99 Sentences With "headstreams" | Random Sentence Generator

The entities they set up, in Hong Kong and the Cayman Islands, with names such as Headstreams Investment and Tang Dynasty Development, soon gained control over a large stake in the HNA Group.

HNA holds 1.2 trillion yuan ($180.4 billion) worth of assets, according to the company's latest filings, and Bhise said he had previously held approximately a 12.5 percent stake in HNA as the beneficial shareholder of Headstreams Investment Co, a Hong Kong registered firm.

The catchment areas of the Murg headstreams and its tributary, the Schönmünzach, have an area flow rate of 50 l/s.km2, the highest in Baden-Württemberg.

The district is entirely located in the Bavarian Forest. It is named after the Regen river and its two headstreams, the Black Regen and the White Regen.

On the western slopes of the Weißtannenhöhe rise numerous springs for the Ödenbach, one of the main headstreams of the Ravenna which flows through the well known Ravenna Gorge.

The West Morava originates in the Tašti field, east of the town of Požega, from the Golijska Moravica and Đetinja headstreams. Đetinja receives from the left its main tributary, the Skrapež. Less than a kilometer after the confluence, it meets the Golijska Moravica flowing from the south, forming the West Morava. Given the proximity of the confluences of Đetinja, Skrapež and Golijska Moravica, some sources consider all three rivers to be direct headstreams of the West Morava River.

It lies entirely within the Austrian state of Vorarlberg and includes the upper reaches of the river Lech with its headstreams in a horseshoe shape as well as the Upper Großwalsertal valley.

Seebach is a river of Thuringia, Germany. The Seebach is formed as the confluence of the two headstreams Mühlbach and Wilder Graben, southeast of Niederdorla. It discharges into the Unstrut in the village Seebach.

Bayreuth lies on the Red Main river, the southern of the two headstreams of the River Main, between the Fichtelgebirge Mountains and Franconian Switzerland. The town is also part of the Nuremberg Metropolitan Region.

Kelchsauer Ache is a river of Tyrol, Austria. The source of the Kelchsauer Ache is the confluence of its two headstreams, the and the near . It discharges into the Brixentaler Ache at Hopfgarten im Brixental.

The Billbach is a right-hand tributary of the Mud in Bavaria's Odenwald forest. It begins at the confluence of the Marsbach and Morre west of Schneeberg. Both headstreams rise in the state of Baden-Württemberg.

The district is located in the mountains of the Upper Palatine Forest (Oberpfälzer Wald). The two headstreams of the River Naab, the Waldnaab and Haidenaab, both run through the district to merge in the south of the area.

After the confluence of its headstreams, the Billbach crosses under the B 47 and flows through Amorbach. At the northwestern edge of the town it empties into the 25-kilometre-long Mud at the start of the B 469.

The district, surrounding the ancient city of Kulmbach, is located on the southern edge of Franconian Forest (Frankenwald) and Fichtelgebirge. The two headstreams of the Main River, White Main and Red Main, meet in the centre of the district.

Kulmbach is located in the middle of the Bavarian province of Upper Franconia, about northwest of the city of Bayreuth. To the south of Kulmbach, the River Main begins at the confluence of its headstreams, the White Main and Red Main.

The Gundia river is a tributary of the Kumaradhara river which in turn flows into the Netravathi. The Gundia's headstreams include the Yettinahole, Kerihole, Hongadahalla and Bettakumbri streams and the river basin straddles the districts of Dakshina Kannada and Hassan.

Gänsbach is a creek in Hesse, Germany. It is about 4.5 kilometres long and one of the headstreams of the Merkenfritzerbach (the other is the Mühlbach river). However, some people consider the Gänsbach creek to be the upper part of the Mühlbach river.

Mühlbach is a creek of Hesse, Germany. It is about 5 kilometres long and one of the headstreams of the Merkenfritzerbach (the other being the Gänsbach). Some consider the Gänsbach being the upper part of the Merkenfritzerbach and thus the Mühlbach a tributary.

The Porečka River ( / Porečka reka, "Poreč River") is a river in eastern Serbia, a 50 km-long right tributary to the Danube in the Đerdap gorge. It originates from two headstreams, the Šaška and the Crnajka rivers, which meet at the village of Miloševa Kula.

Line 17 is known for its artistic elements embedded into its stations. Due to the proximity of the line to various cultural and scenic attractions, specifically the ancient water town of Zhujiajiao and Dianshan Lake, the line's theme is water towns and headstreams of Shanghai.

Villingen-Schwenningen lies on the eastern edge of the Black Forest about above sea level. The source of the River Neckar is in Schwenningen (Schwenninger Moos) whereas Villingen is traversed by the river Brigach which is the longer one of the two headstreams of the Danube.

The Geiselbach is a right tributary of the Kahl in the northern Spessart in Bavaria and Hesse, Germany. It is 5,2 km (3,2 mi) long and begins at the confluence of multiple headstreams in Geiselbach. The largest tributary is the Omersbach. It discharges near the Teufelsmühle ("Devil's Mill").

The water supplies a plant located in Porompat. It is one of the headstreams of the Manipur River. The Iril River still has a large population of endangered indigenous fish called ngaton, Meitei sareng. These fish are captured by local fisherman in the months of July and August.

