Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers in the course of the season, can also be appropriate for exploring Lake Altmühlsee in a relaxed manner. A delivery line on which the MS Altmühlsee operates connects the three lake centers (Wald, Muhr am See and Schlungenhof). Weißenburg-Gunzenhausen district: Northern and western part of the district, with the communities of Absberg, Alesheim, Muhr a.See, Bergen, Burgsalach, Dittenheim, Ellingen, Ettenstatt, Gnotzheim, Gunzenhausen, Haundorf, Heidenheim, Höttingen, Markt Berolzheim, Meinheim, Nennslingen, Pfofeld, Pleinfeld, Polsingen, Raitenbuch, Theilenhofen and Westheim. In: Historic Atlas of Bavaria, a part of Franconia. From right here the Altmühl is a component of the main-Danube Canal, which is accompanied on this route on the left and right by quite a lot of remnants of its predecessor, the Ludwig-Donau-Essential Canal, some of which are additionally connected to it. From right here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the eastern move around the Altmühlsee. Section additionally runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. Schafgraben, from the left and northwest to under 418 m above sea stage.

Hesselbach, from the left and north-northeast to below 418 m above sea level. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea level. This floodplain ditch is the fitting branch of the earlier one at around 414 m above sea level. Drains in an identical meandering course as the Fallach talked about above to beneath 414 m above sea degree. Arises beneath 420 m above sea stage. Arises at round 420 m above sea level. Flows at about 420 m above sea degree. Wieseth, from the precise and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the proper and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at beneath 414.9 m above sea level. Northeast at beneath 418 m above sea degree. Arises at around 418 m above sea stage. Arises at over 418 m above sea degree. Ant ditch, from the left and north-northwest at 418 m above sea level. Betzengraben, from the left and north to over 416 m above sea stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the suitable; The final one arises immediately on the Altmühl feeder and appears to be the lower reaches of an old right estuary of the Wieseth, which is not continuous attributable to the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other side of the feeder, which now flows is initiated into this.

Within the Franconian Lake District the trail continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the main branch north of the mill, the secondary branch about 500 meters west of it. The two upper reaches up to the Heidweiher are additionally called Wiesengraben. There are additionally two moats towards the top of the mountain spur, certainly one of which remains to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the native area, slightly offset in front of a dry valley mouth from the course of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Sometimes karstification also results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 416 m above sea degree. Raingraben, from the left and north at over 416 m above sea level. North at over 405 m above sea degree. Heglauer Mühlbach, from the left and north at over 414.7 m above sea level. Inlet of the Heidental dry valley, from the left and north at 338.2 m above sea level.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea level. NN on the northwest beach of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Center and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly because the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The record of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also called Schambach, from left and east to lower than 410 m above sea degree. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn constructing to 415.Three m above sea degree. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises below 365 m above sea level.