153 Sentences With "debouches" | Random Sentence Generator

He debouches in a laboratory where, in the necessary pitch-dark and silence, a young scientist sits watching deep space to catch, if he can, the invisible tremor of dark matter on the last, least particles that humans can observe.

What elevates this perfectly reasonable 224.99,226-mile northbound wander through Africa, from the trickle of the river's source in Rwanda to where it debouches by the grubby gravel of an Egyptian beach, is how Wood deals with the very lowest point of the trip, when one of his party falls desperately ill and dies.

The Smeerenburgbreen glacier debouches into the head of the fjord.

The glacier Recherchebreen debouches into the fjord from south, and Renardbreen from west.

Esmarkbreen debouches into Ymerbukta. Esmarkbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It is named after geologist Jens Esmark. The glacier has a length of 15 kilometers, and debouches into the bay Ymerbukta at the northern side of Isfjorden.

Borebukta is a bay in Oscar II Land at Spitsbergen, Svalbard. It is located at the northwestern side of Isfjorden, west of Bohemanflya, and has a width of about 4.5 kilometers. The glacier Borebreen debouches into the bay. Also the Nansenbreen glacier debouches into Borebukta.

The Birgi is a river in the Province of Trapani, which debouches in the Tyrrhenian Sea between Marsala and Trapani.

Ayerfjorden is the western branch of Raudfjorden in Albert I Land at Spitsbergen, Svalbard. The glacier Chauveaubreen debouches into the fjord.

Deltabreen (The Delta Glacier) is a glacier at Edgeøya, Svalbard. The glacier debouches into the lagoon of Tjuvfjordlaguna, at the eastern side of Dyrdalen.

The Río de Oro is a river of Chaco Province, Argentina. It is a tributary of the Paraguay River, which is debouches into near Humaitá, Paraguay.

The river Agardhelva debouches into the bay. The coastal plain Belemnittsletta is to the east of the bay. Inside of the bay is the inlet Båtbogen.

Grøndalselva is a river in Nordenskiöld Land at Spitsbergen, Svalbard. It flows from Grøndalspasset through the nineteen kilometer long valley of Grøndalen, and debouches into Grønfjorden.

Brageneset is an island at Nordaustlandet, Svalbard. It is located at the mouth of Wahlenbergfjorden. The ice cap Vestfonna has the glacier arm Bragebreen which debouches east of Brageneset, and another glacier arm, Gimlebreen debouches into Hinlopen Strait north of Brageneset. Brageneset was believed to be a headland until the summer of 2019, when the ice cap retreated far enough to reveal that it is actually an island.

Vaigattbogen is a bay at the eastern side of Spitsbergen, located between Ny- Friesland and Olav V Land, and opening into Hinlopen Strait. The glacier Hinlopenbreen debouches into Vaigattbogen.

Etonbreen is a glacier located on the west coast of Nordaustlandet, Svalbard. Etonbreen is a glacier on Nordaustlandet, Svalbard. The glacier debouches into Wahlenbergfjorden. It is named after Eton College.

The four largest rivers (the Amazon, the Ganges-Brahmaputra, the Yangtze and the Yellow) are responsible for 20% of the global discharge of sediment in to the oceans by debouches.

Sassenelva is a river flowing through Sassendalen in Sabine Land at Spitsbergen, Svalbard. The river feeds from the glacier Rabotbreen and side glaciers of Nordmannsfonna and Hellefonna, and debouches into Sassenfjorden.

Only familiar with Alpine glaciers, they had difficulty negotiating seracs and retired back at where the West Rongbuk Glacier debouches. Note: the glaciers have lowered and retreated considerably since that time.

Uvêrsbreen (Bad Weather Glacier) is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about 25 kilometers. The glacier debouches into Engelskbukta, after merging with Comfortlessbreen.

Femmilsjøen is a lake in Ny-Friesland at Spitsbergen, Svalbard. The glacier Longstaffbreen debouches into the lake at the eastern end. The western end of the lake is relatively close to Wijdefjorden.

Hinlopenbreen ("Hinlopen glacier") is a glacier stream in Spitsbergen, Svalbard. The glacier debouches into Vaigattbogen in Hinlopen Strait. The glacier has a length of about 70 km, and drains an area of about .

Yoldiabukta is a bay in Nordfjorden at Spitsbergen, Svalbard. It has a width of about and is located between the northern side of Bohemanflya and Muslingodden. The long glacier Wahlenbergbreen debouches into Yoldiabukta.

Ulvebreen is a glacier in Sabine Land at Spitsbergen, Svalbard. It is named after Arctic explorer Erik Andreas Ulve. The glacier is a tributary to Nordmannsfonna, and debouches into the bay of Dunérbukta.

Monacobreen as seen from Liefdefjord Monacobreen is a glacier in Haakon VII Land on Spitsbergen, Svalbard. The glacier debouches into Liefdefjorden. Former names of the glacier include Glacier de Monaco and Liefde Bay-bræ.

Brånevatnet ("Melting lake") is a lake at Nordaustlandet, Svalbard. It is located between Winsnesbreen and Oxfordhalvøya, to the north of Etonbreen. The river of Oxfordelva flows from Brånevatnet through Oxfordhalvøya and debouches into Bodleybukta.

Rijpbreen is a glacier in Gustav V Land at the northern side of Nordaustlandet, Svalbard. The glacier debouches into Bengtssenbukta, a western branch of Rijpfjorden. The glacier is named after Dutch explorer Jan Rijp.

Tjuvfjordlaguna is a lagoon at Edgeøya, Svalbard. It is located just inside the head of Tjuvfjorden, at the southeast side of the valley Dyrdalen, and northwest of Schneiderberget. The glacier Deltabreen debouches into the lagoon.

Renardbreen (The Fox Glacier) is a glacier in Wedel Jarlsberg Land at Spitsbergen, Svalbard. The glacier has a length of about . It is located between the ridges of Activekammen and Bohlinryggen, and debouches into Recherche Fjord.

Storbreen, Isskiltoppane, Bendefjellet, Flatbreen Storbreen ("The Large Glacier") is a glacier in Torell Land at Spitsbergen, Svalbard. It has a length of about fifteen kilometers, and debouches towards the bay of Brepollen, the inner part of Hornsund.

Hochstetterbreen is a glacier located in Olav V Land on Spitsbergen. Hochstetterbreen is a glacier in Olav V Land on Spitsbergen, Svalbard. It debouches into Hinlopen Strait. The glacier is named after Austrian geographer Ferdinand von Hochstetter.