The Werse rises in the Beckum Hills near Beckum from three headstreams: the Lippbach, Kollenbach and Siechenbach. The name Werse is used from the Osttor and above the Kollenbach. From Beckum the Werse flows westwards. Shortly before Ahlen it turns northwest and, near Drensteinfurt, then via Albersloh it flows northwards.

After the confluence of its headstreams, the Warme Bode flows over the waterfall of the Unterer Bodefall towards Braunlage. There it is joined by the Ulrichswasser. It continues in the direction of Sorge. From the state border with Saxony-Anhalt it runs parallel to the B 242 federal road to Tanne.

The parish is in the barony of Tulla Upper and contains the villages of Scarriff and Tomgraney. It is and covers . The parish is rugged, with heights ranging from above sea level. It contains the Scariff river from its headstreams through Lough O'Grady to its mouth in Scarriff bay, Lough Derg.

The river's total length, including its headstreams, the Great Regen and Black Regen, is . The Little Regen crosses the Frauenau Reservoir. The Regen Valley forms the main valley crossing the Bavarian Forest; many settlements within the mountains are located along the river. Cities along the Regen river include Cham and Regensburg.

The Rzav (, ) is a river in western Serbia and eastern Bosnia and Herzegovina. The 72 km long right tributary to the Drina river, it originates from two headstreams, the Crni Rzav and the Beli Rzav. The river is sometimes referred to as the Zlatiborski Rzav (Serbian Cyrillic: Златиборски Рзав; "Rzav of Zlatibor").

Bhagirathi River at Gangotri. Devprayag, confluence of Alaknanda (right) and Bhagirathi (left) some rivers, beginning of the Ganges proper. Himalayan headwaters of the Ganges River in the Garhwal region of Uttarakhand, India. The headstreams and rivers are labelled in italics; the heights of the mountains, lakes, and towns are displayed in parentheses in metres.

The region is characterized by loess deposits from the ice age. On the plains there are virtually no woods. These are to be found exclusively on the valley slopes of the rivers (the Mulde and its headstreams, the Freiberger and Zwickauer Mulde). The Central Saxon Loess Hill Country is of great importance for agriculture, e.g.

The Zorge discharges into the Helme northeast of Heringen. The headstreams of the Zorge, like other streams such as the Wieda, drain one of the rainiest regions of the Harz. The quantities of water it carries to the Helme are one of the reasons for the construction of the Kelbra Reservoir on the Helme.

There was also enough water at first for the water wheels of the ironworks; when eventually the available water finally became insufficient, they promptly drove channels from the highest headstreams of the Main and the Steinach, and diverted the water. One example was the Bocksgraben. A thriving iron industry rapidly developed. Iron ore was processed in the royal foundry.

One kilometre away to the north-northeast is its smaller brother, the Kleiner Finsterberg or Finsterberger Köpfchen (). Two less spectacular eastern subpeaks, 2 to 3 kilometres distant both bear the name Rosenkopf ( and ). To the west, northwest and north the Finsterberg is bounded by the Freibach and, to the southeast, by the Taubach, both headstreams of the Ilm.

The Steinhuder Meerbach is the natural tailstream of Lake Steinhude. Its channel flow significantly exceeds the inflow of above-ground headstreams of the lake. It leaves the lake at its northwestern end and then flows west through the Meerbruch nature reserve and the village of Rehburg. It then swings northwards and empties, after , into the Weser at Nienburg.

Before it was renaturalised its upper course acted as a drainage ditch for the former raised bog, now afforrested, in the narrow valley (nature reserve).Nature reserve "Valley of the Kleine Örtze" with overview map On the headstreams of the Landwehrbach lies the Faßberg Air Base (north of Schmarbeck) and numerous old kieselgur pits (either side of the Sothrieth).

According to other sources, the Lommatzscher Pflege and the so-called Oschatz Hill Country (Oschatzer Hügelland) - the latter only referred to in specialist literature - may be included. The most important rivers in the Central Saxon Hills are the Mulde with its two headstreams, the Freiberger Mulde and Zwickauer Mulde. The largest towns are Döbeln and Grimma.

Then it meets the Kiến Giang River, and together they form the Nhật Lệ River. The Nhật Lệ River flows generally northeastwards before emptying into South China Sea at Đồng Hới. The Long Đại River used to cause flooding in the rainy season (from September to December). However, the severe flooding has been prevented thanks to the dam at its headstreams.

The Rzav () is a river in southwestern Serbia. The 62 km long left tributary to the Golijska Moravica river, it originates from two headstreams, the Veliki Rzav and the Mali Rzav. The river is sometimes referred to as the Golijski Rzav (Serbian Cyrillic: Голијски Рзав, "Rzav of Golija") to distinguish it from another Rzav river in Serbia, the Rzav of Zlatibor.

The Enz is a river flowing north from the Black Forest to the Neckar in Baden- Württemberg. It is 106 km long. Its headstreams – the Little Enz () and the Great Enz or Big Enz (Große Enz) – rise in the Northern Black Forest, the latter at Enzklösterle. In Calmbach, the Little Enz and the Big Enz join to form the Enz.

