Find link

language: af: Afrikaans als: Alemannisch [Alemannic] am: አማርኛ [Amharic] an: aragonés [Aragonese] ar: العربية [Arabic] arz: مصرى [Egyptian Arabic] as: অসমীয়া [Assamese] ast: asturianu [Asturian] az: azərbaycanca [Azerbaijani] azb: تۆرکجه [Southern Azerbaijani] ba: башҡортса [Bashkir] bar: Boarisch [Bavarian] bat-smg: žemaitėška [Samogitian] be: беларуская [Belarusian] be-tarask: беларуская (тарашкевіца) [Belarusian (Taraškievica)] bg: български [Bulgarian] bn: বাংলা [Bengali] bpy: বিষ্ণুপ্রিয়া মণিপুরী [Bishnupriya Manipuri] br: brezhoneg [Breton] bs: bosanski [Bosnian] bug: ᨅᨔ ᨕᨘᨁᨗ [Buginese] ca: català [Catalan] ce: нохчийн [Chechen] ceb: Cebuano ckb: کوردیی ناوەندی [Kurdish (Sorani)] cs: čeština [Czech] cv: Чӑвашла [Chuvash] cy: Cymraeg [Welsh] da: dansk [Danish] de: Deutsch [German] el: Ελληνικά [Greek] en: English eo: Esperanto es: español [Spanish] et: eesti [Estonian] eu: euskara [Basque] fa: فارسی [Persian] fi: suomi [Finnish] fo: føroyskt [Faroese] fr: français [French] fy: Frysk [West Frisian] ga: Gaeilge [Irish] gd: Gàidhlig [Scottish Gaelic] gl: galego [Galician] gu: ગુજરાતી [Gujarati] he: עברית [Hebrew] hi: हिन्दी [Hindi] hr: hrvatski [Croatian] hsb: hornjoserbsce [Upper Sorbian] ht: Kreyòl ayisyen [Haitian] hu: magyar [Hungarian] hy: Հայերեն [Armenian] ia: interlingua [Interlingua] id: Bahasa Indonesia [Indonesian] io: Ido is: íslenska [Icelandic] it: italiano [Italian] ja: 日本語 [Japanese] jv: Basa Jawa [Javanese] ka: ქართული [Georgian] kk: қазақша [Kazakh] kn: ಕನ್ನಡ [Kannada] ko: 한국어 [Korean] ku: Kurdî [Kurdish (Kurmanji)] ky: Кыргызча [Kirghiz] la: Latina [Latin] lb: Lëtzebuergesch [Luxembourgish] li: Limburgs [Limburgish] lmo: lumbaart [Lombard] lt: lietuvių [Lithuanian] lv: latviešu [Latvian] map-bms: Basa Banyumasan [Banyumasan] mg: Malagasy min: Baso Minangkabau [Minangkabau] mk: македонски [Macedonian] ml: മലയാളം [Malayalam] mn: монгол [Mongolian] mr: मराठी [Marathi] mrj: кырык мары [Hill Mari] ms: Bahasa Melayu [Malay] my: မြန်မာဘာသာ [Burmese] mzn: مازِرونی [Mazandarani] nah: Nāhuatl [Nahuatl] nap: Napulitano [Neapolitan] nds: Plattdüütsch [Low Saxon] ne: नेपाली [Nepali] new: नेपाल भाषा [Newar] nl: Nederlands [Dutch] nn: norsk nynorsk [Norwegian (Nynorsk)] no: norsk bokmål [Norwegian (Bokmål)] oc: occitan [Occitan] or: ଓଡ଼ିଆ [Oriya] os: Ирон [Ossetian] pa: ਪੰਜਾਬੀ [Eastern Punjabi] pl: polski [Polish] pms: Piemontèis [Piedmontese] pnb: پنجابی [Western Punjabi] pt: português [Portuguese] qu: Runa Simi [Quechua] ro: română [Romanian] ru: русский [Russian] sa: संस्कृतम् [Sanskrit] sah: саха тыла [Sakha] scn: sicilianu [Sicilian] sco: Scots sh: srpskohrvatski / српскохрватски [Serbo-Croatian] si: සිංහල [Sinhalese] simple: Simple English sk: slovenčina [Slovak] sl: slovenščina [Slovenian] sq: shqip [Albanian] sr: српски / srpski [Serbian] su: Basa Sunda [Sundanese] sv: svenska [Swedish] sw: Kiswahili [Swahili] ta: தமிழ் [Tamil] te: తెలుగు [Telugu] tg: тоҷикӣ [Tajik] th: ไทย [Thai] tl: Tagalog tr: Türkçe [Turkish] tt: татарча/tatarça [Tatar] uk: українська [Ukrainian] ur: اردو [Urdu] uz: oʻzbekcha/ўзбекча [Uzbek] vec: vèneto [Venetian] vi: Tiếng Việt [Vietnamese] vo: Volapük wa: walon [Walloon] war: Winaray [Waray] yi: ייִדיש [Yiddish] yo: Yorùbá [Yoruba] zh: 中文 [Chinese] zh-min-nan: Bân-lâm-gú [Min Nan] zh-yue: 粵語 [Cantonese]

jump to random article

Longer titles found: The River Flows Eastwards (view), Where the River Flows (view)

searching for The River Flows 548 found (4150 total)

alternate case: the River Flows

De Lank River (341 words) [view diff] case mismatch in snippet view article find links to article

Camel. The De Lank's course is within the civil parish of St Breward. The river flows through an isolated area with few riverside settlements. Its upper

elevation of 1,341 m (4,400 ft) in the Kodagu district of Karnataka. The river flows for about 320 km (200 mi) through the Deccan plateau in Karnataka before

number of tributary streams it is impounded by the dam at Lamaload. The river flows on to and passes through the village of Rainow, the town of Bollington

south of Bread Loaf Mountain near the crest of the Green Mountains. The river flows east to the town of Granville, where it receives the outflow from the

received a majority of its water from karst springs along its course. The river flows through one of the richest gold-producing areas in the world, which

boundary of the town of Stratton near the crest of the Green Mountains. The river flows north, forming the eastern boundary of the Lye Brook Wilderness of

prominent rocky knob at the southeast margin of the White Mountains. The river flows south into lowlands at the base of the mountain and arrives at Chocorua

The river flows southeast through wetlands and past low hills, passing through Colcord Pond just west of the downtown part of Exeter. The river flows

to be laden with sediment; in the dry season, the river flows with relatively clear water. The river flows through important farming areas, and its basin

source)) at an elevation of 1,700 feet (520 m) in Sandy River Plantation. The river flows south to a confluence with Chandler Mill Stream in Maine Township E

length of 73 km (45 mi), including the Sihlsee reservoir, through which the river flows. Water is abstracted from the river at the Sihlsee, leading to decreased

Tablelands and Mid North Coast districts of New South Wales, Australia. The river flows through the small locality of Cooplacurripa, after which it is named

the east side of Mount Cabot, the highest peak in the Pilot Range. The river flows east into Berlin, passing the Berlin National Fish Hatchery at York

tributary of the Connecticut River, which flows to Long Island Sound. The river flows parallel to and approximately 5 miles (8 km) south of the Sugar River

on the southern slopes of 3,654-foot-high (1,114 m) Rump Mountain. The river flows southeast, quickly entering the state of Maine, where it ends at Aziscohos

The Songo River is a 3.1-mile-long (5.0 km) river in Maine. The river flows from Brandy Pond at the south end of Long Lake into Sebago Lake at Sebago

and Blood Brook at the center of the town of Goshen, New Hampshire. The river flows north, reaching the Sugar River near the center of the town of Newport

Hill and north of Crown Hill, among foothills of the White Mountains. The river flows southeast across a corner of Eaton, New Hampshire, then turns northeast

tributary of the Androscoggin River in western Maine in the United States. The river flows from Androscoggin Lake, northwest through the town of Leeds 7 miles

relatively undisturbed and are privately owned. However, the lower part of the river flows through developed areas as well as past fynbos and plantations of invasive

north, collecting streamflow from the west side of the Belknap Range. The river flows through a wide valley in the center of Gilford, passing the town's

Sawyer Brook and Stocker Brook in the town of Grantham, New Hampshire. The river flows south through the town of Croydon, reaching the Sugar River in the

in Stewartstown, New Hampshire, just south of Little Diamond Pond. The river flows south through forests and fields, joining the West Branch at the village

Swift River Pond, a small water body southeast of the Rangeley Lakes. The river flows south into Oxford County through the towns of Byron, Roxbury, and Mexico

independently. The first new release on the label was the 2002 box set The River Flows, which featured their then-out-of-print first three albums (all remastered

Park near Merrinyaginya Spring and flow is a northerly direction. The river flows through Lake Poongkaliyarra and out through Lockyer Gap. The river

headwaters of the river rise between the Caroline and Gibb Ranges. The river flows in a northerly direction until merging with the Drysdale River, of

ground in the southern corners of Alton and New Durham, New Hampshire. The river flows southeast into Strafford, then, running up against the Blue Hills Range

that rises near Jerramungup at the border of the Yilgarn plateau. The river flows in a generally south-easterly direction and the river valley becomes

plateau. The river flows through Mukurthi, Pykara and Glenmorgan dams, and forms part of an important hydro-electric power project. The river flows over a

between Mudget Mountain to the north and Lovering Mountain to the south. The river flows south and is joined by the East Branch at the village of Upper Kidderville

South Branch to form the Gale River at the crossing of U.S. Route 3. The river flows entirely through the White Mountain National Forest, except for a short

begins at the outlet of Merrymeeting Lake in the town of New Durham. The river flows south through a chain of ponds to the village proper of New Durham

descends 312 metres (1,024 ft) over its 22-kilometre (14 mi) course. The river flows within the Water Supply Reserve of Greater Sydney. New South Wales

multipurpose river valley project after India's independence in 1947. The river flows through the states of Chhattisgarh and Odisha, before finally ending

before reaching its confluence with the Abercrombie River, near Hadley. The river flows adjacent to the Abercrombie River National Park, with access at The

