Banfe (Lahn)

The Lahn is a , right (or eastern) tributary of the Rhine in Germany. Its course passes through the federal states of North Rhine-Westphalia (23.0 km), Hesse (165.6 km), and Rhineland-Palatinate (57.0 km).

It has its source in the Rothaargebirge, the highest part of the Sauerland. It meets the Rhine at Lahnstein, near Koblenz. Important cities along the Lahn include Marburg, Gießen, Wetzlar, Limburg an der Lahn, Weilburg and Bad Ems.

Tributaries to the Lahn include the Ohm, Dill, the Weil and the Aar. The lower Lahn has many dams with locks, allowing regular shipping from its mouth up to Runkel. Riverboats also operate on a small section north of the dam in Gießen.

Source area

The Lahn is a -long, right (or eastern) tributary of the Rhine in Germany. Its course passes through the federal states of North Rhine-Westphalia (23.0 km), Hesse (165.6 km), and Rhineland-Palatinate (57.0 km).

The Lahn originates at the Lahnhof, a locality of Nenkersdorf, which is a constituent community of Netphen in southeastern North Rhine-Westphalia, near the border with Hesse. The source area is situated along the Eisenstraße scenic highway and the Rothaarsteig hiking trail.

The river arises in the southeastern Rothaargebirge in the Ederkopf-Lahnkopf-Rücken ridge-line natural area. This ridge is the drainage divide between the Rhine and Weser, and, within the Rhine system, the watershed between the rivers Lahn and Sieg.

The source is at an elevation of and is located southwest of the high Lahnkopf. In the vicinity are also the origins of the Eder (5.5 km northwest of the Lahnhof) and the Sieg (another 3 km north). Whereas the Sieg takes the shortest route to the Rhine (to the west), the Lahn first runs in the opposite direction, paralleling the Eder for many kilometers.

Course

The Lahn first flows in a northeasterly direction through the southeastern Rothaargebirge and its foothills. From about the Bad Laasphe community of Feudingen, it turns primarily to the east.

Upper Lahntal and Wetschaft Depression

The section of the Lahn below the town of Bad Laasphe is geographically known as the Upper Lahn Valley (German: Ober Lahntal). Above Bad Laasphe, where the river flows between the Rothaargebirge on the left (i.e. to the north) and the Gladenbach Uplands on the right, the Lahn Valley is simply considered part of these mountains.

Between Niederlaasphe (of Bad Laasphe) and Wallau (of Biedenkopf), the river crosses the border between North Rhine-Westphalia and Hesse. It then flows in an easterly direction through some districts of Biedenkopf (but not the central town) and the towns of Dautphetal and Lahntal. It is joined from the right by the Perf at Wallau and at Friedensdorf (of Dautphetal) by the Dautphe (which flows in a side valley to the south).

Shortly after the village of Caldern (of Lahn Valley), the ridgeline of the Rothaargebirge on the north ends with the Wollenberg and that of the Gladenbach Bergland with the Hungert. The Lahn leaves the Rhenish Slate Mountains for a long section and reaches the West Hesse Highlands, where it flows through the extreme south of the Wetschaft Depression, north of the Marburger Rücken. Where the Wetschaft flows into it from the Burgwald forest in the north (near the Lahntal village of Göttingen), the Lahn immediately changes direction by 90° to the right.

Marburg-Gießen Lahntal

The now southward-flowing Lahn then enters the Marburg-Gießen Lahntal. Shortly before Cölbe, the Ohm enters from the left at the ''Lahn-Knie'' named area. Flowing from the Vogelsberg through the ''Ohmtal'', the Ohm is the Lahn's longest tributary, with a length of .

The river then breaks through a sandstone mesa (the Marburger Rücken to the west and the Lahnberge to the east) into a valley which encompasses the entire territory of the city of Marburg and its suburbs. The valley begins after the river passes the Marburger Rücken near Niederweimar, where the Allna enters from the right. At the valley's southern end, the Zwesten Ohm enters from the Lahnberge. The right (western) side of the valley is again formed by the Gladenbacher Bergland, from which the Salzböde enters the Lahn. On the left rises the Lumda Plateau, from which the eponymous river Lumda flows into the Lahn near Lollar. Gradually the valley widens into the Gießen Basin.