The You River has two headstreams, the north and south sources. The north source, the Beihe River () is the main stream; it originates in the Qizimei Mountains () in Xuan'en County of Hubei. The south source, commonly named Meijiang River () or Xiushan River () originates in Shanyangxi () of Songtao County, Guizhou. The Meijiang River merges into the main stream at Liangjiangkou () of Shiti Town () in Xiushan County of Chongqing.

The Krems is the backbone of the wine region of Kremstal, it passes Senftenberg and the ruins of Lengenfeld, and after emerging from the granite and gneiss plateau (part of the Bohemian Massif), it flows through the Tulln Basin near Krems. Beneath the castle Burg Hartenstein, at the confluence of the headstreams, is the Gudenus cave by the riverbank, which was inhabited in the Stone Age.

The Lauter (in its upper course also: Wieslauter) is a river in Germany and France. The Lauter is a left tributary of the Rhine. Its length is , of which 39 km is in France and on the France–Germany border. It is formed by the confluence of two headstreams (Scheidbach and Wartenbach) north of Hinterweidenthal in the Palatine Forest in the German state of Rhineland- Palatinate.

Retrieved August 14, 2013. is the official headstream of the Yangtze, and flows from the glaciers of the Gar Kangri and the Geladandong Massifs in the Tanggula Mountains of southwestern Qinghai to the confluence with the Dangqu River to form the Tongtian River. In Mongolian, this section of the river known as the Ulaan Mörön or the "Red River." The Tuotuo is one of three main headstreams of the Yangtze.

The Alaknanda is a Himalayan river in the Indian state of Uttarakhand and one of the two headstreams of the Ganges, the major river of Northern India and the holy river of Hinduism. In hydrology, the Alaknanda is considered the source stream of the Ganges on account of its greater length and discharge; however, in Hindu mythology and culture, the other headstream, the Bhagirathi, is considered the source stream.

The Lugomir originates from two headstreams, the Dulenska reka and the Županjevačka reka. The shorter headstream of Županjevačka reka (Cyrillic: Жупањевачка река) originates from the mountain of Gledićke planine in southern Šumadija region of central Serbia. Its spring is just some 500 m away from the source of Lugomir's another headstream, the Dulenska reka. The river first flows to the east, next to the villages of Nadrlje, Županjevac, Dragovo and Belušić.

Solotvyn, parish church (Catholic, today Greek Catholic) before 1939 Solotvyn (, ) is an urban-type settlement in Bohorodchany Raion of Ivano-Frankivsk Oblast, 40 km from Ivano-Frankivsk. Population: . Solotvyn is situated on the Bystrytsia of Solotvyn (the left of the two long headstreams of the Bystrytsia River, which, in turn, is a tributary of the Dniester), at the foot of the Carpathian Mountains. In the seventeenth century it was named Krasnopil.

Krumme Lutter is a river of Lower Saxony, Germany. The Krumme Lutter is one of the two headstreams of the Lutter in the southern Harz, north of Bad Lauterberg in the district of Göttingen. It rises below 620 m on the Aschentalshalbe and flows towards the south past the former pits WolkenhügelGrube Wolkenhügel bei karstwanderweg.de and Hoher Trost, before it unites with the Grade Lutter in Kupferhütte to become the Lutter.

The Kafni Glacier is located in the upper reaches of the Kumaon Himalayas, to the southeast of Nanda Devi. The glacier gives rise to the Kafni River, which is a tributary of the Pindar River. The Pinder River is a tributary to Alaknanda River, which eventually is one of the two headstreams of the Ganges. This is relatively small glacier but a popular trekking destination along with Pindari Glacier.

The Lachsbach is formed by the merger of its headstreams, the Sebnitz (left, about half the size) and Polenz (right, rather longer) in the Elbe Sandstone Mountains near Porschdorf. The combined confluence section of the two rivers was first recorded in 1543 as die beyde wasser ("the two waters"), a description no longer common today. After only , the Lachsbach empties into the Elbe above Prossen's winter port near Wendischfähre.

A typical Central Upland siepen/siefen Siepen, Siefen, Seifen or Seipen are typical regional words used in northwestern Germany for what are often narrow, wet, ravine-like V-shaped valleys of the German Central Uplands with their small headstreams. In the south German region, such valley forms are usually called Klingen. These words often form a part of placenames especially in the area from the centralz. B. in Herne, vergl.

These headstreams were traditionally called Gießer by the locals. One stream formed from the waters of several of these springs, whose water was clean enough for supplying the growing city, was called the Brunnenbach ("Spring Stream"). The stream was diverted into the city and fed many public wells and private water systems in Augsburg via a water works and water towers. Today, drinking water is no longer extracted from the Brunnenbach.

Amongst the rivers and streams of the Dinkelberg are the Löhrgraben, which flows into the Wiese near , the Bachtelengraben, which empties into the Rhine near Schwörstadt-Unterdorf, the Dürrenbach, which discharges into the Rhine at Rheinfelden and the Hagenbacher Bach and the Waidbach, the headstreams of the Großbach (also called the Warmbach), which also flows into the Rhine, at Rheinfelden-Warmbach. Amongst its lakes belongs the Eichener See near Schopfheim-Eichen.