Coastal Highway south of Karratha then discharges into the Indian Ocean. The river flows through a number of permanent and semi-permanent pools on the way to

edge of the Yilgarn plateau and flows in a south easterly direction. The river flows through the Fitzgerald River National Park winding through gorges cut

Hampshire, 300 meters upstream of the confluence of the West Branch. The river flows east, receiving the outlet of Lake Massasecum, and enters the town

rises in Pinkham Notch, on the eastern slopes of Mount Washington. The river flows northeast to the Androscoggin River in Gorham, New Hampshire, collecting

the eastern slopes of Crystal Mountain, a 7-mile-long (11 km) ridge. The river flows northeast into the Atkinson and Gilmanton Academy Grant, then joins

Pond, whose western end just touches the Canada–United States border. The river flows in a curving route to the east, entering Maine after two miles. The

begins at the outlet of Kezar Lake in the village of North Sutton. The river flows south through a broad wetland, incorporating the outflow of Gile Pond

Brook joins from the right at the first crossing of Fowler River Road. The river flows southeast to a junction with Bog Brook, where it turns north and flows

miles (47,000 km2) of southern Kentucky and north-central Tennessee. The river flows generally west from a source in the Appalachian Mountains to its confluence

The river flows generally south and then east towards the settlement of Toweran where the Bruce Highway crosses the river. From this point the river flows

Upper Beech Pond in the northern part of Wolfeboro, New Hampshire. The river flows north for one mile and enters Lower Beech Pond in the town of Tuftonboro

the southern boundary of Groton State Forest in the town of Groton. The river flows generally southeast through the towns of Ryegate and Newbury, reaching

bear its name, such as Lake Man Park (漫湖公園) and Kokuba Danchi (国場団地). The river flows into the East China Sea. The river and people living around it suffered

River flows across Jharkhand, Chhattisgarh and Odisha states in India. The river flows for 240 kilometres (150 mi) before it meets the Koel River in Odisha

New Hampshire, at the confluence of Rockwood Brook and Quarry Brook. The river flows in a zigzag manner northwest, then southwest, then north to the Ashuelot

miles (47,000 km2) of southern Kentucky and north-central Tennessee. The river flows generally west from a source in the Appalachian Mountains to its confluence

River flows across Jharkhand, Chhattisgarh and Odisha states in India. The river flows for 240 kilometres (150 mi) before it meets the Koel River in Odisha

of Little Pond Red Hill Pond, just east of the village of Sandwich. The river flows north into Red Hill Pond, then turns west to flow past the village

bear its name, such as Lake Man Park (漫湖公園) and Kokuba Danchi (国場団地). The river flows into the East China Sea. The river and people living around it suffered

confluence with the Eerste River. For a significant part of its course, the river flows through the City of Cape Town. A population of the endangered local

the heavily developed barrier beaches of Wells and Drakes Island. The river flows into Wells Harbor, then empties between a pair of jetties into the

of Crescent Lake in the northeastern corner of the town of Acworth. The river flows east into the town of Lempster, then turns south and reenters Acworth

east, Mount Guyot to the south, and South Twin Mountain to the west. The river flows north into the town of Bethlehem, through a deep valley between North

Saddleback Mountain on the border between Northwood and Deerfield. The river flows southeast through Deerfield and quickly enters Nottingham, where it

enters Little Dan Hole Pond, then exits from the pond's northern end. The river flows east, past Moultonville, reaching the Beech River just south of the

border between the towns of Canterbury and Loudon, New Hampshire. The river flows south through gently rolling terrain, soon entering Loudon and passing

descending 876 metres (2,874 ft) over its 277 kilometres (172 mi) course. The river flows through the Dunedoo and is noted for its influence on flood, particularly

(85 mi) long and has a watershed of 1,660 square kilometres (640 sq mi). The river flows from Mount Ōdaigahara to the west. It pours into Kii Channel at Wakayama

081-foot (939 m) Mount Pisgah lies just to the north of the headwaters. The river flows east into the Atkinson and Gilmanton Academy Grant, where it is joined

and Mount Monroe. Leaving the vicinity of the Presidential Range, the river flows westwardly into Grafton County, where it turns southwestwardly. Along

within the Sandwich Wilderness of the White Mountain National Forest. The river flows generally east and then southeast, leaving the national forest, passing

Ocean. The river rises in Nottingham as the outlet of Mendums Pond. The river flows south, passing through Nottingham Lake, and then east, where it joins

begins at the outlet of Tewksbury Pond in Grafton, New Hampshire. The river flows southwest and then southeast through Grafton, passing through Kilton

tourist attraction, with trails and ladders accessing many of the caves. The river flows southeast from Kinsman Notch to Jackman Brook, where the two streams

Black Mountain Ski Area, and southwest of the Baldface mountains. The river flows south through the White Mountain National Forest in an area that is

town of North Hampton, New Hampshire, just west of Interstate 95. The river flows north through gently rolling fields and scattered suburban development

towns of Freedom and Ossipee. The flat, sandy terrain through which the river flows is known as the West Branch Pine Barrens and is the site of a nature

the outlet of Lake Sunapee in the town of Sunapee, New Hampshire. The river flows west through the town of Newport and the city of Claremont. It reaches

(Liparis of the antiquity) is a rivulet in Mersin Province, Turkey The river flows in the mid-southern portion of the Toros Mountains from north to south

channels resembling braided hair. Around 57 kilometres (35 mi) of the river flows through western Belarus. The name of the river is from a Proto-Indo-European

Latin: Selemnus) is a river in the northern part of Achaea, Greece. The river flows entirely in the municipal unit of Rio and empties into the Gulf of

the Ministry of Land, Infrastructure, Transport and Tourism (MLIT). The river flows via towns: Nara Prefecture Yamatokōriyama Osaka Prefecture Kashiwara

Hasdeo River is the largest tributary of Mahanadi River. The river flows in the state of Chhattisgarh. It joins Mahanadi River near Shiladehi(Birra) a

and quickly reaches the lowlands at the base of the White Mountains. The river flows east through Sandwich, entering Tamworth at the juncture of the Cold

Lake on the southeastern outskirts of the resort area of Whistler. The river flows into Cheakamus Lake before exiting it and flowing northwest until it

east of Branga Swamp about 50 kilometres (31 mi) south of Walcha. The river flows generally north and north west for, towards its confluence with the

These meet with other minor streams and join together at Okehampton. The river flows generally north, past the villages of Jacobstowe and Monkokehampton

Omono River (雄物川, Omono-gawa) is located in Akita Prefecture, Japan. The river flows from Mount Daisen on the border of Akita Prefecture with Miyagi and

northern part of Tamworth, New Hampshire, south of Mount Chocorua. The river flows southeast through a narrow valley, which opens up as it reaches Tamworth

flow east, and join near Pura to form the Vedavathi River. From there the river flows through Kadur Taluk Of Chikkamagalur District. Then it enters Hosadurga

Creek and Willacoochee Creek which drain part of southwestern Georgia, the river flows south through Gadsden County east of Quincy, draining part of the Red

judgments by the Massachusetts Executive Office of Environmental Affairs, the river flows through the best red maple swamp in Massachusetts and provides some

most commonly associated with the river Seine in central Paris. Here, the river flows roughly westwards, cutting the city into two parts. When facing downstream

between Moretonhampstead and Postbridge, before joining at Jurston. The river flows for about two miles northwards from source before turning to a generally

Mount Washington, the highest peak in the northeastern United States. The river flows southwest through a wooded mountain valley between the southern part

Hino-gawa) is a major river in the western part of Tottori Prefecture. The river flows east-northeast for 77 kilometres (48 mi), and is the longest river

estuary in Waldoboro, then about 8 miles (13 km) south to Bremen. The river flows through Hockomock Channel into the head of Muscongus Bay. Medomak is

The river rises below Mount Burnside in the Lake Muir State forest. The river flows in a southerly direction through the Shannon National Park until it

Harbor. Its name is derived from the village of Mount Kisco, which the river flows through. The name of Mount Kisco is further derived from "seesquee"

flanks of Jade Dragon Snow Mountain in Lijiang prefecture-level city. The river flows towards the east for approximately 25 km (16 mi) before joining the

a river in Montenegro. Its source is under the mountain of Vojnik. The river flows eastwards for 65 km (40 mi) until it empties into the river Morača

Carrigain and Mount Hancock, where several large brooks converge. The river flows west and southwest through the heart of the Pemigewasset Wilderness

in 1765 for Henry Fox (1705–1774), the 1st Baron Holland of Foxley. The river flows northwest into Cascumpec Bay. Most of the early settlers to this community

is situated on the banks of the river, is named after this river. The river flows through the Neyyar wildlife sanctuary and into the Neyyar resorvoir

Mount Passaconaway to the north, and Mount Wonalancet to the east. The river flows south, paralleled by the Dicey Mill Trail, out of the mountains into

in 1765 for Henry Fox (1705–1774), the 1st Baron Holland of Foxley. The river flows northwest into Cascumpec Bay. Most of the early settlers to this community

is situated on the banks of the river, is named after this river. The river flows through the Neyyar wildlife sanctuary and into the Neyyar resorvoir

southern tip of the Western Ghats(Sahyadri Mountains) at Agastyar Koodam. The river flows 66 km westward and merges with the Arabian Sea at Panathura near Kovalam

hill known as Varaha Parvata at a place called Gangamoola. From here, the river flows through two districts in Karnataka - Chikmagalur District and Shimoga

of Tambo. Formed by the confluence of Larry Creek and Rams Gully, the river flows generally south, much of the river is braided channels, joined by 21

and a basin area of 1101 km2. Its source is 1.5 south of Barlinek. The river flows northwest through Miedwie and Płoń lake. The Płonia flows into Dąbie

the border between Mashpee and Cotuit, Massachusetts on Cape Cod. The river flows southwards from the southern end of Santuit Pond into Popponesset Bay