Von Postbreen is a glacier stream in Sabine Land at Spitsbergen, Svalbard. The glacier is about fifteen kilometers long, and debouches into Tempelfjorden after merging with Tunabreen. It is named after Swedish geologist Hampus Adolf von Post.

Konowbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It is located between Carlsfjella and Konowryggen, and debouches into St. Jonsfjorden. The length of the glacier is 12 kilometers. The glacier is named after Wollert Konow.

Gaffelbreen () is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of seven kilometers, and debouches into St. Jonsfjorden, from the northern side. The upper part of the glacier is split into two branches.

Vegardbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about 5.5 kilometers, runs between Vegardfjella and Vittenburgfjella, and debouches into St. Jonsfjorden. The glacier is named after Norwegian physicist Lars Vegard.

Raudfjordbreen glacier front, Svalbard Raudfjordbreen is a glacier at Spitsbergen, Svalbard, on the divide between Albert I Land and Haakon VII Land. It has a length of 18 kilometers and debouches into Klinckowströmfjorden, the eastern branch of Raudfjorden.

Nordfjorden is a northern branch of the fjord Isfjorden at Spitsbergen, Svalbard. It is located between Bohemanneset and Kapp Thordsen, and branches further into the fjords Ekmanfjorden and Dicksonfjorden. The 30 kilometer long glacier Sveabreen debouches into the fjord.

Chauveaubreen is a glacier in Albert I Land at Spitsbergen, Svalbard. The glacier is located between Renaudfjellet and Marstranderfjellet, and debouches into Ayerfjorden, the western branch of Raudfjorden. It is named after French physician Henri Jean Charles Albert Chaveau.

"Siyin Reserved Forest (Approved)" , United States National Geospatial-Intelligence Agency. It is located about "Siyin, Myanmar" GeoNames.org west of Kalemyo on the Kalemyo - Theizang road. It lies at the mouth of the Siyin Valley where it debouches into the Kale Valley.

Charlesbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It is located between Gunnar Knudsenfjella and Vegardfjella, and debouches into St. Jonsfjorden from the south side. The length of the glacier is ten kilometers. The glacier is named after Charles Robertson.

The Cascade River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map , accessed May 7, 2012 river in northeastern Minnesota, United States. Running through Cook County, it debouches into Lake Superior between Grand Marais and Lutsen.

Longstaffbreen is a glacier in Ny-Friesland at Spitsbergen, Svalbard. It is a branch from the ice areas of Åsgardfonna and Valhallfonna, and the glacier debouches into the lake of Femmilsjøen. The glacier is named after Arctic explorer and mountaineer Tom George Longstaff.

Birpai were in possession of some of Mid North Coast land, from Gloucester eastwards to the where the Manning River debouches into the Pacific at Taree. They were mainly located north of the Manning, and on the Forbes, Hastings (Dhungang) and Wilson rivers.

Norman Tindale estimate Nimanburu tribal lands to extend over roughly from the King Sound coast, around Repulse Point southwards to the swamp plain where the Fraser River debouches into the sea. Their inland extension ran as far as the headwaters of that river.

The Sutlej and its tributary, the Buddha Nala, constitute the chief hydrographic features of the district. A brief description of these is as follows. ; Sutlej River: originates from Lake Manasarovar in Tibet. After flowing through Himachal Pradesh, it debouches from the Shivaliks.

Martinbreen is a glacier in Nathorst Land at Spitsbergen, Svalbard. It is named after Swedish botanist Anton Rolandsson Martin. The glacier has a length of about five kilometers. It is located between the ridges of Mjellegga and Breskarvet, and debouches into the valley of Davisdalen.

Osbornebreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of 21 kilometers, merges with the glaciers Devikbreen, Klampebreen and Vintervegen, and debouches into St. Jonsfjorden. The mountain ridge Goldschmidtfjella forms a six kilometer long nunatak in the glacier.

Vargsundet is a strait in Hammerfest Municipality in Troms og Finnmark county, Norway. It separates the island of Seiland from the mainland. Vargsundet opens up into Altafjorden to the southwest, and to Straumen to the northeast. The river Porsa debouches into the strait, from southeast.

Grøndalen is a valley in Nordenskiöld Land at Spitsbergen, Svalbard. It has a length of about 19 kilometers. The valley stretches westwards from the mountain pass Grøndalspasset, and debouches into Grønfjorden, at the eastern side of the fjord. The river Grøndalselva flows through the valley.

Vintervegen (Winter Road) is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about . The glacier borders to the mountain of Klampen, merges with Osbornebreen and other glaciers, and the merged glacier stream debouches into the head of St. Jonsfjorden.

Nathorst glacier, Svalbard, in midnight sun Nathorstbreen is a glacier located on the southern part of Spitsbergen, emptying into Van Keulenfjorden. Nathorstbreen is a glacier on Spitsbergen, Svalbard. It has a length of about , and debouches into Van Keulenfjorden. It has several side glaciers.

Usherbreen is a glacier in Sabine Land at Spitsbergen, Svalbard. It has a length of about 9.5 kilometers, and is located between Kroghfjellet and Domen. Usherbreen is a tributary glacier to Nordmannsfonna, and debouches towards Storfjorden. It is named after Scottish businessman Thomas Leslie Usher.

Braganzavågen is a bay located in the inner northern branch of Van Mijenfjorden, at Spitsbergen, Svalbard, within Heer Land and Nordenskiöld Land. The valley Kjellströmdalen debouches into the bay. The mining settlement Sveagruva is located at the western side of Braganzavågen, below the mountain Liljevalchfjellet.

Gipsdalen is a valley in Bünsow Land at Spitsbergen, Svalbard. It has a length of about 22 kilometers. The river Gipsdalselva flows through the valley and debouches into Gipsvika in Sassenfjorden. At the western side of the valley are Norströmfjellet, Meakinsfjellet, Grahamkammen, Usherfjellet and Gipshuken.

On the approach to Whitby, walkers pass under one of the most striking features of the walk, the Victorian Larpool Viaduct. Finally, the river debouches into the North Sea in Whitby's scenic harbour. A train can be caught back to the day's start point.

Flatbreen, Hornbreen, Storbreen Hornbreen ("Horn glacier") lies between Torell Land and Sørkapp Land on Spitsbergen, Svalbard. The glacier debouches into Hornsund. Former names of the glacier include Ramme Gletscher and Horn Glacier. Hornbreen has a length of about 15 km, and width of 8 km.

Flow rate is in winter and during summer. 41 small streams debouches into the lake, of those 21 originate in Torugart Range and 20 - in Atbashi Range. Negative water balance of the lake over the last decades causes the decline in the lake level.