Near Grassau the Tiroler Achen reaches the Alpine Foreland. The Tiroler Achen finally discharges into the lake of Chiemsee and, thence via the river Alz, belongs to the right-hand river system of the Inn, and the Danube, whose waters eventually reach the Black Sea. Its main tributaries, apart from its headstreams, are the Kitzbühler, Fieberbrunner and , shortly before Kössen the from Reit im Winkl, and in Kössen the and from the lake of Walchsee.

Myitkyina (, ; (Eng; mitchinar) Jinghpaw: Myitkyina, ) is the capital city of Kachin State in Myanmar (Burma), located from Yangon, and from Mandalay. In Burmese it means "near the big river", and Myitkyina is on the west bank of the Ayeyarwady River, just below from Myit-son (Burmese for confluence) of its two headstreams (the Mali and N'mai rivers). It is the northernmost river port and railway terminus in Myanmar. The city is served by Myitkyina Airport.

The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The main fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell, followed by the lower Lank Rigg group. Kirk Fell sits squarely at the head of Wasdale, rising between the main headstreams of Mosedale and Lingmell Becks. From this direction it appears as a truncated cone, steep sided with a wide level top.

The surrounding area has leached, gravelly-sandy soils with layers of hardpan, covered by open sand, large areas of heathland and extensive coniferous forest. The heathland is grazed by a variety of moorland sheep, known as the Heidschnucke. The Wilseder Berg lies on a watershed, from which several headstreams emerge, such as those of the Este, Luhe, Wümme and Böhme. Some of these streams feed the river system of the Weser, others flow eventually into the Elbe.

The Harle (in its upper course: Norder Tief) is a river of Lower Saxony, Germany, in the district of Wittmund in East Frisia. Its entire course is within the borough of Wittmund and it discharges near Harlesiel through a Siel, a sluice in the dyke, into the North Sea. Near the village of Willen two headstreams Nordertief and Südertief join forming the Harle. Both tributaries are streams that originate in bogland depressions in the neighbouring borough of Aurich.

The southern part of the municipality is less mountainous, but some single fjells (tunturi, which means hills towering above the timber line) rise above the otherwise rather flat surrounding area. Below, a part of the Pallastunturi–Ounastunturi-massif extends into Enontekiö's territory. A little more than 5% of the municipality's area consists of water. Several large rivers originate in Enontekiö: The Muonionjoki, Ounasjoki, Ivalojoki, and one of the headstreams of the Tenojoki have their sources in the municipality.

South of Kulmbach, near Steinenhausen Castle, it is united with the White Main, which rises in the Fichtelgebirge mountains near Bischofsgrün. The Red Main is long (source to mouth), the White Main . At the confluence of the two headstreams a bridge was built in 2009 where the young Main may be crossed right at its beginning. Information boards on the bridge describe the rest of the river's course, the local walking and cycle routes and the surrounding countryside.

Fichtelberg lies on the southeastern slopes of the Ochsenkopf, the second highest summit of the Fichtelgebirge mountains, and the most populous place in the Fichtelgebirge Nature Park. Fichtelberg lies on a major European watershed. Two rivers rise above the suburb of Neubau, the White Main, one of the two headstreams of the Main, which flows westwards to the Rhine, and the Fichtelnaab, which flows south and enters the Danube. Since 1857 Fichtelberg has belonged to the Bavarian provinces of Upper Franconia.

The Toutle River Sediment Retention Structure was built by the U.S. Army Corps of Engineers on the river in 1989 to prevent this sediment from traveling downstream and clogging the shipping channel of the Columbia River. The upper part of the North Fork Toutle River watershed was redirected to the crater of Mount St. Helens itself until 1982. The river's headstreams begin on a volcanic ash deposit roughly long and deep, which is the source of much of the excess sediment.

Previously these headstreams combined with regular heavy rainfall to cause flooding, so that in the 1940s work began to build dykes around the lake. In the period 1941-1945 foreign forced labour was used for this on a large scale. The reclamation and subsequent lack of annual flooding resulted in algae growing in large quantities in the lake and hence depriving most other organisms of oxygen. The low water level was caused by heavy silting, also a result of dyking the lake.

The reservoir collects the water on the eastern slopes of the rainy main crest of the Northern Black Forest, below the mountains of Hornisgrinde, Mehliskopf and Badener Höhe. The Schwarzenbach and Seebach streams are directly impounded, the water of the Biberach and Hundsbach (headstreams of the Raumünzach) are led by galleries from neighbouring valleys. In addition, the water of the Murg from the Murg Dam is pumped into the reservoir. The dam system provides load balancing in the energy supply.

Although many small streams comprise the headwaters of the Ganga, the six longest and their five confluences are considered sacred. The six headstreams are the Alaknanda, Dhauliganga, Nandakini, Pindar, Mandakini and Bhagirathi. Their confluences, known as the Panch Prayag, are all along the Alaknanda. They are, in downstream order, Vishnuprayag, where the Dhauliganga joins the Alaknanda; Nandprayag, where the Nandakini joins; Karnaprayag, where the Pindar joins; Rudraprayag, where the Mandakini joins; and finally, Devprayag, where the Bhagirathi joins the Alaknanda to form the Ganges.