Singhbhum in the Indian states of Odisha and Jharkhand respectively. The river flows through industrial and iron ore mining areas and Saranda forest before

and through Regalica into Dąbie Lake in the delta of the Oder river. The river flows through the Lower Oder Valley forming, along with the Western Oder

in the Drysdale River National Park at the foot of Tadarida Scarp. The river flows easterly until discharging into the Forrest River, of which it is a

Formed by the confluence of the Packsaddle Creek and California Creek, the river flows east through the Bullings Claim mineral occurrence and several mine

north western slopes of McKinnon Peak in the Southern Alps. From there the river flows in a west direction reaching the Whataroa River 15 kilometres (9 mi)

limestone surface, creating potholes and underwater caves, into which the river flows through some of the summer, when water levels have decreased significantly

Poland along the border with Germany. It flows into the Oder Lagoon. The river flows through the Lower Oder Valley forming, along with the Eastern Oder

a river in the Hudson Plains ecozone of northern Ontario, Canada. The river flows 100 km northeast from the confluence of the Mattagami and Missinaibi

Paleogeographic Lake Agassiz laid down the Red River Valley Silts. The river flows north through a wide ancient lake plain to Lake Winnipeg. The geography

between Mount Hancock to the north and Mount Huntington to the south. The river flows east, paralleled by the Hancock Notch Trail, into a broad valley with

The river has its source to the southwest of Sussex, New Brunswick. The river flows into the Bay of Fundy near Fundy-St. Martins, and serves as the endpoint

China. It is part of the Bohai Sea basin and empties into Laizhou Bay. The river flows through the major city of Jinan. It is 216 kilometres (134 mi) long

of Monument Beach and Pocasset along the western coast of Cape Cod. The river flows westward through a series of small ponds and wetlands, with a total

per kilometre (240 ft/mi) that flows from Lake Lea to Lake Gairdner. The river flows during the Tasmanian winter and spring, with flow reducing over the

The headwaters of the river rise in the Durack Range near Yulumbu. The river flows in a northerly direction along the range until it merges with the Pentecost

European to cross the river. The traditional owners of the area that the river flows through are the Kitja, Ola and Wilawila peoples. "History of river

kilometres (5,698 sq mi). The traditional owners of the area that the river flows through are the Unggumi people. Forrest, Alexander (8 February 1880)

Blackboy Hill approximately 7 kilometres (4 mi) south of Wellstead. The river flows in a south-easterly direction and discharges into Cheynes Inlet and

of Malham. At Airton the valley widens and becomes Airedale proper. The river flows past Skipton on to Keighley, Bingley, Shipley, and Leeds. Airedale

Uplands, part of the Atherton Tableland in the Great Dividing Range. The river flows generally south by southwest through the Blackbraes National Park before

departments of Haute-Vienne, Charente, Vienne and Charente-Maritime. The river flows into the Atlantic Ocean near Rochefort. The Charente was described

Bitoi River is a river located in Morobe Province, Papua New Guinea. The river flows into the Huon Gulf south of Salamaua. Transactions of the Institution

England. Rising on Gannow Fell, south west of the Forest of Bowland, the river flows southward, meeting the River Ribble at Ribchester. Stydd Brook flows

impounds the river to form North Hartland Lake. Near the state park, the river flows through the 165-foot-deep (50 m) Quechee Gorge. The U.S. Rt. 4 bridge

below Kangaroo Hill and near Bedford Downs, then flow north-east. The river flows past Nellie Range, through Devils Elbow and Gordons Gorge and through

Creek and Mud Creek, about 10 miles (16 km) southeast of Valdosta. The river flows southeast through Echols County, crossing into Hamilton County, Florida

the Paterson River, which was named after Colonel William Paterson. The river flows from Barrington Tops to the Hunter River at Morpeth. The district was

Australia. The headwaters of the Edmund rise north of the Barlee Range. The river flows south-west joined by the Dundagee, Edmund Claypan, Bobbamindagee, Rock

is located on the bank of the Elbe river, approx. 20 km east before the river flows into the North Sea. As of December 2019, the total population of Brokdorf

Richenda river is Dyson Creek. The traditional owners of the area that the river flows through are the Bunuba people. "Bonzle Digital Atlas – Map of Richenda

Mattapoisett River as "the Herring Run", and a highway sign where the river flows under US Route 6 once identified the river by this unofficial name

States Bavaria and Baden-Württemberg for about 50 kilometres (31 mi). The river flows into the Danube in the city centre of Ulm. The Iller has a catchment

or Simaia River is a river in Sandaun Province, Papua New Guinea. The river flows through Green River Rural LLG. Various Papuan languages are spoken

is formed by the confluence of Myall Creek and another minor creek. The river flows in a westerly direction an eventually discharges into Albatross Bay

along the Peninsula Developmental Road in the Great Dividing Range. The river flows in an easterly direction crossing the Peninsula Developmental Road

Cape York Peninsula. Formed by the confluence of two unnamed creeks, the river flows in a westerly direction eventually discharging to the Gulf of Carpentaria

5901°W / 45.2817; -69.5901 (Piscataquis River source)) in Blanchard. The river flows in a mostly eastern direction until it meets the Penobscot at Howland

juncture of the West Branch and the Third East Branch of the Magalloway. The river flows south through logging country to 2.5-mile-long (4.0 km) Parmachenee

South Stream joins the Roaring Branch northwest of town. From here the river flows westward as the Walloomsac River and joins the Hoosic River below Hoosick

joined by three major tributaries, the Carron, Clara and Yappar Rivers. The river flows through Normanton before entering the Gulf of Carpentaria through the

2.2-mile-long (3.5 km) stream in the U.S. state of Massachusetts. The river flows south from Copicut Reservoir (formerly the Copicut Swamp), in Dartmouth

caldera lake that lies on the border of Aomori and Akita Prefectures. The river flows in a generally eastern direction, through the municipalities of Towada

Surveyor General at the time. The traditional owners of the area that the river flows through are the Ngarinjin and the Yeidji peoples. "History of river

5901°W / 45.2817; -69.5901 (Piscataquis River source)) in Blanchard. The river flows in a mostly eastern direction until it meets the Penobscot at Howland

Mattapoisett River as "the Herring Run", and a highway sign where the river flows under US Route 6 once identified the river by this unofficial name

is located on the bank of the Elbe river, approx. 20 km east before the river flows into the North Sea. As of December 2019, the total population of Brokdorf

Coast of New Zealand's South Island. Rising on the slopes of Bald Hill the river flows north then west to reach the Tasman Sea two kilometres north of Ross

headwaters of the river originate in the area north of Laytonsville, and the river flows southeast, entering the Patuxent about 1.5 miles (2.4 km) below the

Book Award, was published in 2001; Left Alive was released in 2005; The River Flows North in 2009, and The Madness of Mamá Carlota in 2012. Her latest

Manawatū River is a major river of the lower North Island of New Zealand. The river flows from the Ruahine Ranges, through both the Manawatū Gorge and the city

Northern India, and thus forms part of the drainage system of the Ganges. The river flows north-northeast through Madhya Pradesh, running for a brief time through

Pokhi (And The River Flows…) A screenshot Directed by Jahnu Barua Written by Jahnu Barua Produced by Sailadhar Baruah Starring Bishnu Kharghoria Haramohan

Bow River in his family's ancestral home of County Clare, Ireland. The river flows into the Ord River at Lake Argyle. There are 12 tributaries of the

South Branch of the Manitowoc River, which flows to Lake Michigan. The river flows for its entire course in central Calumet County. It rises about 3 miles

the city of Bonn. After passing the cities of Hennef and Siegburg, the river flows into the Rhine at the Naturschutzgebiet Siegaue, a protected area immediately

its source, that portion of the river being classified as a creek. The river flows northward, as does the St. Johns River and many of the other tributaries

railway bridge area. The area of the basin is 500 square kilometres. The river flows throughout the year. Some believe that a Hindu Shastrakar, Manu, used

that has its headwaters south-east of Kojonup just below Byenup Hill. The river flows is a north-westerly direction crossing Albany Highway south of Kojonup

Porlock into Porlock Bay near Hurlstone Point on the Bristol Channel. The river flows into the sea though a shingle ridge at Bossington beach, where it forms

Western Australia. The headwaters of the river rise near Tenterden. The river flows in a south-westerly direction, crosses the Muirs Highway east of Rocky

follows a winding course 45 miles (72 km) south to Thomaston, where the river flows into the estuary and runs about 12 miles (19 km) southwest to Muscongus

river originates in the Blue Ridge Mountains in northern Georgia. The river flows for 51.1 miles (82.2 km) into the artificial Hiwassee Reservoir in

Kalpowar Aboriginal land northwest of Hope Vale and west of Starke. The river flows in a north easterly direction through mostly uninhabited country past

The headwaters of the Lyons rise just west of the Teano Range and the river flows generally south-west, joined by 36 tributaries including the Edmund

Left Bank) is the southern bank of the river Seine in Paris. Here the river flows roughly westward, cutting the city in two parts. When facing downstream

Wallachian Plain, on the right bank of the Olt River, close to where the river flows into the Danube. Izbiceni is located in the southeastern extremity

McIlwraith Range, part of the Great Dividing Range, northeast of Coen. The river flows generally south, then south by east and then finally east, joined by

Autonomous Region of Bougainville, in northeastern Papua New Guinea. The river flows into the Solomon Sea on the western side of Bougainville Island. During

director of the New Zealand Company in early colonial New Zealand. The river flows roughly along the course of an active geologic fault, which continues

river lying mostly between eastern Bangladesh and Mizoram, India. The river flows northwards and exits into the Karnaphuli River at 22°52′43″N 92°26′52″E

Holston River at Knoxville forms the beginning of the Tennessee River. The river flows through the counties of Transylvania, Buncombe, Henderson, and Madison

tributary creeks drain land to the north of the Cook River / Weheka. The river flows under a bridge of SH 6 just north of the Fox Glacier township and passes

Australia. The headwaters of the river rise in the Kenneth Range. The river flows in a south-westerly direction, joined by one minor tributary until

the main tributary of the Mattabesset River. It is 16.1 mi long, and the river flows northwards from a point approximately 1.8 mi south of the Durham line

