Reppisch
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Reppisch upper run name: Chrebsbach |
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 Reppisch shortly before the confluence of the Dönibach |
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| Data | ||
| Water code | CH : 11105 | |
| location | Switzerland | |
| River system | Rhine | |
| Drain over | Limmat → Aare → Rhine → North Sea | |
| source | overturned on the southwest slope of the Hochwacht a little north of Tüfenbach 47 ° 15 ′ 53 ″ N , 8 ° 31 ′ 30 ″ E |
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| Source height | 742 m above sea level M. | |
| muzzle | near Dietikon in the Limmat coordinates: 47 ° 24 '58 " N , 8 ° 24' 18" E ; CH1903: 672 929 / 252 156 47 ° 24 '58 " N , 8 ° 24' 18" O |
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| Mouth height | 381 m above sea level M. | |
| Height difference | 361 m | |
| Bottom slope | 13 ‰ | |
| length | 27 km | |
| Catchment area | 69.1 km² | |
| Discharge at the Türlersee discharge level A Eo : 5.9 km² |
NNQ (1997) MQ 1983–2015 Mq 1983–2015 HHQ (1994) |
6 l / s 106 l / s 18 l / (s km²) 1.38 m³ / s |
| Discharge at the Birmensdorf gauge before Wüeribach A Eo : 23.7 km² |
NNQ (1976) MQ 1970–2016 Mq 1970–2016 HHQ (1994) |
1.2 l / s 410 l / s 17.3 l / (s km²) 32.4 m³ / s |
| Discharge at the Dietikon gauge before the A Eo mouth : 69.1 km². Location: 780 m above the mouth |
NNQ (2003) MQ 1986–2016 Mq 1986–2016 HHQ (1999) |
69 l / s 1.2 m³ / s 17.4 l / (s km²) 93.6 m³ / s |
| Left tributaries | Wüeribach , Lunnerenbach , Rummelbach , Dönibach | |
| Right tributaries | Lattenbach, Loomattbach, Schwandenbach, Stoffelbach | |
| Communities | Aeugst am Albis , Stallikon , Birmensdorf , Urdorf , Bergdietikon , Dietikon | |
| Residents in the catchment area | about 30,000 | |
 The Reppisch from the confluence of the Stoffelbach near Dietikon in March |
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The Reppisch (in front of the Türlersee Chrebsbach ) is a 27 km long left tributary of the Limmat in the Swiss cantons of Zurich and Aargau . It rises at Albis as Chrebsbach leaves the Türlersee in Aeugst am Albis as Reppisch, crosses the Reppischtal and flows Dietikon in the tailrace of the power station Dietikon, which unites briefly later with the Limmat. The approx. 70 square kilometers large catchment area of the Reppisch drains with an average 1.21 m³ / s near the mouth. This makes it the most important tributary of the Limmat behind the Sihl and in front of the Furtbach .
On its way to the estuary, it meanders through the Reppisch Valley in many natural places and is only bordered by woodland, herbaceous fringes and meadows. With the exception of the sections in Dietikon and Birmensdorf, the banks of the river are not very well developed, making them one of the last remaining natural rivers in the Canton of Zurich. Above all, the six-kilometer section between the hamlet of Gamlikon in Stallikon and Birmensdorf was able to maintain its natural course of the river.
Between Birmensdorf and Dietikon the river runs through a narrow valley that the in the near infantry - barracks stationed troops of the Swiss army as a shooting range is used. This section of the Reppisch Valley can therefore be closed in places on weekdays. Otherwise the valley is a popular area for walkers and cyclists.
Shortly before Dietikon, the river crosses the Mutschellenpassstrasse and the tracks of the Bremgarten-Dietikon-Bahn . In this area there was severe flooding in the spring of 1999, which interrupted the road and the railway line for several days.
geography
course
The Reppisch rises near Tüfenbach in the Flur Berg as Chrebsbach . After 2 kilometers this flows into the southeast end of the Türlersee. After leaving the lake, it initially flows to the northwest, accompanied by a thick forest edge, and flows around the Aeugsterberg on its eastern and northern slopes. It is dammed a little north of Seehüsli to a small pond before it flows through Chloster and Aeugstertal . Here, after several small inflows, the Reppisch has an average discharge of 0.1 m³ / s.