Tos- Bulak is the area of open fields and mineral springs which lies immediately south of Kyzyl. Kyzyl stands at the point where the Yenisei River meets the Maly Yenisey River to form the (Улуг-Хем). Most development takes place south of the river and follows the curves of the river, with the highest development centered where the two headstreams of the Yenisei, the Bii-Khem (), and the Kaa-Khem (), meet. A monument was built in 1964 on the river bank to mark this.

Depot Creek flows west and northwest to join the Chilliwack River and, ultimately, the Fraser River, which flows into the Pacific Ocean in British Columbia. On the south side of Spickard are some headstreams of Perry Creek, which flows east to Little Beaver Creek and, via Ross Lake, the Skagit River. To the north Silver Lake Glacier sends meltwater into Silver Lake. Meltwater streams from glaciers on the east side of Mount Spickard join the outflow, Silver Creek, which flows east from Silver Lake to Ross Lake.

The Auerberg is a mountain about in the Rosalia Mountains in Lower Austria. It lies northeast of the Hochwolkersdorf hamlet of Hollerberg and southwest of the Forchtenstein hamlet of Rosalienhäuser. Only about 200 metres east of the summit is the border with Burgenland, where there is a 699-metre-high saddle across which the federal road from Hochwolkersdorf to Forchtenstein runs. To the northeast on the terrain of Forchtenstein is the head of the Heidbach valley and to the north, south and east rise the headstreams of the Ofenbach.

The Bhāgīrathī (Pron:/ˌbʌgɪˈɹɑːθɪ/) is a turbulent Himalayan river in the Indian state of Uttarakhand, and one of the two headstreams (or source) of the Ganges, the major river of Northern India and considered holy in Hinduism. In Hindu faith and culture, the Bhagirathi is considered the source stream of the Ganges. However, in hydrology, the other headstream, Alaknanda, is considered the source stream on account of its great length and discharge. The Ganga is the most important river of India both from the point of view of its basin and cultural significance.

From the confluence of its two headstreams (Rechtmurg and Rotmurg) in Baiersbronn- Obertal to its mouth on the Rhine the Murg is 72.350 km (~ 72.4 km) long. Together with the Rotmurg which rises at the Rotmurgbrunnen near Ruhestein it is 79.661 km (~ 79.7 km) long and together with the Rechtmurg which begins on the Schliffkopf at the Murgursprung and has a length of 7.881 km it is 80.231 km (~ 80.2 km) long. The catchment of the Murg covers 617 km2. In relation to its catchment the Murg has a high volumetric flow (18.4 m³/s).

The headstreams in the valley do not carry water all year round; but have nonetheless carved out the V-shaped valley. In the post-glacial period the quantities of water flowing out of the Central Uplands were greater, so that the streams were able to cut down more strongly into the terrain than they are today. The Meersiepen in the Burgholz State Forest esat of the Wupper The word also refers to the wet meadow valleys which result, with their steep hillsides. The name of the Siebengebirge hills may possibly have the root Siepen.

Tugaloo was one of the Chickamauga Cherokee "Lower Towns", the principal one being Keowee. The terms "Lower Towns" and "Lower Cherokee" were given by the English colonists to refer to the Cherokee who lived on the Keowee River, Tugaloo River, and other headstreams of the Savannah River. The terms correspond in general with the Eastern Dialect of Cherokee, which was originally spoken by what the English called the Lower Cherokee in the region of the Lower Towns. Gen. James Moore ordered an expedition into the lower Cherokee towns in 1715.

The Erlenbach has a main source and a rather smaller subsidiary source, which are only a few hundred metres from one another on the eastern flank of the 445-metre-high Löffelsberg. They are located in the Wasgau, which comprises the southern part of the Palatinate Forest and the adjoining northern part of the French Vosges Mountains. Initially the stream flows eastwards passing through the parish of Oberschlettenbach, its two headstreams meeting after 2 km, the smaller brook emptying from the right into the bigger one. The combined Erlenbach swings south and passes the villages of Vorderweidenthal and Erlenbach.

The river rises from several short headstreams in southern McLean County that arise from a glacial moraine southeast of Bloomington- Normal, Illinois. Part of the moraine is publicly owned as the Moraine View State Recreation Area. The river's course forms a large arc through central Illinois, first flowing east into Champaign County, Illinois, south through Mahomet, then west through Monticello and Decatur, then turning northwest to flow along the north side of Springfield. It receives Salt Creek at , approximately north-northwest of Springfield; then the river turns west, forming the southern boundary of Mason County with Menard and Cass counties.

It is bisected by the Schwarzbach and Moosalb rivers. To the southwest other ridges separate the valleys of the Merzalbe and the headstreams of the Wieslauter. It is therefore possible to walk from Neustadt an der Weinstraße to Leimen or Kaiserslautern- Mölschbach without dropping below the 450 metre contour line. North of the line from Hochspeyerbach to Speyerbach the highest points are the 570.8 m high Drachenfels and the Hoher Stoppelkopf (Stoppelkopf; 566.2 m). In the triangle formed by the Isenach to the north and German Wine Route to the east are other hills over 500 metres in height.