Recherchebreen is a glacier in Wedel Jarlsberg Land at Spitsbergen, Svalbard. The glacier has a length of about . It is located in a valley between Martinfjella and Observatoriefjellet, and debouches into Recherche Fjord. Among its tributary glaciers are Foldnutfonna, Varderyggfonna, Dollfusbreen, Ramondbreen and Bjørnbreen.

In Norman Tindale's estimation the Wanjuru's tribal lands covered some , from an area south of where the Russell River debouches into the Coral Sea down to Cooper Point and Innisfail. Like the other rainforest dwellers in this area, the Kunja, their inland extension lay about Babinda.

Ymerbukta, with Värmlandryggen to the left Ymerbukta is a bay in Oscar II Land at Spitsbergen, Svalbard. The glacier Esmarkbreen debouches into the bay. It is about long, located at the northern side of Isfjorden. The bay is separated from Trygghamna by the mountain chain Värmlandryggen.

The Choita River in the monsoon season, from the Kharua Rajapur Bridge The Choita River () flows west and south of Kharua Rajapur. Choita River is a branch of Ichamati river. Choita River debouches into the Jamuna River in Gaighata. The length of the river is 40 km.

Bullbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about six kilometers, originates from Svartfjella, runs between Holmesletfjella and Bulltinden, and debouches into St. Jonsfjorden. The glacier is named after Norwegian military officer and politician Karl Sigwald Johannes Bull.

Klinckowströmfjorden is the eastern branch of Raudfjorden at Spitsbergen, Svalbard, on the divide between Albert I Land and Haakon VII Land. It is named after Swedish zoologist Axel Klinckowström. The glacier Raudfjordbreen debouches into the fjord. The peninsula Buchananhalvøya separates Klinckowströmfjorden from the western fjord branch Ayerfjorden.

Leaving the city-state the Lower Elbe then passes between Holstein and the Elbe-Weser Triangle with Stade until it flows into the North Sea at Cuxhaven. Near its mouth it passes the entrance to the Kiel Canal at Brunsbüttel before it debouches into the North Sea.

Tunabreen is a glacier stream at Spitsbergen, Svalbard. The glacier is about 23 kilometers long, and divides Sabine Land from Bünsow Land. It starts from Lomonosovfonna, flows southwards between the mountains of Langtunafjella and Ultunafjella, merges with Von Postbreen, and the combined glacier debouches into Tempelfjorden.

Bjørnfjorden (The Bear Fjord) is a fjord in Albert I Land at Spitsbergen, Svalbard. The fjord is located between Reuschhalvøya and Vasahalvøya, and is an inner branch of Smeerenburgfjorden. Smeerenburgbreen debouches into the fjord. At the south side of the fjord are Scheibukta and St. Laurentiusbukta.

Tinayrebreen Tinayrebreen is a glacier in Haakon VII Land at Spitsbergen, Svalbard. It has a length of about ten kilometers, and extends from the glacier cap of Isachsenfonna to Möllerfjorden, where it debouches into the bay of Tinayrebukta. The glacier is named after French painter Jean Paul Louis Tinayre.

Tinayrebukta is a bay in Haakon VII Land at Spitsbergen, Svalbard. It is located at the east side of Möllerfjorden, and is surrounded by the mountains of Fallièresfjella and Generalfjella. The glacier of Tinayrebreen debouches into the bay. The bay is named after French painter Jean Paul Louis Tinayre.

Eidembukta is a bay in Oscar II Land at Spitsbergen, Svalbard. It has a width of about 4.5 kilometers, and is located at the southeastern side of Forlandsundet. The glacier of Eidembreen debouches into the bay. The bay is named after Norwegian politician and naval officer Ole Thorenius Eidem.

Porsa is a river in the municipality of Hammerfest in Troms og Finnmark county, Norway. The river drains and area of and debouches into the strait of Vargsundet. Two hydroelectric power stations, Nedre and Øvre Porsa, are located in the river, with a total installed capacity of 15.3 MW.

Mittag-Lefflerbreen is a glacier at Spitsbergen, Svalbard. The glacier is located in Ny-Friesland, Dickson Land and Olav V Land, and debouches into Austfjorden. It is named after mathematician Gösta Mittag-Leffler. The lower, northern part of the glacier is included in the Indre Wijdefjorden National Park.

Aavatsmarkbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It is named after politician and military officer Ivar Aavatsmark. The glacier debouches into Forlandsundet, in the bay of Hornbækbukta. At the southern side of the glacier, between Aavatsmarkbreen and Kaffiøyra, is the mountain range of Prins Heinrichfjella.

Svenskebukta is a bay at the northern side of Kongsøya of Kong Karls Land, Svalbard. It is located between Kapp Oscar and eastwards towards a point west of Nordaustpynten. Former name variants of the bay are Holmbukta, and Swedish Yacht Club Bay. The glacier Rundisen debouches into the bay.

Mayerbreen is a glacier in Haakon VII Land at Spitsbergen, Svalbard. The glacier has a length of about twelve kilometers. It originates from Neubauerfjellet, and debouches into the bay of Mayerbukta in Möllerfjorden. The glacier is named after Louis Benoit Joseph Mayer, counsellor of Albert I, Prince of Monaco.

Aerial view of the Serpentine River within the Bering Land Bridge National Preserve Serpentine River is a waterway on the Seward Peninsula in the U.S. state of Alaska. It debouches at Shishmaref Inlet from the southeast. It was explored and named in 1900 by the prospector Charles McLennan.

The river debouches into the plains near Jholiapur. Much of the upper basin has poor soils and agriculture here is largely of wheat and gram. The lower basin has better soils and a flatter slope and has been used extensively bunded allowing for impounding water during the monsoons.

Colesdalen, with Colesbukta to the right Colesbukta is a bay at the southern side of Isfjorden, in Nordenskiöld Land at Spitsbergen, Svalbard. The bay is about 4.5 kilometer wide. A railway for coal transport was earlier operated between Grumantbyen and shipment facilities in Colesbukta. The valley Colesdalen debouches into Colesbukta.

Colesdalen is a valley in Nordenskiöld Land at Spitsbergen, Svalbard. The valley debouches into the bay Colesbukta, at the southern side of Isfjorden. Colesdalen is located north of the Nordenskiöld Land National Park, but not included in the park, due to mining interests. The Coleselva River flows through the valley.

Paulabreen debouches into Rindersbukta. Paulabreen is a glacier in Nathorst Land and Heer Land at Spitsbergen, Svalbard. It has a length of about fifteen kilometers, extending from the mountain of Kjølberget to the bay of Rindersbukta. The glacier is named after Paula, the wife of shipmaster Richard Ritter von Barry.

