the Rocky Mountains and sail down the Snake and Columbia rivers to the Pacific Ocean.[62] Meriwether Lewis supposedly became the first American to sight the drainage basin of the Snake River after he crossed the mountains a few days ahead of his party on August 12, 1805, and sighted the Salmon River valley (a major Snake tributary) from Lemhi Pass, a few miles from the present-day site of Salmon, Idaho. The party later traveled north, descended the Lemhi River to the Salmon and attempted to descend it to the Snake, but found it impassable because of its violent rapids. The expedition named the Snake River the Lewis River, Lewis's River, or Lewis Fork, in his honor, and they traveled northwards to the Lochsa River, which they traveled via the Clearwater River into the lower Snake, and into the Columbia. They also referred to the Shoshone Indians as the "Snake Indians", which became the present-day name of the river.[63][64] The name "Lewis Fork", however, did not last.[62]

text:
Later American explorers traveled throughout the Snake River area and up its major tributaries beginning in 1806, just after Lewis and Clark had returned. The first was John Ordway in 1806, who also explored the lower Salmon River. John Colter in 1808 was the first to sight the upper headwaters of the Snake River, including the Jackson Hole area.[65]
In 1810, Andrew Henry, along with a party of fur trappers, discovered the Henrys Fork of the Snake River, which is now named after him. Donald Mackenzie sailed the lower Snake River in 1811, and later explorers included Wilson Price Hunt of the Astor Expedition (who gave the river the name "Mad River"),[66] Ramsay Crooks, Francisco Payelle, John Grey, Thyery Goddin, and many others after the 1830s.[65] Many of these later explorers were original members of the Lewis and Clark Expedition who had returned to map and explore the area in greater detail. Even later, American fur trappers scouted the area for beaver streams, but Canadian trappers from the British Hudson's Bay Company were by now a major competitor.

text: The Hudson's Bay Company first sent fur trappers into the Snake River watershed in 1819. The party of three traveled into the headwaters of the Owyhee River, a major southern tributary of the Snake, but disappeared.[67] Meanwhile, as American fur trappers kept coming to the region, the Hudson's Bay Company ordered the Canadian trappers to kill as many beavers as they could, eventually nearly eradicating the species from the Snake River watershed, under the "rationale [that] if there are no beavers, there will be no reason for the Yanks ([Americans]) to come."[67] Their goal was to eventually gain rights over the Oregon Territory, a region covering Washington, Oregon, Idaho, and parts of Montana and Wyoming (most of the present-day region called the Pacific Northwest).[68] However, the area was eventually annexed into the United States.

text: By the middle 19th century, the Oregon Trail had been established, generally following much of the Snake River. One crossing the trail made over the Snake River was near the present-day site of Glenns Ferry. Several years later, a ferry was established at the site, replacing the old system where pioneers had to ford the wide, powerful and deep Snake. Another place where pioneers crossed the Snake was further upstream, at a place called "Three Island Crossing", near the mouth of the Boise River. This area has a group of three islands (hence the name) that splits the Snake into four channels each about 200 feet (61 m) wide. Some emigrants chose to ford the Snake and proceed down the west side and recross the river near Fort Boise into Hells Canyon, continue down the drier east side into the gorge, or float the Snake and Columbia to the Willamette River, the destination of the Oregon Trail. The reason for the Three Island Crossing was the better availability of grass and water access.[69] Numerous ferries have provided crossings of the upper Snake from the Brownlee Ferry at the head of Hell's Canyon[70] to Menor's Ferry,[71] which operates today at Moose, Wyoming. Sophistication varied from reed boats pulled by Indians on horse back at Snake Fort, Fort Boise, as described by Narcissa Whitman[72] in 1836 to an electric operated ferry, the Swan Falls Ferry,[73] at Swan Falls Dam of the early 20th century.