The headwaters of the river are in the Whicher Range near Claymore. The river flows in a north-westerly direction through Yoganup then through Ludlow and

Massachusetts and downstream, the boundary between Scituate and Marshfield. The river flows into Massachusetts Bay at New Inlet, where it also converges with the

9 km) river crosses present-day Jackson, Calhoun and Gulf counties. The river flows through what is now preserved as the Dead Lakes State Recreation Area

length of 95 km (59 mi) and a drainage basin of 805 km2 (311 sq mi). The river flows across Sarysu District of the Zhambyl Region. There are Cambrian limestones

Pelican Creek, Macphee Creek, Rabbit Creek and Pumpkin Lookout Creek. The river flows through one permanent waterhole, Flying Fox waterhole, toward the end

Province, People's Republic of China. From Zhoukou City in Henan, the river flows through Fuyang City in Anhui Province then empties into the Huai River

canal and river now serve as one boundary of the Elk Neck Peninsula. The river flows through Cecil County, Maryland, with its watershed extending into New

Berkeley River is a river in the Kimberley region of Western Australia. The river flows for 135 km to the Timor Sea via the Joseph Bonaparte Gulf near Reveley

the second-largest river in the Zhejiang province of eastern China. The river flows 388 kilometers (241 mi) before finally reaching the city of Wenzhou

Western North Carolina before emptying into the Tuckasegee River. The river flows through the Qualla Boundary, a federal land trust that serves as a

Mountains of Chagang Province and emptying into the Yellow Sea at Sinanju. The river flows past Myohyang-san and through the city of Anju, South P'yŏngan Province

Sawmill (Odertaler Sägemühle) by the barrage of the Oder Dam. Thereafter the river flows through Bad Lauterberg and leaves the Harz. In Bad Lauterberg the Oder

Western Australia. The headwaters of the river rise below Donkins Hill. The river flows in a south-westerly direction until it discharges into Prince Frederick

a tributary of the Lamandau River. The river flows through the north side of Pangkalan Bun town. The river flows in the southern area of Kalimantan with

west for about 6 kilometres (4 mi) to join the River Axe near Loxton. The river flows through a gap in the Mendip Hills between Crook Peak and Bleadon Hill

Hillman River, Kojonup Brook, Narrogin Brook and Yilliminning River. The river flows in a generally south-westerly direction until it meets with the Balgarup

until merging with the Nullagine River to form the De Grey River. The river flows through many permanent pools on its journey, including Toocoonaragee

(175 km) tributary of the Delaware River in eastern Pennsylvania. The river flows in a generally southward pattern from the Pocono Mountains in Northeastern

is popular among rafting enthusiasts owing to its turbulent waters. The river flows past the towns of Jorethang, Pelling and Legship. During its final

a tributary of the Lamandau River. The river flows through the north side of Pangkalan Bun town. The river flows in the southern area of Kalimantan with

Lambourn, about 5.5 miles (8.9 km) north of Hungerford in West Berkshire. The river flows through the village, dividing many houses from the main road, so that

into which the Sit used to flow before the reservoir was filled). The river flows for 159 kilometres (99 mi) through Sonkovsky District of Tver Oblast

until merging with the Nullagine River to form the De Grey River. The river flows through many permanent pools on its journey, including Toocoonaragee

creek gathering strength on its way to become the river Dandavati. The river flows via Kuppe and joins the Varada river at a place called Bankasana near

lake extends into the neighboring municipality of Evje og Hornnes. The river flows out of the lake Åraksfjorden to the north and into the Byglandsfjorden

Australia. The headwaters of the river rise below the Chichester Range. The river flows in a northerly direction past Marble Bar then through the Gorge Range

River is approximately 20 kilometres (12 mi) west of Busselton where the river flows into Geographe Bay. The Carbunup River is 36 kilometres (22 mi) in

in the vicinity of its crossing by U.S. Route 17. From that point, the river flows through salt marshes and widens considerably, crossing under Georgia

their confluence forms the Pomperaug and Woodbury developed here. The river flows through Woodbury and the Town of Southbury, where it empties into the

drains the eastern slopes of Drum, a mountain in the Carneddau range. The river flows through the village of Rowen before joining the River Conwy. The river

the east of the Bensbach River, and to the west of the Fly River. The river flows through the Trans-Fly savanna and grasslands. The mouth of the river

great rivers that define Mesopotamia, the other being the Euphrates. The river flows south from the mountains of the Armenian Highlands through the Syrian

Lake, drops down the headwall below the lake starts to turn north. The river flows generally north until it converges with the Middle Fork Snoqualmie

Range in the Great Dividing Range and flow in a westerly direction. The river flows across mostly uninhabited plains country and discharges into the Gulf

descends over the spectacular Coomera Falls in the Coomera Gorge. The river flows generally north through large rural properties in the upper reaches

River drain the Richardson Range, part of the Great Dividing Range. The river flows generally west through stringybark woodlands, tropical savanna plains

flows 500 km (310 mi) northwest to its confluence with the Mackenzie. The river flows through a deep canyon as it flows through the Peel Plateau. The Gwich'in

Brook are the main tributaries, both joining the Chew from the left. The river flows northwest from Chewton Mendip through Litton, Chew Valley Lake, Chew

The headwaters of the Irwin are located below Canna near Pindar. The river flows west until discharging into Arurine Bay near Dongara. The river passes

Charles Burrowes, in 1886. The traditional owners of the area that the river flows through are the Ngarinjin, Miwa and Wilawila peoples. "Bonzle Digital

into the Solway Firth at Airds Point. The territory through which the river flows is called Nithsdale (historically known as "Stranit" from Scottish

needed]. The shore's land is rich in grass and fertile, featuring trees. The river flows through many semi-permanent pools of water on the way to the coast

river and the Carbunup River have fishery resource issues in common. The river flows through agricultural land that is predominantly used for raising beef

through Boulia towards the Simpson Desert in the Lake Eyre Basin. The river flows into Eyre Creek, a tributary of the Georgina River. The Hamilton River

through the Youarling State Forest then the Serpentine National Park. The river flows through Serpentine Dam then flows over Serpentine Falls just south

Rusk County, Texas, United States. A tributary of the Neches River, the river flows southeast for 120 miles (193 km) and forms the boundaries between Cherokee

weir and boathouse were created to the west of Saint Oswald's Church. The river flows northwest towards Parkmill Farm, where again a weir was constructed

rises about 4 kilometres (2.5 mi) north of the village of Busbys Flat. The river flows generally east, north, east, and then south before reaching its confluence

ancient river Rubicon, famously crossed by Julius Caesar in 49 BC. The river flows for around 80 km (50 mi) from the Apennine Mountains to the Adriatic

long. The river's source is in the Antrim Hills at 480m. From there the river flows northwest, with a bend at the town of Armoy. It then flows west, passing

Pecos, New Mexico, at an elevation of over 12,000 feet (3,700 m). The river flows for 926 miles (1,490 km) before reaching the Rio Grande near Del Rio

village of Mar'ivka in the suburbs of Kramatorsk in Donetsk Oblast, the river flows through the oblasts of Kharkiv (briefly) and Dnipropetrovsk (for most

Deadman Hill in the Ophthalmia Range about 30 km south of Newman. The river flows in a northerly direction parallel with the Great Northern Highway until

three miles south east of Glossop and just north of Kinder Scout. The river flows approximately ten kilometres east, following the Sheffield to Manchester

through Lunedale before reaching Teesdale where it joins the River Tees. The river flows through two reservoirs on the way: Selset Reservoir and Grassholme

from its eastern suburbs, primarily Bourj Hammoud and Sin el Fil. The river flows mostly east to west from snow drains and springs on the western slopes

United States. From the meeting of its branches in Hancock, New York, the river flows for 282 miles (454 km) along the borders of New York, Pennsylvania

headwaters of the river rise in the Elizabeth and Catherine Range. The river flows in a north-westerly direction past the Whately Range and discharges

County, with only a small part of its East Branch entering Leon County. The river flows through the Apalachicola National Forest and the Bradwell Bay Wilderness

on the lake and it is located on the northwestern part of the lake. The river flows out of the lake and later joins the lake Åsrumvannet and then it eventually

within the Great Dividing Range, southwest of the Carrai National Park. The river flows generally north northwest, joined by a minor tributary before reaching

(226 mi) and a drainage basin of 19,600 square kilometres (7,600 sq mi). The river flows into the Dnieper through the Kremenchuk Reservoir, with which it forms

to the smooth, sloping rock face along the river.[citation needed] The river flows south from Pathfinder Lake through a group of other large lakes (such

rise to the name Mühltal ("Mill Valley"), a district through which the river flows. It passes through Darmstadt, and Ober-Ramstadt, and Pfungstadt, and

the northern Vardousia mountains, near the village Artotina, Phocis. The river flows in a generally southwestern direction, for most of its length in Aetolia-Acarnania

Australia. With its headwaters rising west of the Hamersley Range, the river flows in a north-westerly direction through the Cane River Conservation Park

valley providing the route of the southern part of the Cotswold Line. The river flows for 45 miles (72 km) from source to the River Thames. The name Evenlode

near the Karlsruhe borough of Hagsfeld and one by Dettenheim-Rußheim. The river flows through Pfinztal and lent its name to the town of Pfinztal. The town

near Montereale and Lago di Campotosto in the province of L'Aquila. The river flows in a southeastern direction past Pizzoli, L'Aquila, Paganica, San Demetrio

confluence with the Râul Mic, the river is also called the Râul Mare. The river flows entirely in Sibiu County. The Cibin is an important tributary of the

valley providing the route of the southern part of the Cotswold Line. The river flows for 45 miles (72 km) from source to the River Thames. The name Evenlode

the U.S. Route 84 crossing of the two creeks southwest of Screven. The river flows south as the boundary between Wayne and Pierce counties, then turns

