Downstream from the Araguaia confluence, in the state of Pará, the river used to have many cataracts and rapids, but they were flooded in the early 1980s by the artificial lake created by the Tucuruí dam, one of the world's largest.

Downstream some forty kilometers north of Hanover, near Schwarmstedt, the river joins the Aller and reaches the North Sea via the Weser.

Downstream of the East-Link bridge, the river is still mainly used for commercial and ferry traffic, with some recreational use also.

Downstream from Viet Tri, the river and its many distributaries spread out to form the Red River Delta.

Downstream of its confluence with the Namekagon, the Ojibwa renamed the river as Gichi-ziibi ( Big River ) or Okijii-ziibi ( Pipestem River )

Downstream from there, the river broadens into an estuary before flowing into the Atlantic Ocean.

Downstream from the forks, the river flows through a wooded area known as Crothers ' Woods which is designated as an Environmentally Sensitive Area due to the high quality beech-maple forest that grows on the ravine slopes.

Downstream from the dam the river flows north through Saskatoon and joins the North Saskatchewan River east of Prince Albert at the Saskatchewan River Forks — thus forming the Saskatchewan River.

Downstream on the River Tees is Portrack Marsh Nature Reserve, a nature reserve by the northern bank of the river between the Tees Barrage and the Tees Viaduct near Portrack housing estate.

Downstream, the river descends hundreds of meters in a series of rapids known as the Livingstone Falls to reach sea level at the port of Boma after a trajectory of 300 km.

Downstream is Cornwall's largest natural lake Loe Pool, formed when a shingle bar blocked the mouth of the river by rising sea levels forming a barrier beach.

Downstream of Indian Falls, Tonawanda Creek flows through the Tonawanda Indian Reservation, and there is an NYS historical marker where George Washington made a troop fording across the river.

Downstream of Asheville, the river proceeds north through Madison County, where it flows through its county seat of Marshall.

Downstream from the reservoir dam it flows south, through Lake Hiawatha, where the river splits and joins again.

Downstream of Rickety-Rack, a high bluff can be seen on the right where Mud Creek enters on river right.

Downstream from the Truman Dam, the river becomes the serpentine Lake of the Ozarks, stretching eastward for nearly to Bagnell Dam in Camden County and southwestern Miller County.

Downstream from the dam the river flows east past Fallon, then northeast into the Carson Sink.

Downstream from its source, the river receives Noah Creek from the right from the river mouth.

Downstream of the rapids, the river receives Scott Creek, Slide Creek, and Hatchery Creek, all from the right, and Line Creek from the left before reaching the unincorporated community of Tidewater, about from the mouth.

Downstream Korumbyn Creek and then at Byangum the larger Oxley River enters the river, before it flows through Murwillumbah.

Downstream of Ironwood the river passes over Saxon Falls and Superior Falls and enters Oronto Bay on the southwestern shore of Lake Superior, approximately northwest of Ironwood, at Michigan's westernmost point.

Downstream of the refuge, the river flows roughly parallel to U. S. Route 97, receiving Spring Creek from the right at Collier Memorial State Park, about north of Chiloquin.

Downstream from its headwaters, it splits into two ; one-third of its flow passes through the Brazo Casiquiare ( Casiquiare Channel ) into a tributary of the Amazon, and the remainder passes into the main Orinoco channel.

Downstream from its confluence with the South Fork, the river flows generally west, and adds the major tributary of Mores Creek along Highway 21, and passes through Lucky Peak Dam to emerge from the foothills southeast of Boise.

Downstream from Zanyukhcha, the Pinega passes historical selos of Sura and Verkola, accepts the Yula from the west, and passes the selo of Kevrola, which was the historical center of the area before 19th century, on the left bank, and the selo of Karpogory, which is the current administrative center of the Pinezhsky District, on the right bank.

Downstream from the confluence of its branches it flows south past Selinsgrove, where it is joined by its Penns Creek tributary, and cuts through a water gap at the western end of Mahantongo Mountain.

Downstream of the dam, the Mojave River flows north and east, underground in most places, through Hesperia, Victorville, and Barstow.

Downstream from Ennis, the Madison flows through Bear Trap Canyon, known for its class IV-V whitewater.

Downstream of the outlet, the water runs through surface canals called jubs ( jūbs ) which run downhill, with lateral branches to carry water to the neighborhood, gardens and fields.

Downstream from the dam, the Osage flows freely to the northeast in broad oxbow meanders through forested bluffs, joining the Missouri approximately east and downstream of Jefferson City.

Downstream from its confluence with the Chitina it flows southwest, passing through a narrow glacier-lined gap in the Chugach Mountains east of Cordova Peak.

Downstream from the reservoir it flows west past Sweet Home, where it turns northwest, passing through the foothills into the Willamette Valley near Lebanon.

Downstream of the connection with the Semayang and Melintang lakes, the Mahakam meets three other main tributaries-the rivers Belayan, Kedang Kepala, and Kedang Rantau-and flows south-eastwards through the Mahakam delta distributaries, to the Makassar Strait.

Downstream of Mundubbera, the river swings east, going through the townships of Gayndah and Wallaville before entering the city of Bundaberg.

Downstream it flows through Bob Creek Wildland Park and Black Creek Heritage Rangeland.

Downstream of Marshall the Redwood flows through a flat till plain and turns eastward into Redwood County, passing Vesta and Seaforth ; sections of the river in this stretch have been straightened to form agricultural ditches.

Downstream from Grant it is followed by U. S. Highway 285 until Bailey, where it cuts through a remote section of the foothills.

Downstream of Mosby, it collects the East Fork Fishing River, which rises at the town of Lawson and flows generally southward through Ray and Clay counties, past the town of Excelsior Springs.

Downstream of Success Dam, the river flows west through Porterville.

Downstream of village Preobrazhenskoye the Lower Tunguska flows in the narrow and deep valley with high, often rocky shores.

Downstream of the community of Millboro Springs the river becomes deep enough for year round boating ; there are several boat launch sites along the river in Bath County.