text: Steamboats[edit]

text: Unlike the Columbia River, it was far more difficult for steamboats to navigate on the Snake. The Columbia River drops 2,690 feet (820 m) from source to mouth, while the Snake drops over 8,500 feet (2,600 m) in elevation over a length more than 200 miles (320 km) shorter. Still, from the 1860s to the 1940s, steamboats traveled on the Snake River from its mouth at the Columbia River to near the mouth of the Imnaha River in lower Hells Canyon.[74] However, most of the steamboats only sailed from the river's mouth to Lewiston, located at the confluence of the Snake and Clearwater rivers.[75] This stretch of the river is the easiest to navigate for watercraft since it has the least elevation change, although it still contained over 60 sets of rapids.[76]

text: Passenger and freight service downstream of Lewiston lasted throughout the late 19th century and persisted until the introduction of railroads in the Palouse Hills grain-growing region and ultimately, the construction of dams on the lower Snake to facilitate barge traffic, which caused the demise of both the steamboats and the railroad. Lewiston, 140 miles (230 km) from the confluence of the Snake and Columbia and 465 miles (748 km) from the mouth of the Columbia on the Pacific Ocean, became connected with Portland and other Pacific ports via steamboat service from the mouth of the Snake through the Columbia River Gorge.[77] A commonly traveled route was from Wallula, Washington, 120 miles (190 km) downstream of the Snake River's mouth, upstream to Lewiston.[78] The Oregon Steam Navigation Company launched the Shoshone at Fort Boise in 1866 which provided passenger and freight service on the upper Snake for the Boise and Owyhee mines.[79]

text: By the 1870s, the OSN Company, owned by the Northern Pacific Railroad, was operating seven steamboats for transporting wheat and grain from the productive Palouse region along the Snake and Columbia to lower Columbia River ports. These boats were the Harvest Queen, John Gates, Spokane, Annie Faxon, Mountain Queen, R.R. Thompson, and Wide West, all of which were built on the Columbia River.[80] However, there were more resources along the Snake River than wheat and grain. In the 1890s, a huge copper deposit was discovered at Eureka Bar in Hells Canyon. Several ships were built specifically to transport ore from there to Lewiston: these included Imnaha, Mountain Gem, and Norma.[81] In 1893 the Annie Faxon suffered a boiler explosion and sank on the Snake below Lewiston.[75][82]

text: River modifications[edit]

text: Dams[edit]

text: A total of fifteen dams have been constructed along the Snake River for a multitude of different purposes, from its headwaters in the Rocky Mountains to its mouth on Lake Wallula, the reservoir formed behind McNary Dam on the Columbia River. Dams on the Snake can be grouped into three major categories. From its headwaters to the beginning of Hells Canyon, many small dams block the Snake to provide irrigation water. Between here and Hells Canyon, the first dam on the Snake, Swan Falls Dam, was built in 1901. In Hells Canyon, a cascade of dams produce hydroelectricity from the river's steep fall over a comparatively short distance. Finally, a third cascade of dams, from Hells Canyon to the mouth, facilitates navigation. Many different government and private agencies have worked to build dams on the Snake River, which now serve an important purpose for people living in the drainage basin and trade of agricultural products to Pacific seaports.

text:
The Minidoka Irrigation Project of the U.S. Bureau of Reclamation, created with the passage of the Reclamation Act of 1902, involved the diversion of Snake River water into the Snake River Plain upstream of Shoshone Falls in order to irrigate approximately 1,100,000 acres (4,500 km2) in the Snake River Plain and store 4,100,000 acre feet (5.1 km3) of water in Snake River reservoirs.[83]
The first studies for irrigation in the Snake River Plain were conducted by the United States Geological Survey in the late 19th century, and the project was authorized on April 23, 1904.[84] The first dam constructed for the project was Minidoka Dam in 1904; its power plant began operating in 1909, producing 7 MW of electricity. This capacity was revised to 20 MW in 1993.[85]

text: Jackson Lake Dam, far upstream in Wyoming's Grand Teton National Park, was built in 1907 to raise Jackson Lake for providing additional water storage in dry years. American Falls Dam, upstream of Minidoka, was completed in 1927 and replaced in 1978.[84] As the dams were constructed above Shoshone Falls, the historical upriver limit of salmon and also a total barrier to boats and ships, no provisions were made for fish passage or navigation. Several other irrigation dams were also built - including Twin Falls Dam and Palisades Dam.