Australia. With its headwaters rising west of the Hamersley Range, the river flows in a north-westerly direction through the Cane River Conservation Park

length of 71 km (44 mi) and a drainage basin of 571 km2 (220 sq mi). The river flows across Sarysu district of the Zhambyl Region and Sozak District of

the Australian state of Victoria. A permanent camping ground which the river flows passed to the south is also called Tidal River. The Tidal River rises

Gopalganj in Seoni, Madhya Pradesh. It is a key tributary of the Godavari. The river flows south in a winding course through the states of Madhya Pradesh and

(138 mi) and a catchment area of 4,360 square kilometres (1,680 sq mi). The river flows from the Ulytau District, Karaganda Region into the Yrgyz District

the assistance of World Bank near Gram Machka in Dhamtari district. The river flows through Sitandi sanctuary before merging with Mahanadi. Hydrology and

is Crystal Lake in the Mummy Range of Rocky Mountain National Park The river flows through Lawn Lake before a confluence with the Fall River in Horseshoe

Вовча) is a river in Dnipropetrovsk and Donetsk Oblasts, Ukraine. The river flows for 323 kilometres, covering a basin area of 13,300 km2. It runs through

market town of Innichen, in the Puster Valley of South Tyrol, Italy. The river flows eastwards through East Tyrol and Carinthia in Austria into the Styria

river rise below the Chinaman Ridges in the Great Dividing Range. The river flows generally west past Mount Bridget where the river veers south and crosses

Meramec forms the border between Jefferson and Saint Louis counties. The river flows through Washington State Park, St. Francois State Park, and the Lead

Colorado. Originating in Forest Canyon in Rocky Mountain National Park, the river flows into Lake Estes in the town of Estes Park and then through Big Thompson

flows westwards through High Bentham, Low Bentham and Wennington. The river flows for 14.09 miles (22.67 km) and drains an area of 24.9 square miles

counties: Yuba, Sutter, Placer, and Nevada. About 73 miles (117 km) long, the river flows generally southwest through the Sierra then west through the Central

in the Great Dividing Range and flow in a northeasterly direction. The river flows roughly parallel with the Hervey Range Developmental Road past Mount

slopes of the Western Ghats part of the Wayanad district. Initially, the river flows through the hilly eastern towns of the Kozhikode district like Vilangad

have grown birch and juniper trees. 40 km west at Sarhad-e Broghil the river flows in a dramatic basin 3 km wide. Little if any vegetation, except dwarf

northern section of the river flows north almost entirely through the Nubian Desert to Cairo and its large delta, and the river flows into the Mediterranean

crossing the River Thames in an east–west direction in central London. The river flows north at the crossing point. Downstream, the next bridge is Westminster

highwayman George Lyons held up his victims during the 18th century. Today, the river flows through the middle of Skelmersdale in large culverts. It emerges near

Range on Cape York Peninsula northeast of the settlement of Kimba. The river flows in a north easterly direction, joined by four minor tributaries, crosses

(8 km) and joins the Thames estuary on the south side of Norwich. The river flows through a rural section of New England, despite the historical presence

(3,760 km2) and about the same size as the state of Rhode Island. The river flows through canyons along most of its route and is a popular destination

drainage from a 80,300-square-kilometre (31,000 sq mi) watershed. The river flows through the Liupanshui, Anshun, Guiyang (the capital), Qiannan, and

(43 mi) long and drains a basin of about 58,534 ha (226 square miles). The river flows through a traditional area of ancient villages and tea plantations

stem from the natural tannic acid that darkens the water in places. The river flows in a generally northwest direction, with its valley dividing the Adirondack

clear from a group of large limestone springs. From its headsprings, the river flows approximately 12 miles (19 km) south through a broad cypress swamp

(86 mi) long, and has a 1,240 square kilometres (480 sq mi) basin. The river flows through the Greater Tokyo Area, on the dividing line between Tokyo

central Texas to a man-made reservoir called Stillhouse Hollow Lake. The river flows about 84 miles southeast through Lampasas, Burnet, and Bell Counties

West Yule River, Pilbara Creek, Friendly Creek and Coorong Creek. The river flows through a number of permanent pools, including Kangan Pool and Moolkamudda

Ojibwe: Pasapkedjinawong) is a river in Eastern Ontario, Canada. The river flows north from Upper Rideau Lake and empties into the Ottawa River at the

fifth-largest tributary by drainage area of the Yangtze tributaries. The river flows generally northeast through the provinces of Guangxi and Hunan, its

spring upstream on the lower river until blocked by the Shawano Dam. The river flows through mostly undeveloped forestland southerly from central Forest

of the hill topped by Clitheroe Castle. In the south of the town, the river flows into the mill lodge of the old Primrose Mill and then into Pendleton

of 164 km (102 mi) and a drainage basin of 1,290 km2 (500 sq mi). The river flows across the Sarysu District of the Zhambyl Region. There are two inhabited

Beginning near the southeastern end of Summit Lake in the Alaska Range, the river flows generally south to meet the larger river 9 miles (14 km) northeast

(400 km) tributary of the Yukon River in the U.S. state of Alaska. The river flows northeast from the Kuskokwim Mountains through Nowitna National Wildlife

Mills to generate hydro-electricity for the machinery, after which the river flows over the Fairy Falls, a popular attraction. Coed Crafnant, an area

failures and resulting flooding on May 19, 2020. In Saginaw County, the river flows through Tittabawassee Township, which is named for the river and contains

is a perennial river located in north western Tasmania, Australia. The river flows for 61 kilometres (38 mi) before joining into the Arthur River. High

which is drained in winter. Here, it forms rapids and a waterfall. The river flows further northwards through a region called the Lechrain, and passes

(about 320 kilometres (200 mi)). Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island

into the Rhine in Brühl. Between the cities of Wiesloch and Walldorf the river flows through the Leimbach Park linear-park close to Wiesloch-Walldorf station

length of 105 km (65 mi) and a drainage basin of 1,460 km2 (560 sq mi). The river flows across the road that runs roughly from east to west between Koskol

watercourse running through Rutland County and Addison County. The mouth of the river flows into Lake Champlain. Settled by indigenous peoples at least 10-11,000

approximately 10 kilometres (6.2 mi) north of the village of Kiandra. The river flows generally south and southeast before emptying into Lake Eucumbene where

which is drained in winter. Here, it forms rapids and a waterfall. The river flows further northwards through a region called the Lechrain, and passes

into the Rhine in Brühl. Between the cities of Wiesloch and Walldorf the river flows through the Leimbach Park linear-park close to Wiesloch-Walldorf station

town of Snoqualmie just above the Snoqualmie Falls. After the falls the river flows north through rich farmland and the towns of Fall City, Carnation,

cessation of all the coal-mining and a decline in the steel industry. The river flows into the Meuse at Namur, Belgium. The navigable waterway is managed

in Sanjay Gandhi National Park in the northern reaches of the city. The River flows roughly North-West for a total of 12 kilometres through the localities

Fork meets the others at Lake Success. Downstream of Success Dam, the river flows west through Porterville. The river used to empty into Tulare Lake

of 235 km (146 mi) and a drainage basin of 4,940 km2 (1,910 sq mi). The river flows by Baikonur village. Ancient petroglyphs have been found on rocks along

Pine River watershed drains an area of 265 square miles (690 km2). The river flows through a section of the Huron–Manistee National Forest, with multiple

long as the sun shines, as long as the grass grows, and as long as the river flows." Due to a lack of support, Iveson abandoned the flag redesign in 2017

After about 96 km, it joins the Adige river south of Bolzano. At first the river flows through the Wipptal and after the village of Vahrn through the Eisacktal

land’, and like (/léyki/), ‘sitting’, plus hvcce (/háčči/), ‘stream’. The river flows north from its source, Lake Conlin, through the Econlockhatchee River

the eastern edge of Marlborough, where it joins the River Kennet. The river flows through a gap in the Marlborough Downs, which creates a natural transport

Vučica discharges into Karašica between Valpovo and Ladimirevci and the river flows into the Drava north of Josipovac. There are several suggested etymologies

is on the boundary between the communes of Casamaccioli and Corte. The river flows through marshy land above and below the lake. Way: Lac de Nino (28890021)

length of 105 km (65 mi) and a drainage basin of 1,460 km2 (560 sq mi). The river flows across the road that runs roughly from east to west between Koskol

part of the extensive network that contributes to the Ganges basin. The river flows through the Udaipur city and is its larger drainage body. The spill

Luánhé, formerly known as Lei Shui, or Ru Shui) is a river in China. The river flows northwards from its source in the province of Hebei into the province

approximately one mile upstream of Grant, Colorado. North of Dillon, the river flows north-northwest along the eastern slope of the Gore Range and joins

To the west is Winterborne Tomson and to the north-east is Almer. The river flows through both these villages as well. The parish church is dedicated

9; -69.85 (Soper River)) is a waterway on Baffin Island, Nunavut. The river flows over 100 km (62 mi) and then empties into Soper Lake and Pleasant Inlet

Oxfordshire/Warwickshire border near Traitor's Ford. The first settlement that the river flows through is the village of Stourton. The River Stour then turns to the

blackwater river in Pasco County, Florida. Originating near Crews Lake, the river flows for over 23 miles (37 km) to the south and west, flowing through the

confluence of the Khari and Mithari Rivers near the Bombadra pickup weir. The river flows for approximately 45 km before merging with the Luni River near the

is a gorge in Slovenia that was carved by the Tržič Bistrica River. The river flows through unique waterfalls over large rounded blocks of white quartz

villages of Knežina, Belčji Vrh, and Mali Nerajec. In its upper course the river flows towards the north in a narrow bed with a very shallow gradient, resulting

1870) département Meurthe. Channelled during its route through Nancy, the river flows into the Moselle at Pompey on the northern edge of Nancy, a short distance

Kwango River just before this stream enters the Kasai River. In the DRC the river flows past the towns of Gungu, Kikwit, Bulungu, Bagata, Rutherfordia and

and has a drainage basin of 9,220 square kilometres (3,560 sq mi). The river flows through the territory of Akmola and North Kazakhstan regions. The name

mountains and passes through the city of Chalus in Mazandaran Province. The river flows northward through the Central Alborz mountain range, to its river mouth

and east through a lake district and on through Schoolcraft County. The river flows into the 8,659 acre (35 km2) Indian Lake at 46°17′36″N 86°42′20″W