It has a natural drop of and water reserves of 90,000 kilowatts. It arises near the border with Sichuan Province at , flows northwest and debouches into the Han River at . The main branch of the Muma River is navigable by small boats as far south as the village of Matsung T'an.

Dunérbukta is a bay at the western shore of Storfjorden in Sabine Land at Spitsbergen, Svalbard. It is named after Swedish astronomer Nils Christoffer Dunér. The glacier of Ulvebreen debouches into the bay. At the northern side of the bay is the mountain of Domen and the ridge Kapp Johannesen.

Reindalen is a valley in Nordenskiöld Land at Spitsbergen, Svalbard. It has a length of about 38 kilometers. The valley stretches westwards from the mountain pass Reindalspasset, and debouches into Van Mijenfjorden, in the bay Kaldbukta at the northern side of the fjord. The river Reindalselva flows through the valley.

Kjellströmdalen is a valley at Spitsbergen, Svalbard. It has a length of about 27 kilometers, and forms the border between Nordenskiöld Land, Heer Land and Sabine Land. The valley is named after topographer Carl Johan Otto Kjellström. The valley debouches into Braganzavågen, a bay in the inner part of Van Mijenfjorden.

Løvliebreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about five kilometers, and is located between the mountain ranges of Gunnar Knudsenfjella and Holmesletfjella. The glacier debouches northwards towards St. Jonsfjorden. It is named after Norwegian businessperson Andreas Løvlie along with the nearby mountain of Løvliefjellet.

The fjord ranges from to wide throughout its course. The Beiar River debouches into the head of Beiar Fjord. The Beiar Fjord splits into several basins at some of the narrow sounds among which the innermost one is the largest. This area is a beautiful spot known to local boaters and tourists.

Lilliehöökbreen Lilliehöökbreen is a glacier complex in Albert I Land and Haakon VII Land at Spitsbergen, Svalbard. It has a length of about 22 kilometers. The glacier debouches into Lilliehöökfjorden, and calved icebergs may fill large parts of the fourteen kilometer long fjord. The glacier is named after Swedish commander Gustaf Bertil Lilliehöök.

Comfortlessbreen Comfortlessbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about fourteen kilometers, and a maximum width of three kilometers. The glacier debouches into Engelskbukta, after a merge with Uvêrsbreen. Comfortlessbreen is separated from Uvêrsbreen by the mountain range of Trondheimfjella (with Domkyrkja in the west).

Feather River is a stream, long, on the Seward Peninsula in the U.S. state of Alaska. Flowing west in the Nome mining district, it debouches a little north of Cape Woolley on the Bering Sea. Its creeks include Livingston, from the east; Thistle and Wills, from the north; and Johnston, from the east.

Mayerbukta is a bay in Haakon VII Land at Spitsbergen, Svalbard. It is located at the eastern side of Möllerfjorden, and has a width of about 1.5 kilometers. The glacier of Mayerbreen debouches into the bay. The bay is named after Louis Benoit Joseph Mayer, counsellor of Albert I, Prince of Monaco.

View of Eidembreen glacier from the southernmost coast of Oscar II Land. Eidembreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about eighteen kilometers, and debouches into Eidembukta in Forlandsundet, between St. Jonsfjorden and Isfjorden. The glacier is named after Norwegian politician and naval officer Ole Thorenius Eidem.

Bakaninbreen merges with Paulabreen before the combined glacier debouches into the bay of Rindersbukta. Bakaninbreen is a glacier in Heer Land at Spitsbergen, Svalbard. It has a length of about 9.5 kilometers, and merges with the glacier of Paulabreen. The glacier is named after a member of the Swedish-Russian Arc-of-Meridian Expedition.

RGO expedition to Spitzbergen: landing at Negribreen, 2014, watercolor on paper Negribreen is glacier at Spitsbergen, Svalbard. The glacier debouches into Storfjorden, in Olav V Land and Sabine Land, and forms a wide glacier front with the moving extreme point Kapp Antinori. The glacier covers an area of about . It is named after Italian geographer Christoforo Negri.

The Toce () is a river in Piedmont, Italy, which stretches the length of the Val d'Ossola from the Swiss border to Lake Maggiore into which it debouches near Fondotoce in the commune of Verbania. The river is long and is formed in the upper Val Formazza by the confluence of a number of torrents in the plain of Riale.

Veteranen (The Veteran) is a glacier in Ny-Friesland at Spitsbergen, Svalbard. It has a length of about 25 kilometers and a width of up to five kilometers. The glacier debouches into Lomfjorden, and is connected with Kvitbreen at the other side of Trebrepasset. The name of the glacier was suggested by Adolf Erik Nordenskiöld in 1863.

Devikbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It is located between Devikfjellet and Krymlefjellet to the north/west, and Tispa, Kvelpane and Klampen to the south/east. Devikbreen merges with several other glaciers, including Osbornebreen, Klampebreen, and Vintervegen, and the merged glacier debouches into St. Jonsfjorden. The length of the glacier is six kilometers.

De Geerdalen is named after Swedish geologist Gerard De Geer De Geerdalen is a valley in Nordenskiöld Land at Spitsbergen, Svalbard. It is named after Swedish geologist and Arctic explorer Gerard De Geer. The mountain pass of Kreklingpasset divides De Geerdalen from Helvetiadalen. The river of De Geerelva flows through the valley, and debouches into Sassenfjorden at Elveneset.

Hayesbreen is a glacier in Sabine Land at Spitsbergen, Svalbard. It is named after American politician and Arctic explorer Isaac Israel Hayes. The glacier has a length of about eighteen kilometers, and debouches into the bay of Mohnbukta. Surrounding mountains are Aagaardfjellet to the north, Jebensfjellet to the south, and Panofskyfjellet where Hayesbreen joins the glacier of Königsbergbreen.

Semmeldalselva is a river in Nordenskiöld Land at Spitsbergen, Svalbard. The river flows through the valley of Semmeldalen, and has a length of about fifteen kilometers. It starts as a continuation of Isbjørnelva where this river joins with a river from Skiferdalen. Semmeldalselva debouches into the bay of Kaldbukta, at the northern side of Van Mijenfjorden.

Oxfordhalvøya is a peninsula in Wahlenbergfjorden at the southwestern side of Nordaustlandet, Svalbard. It is located between Bodleybukta and Etonbreen at the head of the fjord. The bay Kløverbladbukta cuts into the peninsula, and its highest point is Carfaxhaugen at 103 m.a.s.l. The river of Oxfordelva flows from the lake of Brånevatnet through Oxfordhalvøya, and debouches into Bodleybukta.