In Gießen, after the inflow of the Wieseck from the left, the Lahn's general direction of flow changes from the south to the west. The Gießen Basin extends a few more miles downstream to Atzbach, a suburb of Lahnau. From the 1960s until the 1980s, there was extensive gravel mining in this area. The area between Heuchelheim, Lahnau, and the Wetzlar borough of Dutenhofen was to be completely mined and a water sports center with an Olympic-suitable rowing course built. This plan was partly realized, and the Heuchelheim Lake and Dutenhofen Lake are now popular recreational destinations for the surrounding region. Nature conservation organizations, however, were able to prevent further gravel mining, so the area is now one of the largest nature reserves in Hesse. Dutenhofen Lake marks Kilometer 0 of the Lahn as a federal waterway.

The Gießen Basin is surrounded by the mountain peaks of the Gleiberg, the Vetzberg, the Dünsberg, and the Schiffenberg. At Wetzlar, the Lahn is joined by its second longest tributary, the Dill, which has a length of . At this location, the valleys of the Lahn and Dill separate three parts of the Rhenish Slate Mountains from each other: the Gladenbach Bergland, the Westerwald to the northwest, and the Taunus to the south.

Weilburg Lahntal

After Wetzlar, the valley of the Lahn gradually narrows and at Leun enters the Weilburger Lahntal. The Weilburger Lahntal belongs to the larger Gießen-Koblenzer Lahntal physiographic province, considered part of the Rhenish Slate Mountains.

In the upper area of the Weilburg Lahntal (the Löhnberg Basin) are mineral springs, such as the famous Selters mineral spring in the municipality of Löhnberg. In the lower area, where the river turns again to the south, the Lahn is entrenched canyon-like below the level of the surrounding geographic trough.

The city of Weilburg is wrapped by a marked loop of the river. The neck of this noose is traversed by a boat tunnel, unique in Germany. A little below Weilburg, the Weil, originating in the High Taunus, enters the Lahn.

Limburger Basin

At Aumenau in the municipality of Villmar, the course of the Lahn reverses to the west again and enters the fertile Limburger Basin, where the river is incised to a depth of about . Here the river is joined by two tributaries, the Emsbach coming from the Taunus and the Elbbach from the Westerwald. In this area are frequent outcroppings of Devonian limestone, the so-called Lahn Marble (German: ''Lahnmarmor''), such as at Limburg an der Lahn, where the Limburg Cathedral crowns such an outcropping. At Limburg, the river again enters a wider valley.

Lower Lahntal

Below Diez, the Lahn absorbs the Aar from the south. At Fachingen in the municipality of Birlenbach, it leaves the Limburger Basin and enters the Lower Lahntal. Its course is incised over deep in the Slate Mountains. Near Obernhof, the Gelbach enters the Lahn opposite Arnstein Abbey. Then, after passing Nassau and Bad Ems, where, as in Fachingen, mineral springs (sources of Emser salt) can be found, it completes its run, entering the Rhine in Lahnstein, located five kilometers south of Koblenz at an elevation of .

History

Early history

The Lahn area was settled as early as in the Stone Age, as shown by archeological finds near Diez, in Steeden in the community of Runkel, and in Wetzlar. Recent discoveries in Dalheim on the western edge of Wetzlar show a ca. 7000-year-old Linear Pottery culture settlement. There are also remains a Germanic settlement in the location, dated to around the 1st century, situated above a bend of the Lahn.

In the Roman Era, the Lahn presumably was used by the Romans to supply their fort at Bad Ems, Kastell Ems. Here the '' Limes Germanicus'' on the borders of Germania Superior and Rhaetia crossed the Lahn. Archaeological finds are known from Niederlahnstein, as well as from Lahnau. One Lahnau site, the Waldgirmes Forum in the community of Waldgirmes, was discovered in the 1990s and had been the site of a Roman town. Another site in the community of Dorlar has the remains of a Roman marching camp (or ''castra''). These Lahnau sites have significant altered the current understanding of the history of the Romans east of the Rhine and north of the ''Limes''.

During the Migration Period, the Alamanni settled in the lower Lahntal. They were later ousted by the Franks.

The origin and meaning of the name Lahn are uncertain; it is possible that it is a pre-Germanic word. The form of the name changed over time; before 600, variations like Laugona, Logana, Logene or Loyn are typical. The oldest known use of the current spelling of the name dates to 1365.

The oldest mention of the staple right of Diez dates to the early 14th century and is an indication of significant shipping on the Lahn by that time. In 1559, John VI of Nassau-Dillenburg laid out a towpath on the lower Lahn. In 1606, for the first time, the Lahn was deepened to allow small scale shipping and the lower reaches became navigable for four to five months of the year. However, there were numerous weirs with only narrow gaps, so the traffic remained restricted to small boats.

In the 17th and early 18th centuries, there were several initiatives of adjacent princes to further expand the Lahn as a waterway, but they all failed due to lack of coordination. In 1740, the Archbishopric of Trier

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