Na’ [pronunciation?]. Fed by the Tangle Lakes of the Alaska Range, the river flows north to meet the larger river near Big Delta. It is older than the

Park in Bethel, with a watershed of approximately 430 acres (170 ha). The river flows generally southerly through Redding, Connecticut, to the Aspetuck Reservoir

near the village of Rozhnivka in Pryluky Raion, Chernihiv Oblast. The river flows through the Dnieper Lowland, within the Chernihiv Oblast and the Poltava

of Alaska. Heading in the Endicott Mountains of the Brooks Range, the river flows generally west then south to meet the larger river about 80 miles (130 km)

Ко́торосль) is a right tributary of the Volga in Yaroslavl Oblast, Russia. The river flows from Lake Nero near Rostov past Karabikha and enters the Volga in Yaroslavl

Inlet. The tidal influence is 5 kilometres (3 mi) upstream from where the river flows into the inlet. The Hay River flows all year and the water quality

Noongar, called the river "Koorrabup" meaning "place of the black swan". The river flows through Denmark Pipehead Dam. The two tributaries of the river are

Pesole (which is near Forenza and Filiano) in the province of Potenza. The river flows southeast near Monte Torretta, Acerenza, and Oppido Lucano. After crossing

Sardab Rud is a river located in Mazandaran Province of northern Iran. The river flows northwards, through the Central Alborz mountain range. It is a tributary

Winfield. The river flows through Alberta and into Saskatchewan, where it discharges into the North Saskatchewan River at Battleford. Over its course, the river

fortifications of Wadbury Camp to the north and Tedbury Camp to the south. The river flows through the western part of the Harridge Woods nature reserve. Mells

approximately 9 kilometres (5.6 mi) north of Coolangubra Mountain. The river flows generally southeast and then northeast, joined by twelve tributaries

the U.S. state of Michigan. Rising in the Northern Lower Peninsula, the river flows in a generally southeasterly direction to its mouth at Lake Huron at

The Nyong (formerly German: Yong) is a river in Cameroon. The river flows approximately 690 kilometres (430 mi) to empty into the Gulf of Guinea. The

Central America was an important shipping staging point. Just after the river flows from Lake Izabal it is spanned by one of the biggest bridges in Central

Senne". The spring of the Senne is near Soignies. After Soignies, the river flows through Brussels. Soignies is also well known for its blue limestone

through the northern part of the country and joins the Achwa River. The river flows next to Kitgum Matidi in Kitgum district. It covers a total distance

of the Blue Ridge Mountains near Buchanan, Virginia. From Buchanan the river flows along the base of the Blue Ridge Mountains until it joins the Maury

the U.S. state of Michigan. Rising in the Northern Lower Peninsula, the river flows in a generally southeasterly direction to its mouth at Lake Huron at

The Nyong (formerly German: Yong) is a river in Cameroon. The river flows approximately 690 kilometres (430 mi) to empty into the Gulf of Guinea. The

Cikapundung River divides the city of Bandung, in West Java, Indonesia. The river flows from its headwaters in Lembang on the northern edge of the city, to

of the Blue Ridge Mountains near Buchanan, Virginia. From Buchanan the river flows along the base of the Blue Ridge Mountains until it joins the Maury

river's course is through the dense forests of Nabarangapur & Bastar. The river flows for 535 kilometres (332 mi) and has a drainage area of 41,665 square

rocks are the same as the ones found at Tunnel Creek and Geikie Gorge. The river flows freely through the gorge during the wet season but during the dry season

confluence of Toongabbie Creek and Darling Mills Creek at North Parramatta, the river flows in an easterly direction to a line between Yurulbin in Birchgrove and

long and has a basin area of 19,100 square kilometres (7,400 sq mi). The river flows west-southwest from the border with China before turning northwestward

originates from the southern tip of the Western Ghats at Agastya Mala. The river flows 68 kilometres (42 mi) westward and merges into the Arabian Sea at the

border with Ticino and is surrounded by up to 3100m high mountains. The river flows through the Lumnezia. In Suraua, the Vals Rhine flows into the Glogn

heron, grey wagtail and white-throated dipper are common sights too. The river flows by the site of the former Calderwood Castle (demolished 1947–1951)

statement made by Dennis Skinner, (MP) in the House of Commons in 1992. The river flows through the site of the former Coalite plant near Bolsover, where coke

The Ledava is the only outflow from the lake. In its lower course the river flows through Murska Sobota and Lendava. It has several (mainly left) tributaries

into Floras Creek, where the combined streams form the New River. The river flows north behind a foredune until veering west and entering the Pacific

the River Dibb at a point some 2.5 miles (4 km) from Appletreewick. The river flows for 5.2 kilometres (3.2 mi), and must maintain a flow of 273,000 cubic

river in the 20th century for flood control and hydropower generation. The river flows through five major impoundments: Fontana Dam, Cheoah Dam, Calderwood

River completes a journey of approximately 110 kilometres (68 mi). The river flows through the Werribee Gorge State Park before being utilised for irrigation

Java province, about 210 km to the southeast of the capital Jakarta. The river flows from Mount Cikuray and discharges into the Indian Ocean at the Cikaengan

(itself a tributary of the River Derwent) in North Yorkshire, England. The river flows for 13 miles (20.5 km) down Bilsdale and meets the Rye near the village

staff of the hydroelectric plant. From the reservoir to Tash-Kömür the river flows through a gorge with a series of dams (the 'Lower Naryn Cascade').

both merge at a deep pool known locally as the Joinings Pool. Then the river flows on for about a mile and silently under the Eden Bridge which was built

Three Sisters. Starting in the Devil's Bit Mountain, County Tipperary, the river flows generally southeast, and then south, before its confluence with the

blackwater river in the Upper Peninsula of the U.S. state of Michigan. The river flows in a generally eastward direction from the Tahquamenon Lakes of Columbus

Rivelin tunnel before it flows into the lower of the Rivelin Dams. The river flows almost its entire length within the Wyming Brook Nature Reserve, a

Amargosa Canyon in California and a small portion at Beatty, Nevada, the river flows above ground only after a rare[quantify] rainstorm washes the region

province of Matera. The river flows for a short distance before entering Lago di Gannano. After exiting the lake, the river flows southeast near Tursi

is the only large Slovak river flowing north into southern Poland. The river flows through the Slovak towns of Poprad, Kežmarok, Stará Ľubovňa, then forms

through Stamford and Greenwich into Long Island Sound, at sea level. The river flows under the Mianus River Bridge, which is part of Interstate 95, U.S

central Missouri, where it drains northwest areas of the Ozark Plateau. The river flows generally easterly, then northeasterly for the final 80 miles (130 km)

the river flows until it meets the North Fork of the river near Woodway, Virginia. The North Folk originates near Keokee, Virginia. The river flows past

above Wallula Gap in southeastern Washington in the United States. The river flows through Umatilla County, Oregon, and Walla Walla County, Washington

Aral Sea, once the world's fourth-largest lake. The point at which the river flows from Tajikistan into Uzbekistan is, at 300 m (980 ft) above sea level

Miramichi Highlands, a region in north-central Northumberland County. The river flows southeast through heavy forests before joining the Northwest Miramichi

Lillehammer). The town is located along the river Hunnselva where the river flows into the lake Mjøsa. The town is traditionally an industrial town with

end of Lake Couchiching. It drains Lake Couchiching and Lake Simcoe. The river flows generally northwest into Georgian Bay, a large bay of Lake Huron. The

325 km (202 mi) and a drainage basin of 10,100 km2 (3,900 sq mi). The river flows across a desert and semi-desert area without permanent settlements

widening to between 100-400 yards at Widows Point. From Widows Point, the river flows due southward, crossing under the Hix Bridge before passing Gull Rock

Lake of which it is the primary source. The depression through which the river flows corresponds to the Futrono Fault. "Cuenca del río Bueno" (PDF). Archived

Randow is exclusively used. The source is near Penkun, from which the river flows both to the North and to the South. The southern fork ends with its

Contrafuerte River is a river in the Los Ríos Region of Chile. The river flows north from the northern slopes of Puyehue-Cordón Caulle following Liquiñe-Ofqui

Timur, near Cipinang Besar Selatan Street and IPN Street, Jakarta. The river flows mainly in the district of Makassar, East Jakarta, with many houses

the Dnieper about 30 kilometres (19 mi) east of the city of Kherson. The river flows through southern spurs of the Dnieper Uplands and then across the Black

has snow feeding. The town of Pugachyov is located along the Irgiz. The river flows to the Volgograd Reservoir of the Volga downstream Balakovo, near Volsk

Buck Mountain Creek, Squaw Creek, Rays Creek, and Tom Long Creek. The river flows west, turns north, and flows west again, through rugged terrain in

of Rolleston. The river flows north, joined by seventeen tributaries, and splits as an anabranch on multiple occasions. The river flows through the Teatree

of the Wind River Canyon near the town of Thermopolis. From there, the river flows through the Bighorn Basin in north central Wyoming, passing through

trout and char, with the season running from 1 March to 30 September. The river flows in the Bluestack Mountains, which are to the north of Donegal Town

tributary of the Main. After leaving the Vogelsberg mountain range the river flows through the Wetterau, a fertile landscape just north of Frankfurt,

southeastern Pennsylvania and northeastern Maryland. Near its mouth, the river flows past downtown Wilmington, Delaware, forming the city's harbor for traffic

795,000 km2 (307,000 sq mi). Beginning in the Bayan Har Mountains, the river flows generally eastwards before entering the 1,500 km (930 mi) long Ordos

and camping area is adjacent to the bridge. Upstream of the gorge the river flows through the Lees Valley. Ashley Gorge is also the name of a small rural

sublacustric sources under the Veliko Lake (Veliko jezero, "Great Lake"). The river flows in the direction south-north and on the way runs through the town,

region). There, the Minho averages 316 m3/s of discharge. Later on, the river flows in a southwest direction until reaching the Portuguese border near