text: The Hells Canyon Project was built and maintained by Idaho Power Company starting in the 1940s, and was the second of the three major water projects on the river. The three dams of the project, Brownlee Dam, Oxbow Dam and Hells Canyon Dam, are located in upper Hells Canyon. All three dams are primarily for power generation and flood control, and do not have fish passage or navigation locks.[86]

text: Brownlee Dam, the most upriver dam, was constructed in 1959, and generates 728 megawatts (MW). Oxbow Dam, the second dam in the project, was built in 1961 and generates 220 MW. The dam was named for a 3-mile-wide (4.8 km) bend in the Snake River, shaped like an oxbow. Hells Canyon Dam was the last and most downriver of the three. It was constructed in 1967 and generates 450 MW.[38]

text: Downriver of Hells Canyon is the Lower Snake River Project, authorized by the Rivers and Harbors Act of 1945 for the U.S. Army Corps of Engineers to create a navigable channel on the Snake River from its mouth to the beginning of Hells Canyon.[87] These dams are, from upstream to downstream: Lower Granite Lock and Dam, Little Goose Lock and Dam, Lower Monumental Lock and Dam, and Ice Harbor Lock and Dam. Dredging work was also done throughout the length of the navigation channel to facilitate ship passage. These dams form a cascade of reservoirs with no stretches of free-flowing river in between. Immediately below Ice Harbor Dam is Lake Wallula, formed by the construction of the McNary Dam on the Columbia River. (McNary Dam is not part of the Lower Snake River Project.) Above Lower Granite Dam, the river channel from Lewiston to Johnson Bar, just below Hells Canyon, is also maintained for jet-boats as this section is too rugged for ships.[88]

text: These dams have been proposed for removal, and if they were to be removed, it would be the largest dam removal project ever undertaken in the United States.[89] The removal has been proposed on the grounds that it would restore salmon runs to the lower Snake River and the Clearwater River and other smaller tributaries.[90] Idaho's Snake river once teemed with sockeye salmon. However, there are almost no wild sockeye salmon left in the river due to a number of factors.

text: There are many reasons why Sockeye Salmon in the Snake River are reduced in number. One reason is that the river runs through three different states, and is over 1,000 miles (1,600 km) long. Salmon swimming upstream in this river are faced with predators and dams. The Snake River has fifteen dams and is extremely difficult for salmon to access because of hydroelectric dams. Hell's Canyon Dam blocks passage to the entire upper Snake River. The Grand Coulee Dam also blocks spawning grounds to the famous "June Hogs" (legendary Chinook salmon that weighed over 100 pounds [45 kg]).

text: Between 1985 and 2007, only an average of 18 sockeye salmon returned to Idaho each year. Serious conservation efforts by wildlife biologists and fish hatcheries have captured the few remaining wild sockeye salmon, collected their sperm and eggs, and in a laboratory, have them spawn. Instead of spawning naturally, these sockeye begin their lives in an incubator in a fishery biologist's laboratory. These baby salmon then are transported by ship, bypassing the dams. (The dams can hurt juvenile baby sockeye salmon with their powerful tides and currents, which suck the baby salmon down.) Another conservation effort that has helped the salmon recover, is the destruction of old, outdated dams, such as the Lewiston Dam on the Clearwater River, a tributary of the Snake. After destroying the dam, salmon populations noticeably recovered.[91]

text: Another interesting recovery method conservationists and biologists are using is called Fish Transportation. Since many juvenile salmon perish at each dam while swimming out to the ocean, massive ships filter and collect these baby salmon by size and take them out to the ocean for a ride, where they can be guaranteed to make it alive to saltwater. This method raises controversy to the effectiveness and costs, since this method is extremely expensive, almost costing $15 million. Another similar method to transport fish across the dams is the "Fish Gun" method. Engineers at Whooshh Innovations have developed a "Whooshh Fish Transport System" that literally collects salmon and shoots them above the dam at high speed in an effort to get them across the dams.[92]

text: Overall, these combined efforts have had good success. In the summer of 2006, the Snake River reportedly only had 3 sockeye salmon that returned to their spawning grounds.  In the summer of 2013, more than 13,000 sockeye salmon returned to the spawning grounds.[93]

text: Navigation[edit]

text: In the 1960s and 1970s the U.S. Army Corps of Engineers built four dams and locks on the lower Snake River to facilitate shipping. The lower Columbia River has likewise been dammed for navigation. Thus a deep shipping channel through locks and slackwater reservoirs for heavy barges exists from the Pacific Ocean to Lewiston, Idaho. Most barge traffic originating on the Snake River goes to deep-water ports on the lower Columbia River, such as Portland. Grain, mostly wheat, is the main product shipped from the Snake, and nearly all of it is exported internationally from the lower Columbia River ports.