The Cheyyeru is formed by the confluence of the rivers Bahuda and Puncha that originate in the Chittoor district of Andhra Pradesh. The two streams join at Rayavaram to form the Cheyyeru which then flows for 87 km before joining the Pennar as a right bank tributary at Gundlamada in the Sidhout taluk of Cuddapah district, draining a total area of 7,325 km2. The Gunjana river is a tributary of the Cheyyeru and along the Gunjana valley several paleolithic settlements have been discovered. There are several gorges on the river including one after the confluence of its headstreams and the Balarajupalle gorge.

The Perlenbach, in East Belgium called the Schwalmbach, is formed from several headstreams and tributaries, most of which rise on Belgian soil in the Elsenborn Training Area near Rocherath in the Province of Liège. There, where it is still called the Schwalmbach, it comes together from the Rinnsaler Schwalmbach, Krockesbach, Kranbach, Drosbach, Lienbach, Büllingerbach (or Fuhrstbach), the Wolfsbach and the Heisterbach. From its confluence with the Heisterbach it is then known as the Perlenbach. It flows northwards, is impounded by the Perlenbach Dam and discharges into the Rur in Germany, west of the town of Monschau in North Rhine-Westphalia.

The Salzachgeier () is a rugged peak on the edge of the Kitzbühel Alps on the border of the Austrian states of Salzburg and Tyrol. In the cirques and high alpine meadows (Hochalmen) of its eastern slopes and the two neighbouring peaks of Fünfmandling (2,401 m) and Schwebenkopf (2,354 m) are the headstreams of the Salzach, the largest river north of the Salzburg Central Alps. The Salzachgeier has a double summit where five sharp ridges run together. The eastern summit is only three metres lower and towers immediately above the two aforementioned source regions (the Salzachboden and Schwebenalm).

The Murg valley is one of the largest and deepest valleys in the Black Forest (up to over 700 metres deep) and generally runs in a northerly direction. It separates the precipitation-rich main crest of the Northern Black Forest, including the Hornisgrinde (1,164 m), to the west, from the densely forested bunter sandstone plateaux in the east. The Murg originates from 2 large headstreams in the western part of the municipality of Baiersbronn. Below the Schliffkopf at about , the main headstream of the Right Murg (Rechtmurg) is formed by the Schurbach stream and Tränkenteich pond, a little above the Murgursprung ("Murg Source").

The other, left-hand headstream is the Red Murg (Rotmurg), whose source is the Red Murg Spring (Rotmurgbrunnen, also 915 m) which leaves the pass summit of Ruhestein (915 m) and is fed by brooks such as the Finsterbächle and Muckenbächle. From the confluence of its two headstreams at about 595 m the Murg flows southeast through the valley of Mitteltal to Baiersbronn, where it swings into line with the Forbach which joins from the south. From here it is followed by the B 462 and the Murg Valley Railway. Initially it runs northeastwards to Klosterreichenbach, but thereafter it heads north-northwest.

Gradient and course of the Mehner Bach The source region of the Mehner Bach consists of two stream runs and lies in the Wiehen Hills. The eastern headstream rises not far from the summit of the Kahle Wart near the boundary with the parish of Hüllhorst, the western one in an area that is known as Gerliethe. Both headstreams merge 300 metres south of the village of Obermehnen. The Mehner Bach then flows generally north-northwest through the Lübbecke Loessland, through the two villages of Obermehnen and Untermehnen, then through Blasheim and Eikel and finally through the Hollwinkel Wood.

At village Banovo Polje two major headstreams, Jovača and Prekopac, meet and from that point the river is called Zasavica. Near the village of Zasavica, the river enters the marshy area of the Zasavica bog where the 50–60 metres wide stream spreads to almost 300 meters and gets 2 metres deep, and meanders through the middle of it until it flows into the Sava at Mačvanska Mitrovica, right across the town of Sremska Mitrovica on the Sava. The final section is channeled (Bogaz canal) and the river often floods the surrounding area. The name of the river could be translated as the “behind Sava”.

There are two options for the northern course of the Palatine Watershed, depending on whether the confluence of the Nahe at Bingen is counted as part of the Upper Rhine or is seen as belonging to the Middle Rhine. If the former is assumed, it runs south of the catchment area of the Nahe; if the latter, it runs to the east of it. South of Kaiserslautern the western branch of the watershed runs below the Hohenecken Castle. In the first, more usually accepted case, the watershed is identical with that of the Schwarzbach and its headstreams (especially the Moosalb, Rodalb, Wallhalb and Hornbach) with the Nahe tributary of the Glan.

The Brexbach is formed by the uniting of the Hinterster Bach and Vorderster Bach in the Grenzhausen municipal forest east of Höhr-Grenzhausen. Many consider the Hinterster Bach simply as the name for the upper reaches of the Brexbach. From the confluence of its two headstreams by some fish ponds, the Brexbach initially runs along the upper edge of the municipality of Höhr-Grenzhausen. In the upper Brexbach valley there was once a mustard mill (Senfmühle), which burned down in 1914 - a memorial stone marks the spot - and other mills: the Farbmühle, Niesmühle and the Kühnsmühle, none of which are used as mills any longer.