Wakpá Owóthaŋna, the Dakota name for the river. Despite its name, the river flows in a winding course, though its valley is fairly straight. The river

southeastern Pennsylvania and northeastern Maryland. Near its mouth, the river flows past downtown Wilmington, Delaware, forming the city's harbor for traffic

provincial capital. The Kunduz River valley dominates the Kunduz Province. The river flows irregularly from south to north into the Amu Darya river which forms

River or Chalakudy Puzha is the fifth longest river in Kerala, India. The river flows through Thrissur district, Palakkad district and Ernakulam district

managed by the Massachusetts Department of Conservation and Recreation. The river flows from Jamaica Pond through Olmsted Park's Wards Pond, Willow Pond, and

tributary of the Krishna River and finally empties into the Bay of Bengal. The river flows through the village of Kavadi in the Pune district, witnesses many

passes the site of Nelson and Colne College. From this point onwards, the river flows west past the Lomeshaye Industrial Estate alongside the Leeds and Liverpool

Haugsjåsund in Nissedal municipality in southern Telemark county. The river flows south into the Skagerrak at the city of Arendal. The watershed covers

direction to its mouth at Lake Michigan in the city of Grand Haven. The river flows through a number of cities, including Jackson, Lansing, Ionia, and

rises near the heart of the city of Curitiba. For most of its course, the river flows through Brazil; however, most of the falls are on the Argentine side

lower course, and causes flooding somewhere along its line most years. The river flows entirely within the jurisdiction of Dublin City Council. The origins

The headwaters of the river rise below Three Wells near Broomehill. The river flows in a south-westerly direction parallel with the Great Southern Highway

the city of Wausau. It is divided in two by the Eau Claire River. The river flows through a rocky gorge to form cascades and waterfalls as it passes

when it passes by Montería. The river flows between the eastern and middle prongs of the Cordillera Occidental. The river flows through the Sinú Valley dry

Plateau in north-central West Virginia and Southwestern Pennsylvania. The river flows from the confluence of its west and east forks in north-central West

pollution from human and domestic animal populations. In addition, the river flows underground for part of its journey. As it passes underground, the

and East Molesey post towns based on the south side of the river. As the river flows north past Hampton Wick and Kingston, it is actually west of Kingston

Dimitrovgrad in Bulgaria to Edirne in Turkey. East of Svilengrad, Bulgaria, the river flows eastwards, forming the border between Bulgaria (on the north bank)

From its source at the southern slopes of Dorset Mountain, Vermont, the river flows southwards for 17 miles, flowing through Mettawee Valley in Vermont

south of Sydney and about 15 kilometres (9.3 mi) from the Tasman Sea. The river flows north in an unpopulated water catchment area into Nepean Reservoir

It is located on the lower reaches of the River Murray, near where the river flows into Lake Alexandrina. It is linear in layout since it is constrained

northwestern Turner County, Georgia, 7 miles (11 km) northwest of Ashburn. The river flows southeast into Tift County, passing west of Tifton, then turns more

Eastern Norway before emptying into Mjøsa, the largest lake in Norway. The river flows through the municipalities of Lesja, Dovre, Sel, Nord-Fron, Sør-Fron

credible is a derivation from the Mi'kmaq word for river, "Seboo." The river flows out of a chain of lakes near the border with Annapolis County, named

river in located between Tabora Region and Shinyanga Region, Tanzania. The river flows eastwards into Lake Kitangiri. During the dry season, from June to

No.1 (built in 1900). The river flows in northerly direction and is crossed by the Bruce Highway near Howard. The river flows past Pacific Haven before

National Park. The river flows north by east, joined by the Josephine Creek and it has descended over the Josephine Falls. The river flows east of Babinda

into the Vistula River after passing through the town of Oświęcim. The river flows within metres of the Auschwitz concentration camp. The Auschwitz-Birkenau

o te Moana, roughly 30 kilometres (19 mi) southeast of Greymouth. The river flows northwest for its entire length, eventually joining the same river

rises in the Band-e Amir lakes in Bamyan Province in the Hindu Kush. The river flows west, then north, and terminates in irrigation canals in the area of

River, there is a spring festival organized during Easter holidays. The river flows through picturesque landscape featuring some of the more interesting

Russian: Кусак, Chinese: 库萨克; pinyin: Kùsàkè). Along most of its course, the river flows through the very sparsely populated mountainous terrain of the southern

is a 91.25-kilometre (56.70 mi) long river in Jakarta, Indonesia. The river flows from the Bogor area of West Java, passing through the cities of Tangerang

53417°N 72.83167°W / 44.53417; -72.83167 (Browns River source)). The river flows west from Mount Mansfield, through Underhill State Park to the town

-19.833. The river flows for 40 kilometres (25 mi) before dropping down into a narrow gorge at Gullfoss waterfall. Thereafter, the river flows between

Lansing metropolitan area and suburban and rural areas to the east. The river flows through the campus of Michigan State University, and is considered

County, New Mexico, in the Zuñi Mountains at the Continental Divide. The river flows off the western slopes of the Zuñi Mountains in a generally southwesterly

Lakes: ST225152 and then through Churchstanton before entering Devon. The river flows through a predominantly rural area, with small cattle, sheep and dairy

The river then flows along by the village of Corofin. After Corofin, the river flows through Lough Atedaun, Ballyteige Lough, Dromore Lough and Ballyallia

the Bezhanitsy Hills in the northwest of Novosokolnichesky District. The river flows south through a system of lakes to Lake Veryato, where it turns west

National Park draining the eastern slopes of the King William Range. The river flows generally south and to the west of the Gordon Range before flowing

town of Clun until Aston on Clun where it flows roughly southwards — the river flows around the north of Clunbury Hill. The river enters the lower valley

above the eponymous village (Blatnica). After leaving the ravine, the river flows around Jove masiff turn right to the north to the mouth.During Austro-Hungarian

south of France. It flows into the Mediterranean Sea at Valras-Plage. The river flows through the towns of Bédarieux and Béziers, where it is crossed by

Canada. Its seat is McMasterville. It surrounds the Richelieu River as the river flows north from Lake Champlain in the United States to the Saint Lawrence

Salzburg. The river flows eastwards through Tamsweg before crossing the border into the state of Styria. Between Tamsweg and Unzmarkt-Frauenburg the river flows

chinook to the system in an attempt to establish a self-sustaining run. The river flows through coastal rainforest and, in its lower stretches, follows a granite

chinook to the system in an attempt to establish a self-sustaining run. The river flows through coastal rainforest and, in its lower stretches, follows a granite

Maihue Lake, which in turn flows by Calcurrupe River into Ranco Lake. The river flows in a north-south direction along the Liquiñe-Ofqui Fault. List of rivers

tributaries of Kaljani are Dima, Nonai, etc. The major portion of the river flows through the Indian state West Bengal. In 1993, towns like Alipurduar

years, and then in the 19th century for pioneers on the Oregon Trail. The river flows mostly through rugged and arid country, and its valley provides a cultural

reka) is a river in western Bulgaria, a tributary of the Perlovska. The river flows from the northwestern slopes of Cherni Vrah on Vitosha Mountain, crossing

discharge is 2.15 m3/s (76 cu ft/s). The river is used for irrigation. The river flows in vicinity of settlements Bökönbaev and Tört-Kül . Ысык-Көл облусу

urban-type settlements, are located within the catchment area of the Svir. The river flows past the Alexander-Svirsky Monastery, which housed Svirlag (one of

River, the ancient Calycadnus, near its outlet into the Mediterranean. The river flows from the nearby Taurus Mountains and the city is surrounded by attractive

Salzburg. The river flows eastwards through Tamsweg before crossing the border into the state of Styria. Between Tamsweg and Unzmarkt-Frauenburg the river flows

288 km2 (497 sq mi). The Klang River has 11 major tributaries. Because the river flows through Klang Valley, which is a heavily populated area of more than

reaches the Phaleron Bay between Neo Faliro and Moschato. Presently the river flows near or under the A1 motorway, linking Athens and Thessaloniki for

the Bezhanitsy Hills in the northwest of Novosokolnichesky District. The river flows south through a system of lakes to Lake Veryato, where it turns west

Midlands. Aquatic flora is more varied in the lower reaches, where the river flows slowly across a flood plain. Here the marginal vegetation includes

Morris County, New Jersey in the United States. The upper course of the river flows through a wooded mountainous valley, whereas the lower course flows

way, several smaller streams (Diju, Missa River and others) meet it. The river flows through the heart of the Nagaon urban area, dividing the town into

are 2,650 people resident within the Chéticamp watershed in 2011. The river flows from Chéticamp Lake in the Cape Breton Highlands into the Gulf of Saint

where the borders of Iran, Turkey and Iraq meet. From its source, the river flows towards the southeast and then changes course due east through the

in the Ilgaz Mountains, in Kastamonu Province and Karabük Province. The river flows to the north, passes through Bartın, and empties into the Black Sea

Island, in British Columbia, Canada. Its headwater is Cowichan Lake. The river flows east over Skutz Falls and through Marie Canyon towards its mouth at

valley of the Poultney River, which forms the southern edge of the CDP. The river flows west and north to the south end of Lake Champlain on the Vermont/New

Truckee River is a river in the U.S. states of California and Nevada. The river flows northeasterly and is 121 miles (195 km) long. The Truckee is the sole

Spirovsky District, at the southeastern outskirts of the Valdai Hills. The river flows southeast, and makes a stretch of the border between Spirovsky and

also yield hydroelectric power, drinking water, and industrial water. The river flows through the Black Warrior Basin, a region historically important for

and Nangeya Mountains. Streams from these mountains feed the river. The river flows through the Bari country to the east of Torit. Near to Tirangore the

The Shenzhen Reservoir also flows into the river when it is full. The river flows into Deep Bay (also known as Hau Hoi Wan and Shenzhen Bay). The Mai

Kangsha River. A branch of the river flows towards Kalmakanda and meets the Balia River. Another branch of the river flows into the haor areas of Sunamganj