Lilliehöökfjorden. Lilliehöökfjorden is a 14 kilometer long fjord branch of Krossfjorden in Albert I Land at the northwestern side of Spitsbergen, Svalbard. The fjord is named after Gustaf Bertil Lilliehöök. Lilliehöökfjorden is separated from Möllerfjorden by the 12 kilometer long mountain ridge Kong Haakons Halvøy. The Lilliehöökbreen glacier debouches into the fjord, and calved ice may fill large parts of the fjord.

View of Rishikesh from the beach Rishikesh is at . It has an average elevation of . The town is located in the Tehri Garhwal region of the northern Indian state of Uttarakhand. After flowing 249 km (155.343 mi) through its narrow Himalayan valley, the Ganges emerges from the mountains at Rishikesh, then debouches onto the Gangetic Plain at the pilgrimage town of Haridwar.

It is part of the upper region of the Bear River watershed. Bear River drains into the Feather River, which joins the Sacramento River, which finally debouches into San Francisco Bay. The larger part of the Banner Mountain area in the southern part of its tract is drained by Wolf Creek. From Grass Valley, it runs south without larger tributaries.

Mud Slough debouches into the San Francisco Bay near the site of the ghost town of Drawbridge. Its proximity to the bay means its marshy end is affected by tidal action. It goes from freshwater, to brackish to saline. The slough passes the salt evaporation ponds made by the Leslie Salt Company, where it joins the larger Coyote Creek and the bay.

Ytterdalen and Fritjovbreen Fridtjovbreen is a glacier in Nordenskiöld Land at Spitsbergen, Svalbard. It has a length of about 14 kilometers, and debouches into the bay Fridtjovhamna at the northern side of Van Mijenfjorden. The name stems from a hunting vessel used during the Torell expedition to Spitsbergen. The lower part of the glacier is included in the Nordenskiöld Land National Park.

Oxfordelva ("Oxford river") is a river at Nordaustlandet, Svalbard. The river flows from the lake of Brånevatnet through the peninsula of Oxfordhalvøya, and debouches into Bodleybukta, a bay in Wahlenbergfjorden. The river is named after Oxfordhalvøya (the Oxford Peninsula), which was named by George Binney, leader of the Merton College Arctic Expedition of 1923 and the Oxford University Arctic Expedition of 1924.

It was named after the English missionary William Duncan. The Duncan Canal Portage is a popular hiking trail across the northern end of the Lindenberg Peninsula. It originally provided access to the northern end of the Duncan Canal directly from Frederick Sound. Butterworth Island is located at the mouth of the Duncan Canal where it debouches into the Sumner Strait past the larger Woewodski Island.

Xaintrailles covered the left wing, with the divisions of Souham and Legrand, 18,000 men in all. This wing spread in the direction of the Rhine, where Souham's force covered Frickthal and Basel, between the Aare and Hüningen, and Legrand's brigade held Altbreisach and Kehl, and observed the debouches from the Black Forest. A division of heavy cavalry reserve also occupied Basel.Shadwell, pp 49-51.

The river runs in a westerly direction, enters Cameroon, then Nigeria and finally debouches into the Niger River system. The Léré Lake has a length of with a width of . The Tréné Lake has a length of and width of . The Touboiris marsh and Loké marsh are close to the headwaters of the Mayo-Kébbi River which is a plain area but outside the limits of the reserve.

Map of rivers of West Bengal It debouches into the plains in Jalpaiguri district and then flows through Cooch Behar district in West Bengal. The Raidak confluences with the Brahmaputra at chainage 327 km in Kurigram District in Bangladesh, where it is sometimes referred to Dudhkumar River. The total length of the main river is but along with its tributaries, it covers a length of nearly in Bhutan alone.

River des Peres enters underground culverts from north of Forest Park, emerges south of the park into concrete channels, and debouches into the Mississippi. An artificial water flow that emulates the river was created through Forest Park, using the city's water supply. This is often mistakenly considered a re-creation of the original River des Peres. However, the water flow here is deliberately produced, not derived from rainfall, or runoff, etc.

The Dvararvati Sila is a type of Sila or coral stone obtained from the Gomati river (Gomti River) in Dvaraka. Dvaraka is located in the Jamnagar District of Gujarat at the mouth of the Gomati River as it debouches into the Gulf of Kutch. The city lies in the westernmost part of India. In ancient Sanskrit literature Dvaraka was called Dvarawati and was rated as one of the seven most prehistoric cities in the country.

Bakırçay (Latin name: Caicus, also Caecus; , transliterated as Kaïkos; formerly Astraeus (Ἀστραῖος) is the current name of a river of Asia Minor that rises in the Temnus mountains and flows through Lydia, Mysia, and Aeolis before it debouches into the Elaitic Gulf.Herodotus. The Histories. vi. 28; vii. 42.Hazlitt. Classical Gazetteer To the Hittites, it may have been the Seha river, however the modern Gediz river further south is a more likely candidate.

It leaves this valley as a mountain torrent and debouches in a broad, gravel-filled valley, part of the depression already described, which extends along the southern margin of the Kigluaik Mountains. It flows south for to Norton Sound at the Bering Sea. The mouth of the river is about southeast of Nome. The elevation of Nome River at Dexter Creek is less than , which allows the river below that point an average grade of .

Mill Creek rises in Montgomery County, Pennsylvania; runs southeasterly to West Philadelphia, where it enters 19th-century sewer pipes; and debouches roughly five miles later in the Schuylkill River near The Woodlands Cemetery. It starts near Narbeth, where its source is buried, then runs free for a mile or so before entering Philadelphia at the Overbrook station. The creek, which drains about , gave its name to a neighborhood in Philadelphia that it flows under.

Much of its importance is because it is the place where the road from Kashmir debouches into the Indus Valley.Rizvi (1996), p. 31. Close by are the remains of an old fortified customs house.Rizvi (1996), p. 96. There is a fragmentary inscription at Khalatse which carries the name 'Maharaja Uvima' which is attributed to the Kushan king, Vima Kadphises who ruled in the 1st or early 2nd century CE.Stein, R. A. (1972).

Chilkoot River flows from the lake for a short length and debouches into the Lutak Channel at the head of the Chilkoot inlet near Haines. Chilkoot village, a settlement of Chilkoot Indians existed at the outlet of the lake, which was called Tschilkut or Tananel or Chilcoot; the lake is named after this village. This village is now a camping area developed by the State Parks and Outdoor Recreation Division of the Alaska Department of Natural Resources.

