The Gotthardreuss rises in the Gotthard massif, emerging from Lago di Lucendro (reservoir built in 1947; elevation 2,131 m) in the canton of Ticino and passing into the canton of Uri below the Brigghubel (1,898 m).
The Furkareuss rises east of Furka Pass (2,429 m), early joined by the Blaubergbach (sourced by two mountain lakes on 2,649 m) and several other creeks sourced by still existing glaciers, such as Sidelengletscher (3,170 m), Tiefengletscher (3,285 m) in the north, and Muttengletscher (2,908 m) and Witenwassergletscher (2,805 m) in the south, and eventually forms the east–west valley called Urseren, passing Realp at halfway through the valley at 1,540 m in eastern direction until its eastern end at Andermatt. This source is only around 5 km away from, and on the same mountain massif as the source of the Rhône, but will ultimately lead to the opposite side of the continent.
Gotthardreuss and Furkareuss join at Hospental (1,446 m). Downstream of Andermatt the Reuss joins at 1,429 m the village creek Unteralpreuss, finally turns to the north, and passes through the 3 km-long narrow and deep Schöllenen Gorge and under the legendary Devil's Bridge (1,120 m).
At Göschenen (1,057 m) it is joined by the Göschenerreuss, sourced by the glaciers Dammagletscher (3,430 m) and Flachensteinfirn (3,150 m) besides several others. From here it forms the main valley of the canton of Uri, the Urner Reusstal, passing below Wassen (840 m), Gurtnellen (720 m), Amsteg and Silenen (500 m), and through Erstfeld (460 m), past Attinghausen and Altdorf (440 m), joining the southernmost part of Lake Lucerne (the Urnersee) between Flüelen and Seedorf (434 m). The Reuss leaves Lake Lucerne some 30 km to the north-west, at the city of Lucerne.
Downstream of this confluence, the Reuss forms the border between Aargau and Zürich, passing Merenschwand (Aargau, 389 m) and Ottenbach (Zurich, 384 m), and enters Aargau downstream of Ottenbach.
After the confluence the river continues as the Aare, which flows into the Rhine at Koblenz.
Catchment area
The catchment area of 3,426 km2 (1,323 sq mi)[1] approximately covers Central Switzerland.
The catchment area of the upper Reuss includes almost the entire canton of Uri (with the exception of the Urner Boden, and in the uppermost part of the Gotthardreuss a portion of Ticino (Airolo municipality). The highest point of the drainage basin is the summit of Dammastock, at elevation 3,630 m.
The basin of the lower Reuss adds the catchment areas of other tributaries of Lake Lucerne as well as that of the Kleine Emme, including most of Nidwalden and Obwalden, and parts of Schwyz, Lucerne and Zug. Downstream of Lucerne, further tributaries add other parts of Zug as well as parts of Zürich and Aargau.
Tributaries
Reuss and its tributaries, with length and catchment area, from mouth to source (incomplete):
Ptolemy records the river's pre-Germanic name as Silana (whence the name of Silenen).[4]
The Germanic name is attested as Rusa, Rusia from the 9th century (sometimes recorded as Ursa in the Early Modern period, c.f. Urseren),[5] from an early Germanic *Rūsi, oblique *Rūsjō-.
Greule (1982) interprets the name as an Old European hydronym, directly cognate with Riß.[6] Because of Ptolemy's record of the pre-Germanic name Silana, it is possible that only part of the river was known as *Rūsi in antiquity; alternatively, *Rūsi has been interpreted as a purely Germanic name introduced with Germanic settlement in the early medieval period, a derivation from OHGrūsa, riusa "fish trap".[5]
The main settlement area of Uri was the plain of the Reuss estuary Altdorf (Reussebene). Settlements tended to form on either side of the river, while the river itself was often taken as communal or parish boundary.[7]
The Schöllenen Gorge was made passable the 1230s, opening access to the Gotthard Pass. This resulted in an immense increase of the strategic value of the Reuss valley, as reflected in the grant of imperial immediacy to Uri and the wider political backdrop of the foundation of the Old Swiss Confederacy.