text: The shipping channel is authorized to be at least 14 feet (4 m) deep and 250 feet (76 m) wide. Where river depths were less than 14 feet (4 m), the shipping channel has been dredged in most places. Dredging and redredging work is ongoing and actual depths vary over time.[94] With a channel about 5 feet (1.5 m) deeper than the Mississippi River system, the Columbia and Snake rivers can float barges twice as heavy.[95] Agricultural products from Idaho and eastern Washington are among the main goods transported by barge on the Snake and Columbia rivers. Grain, mainly wheat, accounts for more than 85% of the cargo barged on the lower Snake River. In 1998, over 123,000,000 US bushels (4.3×109 l; 980,000,000 US dry gal; 950,000,000 imp gal) of grain were barged on the Snake. Before the completion of the lower Snake dams, grain from the region was transported by truck or rail to Columbia River ports around the Tri-Cities. Other products barged on the lower Snake River include peas, lentils, forest products, and petroleum.[94]

text: Biology[edit]

text: The World Wide Fund for Nature (WWF) divides the Snake River's watershed into two freshwater ecoregions: the "Columbia Unglaciated" ecoregion and the "Upper Snake" ecoregion. Shoshone Falls marks the boundary between the two. The WWF placed the ecoregion boundary about 50 kilometres (31 mi) downriver from Shoshone Falls in order to include the Big Wood River (the main tributary of the Malad River) in the Upper Snake ecoregion, because the Wood River is biologically distinct from the rest of the downriver Snake. Shoshone Falls has presented a total barrier to the upstream movement of fish for 30,000 to 60,000 years. As a result, only 35% of the fish fauna above the falls, and 40% of the Wood River's fish fauna, are shared with the lower Snake River.[96][97]

text: The Upper Snake freshwater ecoregion includes most of southeastern Idaho and extends into small portions of Wyoming, Utah, and Nevada, including major freshwater habitats such as Jackson Lake. Compared to the lower Snake River and the rest of the Columbia River's watershed, the Upper Snake ecoregion has a high level of endemism, especially among freshwater molluscs such as snails and clams. There are at least 21 snail and clam species of special concern, including 15 that appear to exist only in single clusters. There are 14 fish species found in the Upper Snake region that do not occur elsewhere in the Columbia's watershed, but which do occur in Bonneville freshwater ecoregion of western Utah, part of the Great Basin and related to the prehistoric Lake Bonneville. The Wood River sculpin (Cottus leiopomus) is endemic to the Wood River. The Shoshone sculpin (Cottus greenei) is endemic to the small portion of the Snake River between Shoshone Falls and the Wood River.[98]

text: The Snake River below Shoshone Falls is home to thirty-five native fish species, of which twelve are also found in the Columbia River and four of which are endemic to the Snake: the relict sand roller (Percopsis transmontana) of the Percopsidae family, the shorthead sculpin (Cottus confusus), the maginated sculpin (Cottus marginatus), and the Oregon chub (Oregonichthys crameri). The Oregon chub is also found in the Umpqua River and nearby basins. The lower Snake River also supports seven species of Pacific salmon and trout (Oncorhynchus). There are also high, often localized levels of mollusc endemism, especially in Hells Canyon and the basins of the Clearwater River, Salmon River, and middle Snake River. The mollusc richness extends into the lower Columbia River and tributaries such as the Deschutes River.[98]

text: Animals[edit]

text: Aside from aquatic species, much of the Snake River watershed supports larger animals including numerous species of mammals, birds, amphibians, and reptiles. Especially in the headwaters and the other mountainous areas strewn throughout the watershed, the gray wolf, grizzly bear, wolverine, mountain lion and Canada lynx are common. It has been determined that there are 97 species of mammals in the upper part of the Snake River, upstream from the Henrys Fork confluence.[11] Pronghorn and bighorn sheep are common in the area drained by the "lost streams of Idaho", several rivers and large creeks that flow south from the Rocky Mountains and disappear into the Snake River Aquifer. About 274 bird species, some endangered or threatened, use the Snake River watershed, including bald eagle, peregrine falcon, whooping crane, greater sage-grouse, and yellow-billed cuckoo. Barrow's goldeneye are a species of bird that occurs commonly along the lower section of the Snake River.[11]

