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29-995: The 12.2-kilometre (7.6 mi) long canal links the River Havel north of Spandau to the River Spree near the Hauptbahnhof in Berlin . Because it joins the Havel upstream of the river lock at Spandau, it provides a more direct route from the Spree to the Oder–Havel Canal . The Westhafen , Berlin's largest port with an area of 173,000 m (42.75 acres ) lies on the Berlin–Spandau Ship Canal some 4 kilometres (2.5 mi) from its eastern (River Spree) end. The Westhafen Canal and Charlottenburg Canal also connect

58-520: A stretch of the river. Both routes rejoin in the linked lakes of Breitling See and Plauer See , which leads up to Plaue. Like the preceding stretch of the river, the stretch from Plaue to the confluence with the Elbe at Havelberg is administered as part of the Lower Havel–Waterway. Unlike the previous stretch, this stretch carries considerably less commercial traffic. Vessels heading to or from

87-424: Is a stub . You can help Misplaced Pages by expanding it . This article about a Berlin building or structure is a stub . You can help Misplaced Pages by expanding it . Havel The Havel ( German: [ˈhaːfl̩] ) is a river in northeastern Germany , flowing through the states of Mecklenburg-Vorpommern , Brandenburg , Berlin and Saxony-Anhalt . The 325 kilometres (202 mi) long Havel

116-555: Is a right tributary of the Elbe . However, the direct distance from its source to its mouth is only 94 kilometres (58 mi). For much of its length, the Havel is navigable; it provides an important link in the waterway connections between the east and west of Germany, as well as beyond. The source of the Havel is located in the Mecklenburg Lake District , between Lake Müritz and the city of Neubrandenburg . There

145-644: Is no obvious visible source in the form of a spring, but the river originates in the lakes in the Diekenbruch near Ankershagen , close to and south-east of the watershed between the North and Baltic seas. From there the river initially flows southward, eventually joining the Elbe, which in turn flows into the North Sea. Every river north-east of it flows to the Baltic Sea. The river enters Brandenburg near

174-582: Is not particularly great; in most cases it is less than 2 metres thick. Before the installation of artificial drainage networks excess water often accumulated in the Luche in ponds. In contrast with lowlands with natural watercourses, they were give a different name from the neighbouring Bruche ( carrs ), such as the Oderbruch to the east and the Hohennauen Bruch on the Havel to the west. Most of

203-552: Is placed 11 km downstream. As the course of the Elbe has a higher gradient than the Havel, the water level of the Havel in Havelberg can be kept 1.4 metres below the Elbe (at the junction of the traverse communicating canal, protected by a lock ). Towns along the river include: Fürstenberg , Zehdenick , Oranienburg , Berlin , Potsdam , Werder , Ketzin , Brandenburg , Premnitz , Rathenow and Havelberg. In earlier Greek or Latin sources, such as Tacitus 's Germania ,

232-573: The Elbe Lateral Canal . This stretch of the river descends through locks at Bahnitz , Rathenow , Grütz , Garz and Havelberg . At Rathenow there are two channels, each with a lock. North of Plaue, the river is crossed by the Pritzerbe Ferry . Luch (landform) The term Luch (plural: Luche ) is German and refers to an area of originally expansive, marshy or boggy lowland in northeast Germany , especially in

261-649: The Großes Fenster ( German pronunciation: [ˈɡʁoːsəs ˈfɛnstɐ] ; literally "Great Window") with an unobstructed view upriver, hence the name, followed by the island of Schwanenwerder and the large arm known as the Großer Wannsee . This part of the river can be very busy with leisure craft. The island of Pfaueninsel is also a feature of this stretch of the river. A public ferry crosses these waters between Wannsee and Kladow , carrying passengers and cyclists. The Teltow Canal joins