It now flows to the northeast to Tägerst , then again shortly to the northwest to Aumüli , always accompanied by a mostly loose forest edge, which borders on fields. There follows a larger arch around an extension of the Hörglen , which here creates a narrow valley in which the hamlet of Gamlikon is located. A little later it reaches Stallikon , where, after countless tributaries, mainly from the Albis chain, it has an average discharge of 0.3 m³ / s.
The river passes Sellenbüren and Landikon and flows through Birmensdorf , where two of the most important tributaries flow, the Wüeribach and the Lunnerenbach . The mean discharge to the ARA Birmensdorf is now 0.9 m³ / s. A little later, in the municipality of Urdorf , the Malefizgraben flows , and after the confluence of the Stigelmattbach , which itself briefly forms the border, the Reppisch is a short section of the border river between the two cantons. The Rummelbach now flows out near Rudolfstetten-Friedlisberg and shortly afterwards the Dönibach near Baltenschwil .
The Reppisch now enters the Limmattal near Dietikon , where a small part of the water is diverted to dam the marble pond . The Reppisch is now straightened and there are no major tributaries until it reaches its mouth. It finally flows at 381 m above sea level. M. in the industrial area at the KVA Dietikon in the underwater channel of the Dietikon power station, which joins the Limmat immediately afterwards.
Catchment area
The catchment area of the Reppisch measures 69.1 km² with around 30,000 inhabitants, which corresponds to a population density of around 438 inhabitants per km². Most of this area is in the canton of Zurich and here in the Säuliamt , smaller parts are in the Dietikon district and the Baden and Bremgarten districts in Aargau . At the measuring point just before the mouth, the catchment area is 67.2 km², of which 30.8 km² is agricultural area, 25.2 km² is forest, 10.2 km² is settlement area, 0.7 km² is water and 0.2 km² is unproductive area.
The communities Aeugst am Albis , Stallikon , Birmensdorf , Urdorf , Bergdietikon and Dietikon , through which the river runs, as well as the communities Aesch , Arni , Berikon , Hausen am Albis , Islisberg , Langnau am Albis , Oberwil-Lieli (here the district Lieli), Rudolfstetten-Friedlisberg and Uitikon (here the hamlet of Ringlikon ). The municipalities of Bellikon , Hedingen , Widen and the city of Zurich on the Uetliberg have tiny shares .
The upper part of the catchment area between the Türlersee and the confluence of the Lunnerenbach is an average of 625 m above sea level. M. and has an average annual rainfall of 1204 mm, the lower part between the confluence of the Lunnerenbach and the confluence of the Reppisch in the Limmat lies at an average of 554 m above sea level. M. and has an average annual rainfall of 1126 mm. The highest point of the entire area is 896 m above sea level. M. and is reached on the Albis in the forest field Reifholz northwest of the Albispasshöhe , the deepest point is at the mouth at 381 m above sea level. M. , which corresponds to a difference of 515 meters. Other prominent points in the catchment area are the 870 m above sea level. M. high Uetliberg and the Aeugsterberg with a height of 829 m above sea level. M.
In addition to the Türlersee, it only drains smaller ponds, including the brick ponds in Wettswil , namely the Fischbachweiher , the Fridgrabenweiher and the Sorweiher , as well as the Lochenweiher in Bonstetten , which all feed their water to the Reppisch via the Wüeribach. The opposite also in Wettswil Oakmoss pond drained by the Schleetalbach in the Reppisch. The marble pond in Dietikon is fed by the Reppisch itself. A small canal branches off at the Grunschen play and barbecue area in the Gaissteg corridor , which touches the playground and then bridges the river in a pipe that is located under a footbridge. The water flows back to the Reppisch at the other end of the pond.
Adjacent larger catchment areas are in the south and west that of the Jonen , which drains into the Reuss , and in the east that of the Sihl , which flows into the Limmat in Zurich.
Tributaries
68 named brooks flow into the Reppisch, of which three, namely the Wüeribach , the Rummelbach and the Lunnerenbach , are four kilometers long or more. Furthermore, five tributaries are two kilometers long or more, namely the Dönibach , the Lattenbach , the Schwandenbach , the Tobelbach near Birmensdorf and the Malefizgraben , if you include its right upper course, the Weidbach .