text: Ten amphibian and twenty species of reptiles inhabit the upper Snake River's wetland and riparian zones. Several species of frogs are common in the "lost streams" basin and the northeasternmost part of the Snake River watershed, including the inland tailed frog, northern leopard frog, western toad, Columbia spotted frog, long-toed salamander, spadefoot toad.[11] However, in the lower and middle portions of the Snake River watershed, several native species have been severely impacted by agriculture practices and the resulting non-native species supported by them. Introduced birds include the gray partridge, ring-necked pheasant, and chukar. Other non-native species include the bullfrog, brown-headed cowbird, and European starling, attracted by the construction of cities and towns.[99]

text: Plants[edit]

text: The Snake River watershed includes a diversity of vegetation zones both past and present.[11] A majority of the watershed was once covered with shrub-steppe grassland, most common in the Snake River Plain and also the Columbia Plateau in southeastern Washington. Riparian zones, wetlands and marshes once occurred along the length of the Snake River and its tributaries. In higher elevations, conifer forests, of which ponderosa pine is most common, dominate the landscape. The basin ranges from semi-desert to alpine climates, providing habitat for hundreds of species of plants. In the lowermost part of the watershed, in southeastern Washington, the Snake River is surrounded by an area called the Columbia Plateau Ecoprovince, which is now mostly occupied by irrigated farms. The rest of the Plateau area is characterized by low hills, dry lakes, and an arid, nearly desert climate.[99]

text: The headwaters of the Snake River and the high mountains elsewhere in the watershed were historically heavily forested. These include aspen, Douglas fir, and spruce fir, comprising about 20% of the historic watershed. At the base of mountains and in the Lost River basin, sagebrush was and is the predominant vegetation cover. Because of deforestation, up to one quarter of the forests have been taken over by sagebrush, leaving the remaining forests to cover about 15% of the watershed. However, the lodgepole pine has increased in number, taking over historic stands of other conifers. There are also up to 118 species of rare or endemic plants that occur in the Snake River watershed.[11]

text: Salmon and other anadromous fish[edit]

text:
The Snake River was once one of the most important rivers for the spawning of anadromous fish—which are hatched in the headwaters of rivers, live in the ocean for most of their lives, and return to the river to spawn—in the United States.[100][101]
The river supported species including chinook salmon, coho salmon, and sockeye salmon, as well as steelhead, white sturgeon, and Pacific lamprey. It is known that before the construction of dams on the river, there were three major chinook salmon runs in the Snake River; in the spring, summer and fall, totaling about 120,000 fish, and the sockeye salmon run was about 150,000. The historical barrier to fish migration on the Snake River was Shoshone Falls, a waterfall that occurs as the Snake River passes through the Snake River Plain.[100]

text: Since the early 20th century, when Swan Falls Dam was constructed on the middle Snake River upstream of Hells Canyon, the fifteen dams and reservoirs on the river have posed an increasing problem for migrating salmon. Agricultural lands and their resulting runoff have also had a significant impact on the success rate of migrating fish. Salmon can travel up the Snake River as far as Hells Canyon Dam, using the fish passage facilities of the four lower Snake River dams, leaving the Clearwater, Grande Ronde and Salmon river to sustain spawning salmon. Rising in several forks in the Clearwater Mountains of central Idaho, the Clearwater and Salmon River watersheds are nearly undeveloped with the enormous exception of Dworshak Dam on the North Fork Clearwater River. The watershed of the Grande Ronde in northeastern Oregon is also largely undeveloped. The four reservoirs formed by the lower Snake River dams—Lake Sacagawea, Lake Herbert G. West, Lake Bryan, and Lower Granite Lake—have also formed problems, as the downstream current in the pools is often not enough for the fish to sense, confusing their migration routes.[17][102]

text: At the confluence of the Snake and Clearwater Rivers, young salmon that swim down from spawning gravels in the headwaters of the Clearwater River often delay their migrations because of a significant temperature difference. (Prior to the removal of Lewiston Dam on the main Clearwater and Grangeville Dam on the South Fork Clearwater, the Clearwater was completely unusable by migrating salmon.[103]) Agricultural runoff and water held in reservoirs higher upstream on the Snake warm its waters as it flows through the Snake River Plain, so as the Snake meets the Clearwater, its average temperature is much higher. Directly below the confluence, the river flows into Lower Granite Lake, formed by Lower Granite Dam, the uppermost dam of the Lower Snake River Project. Paradoxically, the combination of these factors gives the young salmon further time to grow and to feed in Lower Granite Lake, so when they begin the migration to the Pacific Ocean, they often have a higher chance at survival, compared to those salmon who migrate to the ocean earlier.[102]

