paragraph_text: The restricted flow of waters from cataclysmic floods from Glacial Lake Missoula, and pluvial Lake Bonneville through the constriction of the Wallula Gap in the Horse Heaven Hills flowed into south-central Washington and north-central Oregon, and were backed up by the Columbia River Gorge, forming Lake Condon. The water remained for a period of 5–7 days before the flood waters drained through the Columbia River Gorge. Lake Condon reached an elevation of about 1200 feet above sea level (today's sea level) before subsiding.

paragraph_text: The Colorado River Compact is a 1922 agreement among seven U.S. states in the basin of the Colorado River in the American Southwest governing the allocation of the water rights to the river's water among the parties of the interstate compact. The agreement was signed at a meeting at Bishop's Lodge, near Santa Fe, New Mexico, by representatives of the seven states the Colorado river and its tributaries pass through on the way to Mexico.

paragraph_text: The W. A. C. Bennett Dam is a large hydroelectric dam on the Peace River in northern British Columbia, Canada. At high, it is one of the world's highest earth fill dams. Construction of the dam began in 1961 and culminated in 1968. At the dam, the Finlay, the Parsnip and the Peace Rivers feed into Williston Lake, also referred to as Williston Reservoir. It is the third largest artificial lake in North America (after the Smallwood Reservoir and Manicouagan) as well as the largest body of fresh water in British Columbia. Williston Lake runs 250 kilometres north-south and 150 kilometres east-west.

paragraph_text: Singapore's water needs are anticipated to double in the next 50 years. Planned Newater output will triple to meet 50% of needs by year 2060 whilst desalination investment will raise output to meet 30% of needs. By the expiry of the 1962 water agreement in 2061, the necessity for Malaysia water import should be eliminated.

paragraph_text: Forward Harbour was a cannery town in the Johnstone Strait region of the Central Coast of British Columbia, Canada, located on the inlet of the same name, which is on the mainland side of Wellbore Channel, to the east of Hardwicke Island. Nearby on the same vicinity on the Mainland, though fronting on other bodies of water, are Jackson Bay to the immediate north, off Sunderland Channel, and Heydon Bay, British Columbia to the east on Loughborough Inlet.

paragraph_text: Richmond is located at 37°32′N 77°28′W﻿ / ﻿37.533°N 77.467°W﻿ / 37.533; -77.467 (37.538, −77.462). According to the United States Census Bureau, the city has a total area of 62 square miles (160 km2), of which 60 square miles (160 km2) is land and 2.7 square miles (7.0 km2) of it (4.3%) is water. The city is located in the Piedmont region of Virginia, at the highest navigable point of the James River. The Piedmont region is characterized by relatively low, rolling hills, and lies between the low, sea level Tidewater region and the Blue Ridge Mountains. Significant bodies of water in the region include the James River, the Appomattox River, and the Chickahominy River.

paragraph_text: Saw Kill may refer to three different bodies of water in New York. Two are tributaries and make up watersheds on the eastern bank of the Hudson River. The northernmost of these is in the Town of Stuyvesant, New York in Columbia County and the southernmost of these is in the Town of Red Hook, New York in Dutchess County. The northern Saw Kill is more commonly known as Mill Creek today. The third tributary drains into Esopus Creek on the Hudson’s west bank. This article refers to the southern body of water on the east bank as Saw Kill (east) and the body of water on the west bank as Saw Kill (west).

paragraph_text: The Bulkley Ranges is mountain range in northern British Columbia, Canada, located between the Skeena and Bulkley Rivers south of Hazelton, north of the Morice River and Zymoetz River. It has an area of 7851 km and is a subrange of the Hazelton Mountains which in turn form part of the Interior Mountains.

paragraph_text: Banderas River () is a river located in the southern part of the Ahuachapán Department of El Salvador. Precipitations along the river are suitable for municipal water, irrigation, and water wells.

paragraph_text: The Muskwa Ranges are a group of mountain ranges in northern British Columbia, Canada. They are part of the Northern Rockies section of the Rocky Mountains and are bounded on their west by the Rocky Mountain Trench and on their east by the Rocky Mountain Foothills. They are delimited on the north by the Liard River and on the south by the Peace Reach of the Lake Williston reservoir (formerly the Peace River), south of which the next major grouping of the Rockies is the Hart Ranges.

paragraph_text: The Salloomt River is a river in the Bella Coola Valley of the Central Coast region of British Columbia, Canada. It is a tributary of the Bella Coola River, flowing southwest out of the southernmost Kitimat Ranges to meet that river just upstream from the community of Hagensborg.

paragraph_text: Teafuone is an islet of Nukufetau, Tuvalu. Teafuone has also been known as Entrance Island as it is by the channel through the reef of Nukufetau.

paragraph_text: Tokinivae is an islet of Nui atoll, in the Pacific Ocean state of Tuvalu.< Nui tradition is that Kolaka, a warrior from Nukufetau came on several raiding expeditions to Tokinivae, until he was killed and buried at Tararorae.

paragraph_text: Murray Mouth is the point at which the River Murray meets the Southern Ocean. The Murray Mouth's location is changeable. Historical records show that the channel out to sea moves along the sand dunes over time. At times of greater river flow and rough seas, the two bodies of water would erode the sand dunes to create a new channel leaving the old one to silt and disappear.

paragraph_text: The Big Bend Ranges are a subrange of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located in Big Bend of the Columbia River north of the Illecillewaet River.

paragraph_text: The Columbia Bar, also frequently called the Columbia River Bar, is a system of bars and shoals at the mouth of the Columbia River spanning the U.S. states of Oregon and Washington. The bar is about 3 miles (5 km) wide and 6 miles (10 km) long.

paragraph_text: The Rainy River is a river in Presque Isle County, Michigan, in the United States. It is located in the northern part of the Lower Peninsula of Michigan, flowing northwest from Rainy Lake to Black Lake. Its waters, after passing through Black Lake, flow via the Black River and the Cheboygan River to Lake Huron.

paragraph_text: Germantown is a town in Columbia County, New York, United States. The population was 1,954 at the 2010 census. Germantown is located in the southwest part of the county, along the east side of the Hudson River.

paragraph_text: The Red River is a tributary of the Kechika River in the far north of British Columbia, Canada, flowing east to meet the Kechika from headwaters in the Cassiar Mountains. In its middle reaches it forms the boundary between the Dease Plateau (N) and the Cassiar Mountains (S) and for its final stretch it crosses part of the Liard Plain. It is crossed by an unnamed road about upstream from its confluence with the Kechika, and is just to the north of Aeroplane Lake.

paragraph_text: Lake Oesa is a body of water located at an elevation of 2,267m (7438 ft) in the mountains of Yoho National Park, near Field, British Columbia, Canada.

Question: Where does the Columbia River meet the ocean where Teafuone is a located in?
Answer: Columbia Bar