The most important tributary of the Reppisch is the approximately 8 kilometer long Wüeribach, which drains the Wettswil and Bonstetten plains and flows into the Reppisch from the left at Birmensdorf. It feeds the Reppisch with an average discharge of 310 l / s. Shortly before its mouth it takes in the Aescherbach , which has an average discharge of 100 l / s and is therefore one of the larger streams in the catchment area. After the Wüeribach, it is the Lunnerenbach and the Rummelbach that feed the Reppisch the most water.
Other major tributaries are the Dönibach, which flows into Dietikon, which rises in Bergdietikon , the Stoffelbach , which has its source in the Honeret forest in Dietikon, and the Malefizgraben, which has its source in Rudolfstetten-Friedlisberg and flows into the Urdorf municipality from the left. These all flow into the lower Reppisch, longer tributaries in the upper reaches are the Lattenbach near the hamlet of Tägerst , the Loomattbach , the Weidelbach and the Diebisbach in the hamlet of Sellenbüren , both Stallikon, and the Schwandenbach in the hamlet of Landikon near Birmensdorf.
Diagram of the tributaries of the Reppisch
- with a length of 2 km and more, listed from the source to the mouth. The tributaries on the left are shown in dark blue, the ones on the right in light blue.
environment
In 1885, after several severe floods, the first corrections were made to the Reppisch. This was also due to the pressure of the population, which threatened to settle elsewhere. During the amelioration between 1938 and 1944, large parts of the Reppisch were canalized in order to improve flood protection and to gain land that was used for cultivation. However, people began to rethink early on, and existing near-natural sections were protected and built-up sections were renatured. A basis for this was the revitalization program for the rivers of the Canton of Zurich, but also the overall nature conservation concept. This was set by the canton on December 20, 1995 and rated the Reppisch as one of the most ecologically valuable rivers in the canton of Zurich.
The canton acquired adjoining parcels over a length of 10 kilometers in order to revitalize this section. In 2007, a 400-meter-long section of the river near Birmensdorf was renatured as part of the construction of the Zurich western bypass . From 2007 to 2009, the last remaining, strongly straightened section from the amelioration was finally renatured over a length of 1.5 kilometers.
flora
The Reppischtal has probably the richest range of natural plant communities in the Swiss plateau . The Albis slopes bordering the river in the Albiskette-Reppischtal landscape monument are characterized by montane red beech forest , in dry and humid sub-communities there are oak-hornbeam forests . There are also submontane maple-ash forests , brook ash forests , steep-slope beech forests rich in yew and whistle-grass pine forests . Limited to smaller areas, there are swampy pine forests and perennial black alder forests. There are also numerous glacial relics , of which the mountain pine deserves a special mention due to its frequent occurrence . Furthermore, around 28 different species of orchids can be found in the landscape monument.
At the Reppisch outdated locations will be rejuvenated through targeted interventions, besides, old and striking individual trees as are oaks , silver willow , black alder and the characteristic of the Reppisch Kopfweiden but spared. This also benefits several species of birds as well as other animal species.
Problems, on the other hand, are caused by the glandular balsam , the Canadian goldenrod , the fleabane and the field thistle , which have spread as neophytes in the Reppisch Valley. Associations have taken on this problem, and so, for example, the Stallikon municipal association carried out a control campaign to protect the biodiversity of the valley.
fauna
Like the flora, the fauna is also relatively high compared to the rest of the Central Plateau. In the Albiskette-Reppischtal landscape monument, for example, reptiles, birds and insects show a wide range of species, the latter of course also benefiting from the diverse occurrence of different orchid species.
The river is a habitat for dragonflies , for the brook lamprey and for the bullhead , but also for amphibians, including the fire salamander . Among the bird species, the kingfisher , the mountain wagtail and the dipper on the river and on the side streams as well as the common raven in the surrounding forests should be mentioned. Three kingfisher breeding sites have been recorded on the Reppisch and Limmat rivers since 1991, and in 2001 a pair of kingfisher brooded on the Reppisch in the municipality of Urdorf.
In addition, as is not unusual in the Central Plateau, wild boars have their habitat here, but the Eurasian lynx has also been observed.
natural reserve
In the catchment area of the Reppisch there are several flat moors as well as several dry meadows and countless other nature reserves and several forest reserves . Since 1983, large parts of the upper Reppischtal have been part of the federal inventory of landscapes and natural monuments of national importance under the property name Albiskette-Reppischtal .
In the catchment area there are two fens, which are registered in the federal inventory of fens of national importance . For example, the Beerimoos moor near Wettswil and the moor south of Seehüsli at the outflow of the Reppisch from the Türlersee. Other flat moors such as the Ried am Honeret in Urdorf are not entered in the federal inventory , but are of supra-municipal importance.