290-549: The Luche in Brandenburg have since been drained by man and have become cultural landscapes. After land improvement , they were commonly used as grassland . Archaeologists like Klaus Goldmann believe that some of this reclamation began during the Slavic period, but that this was reversed by a worsening of the drainage conditions as a result of the construction of mill dams on the Havel. There are many Luche in Brandenburg;

319-891: The Müritz–Elde–Wasserstraße . Other connected waterways are the Lychener Gewässer  [ de ] , the Templiner Gewässer  [ de ] and the Wentow Gewässer . The stretch of the river between the junction with the Oder–Havel Canal near Liebenwalde and the confluence with the Spree at Spandau is administered as part of the Havel–Oder–Wasserstraße , which also includes the Oder-Havel Canal. This stretch of

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348-853: The Templiner See to the Schwielowsee , then northwest to Paretz, whilst the Sacrow–Paretz Canal takes a shorter route due east to Paretz, saving some 13 kilometres (8.1 mi) compared to the 29 kilometres (18 mi) Potsdamer Havel. The Potsdamer Havel is crossed by the Kiewitt Ferry in Potsdam itself, and by the Caputh Ferry at the entrance to the Schweilowsee. At Paretz the two channels join up again, as does

377-756: The Useriner See to the Großer Labussee . The stretch of the river between this lock and the junction with the Oder–Havel Canal is administered as part of the Obere–Havel–Wasserstraße , along with various connecting canals and waterways. From Zwenzow downstream to Liebenwalde is a distance of 92 kilometres (57 mi). In this distance the navigation passes through the lakes of Großer Labussee, Woblitzsee , Wangnitzsee , Großer Priepertsee , Ellbogensee , Ziernsee , Röblinsee , Baalensee , Schwedtsee and Stolpsee . It also descends through

406-470: The Berlin boroughs of Spandau and Reinickendorf respectively. The last 10 kilometres (6 mi) of this stretch of the river, from Hennigsdorf, passes through a series of interconnected lakes, including the large Tegeler See . The river enters Berlin 6 kilometres (4 mi) before Spandau, having formed the boundary for the previous 4 kilometres (2.5 mi). During the partition of Germany , this formed

435-621: The German commercial waterway network, carrying traffic from the Rhine and the North Sea to Berlin and Poland . From a navigation perspective, the Havel can be split into four sections with somewhat different characteristics and different administrative arrangements. The Havel is navigable to canoes and similar small craft from close to its source. Motor craft are prohibited above the first lock at Zwenzow  [ de ] , which links

464-600: The Havel Canal from further upstream. Just downstream of Paretz, the river is crossed by the Ketzin Cable Ferry . At Brandenburg an der Havel, the navigation again splits into two routes. Commercial shipping descends through a lock into the Silo Canal that passes to the north of the city centre. Leisure craft pass through the centre of the city, using the short Brandenburg City Canal , a smaller lock, then

493-517: The Havel downstream, and was built in the 1950s to allow East German vessels to avoid the stretch of the river under the political control of West Berlin . Some 7 kilometres (4.3 mi) further downstream, the Berlin-Spandau Ship Canal joins the river on the east bank, providing a connection to central Berlin without passing through the lock at Spandau. A car ferry crosses the river between Hakenfelde and Konradshöhe , in

522-666: The Rhine and the west of Germany take the Elbe–Havel Canal at Plaue. Whilst the lower reaches of the Havel provide the most direct route to Hamburg and the North Sea ports, variable water levels in the Elbe affect those in the lower Havel; together these can restrict navigation. A less direct, but more reliable route is available via the Elbe–Havel Canal, the Magdeburg Water Bridge , the Mittelland Canal and

551-545: The border between East Germany and West Berlin, and border control points were established for vessels navigating the river. The stretch of the river between the confluence with the Spree at Spandau and the junction with the Elbe–Havel Canal at Plaue is administered as part of the Lower Havel–Waterway , which also includes the stretch of river downstream to the confluence with the Elbe. Between Spandau and Plaue,