Gomukh, "Mouth of a Cow", the pout of the glacier along the river Gomukh, also known as "Gaumukh" or "Gomukhi" (Hindi: गौमुख or गौमुखी ; Assamese and Bengali: গোমুখ or গোমুখী), is the terminus or pout of the Gangotri Glacier and the source of the Bhagirathi River, one of the primary headstreams of the Ganges River. The place is situated at a height of 13,200 ft (4,023 m) in Uttarkashi district in the state of Uttarakhand, India. It is one of the largest in the Himalayas with an estimated volume of over 27 cubic kilometers. It is a holy Hindu pilgrimage site, along with Gangotri, as well as trekking destination.

Shortly before Hammereisenbach-Bregenbach, the Breg is joined by the Linach just below the Linach Dam and, in the village, by the Hammerbach, a short tributary, but the most important thanks to its two large headstreams. Near Bräunlingen, the Breg meets the Röthenbach stream at the Kirnbergsee. Here the Breg leaves the Black Forest and continues via Hüfingen to Donaueschingen, through wide, open countryside on the plateau of the Baar. After 46.2 kilometres, the Breg merges with the Brigach in Donaueschingen to form the Danube - "Brigach und Breg bringen die Donau zuweg" ("Brigach and Breg bring the Danube together") as the well known rhyme goes.

The Lopau rises with two headstreams from the ponds known as the Süderteichen and the Westerteichen in the Westergrund in the Munster North Training Area, near the abandoned village of Lopau, that lies within the borough of Munster. In its upper reaches the Lopau flows through uncultivated grassland, which is becoming increasingly afforested by alders and invaded by the wooded area of the Raubkammer. In Bockum, a village in the municipality of Rehlingen in Lüneburg District, it picks up the Ehlbeck, a left-hand tributary. East of Amelinghausen the river is impounded by a dam by the B 209 federal road to create the tourist lake of Lopausee.

The Main flows through the north and north-west of the state of Bavaria then across southern Hesse; against the latter it demarcates a third state, Baden-Württemberg, east and west of Wertheim am Main, the northernmost town of that state. The upper end of its basin opposes that of the Danube where the watershed is recognised by natural biologists, sea salinity studies (and hydrology science more broadly) as the European Watershed. The Main begins near Kulmbach in Franconia at the joining of its two headstreams, the Red Main (Roter Main) and the White Main (Weißer Main). The Red Main originates in the Franconian Jura mountain range, in length, and runs through Creussen and Bayreuth.

The Enz bears its name without any qualifier until it reaches the town of Calmbach, where the Great Enz (Große Enz) and Little Enz (Kleine Enz) merge. The Great Enz has two headstreams, both approximately 5 kilometres long: the Poppelbach and the Kaltenbach, which unite at Gompelscheuer. As with the source of the Danube in Donaueschingen this purely nominal beginning of the (Great) Enz is symbolized by the nearby Enz Spring (Enzbrunnen) and, likewise, has been erroneously marketed as such to tourists. In terms of water quantity and size of catchment area, the Poppelbach, which flows from the south, is the main headstream, whilst the Kaltenbach, which flows from the west, has a slightly greater length and higher source.

The headstreams of the upper reaches of the Rotbach, known as the Zartenbach, begin on the territory of Hinterzarten (Southern Black Forest Nature Park) southwest of the village of Oberzarten on the eastern mountainside of the Ramselehöhe (1,111,9 m) at about 1,085 metres above sea level. They gather on the bottom of a valley basin with a stepped longitudinal profile that was formed by an ice age glacier. On one of the levels the stream is impounded to form the pond of Mathisleweiher (). Thereafter it flows in a broad left-hand arc around the Windeck (1,209 m) and passes through Oberzarten and Hinterzarten northwards in the broad hollow of the level Hinterzarten Moor (nature reserve).

The fertile loess soils in this region of north Germany are dissected by a host of brooks and headstreams, which used to flow in marshy V-shaped valleys. Not all Sieke are or were, however, crossed by a stream, but at the very least they always consisted of wet ground. During the course of medieval and early modern cultural and agricultural history, people developed these natural landforms by cutting into the edges of the V-shaped valleys (so-called Wiesenbrechen by Wiskenmaker Adolf Schüttler: Das Ravensberger Land. Aschendorff, Münster 1995, S. 13, ) and turning them into trough and box valleys, and any streams were regulated such that they ran in straight beds along the edges of such a box valley.

At from its source to the sea, the Arun is the longest of the rivers flowing entirely within Sussex. It rises as a series of streams, known locally as ghylls or gills, to the east of Horsham, in St Leonard's Forest. It flows westwards, along the southern boundary of Horsham and turns briefly to the north to skirt Broadbridge Heath. Continuing westwards, it is joined by the North River, which is also known as the River Oke, whose headstreams are the heights of Leith Hill and Holmbury Hill in Surrey. After the junction, it passes under the A29 road, which follows the route of the Roman Stane Street at this point, and timber piles of a Roman bridge have been found in the riverbed.

