Question: Both the Emory River and Clinch River flow to what city?

Context articles: Clinch River
Grand Coulee Dam
Kingston Fossil Plant coal fly ash slurry spill
Yarm
North Fork Clinch River
Little Emory River
Guest River
Emory River
Cruces River
Longhunter

The Clinch River rises near Tazewell, Virginia, and flows southwest for more than 300 mi through the Great Appalachian Valley, gathering various tributaries, including the Powell River, before joining the Tennessee River in Kingston, Tennessee.
Grand Coulee Dam is a concrete gravity dam on the Columbia River in the U.S. state of Washington, built to produce hydroelectric power and provide irrigation water.
 Constructed between 1933 and 1942, Grand Coulee originally had only two powerhouses.
 The third powerhouse, completed in 1974 to increase energy production, makes Grand Coulee the largest power station in the United States by nameplate-capacity at 6,809 MW.
 However, in terms of yearly power production, Grand Coulee places fifth after a number of nuclear facilities to the south, like Palo Verde west of Phoenix.
 This is because river flow varies throughout the year.
 For example, while the dam may generate at nameplate-capacity in the spring, decreased river flow in the fall means less power can be generated the rest of the year, resulting in a lower capacity factor.
The TVA Kingston Fossil Plant coal fly ash slurry spill occurred just before 1 a.m. on Monday December 22, 2008, when an ash dike ruptured at an 84 acre solid waste containment area at the Tennessee Valley Authority's Kingston Fossil Plant in Roane County, Tennessee.
 1.1 e9USgal of coal fly ash slurry was released.
 The coal-fired power plant, located across the Clinch River from the city of Kingston, uses ponds to dewater the fly ash, a byproduct of coal combustion, which is then stored in wet form in dredge cells.
 The slurry (a mixture of fly ash and water) traveled across the Emory River and its Swan Pond embayment, on to the opposite shore, covering up to 300 acre of the surrounding land, damaging homes and flowing up and down stream in nearby waterways such as the Emory River and Clinch River (tributaries of the Tennessee River).
 It was the largest fly ash release in United States history.
Yarm is a small town in Stockton-on-Tees, England.
 The town is on the south bank of the River Tees and is historically part of the North Riding of Yorkshire.
 The bridge at Yarm marked the furthest reach of tidal flow up the River Tees until the opening, in 1995, of the Tees Barrage, which now regulates river flow above Stockton.
 As the last bridge on the river before the sea, it was superseded by a new toll bridge opened in Stockton in 1771.
 The oldest part of the town, around the High Street, is situated in a loop of the river, and the newer parts of the town extend to the point where the River Leven meets the River Tees.
The North Fork Clinch River is a river in the U.S. states of Virginia and Tennessee.
 It rises along the slopes of Wallen Ridge in Lee County, Virginia, and empties into the Clinch River at Hancock County, Tennessee, just across the Tennessee/Virginia state line.
The Little Emory River rises in Morgan County, Tennessee near the town of Coalfield.
 It is one of the major tributaries to the Emory River.
 It crosses into Roane County, where it soon becomes an embayment of Watts Bar Lake several miles upstream of its mouth into the Emory.
 (Watts Bar Lake is a relatively deep reservoir and causes "slack water" conditions many miles up several Tennessee River tributaries, not just the main stream.)
The Guest River is a short tributary of the Clinch River in southwestern Virginia in the United States.
 It is part of the watershed of the Mississippi River by way of the Clinch, Tennessee and Ohio Rivers.
 According to the Geographic Names Information System, the river has also been known historically as the Guests River.
The Emory River is a river draining a portion of Tennessee's Cumberland Plateau.
 It flows for just over 46 mi from its source near Frozen Head State Park to its mouth along the Clinch River at Kingston, Tennessee.
The Cruces River (Spanish: "Río Cruces" ) is a river near Valdivia, Chile.
 Río Cruces originates from hills near the Villarica volcano and flows then in south-west direction.
 The southern and final part of the river follows the Valdivian Coastal Range.
 At the latitude of Valdivia it is crossed by Río Cruces Bridge near its outflow into Valdivia River.
 The small village of Punucapa is the main centre for tourism in Río Cruces.
 The river flow through (or near) the cities of Loncoche, Lanco, and Mariquina.
 Some of the wetlands in the river's lower flow are inside Carlos Anwandter Nature Sanctuary, a protected area that in the river that extends roughly from Punucapa in the south to San Luis de Alba Fort in the north.
A longhunter (or long hunter) was an 18th-century explorer and hunter who made expeditions into the American frontier wilderness for as much as six months at a time.
 Historian Emory Hamilton asserts that "The Long Hunter was peculiar to Southwest Virginia only, and nowhere else on any frontier did such hunts ever originate" although the term has been used loosely to describe any unofficial American explorer of the period.
 Most long hunts started in the Holston River Valley near Chilhowie, Virginia.
 The hunters came from there and the adjacent valley of the Clinch River, where they were land owners or residents.
 The parties of two or three men (and rarely more) usually started their hunts in October and ended toward the end of March or early in April.