text: Lower Snake River dam removal[edit]

text: A controversy has erupted since the late 20th century over the four lower Snake River dams, with the primary argument being that removing the dams would allow anadromous fish to reach the lower Snake River tributaries—the Clearwater River, the Tucannon River and the Grande Ronde River—and spawn in much higher numbers. However, removal of the dams has been fiercely opposed by some groups in the Pacific Northwest.[104] Because much of the electricity in the Northwest comes from dams, removing the four dams would create a hole in the energy grid that would not be immediately replaceable.[105] Navigation on the lower Snake would also suffer, as submerged riffles, rapids and islands would be exposed by the removal of the dams. Irrigation pumps for fields in southeastern Washington would also have to reach further to access the water of the Snake River. However, aside from restoring salmon runs, dam removal proponents argue that the power is replaceable, that the grain transportation system could be replaced by railroads, and that only one of the four reservoirs supplies irrigation water. Irrigators in the Snake River Plain would likely need to allow less water into the Snake River during low flow in order to create a current in the four lower reservoirs, and recreation and tourism would likely benefit.[106]

text: Tributaries[edit]

text: The Salmon River is the second largest tributary.  Although the Salmon has a larger drainage than the Clearwater, the Salmon drains much drier country and therefore has a smaller discharger than the Clearwater, about 8,000,000 acre feet (9.9 km3) annually compared to about 11,000,000 acre feet (14 km3) annually for the Clearwater River.

text: The Snake River has over 20 major tributaries, most of which are in the mountainous regions of the basin. The largest by far is the Clearwater River, which drains 9,000 square miles (23,000 km2) in north central Idaho.  Many of the rivers that flow into the Snake River Plain from the north sink into the Snake River Aquifer, but still contribute their water to the river. Aside from rivers, the Snake is fed by many significant springs, many of which arise from the aquifer on the west side of the plain.[11]

text:
Name

Length

Watershed size

Bank

Source to Wyoming-Idaho Border

Heart River

8 1⁄2 mi (14 km)

Right

Lewis River

12 mi (19 km)

Right

Gros Ventre River

642 sq mi (1,660 km2)

Left

Hoback River

55 mi (89 km)

600 sq mi (1,600 km2)

Left

Greys River

65 mi (105 km)

800 sq mi (2,100 km2)

Left

Salt River

70 mi (113 km)

890 sq mi (2,300 km2)

Left

Snake River Plain to Hells Canyon

Henrys Fork (Snake River)

110 mi (177 km)

3,212 sq mi (8,320 km2)

Right

Portneuf River

96 mi (154 km)

1,329 sq mi (3,440 km2)

Left

Raft River

1,506 sq mi (3,900 km2)

Left

Malad River

11 1⁄2 mi (19 km)

3,000 sq mi (7,800 km2)

Right

Salmon Falls Creek

218 mi (351 km)

2,082 sq mi (5,390 km2)

Left

Bruneau River

3,305 sq mi (8,560 km2)

Left

Boise River

75 mi (121 km)

4,100 sq mi (11,000 km2)

Right

Owyhee River

280 mi (451 km)

11,049 sq mi (28,620 km2)

Left

Malheur River

165 mi (266 km)

4,700 sq mi (12,000 km2)

Right

Payette River

62 mi (100 km)

3,240 sq mi (8,400 km2)

Right

Hells Canyon

Weiser River

90 mi (145 km)

1,660 sq mi (4,300 km2)

Right

Burnt River

50 mi (80 km)

Left

Salmon River

425 mi (684 km)

14,000 sq mi (36,000 km2)

Right

Grande Ronde River

212 mi (341 km)

4,000 sq mi (10,000 km2)

Left

Clearwater River

80 mi (129 km)

9,645 sq mi (24,980 km2)

Right

Idaho-Washington border to mouth

Tucannon River

70 mi (113 km)

503 sq mi (1,300 km2)

Left

Palouse River

140 mi (225 km)

3,303 sq mi (8,550 km2)

Right