The Frickenhofer Höhe is located south of the Limpurg Hills, north of Albuch, a part of the Swabian Jura, and east of the Welzheim Forest. The range lies in a triangle formed by the towns of Gaildorf to the northwest, Aalen to the southeast and Schwäbisch Gmünd to the southwest. It takes the shape of an elongated arc running from Schönberg (borough of Gaildorf) in the north to Abtsgmünd in the southeast. Municipalities within the region include Gschwend, Eschach, Göggingen, Ruppertshofen and Schechingen. The northern boundary of the Frickenhofer Höhe and its spurs is the lowest reaches of the ”Fichtenberger” Rot, a river that approaches from the west and empties into the River Kocher near Gaildorf-Unterrot. The other boundaries, running anti- clockwise, are the “Gschwender” Rot and its two headstreams, the Lein and Kocher.

The river continues on the northern slopes of the Blagaja mountain and the villages of Uzići, Rupeljevo and Rasna and enters the low Tašti field, located between the Blagaja, Krstac and Crnokosa mountains, west of the town of Požega. In the field, the Đetinja receives from the left its main tributary, the Skrapež River, but less than a kilometer after the confluence, it meets the Golijska Moravica River from the south, creating the Zapadna Morava. Since the proximity of the confluences of Đetinja, Skrapež and Golijska Moravica, some sources consider all three rivers to be direct headstreams of the Zapadna Morava. Following the direction of the course, the Đetinja is a natural headstream of the Zapadna Morava, but since Golijska Moravica is 23 kilometres longer, the latter is usually considered as the main headstream.

Pregolya River, a southern ethnic border of Lithuanian speaking territory in the 19th century The area of Lithuania Minor embraced the land between the lower reaches of the river Dangė () to the north and the major headstreams of the river Prieglius (, now Pregolya) to the south. The southwestern line ran from the Curonian Lagoon () along the Deimena River to its south, continued along the Prieglius River to the Alna (now Lava) river, up to the town of Alna and hence southward along the Ašvinė (Swine) river to Lake Ašvinis () and from there eastward to the border of Lithuania Major. The region embraced about 11 400 km². The broader understanding of Lithuania Minor includes the area west from the Alna and south form the lower reaches of the Prieglius and the Sambian Peninsula, making up 17–18 thousand km2 in total.

The river rises in two headstreams in the Tian Shan Mountains in Kyrgyzstan and eastern Uzbekistan—the Naryn River and the Kara Darya which come together in the Uzbek part of the Fergana Valley—and flows for some west and north-west through Uzbekistan and southern Kazakhstan to the remains of the Aral Sea. The Syr Darya drains an area of over , but no more than actually contribute significant flow to the river: indeed, two of the largest rivers in its basin, the Talas and the Chu, dry up before reaching it. Its annual flow is a very modest per year—half that of its sister river, the Amu Darya. Along its course, the Syr Darya irrigates the most productive cotton-growing region in the whole of Central Asia, together with the towns of Kokand, Khujand, Kyzylorda and Turkestan.

The FischbachFischbach als GPS-TRack begins at the confluence of the right-hand Glasbach,Glasbach–Fischbach as GPS track also called the Vorderbach, and the left-hand EschbachEschbach–Fischbach as GPS track which, in turn, is formed by the left-hand Hinterbach and right-hand Reutenbach and then collects the Mittelbach, in the village of Fischbach which belongs to the municipality of Niedereschach. The longer and bigger Glasbach is seen as the main headstream. Hydrographically this may even be considered the main source of the River Neckar, because the Fischbach has a higher streamflow than the Badische Eschach which, in turn, is the larger of the two headstreams, and the Badische Eschach is more powerful than and longer than the young Neckar at their confluence. The Fischbach flows in a southeasterly direction and merges with the Baden Eschach near Niedereschach.

There are clues to the historic boundary in the names of settlements like Audun-le-Tiche (Deutsch-Oth or German Audun) and Audun-le-Roman (Welsch-Oth or Romance Audun) or the names of the two headstreams of the Nied, the Nied Allemande (Deutsche Nied or German Nied) and the Nied Française (Französische Nied or French Nied), which lie on either side of the language boundary and merge almost exactly on the line itself. The linguistic boundary was also reflected early on in the administration of the region. In the 13th century, the Duchy of Lorraine was divided into three bailiwicks (administrative and juridical districts. German: Ballei, French: Bailliage): the Bailiwick of Nancy (Bailliage de Nancy), the Bailiwick of Vosges (Bailliage des Vosges) and the German Bailiwick (Bailliage d'Allemagne); the last-named periodically had its administrative seat in the town of Wallerfangen in present-day Saarland.

The Kleiner Gleichberg lies on the Rhine-Weser watershed between the Vogelsberg and Rhön mountains (in the East Hesse Highlands) and the Lange Berge, where the Thuringian Highland adjoins and the watershed also ends not far from the source of the Werra. Whilst the water of the Milz, which is fed by various headstreams on the eastern side of the saddle between the two mountains, flows towards the southwest via the Franconian Saale and Main into the Rhine, the short streams that rise on the extreme northeastern side of the Kleiner Gleichberg and the hills north of it drain via the Werra into the Weser. In the countryside of the Gleichberge are several reservoirs: the Buchenhof, Haina, Römhild, Roth I and Roth II. In 2011, the Roth I reservoir was drained due to safety concerns with the dam. The other basins are used as fishing lakes and provide irrigation for agriculture.