Montana and northern Idaho in the watershed of the Columbia River. The river flows northwest through a long valley at the base of the Cabinet Mountains

discovered that the real source is a glacier higher in the mountains. The river flows south into the Douro river shortly after passing through the city of

the United States. Originating west of Bryce Canyon National Park, the river flows north through a chain of high farming valleys and steep canyons along

being only 1.2 miles (2 km) from the North Sea (to its eastern side) the river flows westwards for 9.9 miles (16 km) into the River Derwent at Haybridge

Service, where the stream is designated the Buffalo National River. The river flows through Newton, Searcy, Marion, and Baxter Counties, from west to east

Deransko Lake. Also, the Krupa is a unique river in Europe, because the river flows both ways. It flows normally from the source to the mouth and from

half-flooded forest country it traverses. For most of its length, the river flows through the Purus várzea ecoregion. This is surrounded by the Juruá-Purus

northeastern Knox County at the confluence of its North and South Forks, the river flows 90 miles (140 km) northeast across Baylor, Archer, Wichita, and Clay

Meldola, the river flows north near Bertinoro, Forlimpopoli, and Forlì before crossing the border into the province of Ravenna. The river flows northeast

in the Jotunheimen mountains of Norway's Jotunheim National Park. The river flows eastward through the Sjodalen valley and Heidal valley into the Gudbrandsdalslågen

The river flows near Verghereto and Bagno di Romagna as it winds through the mountains before entering Lago di Quarto. After leaving the lake, the river

is located east of the village of Lukino in Novoduginsky District. The river flows north, crosses into Sychyovsky District, and downstream of the town

the opposite side of the mouth of the Thelon River. Along its course the river flows through several lakes, including Ennadai Lake and Yathkyed Lake, over

Range of the Cariboo Mountains, west of the community of Valemount. The river flows generally south through the Shuswap Highland towards Kamloops where

Jägala and thence the Baltic Sea. Põhja-Kõrvemaa Nature Reserve, which the river flows through, is the third-largest nature reserve in Estonia, with an area

southern boundary of the Iytwelepenty / Davenport Range National Park and the river flows in a northerly direction through the park passing through a series

of Haryana, built on a raised plinth overlooking the Yamuna River. The river flows into the plains of Haryana after crossing over the last lap of the

Maksatikhinsky District, in the eastern outskirts of Valdai Hills. The river flows east, enters Bezhetsky District, turns north, flows through the town

part of the Liberia-Sierra Leone border. The districts through which the river flows include the Parrot's Beak area of Guinea, Liberia's Lofa County and

Cherokee/Milton) county line, and part of the more recent Milton city limit. The river flows generally from east to west, and divides the Woodstock area to the

the winter, hence the name. To the east is Winterborne Stickland and the river flows on to this village, eventually joining the River Stour. To the southwest

The source of the Sheksna is in the southeastern end of Lake Beloye. The river flows south and subsequently turns east. It joins the northern part of the

sub-group in the Monti Picentini, sub-range of the Apennine Mountains. The river flows first in the province of Avellino, and then in that of Benevento, before

the southern slope of the Volcan Mountains in San Diego County, and the river flows generally southwest for 23.8 miles (38.3 km), draining 346 square miles

part of Kesovogorsky District, close to the village of Puzyryovo. The river flows northeast and enters Sonkovsky District. In the selo of Pereterye it

bridge) spans the point where the bay begins and the Fox River ends, as the river flows south to north into the bay. Around mid-bay are Sturgeon Bay and the

Japan. The river has a drainage basin of 33,800 km2 (13,100 sq mi). The river flows in northeast Asia, on the border between China and North Korea in its

Mountains of East Kalimantan, which form a natural border with Sarawak. The river flows westwards through tropical rainforest to the South China Sea. The Baram

particularly popular with ornithologists, due to a rich variety of birds. The river flows through the Gbele Resource Centre from the west to the southeast. Wilks

of Haryana, built on a raised plinth overlooking the Yamuna River. The river flows into the plains of Haryana after crossing over the last lap of the

shores. In eastern Patagonia it is also the largest by flow rate. The river flows through the Argentine province of Río Negro which is named after it

drains a watershed approximately 1460 square miles (3,780 km²) in size. The river flows through the counties of Le Sueur, Rice, Dakota, and Goodhue. The Cannon

Tweed ranges and containing a catchment area of 1,055 km2 (407 sq mi). The river flows generally north east, joined by eight tributaries including the Oxley

west-central Maine. The East and West Outlets join at Indian Pond and the river flows southward. Harris Station Dam, the largest hydroelectric dam in the

Richmond Hill and Toronto in the Greater Toronto Area of Ontario, Canada. The river flows from the Oak Ridges Moraine to Lake Ontario at the eastern border of

flows then in south-west direction. The southern and final part of the river flows in a south-south-west direction following the eastern flank of Cordillera

of the Yarra Ranges within the Bunyip State Park, near Bunyip Gap. The river flows generally east then south, then west by south, then west, then south

Hualapai Peak at 8,417 feet (2,566 m) is the highest point in the basin. The river flows through the Arrastra Mountain Wilderness. The Big Sandy River flows

River is a river of South Sudan, a tributary of the Bahr al-Arab. The river flows through the Western Bahr el Ghazal, South Sudan. The average elevation

it forms a watershed that has an area of about 294 km2 (114 sq mi). The river flows into Joun Lake, which is part of the Bisri Dam project to improve the

The Big Blue River is the largest tributary of the Kansas River. The river flows for approximately 359 miles (578 km) from central Nebraska into Kansas

Pass. It flows into Lake Lugano at Lugano. On its way downstream, the river flows through the Val Colla valley before reaching the city centre of Lugano

River, which flows northwards along the east side of the village. The river flows north into Quebec, then turns west, passes the north end of the Green

was the boundary between ancient Pamphylia and Cilicia. From there, the river flows south over conglomerated strata for about 90 km, descending through

Falls. Near its mouth at Tautuku Bay, just north of Tautuku Peninsula, the river flows through the Tautuku Estuary, a breeding ground for fernbirds. The river's

and salt water crocodiles. The traditional owners of the area that the river flows through are the Ngarinjin, Miwa and Wilawila peoples. The first European

waters are still fresh at this point, before becoming brackish as the river flows onward toward its mouth in Belfast Lough. Stranmillis Road begins at

Wirral Peninsula to the west, and empties into Liverpool Bay. In total the river flows 69 miles (111 km). Part of the Mersey Railway, a rail tunnel between

drains the western portion of the depression. Leaving the depression the river flows southwards through the Ankara and Kelifely limestone plateaus in deep

Region at the Tangan port town of Pangani. For much of its length the river flows along the regional borders of Kilimanjaro Region and Manyara Region

name Mühltal ("Mill Valley, Mill Dale"), a district through which the river flows. Karl Ferdinand Abt (1903–1945) -Nazi politician Johann Konrad Dippel

River forms the western and northern boundary of the Zanskar Range. The river flows westwards, along with the Kargil-Zanaskar Road, from its source and

about 95 cubic metres per second (3,400 cu ft/s); at the point where the river flows into the Pianura Padana (Po River Plain), it amounts to about 25 cubic

of its upper course, it forms the border between Elis and Achaea. The river flows through the plain of Elis. The river passes through the following villages:

038 km2 (401 sq mi). Its source is near the village of Makov. At first, the river flows in northeastern direction, where it flows around Javorníky on the right

second (20,000 cu ft/s). While 80% of its drainage area is in Quebec, the river flows for a short distance through Ontario before it ends in Hannah Bay off

its northern end, the river flows almost immediately into the western end of Loch Beg. Then from Loch Beg's eastern end the river flows east/northeast across

Canada. Fed by the Illecillewaet Glacier in Glacier National Park, the river flows approximately 62 kilometres (39 mi) to the southwest, where it flows

at the Ashford-Union border, adjacent to Interstate 84. From here, the river flows south through Ashford, roughly paralleling Route 89, and passing under

Tudovka is in the swamps in the westernmost part of Oleninsky District. The river flows north and crosses into Nelidovsky District. The village of Tud is the

Cossatot begins in the Ouachita Mountains southeast of Mena, Arkansas. The river flows through the Ouachita National Forest and then in a generally southerly

Charles River, encompassing 76 square miles (200 km2) of watershed. The river flows from the Lower Mystic Lake and travels through East Boston, Chelsea

of Pali and Udaipur districts. Sukri river is its main tributary. The river flows in a north-west direction for about 96 km (60 mi), before joining Khari

between the province of Perugia and the province of Pesaro e Urbino. The river flows northeast through Pesaro e Urbino before forming the border between

Sumatra, Indonesia, about 900 km northwest of the capital Jakarta. The river flows from Lake Singkarak in West Sumatra eastward to the east coast of Sumatra

the lower Tana consisting of the section downstream of Kora where the river flows for ca. 700 km through semi-arid plains. Its tributaries include some

of the River Tyne, which it joins at Derwenthaugh near Gateshead. The river flows for 35 miles from its origin, where two streams, Beldon Burn and Nookton

the Marshyangdi River to the north of the Annapurna mountain range. The river flows to the east. To the west, the 5,416-metre (17,769 ft) Thorong La pass

begins in Porsea, Toba Regency near the southeast corner of Lake Toba. The river flows in a north-easterly direction, cutting through the upper course of

Apennine Mountains, southwest of Potenza in the province of Potenza. The river flows northeast near Pignola and Potenza before curving east near Vaglio

originates in the Sahyadris near Khatpewadi, north-west of Pune city. The river flows through the Bhugaon, Bhukum, Bavdhan, Pashan, Baner and Aundh areas

Alnmouth and Alnham. For part of its route, directly upstream of Alnwick, the river flows through Hulne Park. The meaning of the name Aln is uncertain, but it

the Garonne. From its source in the Pyrenees near El Pas de la Casa, the river flows north, forming part of the border with Andorra, and passing through

between Ternopil and Khmelnytskyi regions. As it was mentioned above, the river flows through the Podolia Upland sneaking past the Podolian hills also known