Furthermore, several nature reserves can be found in the catchment area, which are entered in the federal inventory of amphibian spawning areas of national importance . So near Birmensdorf the Egghau gravel pit , near Wettswil the old oil dump and near Ribacher in the municipality of Bonstetten and on the Türlersee. Dry meadows, which are entered in the federal inventory of dry meadows and pastures of national importance , can be found at Wolfen , Tägerst , Sellenbüren and Stallikon and at Landikon in the municipality of Birmensdorf.
history
Emergence
The Reppisch flows through a valley that was formed in the last ice age by a meltwater flow that carried much more water at that time, which was fed by the Reuss glacier and has eaten its way down to the Molasse rock over time. At times, a landslide that loosened around 40 million cubic meters of rock from the Aeugsterberg and let it slide into the meltwater channel stopped this erosion process. This landslide created the Türlersee, and the water then probably flowed off to the west through the Hexengraben . The meltwater flow at times also flowed through the Urdorf valley, where the Schäflibach runs today , before a left lateral moraine of a branch of the Linth glacier flowing over the Waldegg blocked its way, which diverted the river towards Dietikon. The river ate deep into the layers of marl and sandstone , creating a narrow valley between the Egg near Birmensdorf and the confluence of the Rummelbach .
Since the last Ice Age, the Reppisch has cut through the former Bonstetten – Birmensdorf – Urdorf valley, through which the Reuss drained into the Limmat.
At the mouth of the river has entrained by the attachment Limmatdruck to the northern side of the valley of the Limmattal pressed, which thereby makes a turn towards north in Dietikon in front of the mouth of the Reppisch.
Origin of name
The origin of the name Reppisch is not completely clear; probably it is derived from the Latin word "Rabiosa" or "Rabiusa", which in turn is a translation of the Gallic word "Londona" and means something like angry . At that time the Gauls thought that the rivers were populated by divine beings, demons and spirits, after whose properties the rivers were then named.
According to Albrecht Greule , however, this is not possible for reasons of sound. He suggests «Rabisa» as the basic form, derived from the Germanic «Rabisô», which means something like the one who touches or hurries along .
Other previously documented names for the river and the valley are Rebistal in 1173 and 1190, Rebstal 1309 and 1470, Reptisch 1333, 1359, 1412, 1442, 1527 and 1545, Rebtysch 1347, Repptisch 1423, Räppisch 1526, Raͤpptisch 1534, Reppischbach 1626 , Repist 1671, Eppich 1696, Reppist 1699 and Rappißbach in 1759. On the Gyger map from 1667 it is named Räppisch Fluss and on the Dufour map it is labeled as Reppisch Bach . The current form of the name first appeared in 1543.
River history
Among the earliest records include a document dated 12 July 1442. In this decision the mayor and the council of Zurich on a dispute between the parish Stallikon (then Stallinkon) and several millers on one side and the Kloster Kappel on the other side about hitting of piles (buzzing) at the outlet of the Reppisch. The monastery finally had to remove the stakes, but was able to place a wire mesh on the threshold as before, which could not be damaged in the event of severe punishment.
The water power of the Reppisch has been used for centuries, the Aumüli near Stallikon was first mentioned in 1328. In Dietikon there were already two mills in the 13th century, one in the upper village on Bergstrasse 61 and the other in the lower village on Bergstrasse 23 . In Dietikon, a small part of the Reppisch has been diverted to the Marmoriweiher for a long time, which was created for the fire fighting water supply and was later used by the marble factory Marmori , which gave it its name.
There were plans for a swimming pool on the Reppisch at an early stage. In 1906 the SP came up with this idea, and later the tourist office campaigned for a swimming pool in Dietikon, which was to be built on the Reppisch for reasons of economy. At first the project failed due to lack of money, later because of the Second World War. Finally in 1943 the marble factory Marmori acquired the water concession and thus prevented the project from being realized.
On older maps of the Canton of Zurich, the Reppisch flows a little further north in what is now the Schachen floodplain into a Limmat, which at that time protruded more to the west. A short section on Vorstadtstrasse in Dietikon, on which the river made a small curve to the west, as well as the section under the Limmattal marshalling yard were straightened later. The course of the river was also changed in Birmensdorf, so the river made a small bend towards the north at the bridge on Stallikonerstrasse to today's Hadenacherstrasse . It then flowed in an arc to the south through the area where the Reppisch and Linden school buildings are today, and then flowed a few meters further south from today's bridge on Zürcherstrasse than today. At Schwerzgrubenstrasse the Reppisch was also straightened and the curve to the north smoothed.
