Basset Brook (New York)
Basset Brook flows into the West Branch Delaware River by Stamford, New York.
North Fork Cache la Poudre River
The North Fork Cache la Poudre River( locally called the North Fork) is a tributary of the Cache la Poudre River, approximately long, in north central Colorado in the United States.
It drains a mountainous area of north central Larimer County northwest of Fort Collins on the western side of the Laramie Foothills.
It rises in remote northwestern Larimer County in the foothills of the Roosevelt National Forest east of the Medicine Bow Range.
It flows generally east, passing south of Virginia Dale, where it is impounded by the Halligan Reservoir.
It turns roughly south, flowing past Livermore and joining the main branch of the Poudre from the north near the mouth of the Poudre Canyon between Poudre Park and Teds Place.
The valley of the North Fork was historically used a trail route between the Colorado Piedmont and the Laramie Plains, including the Cherokee Trail and the Overland Trail.
The valley of the North Fork later became the route of the Union Pacific Railroad, and later of U.S. Highway 287 between Fort Collins and Laramie, Wyoming.
Communities in the valley of the North Fork include Livermore.
Koyukuk River
The Koyukuk River''( Ooghekuhno in Koyukon, Kuuyukaq in Inupiaq) is a tributary of the Yukon River, in the U.S. state of Alaska.
It is the last major tributary entering the Yukon before the larger river empties into the Bering Sea.
Rising at the confluence of the North Fork Koyukuk River with the Middle Fork Koyukuk River, it flows generally southwest to meet the larger Yukon River at Koyukuk.
The river, with headwaters above the Arctic Circle in the Endicott Mountains of the Brooks Range, drains an area north of the Yukon River that includes part of the Gates of the Arctic National Park and Preserve, as well as Kanuti National Wildlife Refuge and Koyukuk National Wildlife Refuge.
The main stem of the river is lined by the communities of Evansville, Bettles, Alatna, Allakaket, Hughes, and Huslia before reaching Koyukuk.
Its headwaters tributaries include the Koyukuk's south, middle, and north forks, the Alatna River, and the John River.
Major tributaries further downstream include the Kanuti, Batzu, Hogatza, Huslia, Dulbi, Kateel, and Gisasa rivers.
Of these, the Alatna, John, and North Fork are National Wild and Scenic Rivers, as is the Tinayguk River, a tributary of the North Fork.
North Fork Koyukuk River
The North Fork of the Koyukuk River is one of the principal forks of the Koyukuk River, approximately 105 mi( 160 km) long, in northern Alaska in the United States.
It has a watershed area of.
It rises on the south slopes of the Continental Divide in the Brooks Range.
It is located in the Gates of the Arctic National Park and Preserve and is part of the Koyukuk Wild and Scenic River as designated by the United States Congress in 1980.
The major tributaries include the Glacier River, Tinayguk River, Clear River and joins the Middle Fork Koyukuk River to form the Koyukuk main stem.
Robert Marshall thoroughly explored the system in 1929, naming many of the major peaks such as Mount Doonerak, Frigid Crags, Boreal Mountain and the Gates of the Arctic pass.
Basset Brook
Basset Brook is a stream formed at a shallow pond located approximately 1.4 miles northwest of Warrenville, Connecticut, United States.
The brook flows south and east from this pond and eventually to its mouth at the Mount Hope River, with a length of approximately 1.4 miles.
Hey Brook
Hey Brook is a watercourse in Rochdale, Greater Manchester and a tributary of the River Roch.
It originates at the confluence of Buckley Brook and Syke Brook, and flows through Wardleworth to the River Roch.
North Fork Toutle River
The North Fork Toutle River is a tributary of the Toutle River in southwestern Washington in the United States.
The river has its headwaters near Spirit Lake, on the north side of Mount St. Helens, and flows to the Toutle River, about upstream of its confluence with the Cowlitz River.
The largest tributary is the Green River, which joins near the unincorporated town of Toutle.
The North Fork's watershed was severely affected by the 1980 eruption of Mount St. Helens, which coated the valley with ash and filled it with successive mudflows.
The result of the eruption was that many hillsides were stripped of forest, and as a result erosion has increased dramatically and the North Fork is now extremely laden with sediment.
Previously, Spirit Lake was the source of the river, but eruptions blocked the outlet and Spirit Lake no longer drains directly into the North Fork; instead, a tunnel was excavated in 1985 to connect the lake with South Coldwater Creek, a tributary of the North Fork.
Once a mature river, the North Fork has transformed into a braided stream of relatively young origin, and its valley floor is less than three decades old.
The Toutle River Sediment Retention Structure was built by the U.S. Army Corps of Engineers on the river in 1989 to prevent this sediment from traveling downstream and clogging the shipping channel of the Columbia River.
The upper part of the North Fork Toutle River watershed was redirected to the crater of Mount St. Helens itself until 1982.
The river's headstreams begin on a volcanic ash deposit roughly long and deep, which is the source of much of the excess sediment.
Moclips River
The Moclips River is a river in the U.S. state of Washington.
It is about long.
Its main tributary, the North Fork Moclips River, is longer than the main stem.
The length of the North Fork, along with the lower main stem below the North Fork's confluence, is .
The drainage basin of the Moclips River is in area.
Tinayguk River
The Tinayguk River is a tributary of the North Fork Koyukuk River in the U.S. state of Alaska.
Heading in the Endicott Mountains of the Brooks Range, the river flows generally west then south to meet the larger river about north of Bettles.
In 1980, the entire river was designated" wild" and added to the National Wild and Scenic Rivers System.
The designation means that the Tinayguk is unpolluted, free- flowing and generally inaccessible except by trail and that its watershed is essentially primitive.
The river's name means" Moose" in Inupiat.
In 1930, forester Robert" Bob" Marshall recommended it as an alternative to" West Fork", a local name that Marshall considered over-used.
Middle Fork Koyukuk River
The Middle Fork Koyukuk River is a tributary of the Koyukuk River in the U.S. state of Alaska.
Formed by the confluence of the Bettles and Dietrich rivers near Wiseman on the southern flank of the Brooks Range, the Middle Fork flows generally southwest to its confluence with the North Fork Koyukuk River, with which it forms the main stem of the Koyukuk.
From its starting point slightly north of Sukakpak Mountain, the river flows generally south or southwest in its upper reaches.
The Dalton Highway and the TransAlaska Pipeline run roughly parallel to the river between its source and a point between Twelvemile Mountain, on the river's right, and Cathedral Mountain, on the left, south of Coldfoot.
Further south, at Tramway Bar, the river turns generally west to its confluence with the North Fork Koyukuk River.

Question: Are Basset Brook and North Fork Koyukuk River both located in the same country?
Answer: yes