The same process of hydropower expansion is also planned for many of the free-flowing rivers of the Balkans including Morača, where the Cem debouches. In Montenegro, the river is ranked as one of the cleanest rivers in the country. As in Albania, before the 1990s, the part nearest to the border was heavily militarized and no activity was allowed in its vicinity. The municipality of Podgorica declared the river canyon a "natural monument" in 2017.

The Manas River (Pron: ˈmʌnəs) is a transboundary river in the Himalayan foothills between southern Bhutan and India. It is named after Manasa, the serpent god in Hindu mythology. It is the largest river system of Bhutan, among its four major river systems; the other three are Amo Chu or Torsa, Wong Chu or Raidak, and Mo Chu or Sankosh. It is met by three other major streams before it again debouches into India in western Assam.

Collinsville is a rural unincorporated community in Solano County, California, USA. It is located at the mouth of the Sacramento River, on the north side of the river where it debouches into the Suisun Bay. Collinsville is effectively separated from the more intense urban development in Contra Costa County immediately across the river, as no bridge exists connecting the two areas. The area was once proposed for a major chemical plant of the Dow Chemical Company in the 1980s.

Formerly, a primitive wagon road threaded its way through the lower Canyon, but most traces of this are long gone. Prominent named crags and caves along this section include Indian House Cave (mile 10.1), Castle Rock (mile 11.3), Blue Rock (mile 16.2), and Bulls Head (mile 16.6), just below which is Peacock Cave (mile 16.6). About 3 miles on (mile 20.7), the river debouches from the Canyon. After another half mile, the South Branch collects the North Fork South Branch just below Cabins.

One of the first bird ringing stations in Europe was opened there in 1929 by a Lithuanian zoologist, Tadas Ivanauskas. Birds ringed at the Cape have been found migrating to Iran, Egypt and even to the Republic of South Africa. Mammals found in the delta include fox, beaver, elk, wild boar and otter. Another of the delta's special features is Lake Krokų Lanka (near where the Nemunas debouches), which formed when the river's outwash separated it from the Curonian Lagoon.

In his classic survey of Australian tribes, Norman Tindale assigned their modern territory to the Djinang people. He writes that the Yan-nhaŋu (Nango) were indigenous to the Wessel Islands east of Brown Strait (from Jirrgari island to Cape Wessel), Galiwin'ku/Elcho Island and Drysdale Island. Their territory also encompassed the Cunningham Islands. With regard to the Crocodile Islands group, Tindale designated Mooroonga and Yabooma as Yan- nhaŋu, adding that they were also present at Banyan Island, where the Woolen River debouches.

The city is located at where the Coatzacoalcos River debouches into the Bay of Campeche. Overland it is connected by road and rail to the Pacific Ocean about away. This location has prompted plans for an interoceanic waterway across the Isthmus of Tehuantepec, or for a much expanded railroad system, for over a century. The city had a 2005 census population of 234,174, making it the third-largest city in the state after Veracruz and Xalapa, but first in metropolitan population.

View of the Macta marshes The river Macta is in Algeria. The Macta is only long and, enters the sea in the Gulf of Arzeu, some west of the mouth of the Chelif. It is formed by the Habra ( long) and the Sig ( long), which rise in the Amour Range and flowing north before uniting in a marshy plain, from whence the Macta debouches. At the Battle of Macta fought on 28 June 1835, Berber warriors defeated a French colonial army.

Important landmarks in the area are the Pandaran Beach at the mouth of the Sampit River, the Orchid Park of Pembuangan Hulu and hunting park of Kotawaringin at the border. ;Pandaran Beach This beach is located towards the sea side at the mouth of Sampat River. It is developed as a park. Its uniqueness lies in the fact that a river debouches into the sea on its northern side while the Java Sea provides a wide expanse of water on its southern side.

The Berg River (also called Great Berg River or in Afrikaans: Bergrivier) is a river located just north of Cape Town in the Western Cape Province of South Africa. It is approximately 294 km (183 mi) long with a catchment area of 7,715 km² (2979 mi²) and debouches into the Atlantic Ocean. About 65% of the Berg River area is under agriculture. The major towns in the Berg River area are Velddrif and Laaiplek near the coast, Piketberg, Hopefield, Moorreesburg and Darling further inland.

The Manas River (Pron: ˈmʌnəs; in Bhutan Drangme Chhu; in China NiamjangTopomap ) is a transboundary river in the Himalayan foothills between southern Bhutan and India. It is named after Manasa, the serpent god in Hindu mythology. It is the largest river system of Bhutan, among its four major river systems; the other three are Amo Chu or Torsa river, Wong Chu or Raidak, Puna Tshang Chu or Sankosh. It is met by three other major streams before it again debouches into India in western Assam.

Lingga () is a small coastal fishing town, in Sri Aman Division, Sarawak, Malaysia, near where the Lupar River (Batang Lupar) debouches into the sea. Commercial activities is limited to seventeen small stores in the town, all of which are run by local Chinese merchants. The population of Lingga has stagnated, the lack of job opportunities has caused significant exodus of local population to more developed towns for better livelihood. Lingga is also popularly known as "Crocodile Town" for numerous sightings of crocodile in the nearby river.

The Grue is a torrent in north-west Italy, a right tributary of the Scrivia, whose course lies entirely within the Province of Alessandria, Piedmont. The river’s source is at Bocchetta del Barillaro, at an elevation of close to the watershed with the Val Borbera. The river follows a tortuous course through the Ligurian Apennines, and between the hills of Tortona, before entering the Po plain at Viguzzolo. From here its path is straighter and it debouches into the Scrivia near Castelnuovo Scrivia at above sea level.

After a course of inside Santiago del Estero, the river reaches the Santa Fe Province as Salado del Norte ("Northern Salty") to finally join the Paraná River in that province, being the last important tributary to the Paraná. The more abundant rainfall in Santa Fe Province causes the Salado's discharge to increase. During rainy summers, the river can overflow its riverbed producing floods. A 2003 flood severely affected the city of Santa Fe. The Salado debouches into the Paraná River southeast of Santa Fe City, in a flooding area with lagoons.

Stancomb-Wills Glacier is a large glacier that debouches into eastern Weddell Sea southward of Lyddan Island. The glacier was discovered in the course of the U.S. Navy LC-130 plane flight over the coast on November 5, 1967, and was plotted by United States Geological Survey (USGS) from photographs obtained at that time. The name was applied by the Advisory Committee on Antarctic Names (US-ACAN) in 1969. The Stancomb-Wills Glacier Tongue () is the extensive seaward projection of the Stancomb-Wills Glacier into the eastern Weddell Sea.