Flood
The Reppisch caused floods, especially in earlier times. The river swelled by 16 feet (about 4.9 meters) on June 22, 1722, causing major damage in Landikon in particular . The water masses were so strong that a small lake was formed here. In July 1831 this event was repeated and the Reppisch flooded again. The low-lying houses were destroyed and residents were forced to leave the area.
In 1828, after severe storms, the Reppisch destroyed the bridge in Dietiker Oberdorf . In August 1852, too, the river overflowed, so badly that rail traffic came to a standstill. The Krone tavern was completely flooded.
Between June 3 and 4, 1878, the Reppisch devastated large parts of the upper village in Dietikon, and all residents along the Reppisch had to flee their homes. For example, the whole gym equipment of the Dietikon gymnastics club was swept away with the floods, and a bar was only found again in the mud at the mouth of the Reppisch. The little prison house on the upper Reppischstrasse, which fortunately was empty, was swept away by the floods. Fertile cultivated land was washed away, houses were washed away, and almost every bridge and footbridge was swept away with the otherwise harmless stream. At the time, it was also far from clear who had to pay for the damage, and so the canton paid just 90,000 francs for a loss of 214,000 francs. The reconstruction had to be taken into their own hands by the population, and whoever was missing from this work paid CHF 3 per day, which was a high sum at the time.
In May 1994, a discharge of 70 m³ / s was determined in Dietikon, and during the flood of the century in May 1999, at 93 m³ / s, 44 times more water flowed into the Limmat than the average.
On June 21, 2007, after heavy rainfall, a discharge of 36 m³ / s was measured. The Reppisch sat in the territory Reppischhof a road and an underpass under water and washed away the railway tracks of the Bremgarten-Dietikon-Bahn . A little later, on August 8, 2007, a discharge of 73 m³ / s was determined. This event particularly hit the Reppischhof area , which was flooded over a large area.
In 2010, the Reppischhof flood protection project was finally completed, which is intended to offer this section more protection against flooding.
Attractions
At Aeugstertal , shortly after the outflow from the Türlersee, the Riedhof mine is on the left side of the river and only a little later at Stallikon is the Aumüli, which used to supply the surrounding communities and has been inhabited continuously for 700 years. A little further down the river, at Sellenbüren , follows the old mill from 1468. The Reppisch flows through the old town of Dietiker and passes, among other things, the Krone Dietikon , where the first tavern was built in 1259 .
In addition, the Reppisch Valley itself is a popular local recreation area in the region. On both sides of the valley, wooded hills are ideal for hiking, and there are footpaths and cycle paths along the Reppisch. The narrow and remote section of the valley between Dietikon and Birmensdorf is closed to motor vehicles and is therefore popular with those looking for relaxation.
Web links
swell
- Geographic information system of the Canton of Zurich
- Geographic information system of the Canton of Aargau
Individual evidence
- ↑ a b c Geographical Information System of the Canton of Zurich
- ↑ a b c d Geoserver of the Swiss Federal Administration ( information )
- ↑ Türlersee - outflow. (PDF) Position 561: monthly samples. In: Office for Waste, Water, Energy and Air, Department of Water Protection. Retrieved September 29, 2017 .
- ^ Reppisch-Birmensdorf. (PDF) Position 541: monthly samples. In: Office for Waste, Water, Energy and Air, Department of Water Protection. Retrieved September 29, 2017 .
- ↑ a b Reppisch-Dietikon. (PDF) Position 572: monthly samples. In: Office for Waste, Water, Energy and Air, Department of Water Protection. Retrieved September 29, 2017 .
- ↑ Eco-Corridor Reppisch Website of the municipality of Stallikon
- ↑ a b c Reppisch natural corridor worthy of protection (PDF) Website of the municipality of Stallikon.
- ↑ Reppisch outflow Türlersee. (PDF) Position 135: monthly samples. In: Office for Waste, Water, Energy and Air, Department of Water Protection. Retrieved October 5, 2015 .