The Reuss was canalised between Attinghausen and Altdorf in 1850–1863, and to the river mouth in 1900–1912, significantly increasing the arable land in the Reuss plain. A small river delta was reconstructed in 1985. After flooding in 1987, improved flood control measures were constructed during 1995–1999.
A small hydroelectric plant was built in Schöllenen Gorge for the construction of the Gotthard Tunnel in 1875. Larger hydroelectric plants were built at Amsteg (1922), Wassen (1949) and Göschenen (1962).
Lower Reuss
The lower Reuss flows along a series of former glacial lakes. Settlements along the river were built on lateral moraines, while the river bed itself was marshy and subject to flooding, and thus unsuitable for settlement. The oldest river crossings are along terminal moraines between the former glacial lakes.
The Reuss valley was under HabsburgAustrian rule during the 14th century.
In the 15th century, the Reuss became the border between territories of the Swiss Confederacy, in 1429 between Lucerne and Zürich, and later between Zug, Zürich and the Freie Ämter condominium, between Freie Ämter and Baden, and between Baden and Berne. The Reuss downstream of Ottenbach came to lie within Aargau with the creation of this canton in 1803.
The Reuss had the status of "imperial road" (freie Reichsstrasse) in the late medieval period. Until 1798, it was the responsibility of cantonal authorities (the Reussherren of Lucerne and Zug) to keep the river navigable. The river was important as waterway for traffic between Lucerne and Zurzach, and via Aare and Rhine to Basel, until the construction of transit roads in the 18th century. River crossings by ferry in the medieval period were at Lunkhofen (mentioned 1160), Windisch, Sins, Mühlau, Oberrüti, and Dietwil. The crossing at Lunkhofen was on the main route from Zürich to Berne. Bridges across the Reuss were in Lucerne, Bremgarten (1230), Mellingen (mentioned 1253) and Gisikon (1432). In 1528, the Catholic cantons blocked the trade routes across the Reuss for Protestant cantons and trade between Zürich and Berne was re-routed through Windisch.[7]
Because ferries and bridges were a source of income, the construction of new crossings was opposed during the early modern period, and only one new bridge was built, commissioned by Zug, at Sins (1640). New bridges were built only after the collapse of the Old Swiss Confederacy, e.g. at Windisch (1799), Ottenbach (1864) and Mühlau (1940).
By the end of the 20th century, there were more than a dozen crossings of the lower Reuss, including a number of railway and motorway bridges.
Projects for canalisation in 1648 (Hans Conrad Gyger) and 1809 (Johann Gottfried Tulla) were not realised.
In 1840, Aargau constructed some canalisation, with limited impact. A large-scale project of river engineering was completed during 1971–1985 (Reusstalsanierung). The hydroelectric plant at Bremgarten-Zufikon was built in 1893 and enlarged in 1975 (Flachsee reservoir).
References
^ abFederal Office for the Environment FOEN, "Topographical catchment areas of Swiss waterbodies 2km2" Sub-catchment area number 94738, Catchment area size [km2] 3425.54.
^Catchment area at outflow including lake's surface area
^Reichert (1968): "zur Zeit des P. hatte für die Reuß noch ihr vorgerm. Name, Silana, gegolten (1, 240ff.; 2, 145ff.)."
^ abH. Reichert, "Riousiaoua" in Hoops (ed.), Reallexikon der germanischen Altertumskunde 25 (1968), p. 27.
^Greule, Albrecht, Riusiava, Riß und Reuß, Blätter für Oberdeutsche Namenforschung, 19 (1982).
Albrecht Greule, Deutsches Gewässernamenbuch: Etymologie der Gewässernamen und der zugehörigen Gebiets-, Siedlungs- und Flurnamen, Walter de Gruyter (2014), 434f.