Djerimanga country consisted of some on the coastal plain where the Adelaide River debouches into the Timor Sea, north to the tip of Cape Hotham, west to Fog Dam, south to an area including the community at Acacia Larrakia and eastwards as far as the Mary River floodplains. Humpty Doo Station, Koolpinyah Station and Djukbinj National Park are also situated within these traditional boundaries. Historically, the Djerimanga had a southern inland extension of their land as far as the Margaret River and the Ringwood Range, but lost it to the eastern Djowei.

These drop 500 ft direct from the summit ridge into the valley below. The eastern end of the fell connects to Hopegill Head without any great loss of height, while the western end of the ridge descends steeply over Whiteside End to the Vale of Lorton. The subsidiary top of Whin Ben (1,355 ft) stands at the south west corner, overlooking the point where Gasgale Gill debouches into the fields of Lanthwaite. The northern slopes are much more extensive with two long ridges being thrown out from the main mass of the fell.

Lourmarin is located in the French region of Provence, at the foot of the Luberon Massif where a southern pass debouches over the Luberon from Apt on the northern side of the Luberon. The pass divides the Grand Luberon from the Petit Luberon range, an area rich in Neolithic remains and noted for its dramatic massifs and rockscapes. The Aigues Brun brook comes out of the pass and runs just to the west of the village (Aigue is a Provençal language word for "water", coming from Latin aqua).

The Kiwalik River flows on the north side of Seward Peninsula. Its origin is in a low ridge that divides the Kiwalik catchment, flows for a length of about in a northerly direction, and finally debouches into Spafarief Bay; this bay protrudes from the Kotzebue Sound in a southeasterly direction. Its traverse further lower down for stretch of , through the flat lowland areas, is through a wide expanse of many miles; the river, however, has a narrow stretch of about in river stretch of a few miles, upstream of Candle. Beyond the Candle, it forms into a lagoon.

Oddly enough, since the construction of the Manapouri power station, there has been about five MW of tide- determined generation. The tailrace tunnel exit by Dusky Sound debouches at sea level, and thus the effective head of the power station is affected by the level of the tide there. If the turbines are operated at a fixed flow aperture, the power produced is not constant but follows the tide, an effect that can be seen in the following graph. Note that the timing follows the tides around the clock, not the usual twenty-four cycle of electricity usage.

Before heading that way, Mallory and Bullock started to investigate the place where, unknown to them, the East Rongbuk glacier debouches. They had to curtail their exploration here because bad news came that the photographs Mallory had taken were all useless because he had been putting the photographic plates in back to front. Photographs were vital as part of the reconnaissance so for two days Mallory and Bullock raced around retaking as many as possible. On this occasion Mallory re-took his photographs from "Island Peak" and Bullock actually reached the Lho La and was able to photograph the Khumbu Icefall.

Across the street (Krakowskie Przedmieście) from the University, in Holy Cross Church, a 1936 plaque by Prus's nephew Stanisław Jackowski, featuring Prus's profile, is dedicated to the memory of the "great writer and teacher of the nation." On the front of Warsaw's present-day ulica Wilcza 12, the site of Prus's last home, is a plaque commemorating the earlier, now-nonexistent building's most famous resident. A few hundred meters from there, ulica Bolesława Prusa (Bolesław Prus Street) debouches into the southeast corner of Warsaw's Triple Cross Square. In this square stands St. Alexander's Church, where Prus's funeral was held.

The Bara Shigri glacier attracted much attention for many years because of the valuable antimony deposits found there. The glacier was first surveyed in 1906 by H. Walker and E.H. Pascoe of the Geological Survey of India. In 1955, the Geological Survey of India sponsored an expedition to this glacier as part of the Indian programme for the International Geophysical Year 1956–57, when a number of Himalayan glaciers were examined and their snout position fixed. The Bara Shigri glacier flows northwards and debouches into the Chenab River where its southerly course is deflected westwards, close to the Spiti border.

After flowing for through its narrow Himalayan valley, the Ganga emerges from the mountains at Rishikesh, then debouches onto the Gangetic Plain at the pilgrimage town of Haridwar. At Haridwar, a dam diverts some of its waters into the Ganges Canal, which irrigates the Doab region of Uttar Pradesh, whereas the river, whose course has been roughly southwest until this point, now begins to flow southeast through the plains of northern India. The Ganga river follows a arching course passing through the cities of Kannauj, Farukhabad, and Kanpur. Along the way it is joined by the Ramganga, which contributes an average annual flow of about to the river.

Denman Glacier is a glacier wide, descending north some , which debouches into the Shackleton Ice Shelf east of David Island, Queen Mary Land. It was discovered in November 1912 by the Western Base party of the Australasian Antarctic Expedition under Sir Douglas Mawson. Mawson named the glacier for Lord Denman, Governor-General of Australia in 1911, a patron of the expedition. The canyon under Denman Glacier has been found by BedMachine Antarctica project (under the leadership of the University of California, Irvine) to be the deepest natural location on land (or at least not under liquid water) worldwide, with the bedrock being below sea level.

It debouches in to the Pacific after dropping over a height of over in its short stretch of from the source and thus having a river gradient of 3.6% (close to a highway gradient). It has several tributaries which have their origin in the western cordillera. Moquegua Valley in Peru. The river basin is bounded on the north by the Tambo River basin, which is a sub-basin of the Vizcachas River; on the east and south, with the Locumba River basin; and on the west by the Pacific Ocean and the region between Moquegua and Tambo, formed by a series of short and medium streams.

Grays Ferry, also known as Gray's Ferry, is a neighborhood in South Philadelphia bounded (roughly) by 25th Street on the east, the Schuylkill River on the west, Vare Avenue on the south, and Grays Ferry Avenue on the north.Official 1968 map of Grays Ferry Redevelopment Area The section of this neighborhood west of 34th Street is also known as Forgotten Bottom.The Forgotten Bottom Remembered: Stories From a Philadelphia Neighborhood. (2002) Grays Ferry shares borders with Southwest Center City to the North, Point Breeze to the East, and Girard Estate to the South. Gray’s Ferry is across from where Mill Creek debouches at about 43rd street.

Jaldhaka River in Kalimpong district The Jaldhaka River (Pron:/ˌdʒælˈdɑːkə/) (), also known as Dichu River in earlier times, is a trans-boundary river with a length of 192 kilometres that originates from the Kupup or Bitang Lake in southeastern Sikkim in the eastern Himalayas and flows through Bhutan and the Kalimpong, Jalpaiguri and Cooch Behar districts of West Bengal, India. At that point the river enters Bangladesh through the Lalmonirhat District and then joins with the Dharla River until the Dharla debouches into the Brahmaputra River near the Kurigram District. Due to the river's wandering over several international borders, only a small length of the river lies within Bangladesh.