580-609: The locks at Wesenberg , Steinhavelmühle , Fürstenberg, Bredereiche , Regow , Zaaren , Schorfheide , Zehdenick , Bischofswerder and Liebenwalde . The Woblitzsee also gives access to the Kammer Canal , which allows vessels to reach Neustrelitz . The Ellbogensee links to the Müritz–Havel–Wasserstraße , which proceeds deeper into the Mecklenburg Lake District, eventually connecting with

609-659: The lower Rhine. At the southern end of the Ruppiner See , weirs can distribute the waters of the Rhin either east- or westwards, rejoining the Havel in two places 67 kilometres (42 mi) apart along a straight line, and more than 160 kilometres (99 mi) apart along the course of the river. The region around and north of the middle Havel is called the Havelland . It consists of sandy heights, sometimes called Ländchen , and low marshes, called luchs . A few kilometres of

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638-516: The name of the river was also written as Habola, Habula, Havela . The river name Havel is related to German Haff, habe, hafen , MHG Hafen meaning port, harbor). The Slavic people who later moved into the Havel area were referred to in German sources as Heveller (occasionally as Havolane ). The Havel is navigable from the Mecklenburg Lake District to its confluence with the Elbe . Whilst its upper reaches carry little other than leisure traffic, further downstream it provides an important link in

667-466: The port to the Spree further downstream in Charlottenburg . On August 26, 2013, author Wolfgang Herrndorf committed suicide by gunshot to the head on the banks of the canal following a long illness . 52°32′12″N 13°21′49″E  /  52.5366°N 13.3637°E  / 52.5366; 13.3637  ( Spandauer-Schiffahrtskanal ) This article related to water transport

696-550: The river before its confluence with the Elbe near Havelberg are in the State of Saxony-Anhalt. Due to its minimal gradient it is susceptible to high waters in the Elbe. Unless in extreme floods, if the dike of the Elbe is submerged, the discharge of the Havel is improved by the Gnevsdorfer Vorfluter (something like "Gnevsdorfer outfall"). By this canal, the mouth of the Havel, that naturally would be near Havelberg,

725-494: The river forms part of the main inland waterway route from Germany to Poland and carries significant commercial traffic. This stretch of the river is 40 kilometres (25 mi) long, and the river descends through two locks at Lehnitz  [ de ] and Spandau. At Hennigsdorf , 30 kilometres (19 mi) downstream of Liebenwalde, the Havel Canal joins the river on the west bank. This canal connects to Paretz , on

754-474: The river forms part of the main inland waterway route from the Rhine and the west of Germany; from Hamburg and the North Sea ports, to both Berlin and Poland. It thus carries a considerable amount of commercial traffic. South of Spandau, the river widens into a wide lake that extends, through some narrower areas, to Potsdam. On the east bank south of Spandau is the Grunewald with several beaches, among them

783-739: The river from the east via the Griebnitzsee just before the city reaches the city of Potsdam, providing an alternative route to the Oder–Spree Canal avoiding central Berlin. The Griebnitz Canal provides a short cut for smaller vessels from the Griebnitzsee to the Großer Wannsee. At Potsdam the navigation splits into two channels. The Havel, here known as the Potsdamer Havel, takes a route southwest through Potsdam and

812-517: The state of Brandenburg . Luche are found mainly in Young Drift regions; but they also occur on Old Drift landscapes. According to Leser the term should not be translated. Luche mainly formed in the main urstromtal valleys or their side valleys. After the end of the Ice Age , the water table rose during the postglacial period resulting in the formation of bogs . The peat thickness

841-620: The town of Fürstenberg . In its upper course and between Berlin and Brandenburg an der Havel the river forms several lakes. The Havel's main tributary is the Spree , which joins the Havel in Spandau , a western borough of Berlin, and is longer and delivers more water than the Havel itself above the confluence. The second largest tributary is the Rhin , named in the Middle Ages by settlers from

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