- ^ Reppisch at Stallikon. (PDF) Position 136: monthly samples. In: Office for Waste, Water, Energy and Air, Department of Water Protection. Retrieved October 5, 2015 .
- ^ Reppisch to ARA Birmensdorf. (PDF) Position 155: monthly samples. In: Office for Waste, Water, Energy and Air, Department of Water Protection. Retrieved October 5, 2015 .
- ↑ a b catchment area Limmat and Reppisch. (PDF) Final report. In: Office for Waste, Water, Energy and Air, Department of Water Protection. Retrieved October 7, 2015 .
- ↑ Total catchment area number 128631. In: Topographical catchment areas of Swiss waters: area outlets . Retrieved October 13, 2015 .
- ^ A b Sophie Rüesch: Over and over again floods - the beloved enemy Reppisch. In: Limmattaler Zeitung . April 22, 2014.
- ↑ Revitalization of the Reppisch near Stallikon - a balance sheet (PDF) ( Memento of the original from October 6, 2015 in the Internet Archive ) Info: The archive link has been inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. FORNAT AG - Research for nature conservation and use.
- ↑ a b The Albiskette-Reppischtal nature reserve, by Hans Leidbundgut in Zurich Nature Conservation Objects of National Scientific Significance by Natural Research Society in Zurich.
- ↑ a b BLN object no. 1306: Albiskette -Reppischtal site of the Pro Uetliberg association.
- ↑ First successes in the fight against balsam and goldenrod community association Stallikon.
- ^ Project Eisvogelbrutwand page of the Reppisch association.
- ↑ Report and proposal from the government council to the cantonal council on the urgent postulate KR no. 201/2007 regarding contributions for substitute plantings on high-stem fruit trees lost due to fire blight (PDF) Official Journal of the Canton of Zurich.
- ^ Albert Heim: Molasseland and Jura Mountains . H. Tauchnitz, 1919 ( Räppisch on p. 385 in the Google book search).
- ↑ Borders, waters and terrain (PDF)
- ^ The last ice age around Zurich (PDF), edited by J. Hug by the Natural Research Society in Zurich.
- ↑ Urdorf field names (PDF)
- ^ Daniel Gut: Lunnern. London's twin in the Reuss Valley: a linguistic and cultural-historical location of settlement names . BoD - Books on Demand, 2013, p. 124 ( Reppisch on p. 50 in Google book search).
- ↑ Neujahrsblatt von Dietikon 1949, place and field names of Dietikon (PDF), from Karl Heid Commission for local history Dietikon.
- ↑ a b Albrecht Greule: Pre and early Germanic river names on the Upper Rhine . Winter, 1973, p. 228 ( Reppisch on p. 144 in Google book search).
- ^ Heinrich Meyer: The place names of the canton of Zurich: collected from the documents and explained . Meyer and Zeller, 1848, p. 183 ( Reppisch on p. 156 in the Google book search).
- ↑ a b Entry for the Reppisch on Ortsnamen.ch.
- ^ Gerold Meyer von Knonau: The regests of the former Cistercian Abbey Cappel in the Canton of Zurich . Hitz, 1850, p. 31 ( Reppisch on p. 31 in the Google book search).
- ↑ a b Dietikon: City air and village spirit: from the beginnings to the present . Chronos, 2003, p. 319 ( Reppisch on p. 44 in the Google book search).
- ↑ a b Sandro Zimmerli: The Reppisch Quiz: Test your knowledge! In: Limmattaler Zeitung. September 1, 2015.
- ↑ See the sources
- ↑ Gerold Meyer von Knonau: The Canton Zurich, historically, geographically and statistically portrayed from the oldest times to the present . Huber and Compagnie, 1846, p. 567 ( Reppisch on p. 420 in the Google book search).
- ↑ Storm damage in Switzerland in 2007 (PDF) ( Memento of the original from March 4, 2016 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. Federal Research Institute for Forests, Snow and Landscape WSL.
- ↑ History of the STV Dietikon ( Memento of the original from October 6, 2015 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. Site of the Dietikon gymnastics club.
- ↑ Flood protection Dietikon ( page no longer available , search in web archives ) Info: The link was automatically marked as defective. Please check the link according to the instructions and then remove this notice. Website of the Dietikon community.
- ↑ Severe weather hazard map (PDF) Spatial Development Department and Landscape and Waters Department of the Canton of Aargau.
- ↑ Flyer Reppisch (PDF) Website of the municipality of Stallikon.