Lumaha‘i Beach at the mouth of the river The Lumaha'i River rises in the central mountains of Kauai at an elevation of . It drains a catchment area of . After flowing through a narrow valley with cliff banks, it opens out midway along its course into a wide valley, where the banks of the river are steep. The river debouches into the Pacific Ocean on the northwestern coast of the island, just east of Wainiha, on the western edge of Lumaha'i Beach. The beach at the western end, formed at the mouth of the river, is called the Lumaha‘i Beach which is located to the northwest of Hanalei.

Besides these, the Kandi region is full of seasonal streams. It falls into two nearly equal portions of hill and plain country. Its eastern face consists of the westward slope of the Solar Singhi Hills; parallel with that ridge, a line of lower heights belonging to the Siwalik Range traverses the district from south to north, while between the two chains stretches a valley of uneven width, known as the Jaswan Dun. Its upper portion is crossed by the Sohan torrent, while the Sutlej sweeps into its lower end through a break in the hills, and flows in a southerly direction until it turns the flank of the central range, and debouches westwards upon the plains.

As the Ravi flows past Lahore in Pakistan ( below Amritsar in India) it is called "The river of Lahore" since that city is on its eastern bank. After passing through Lahore the river takes a turn at Kamalia and then debouches into the Chenab River, south of the town of Ahmadpur Sial. On its western bank is the town of Shahdara Bagh with the tomb of Jahangir and the Tomb of Noor Jahan. ;Change of river course According to satellite imagery studies carried out over a period of 20 years (between 1972–1973 and 1991–1993), the river coursing along the India–Pakistan border meanders substantially in the alluvial plains of the Amritsar, pathankot and Gurdaspur districts of Punjab.

The culminating clause was a two-pronged northern campaign which would end in the seizure of the North China Plain and the reestablishment of the Han dynasty. One advance would be from Yi Province in the west, north through the Qin Mountains, which debouches into the Wei River valley and achieving a strategic position in the west from which to dominate the great bend of the Yellow River and the Guanzhong region. The second advance would be from Jing Province north toward Luoyang, the old imperial capital of the Han dynasty, and the surrounding plains. Such a campaign would presumably occur at an opportune moment of destabilisation of Cao Cao's regime but that moment was not specified.

Paschal Glacier () is a glacier about 20 nautical miles (37 km) long and 4 nautical miles (7 km) wide, draining northwest between two ridges, the terminal points of which are Mount McCoy and Lewis Bluff. The lower end of this glacier merges with the flow of White Glacier and the larger Land Glacier near Mount McCoy before the latter feature debouches into Land Bay on the coast of Marie Byrd Land. Paschal Glacier was photographed from aircraft of the United States Antarctic Service (USAS), 1939–41, and was mapped by United States Geological Survey (USGS) from surveys and U.S. Navy aerial photography, 1959–65. Named by Advisory Committee on Antarctic Names (US-ACAN) for Evans W. Paschal, Scientific Leader at Byrd Station, 1970.

The river next passes under Route 108 at the site of the former "Singing Bridge", a metal bridge which was recently replaced. The river then debouches into Great Bay, a broad and shallow tidal estuary, just south of the mouth of the Lamprey River, arriving at the bay from Newmarket. The Squamscott, also spelled Swampscott and Swamscott, gets its name from the Squamscott Indians who called it Msquam-s-kook (or Msquamskek) translated as 'at the salmon place' or 'big water place.' Plentiful game, the marshes and lush river-fed vegetation, and an abundance of fish supported the northeast Native American Indians who were present in the region for thousands of years until English settlers displaced them in the early 17th century.

Adams Glacier (), also known as John Quincy Adams Glacier, is a broad channel glacier in Wilkes Land, Antarctica which is over long. It debouches into the head of Vincennes Bay, just east of Hatch Islands. It was first mapped in 1955 by G.D. Blodgett from aerial photographs taken by U.S. Navy Operation Highjump (1947), and it was named by the Advisory Committee on Antarctic Names (US- ACAN) for John Quincy Adams, sixth President of the United States. Adams was instrumental while later serving as U.S. representative from Massachusetts in gaining congressional authorization of the United States Exploring Expedition (1838–42) under Lieutenant Charles Wilkes, and perpetuating the compilation and publication of the large number of scientific reports based on the work of this expedition.

Joining Russo-Turkish War of 1877–1878, he usually fought under Iosif Gurko, who led the spearhead of the Russian invasion, took Tarnovo on July 7, crossed the Balkans by the Haim Boaz pass—which debouches near Hainkyoi—and, despite considerable resistance, captured Uflani, Maglizh and Kazanlak; on July 18 he participated attack on Shipka, which was evacuated by the Turks the following day. He returned to Caucasus after Treaty of Berlin and received awards for his bravery and participation. He was transferred to the Life Guards Cossack Regiment of His Majesty with rank of cornet on April 21, 1879. He served as from 1890 to 1895 Rittmeister of the army cavalry and as adjutant to commander of Caucasus Military District.

"The first operations of field engineering were, necessarily, the securing of our debouches to the other shore and establishing of a strong point to strengthen our hold of Alexandria. The works required for these limited objects (though being really little towards constructing a defensive line) were nevertheless, considering the small number of troops available, arduous undertakings."U.S., War Department, The War of the Rebellion: A Compilation of the Official Records of the Union and Confederate Armies, (Washington, DC: The Government Printing Office, 1880–1901), Series I, Volume 5, pp. 678-679 In the seven weeks that followed the occupation of Arlington and the beginning of work on Fort Corcoran, Barnard and his engineers were forced to focus virtually all of their effort on Corcoran and Runyon, owing to the limited resources available.

Tank locomotive, built around 1907 for service on the Bolān Pass railway From Sibi the line runs south-west, skirting the hills to Rindli, and originally followed the course of the Bolān stream to its head on the plateau. The destructive action of floods, however, led to the abandonment of this alignment, and the railway now follows the Mashkaf valley (which debouches into the plains close to Sibi), and is carried from near the head of the Mashkaf to a junction with the Bolān at Machh. An alternative route from Sibi to Quetta was found in the Harnai valley to the N.E. of Sibi, the line starting in exactly the opposite direction to that of the Bolān and entering the hills at Nari. The Harnai route, although longer, is the one adopted for all ordinary traffic, the Bolān loop being reserved for emergencies.