Swist
The Swist is a stream, long, in the German Rhineland. It rises on the northern edge of the Eifel at 330 metres above sea level and empties from the right and southeast into the Rhine tributary, the Erft, between Weilerswist and (a district of Erftstadt). Occasionally the Swist is also called the "Swistbach", and locals often just call it "der Bach" ("the stream"). The Swist flows through the municipality Swisttal, the town of Meckenheim and Flerzheim. There are cycle paths by the side of the stream along this stretch. The Swist gave its name to Swisttal and the town  of Weilerswist. Its source area is situated at the northern edge of the Eifel. Geography. Course. Its source lies at in the northern part of the Eifel in the Ahr Hills, north of the village of Kalenborn in the collective municipality of Altenahr in the county of Ahrweiler. The Swist has an average gradient of 5 ‰ and flows initially to Vettelhoven (Grafschaft) in a northeasterly direction and then descends at a gradient of just 1.3 ‰ through the Fore-Eifel. It continues along the western slopes of the hill ridge in the börde landscape of the Rheinbach Loess Plateau through Meckenheim , Flerzheim, Morenhoven, Heimerzheim and . At the Swist empties into the Erft between Weilerswist and Bliesheim. Catchment. Its catchment area lies between that of the Rhine near Bonn and its smaller tributaries like the Hardtbach or to the northwest and that of its parent river, the Erft around Euskirchen right in the west and peters out quickly towards the north-northwest. It is rural and, in the open country, arable fields predominate. Around the upper courses of the stream and its especially along its important left-hand tributaries there is a large contiguous forest as well as pastures and meadows. The  largest part of the catchment belongs to the state of North Rhine-Westphalia, the source region is in Rhineland-Palatinate. Tributaries. The most important tributary of the Swist is the "Steinbach", which joins from the left at river kilometre 15.7 as the "Jungbach". Between and Essig it bears the name "Orbach". The stream has a catchment of which is about 17% that of the Swist. The tributaries of the Swist are listed below. River history. Originally the River Ahr flowed in what is now the riverbed of the Swist. After the uplifting of the Ahr Hills, and its route northwards  was barred, the Ahr tried to find a way directly to the Rhine. In places it is said that the Swist is the longest stream (i.e. German "Bach", small river) in Europe This probably goes back to when its course was marked by wide meanders in the area of the low gradient between Vettelhoven and its mouth. Since the straightening of the Swist in the early 20th century and certainly no later than its canalisation in the 1960s it has probably lost this record. Historic bridges. The Roman aqueduct to Cologne crossed the valley of the Swist between Meckenheim and  Rheinbach on an arched bridge which was 1,400 metres long and up to 10 metres high. Archaeologists have worked out that the bridge must have once had 295 arches with an inside width of . Nothing is left of the structure apart from a low strip of rubble. In Lützermiel the foundations of a Prussian bridge have survived. The bridge once carried the district road ("Bezirksstraße") from Bonn to Schleiden, built in 1823, over the Swist.