The passenger ship, which travels between the lake centers throughout the season, is also suitable for exploring Lake Altmühlsee in a relaxed manner. A shipping 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 part of the main-Danube Canal, which is accompanied on this route on the left and right by a variety of remnants of its predecessor, the Ludwig-Donau-Important Canal, a number of of that are also connected to it. From here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the eastern flow across the Altmühlsee. Section additionally runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to below 418 m above sea level.

Hesselbach, from the left and north-northeast to under 418 m above sea level. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the suitable branch of the previous one at around 414 m above sea degree. Drains in an analogous meandering course because the Fallach mentioned above to below 414 m above sea stage. Arises under 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea degree. Wieseth, from the correct and southeast or southwest to below 416 m above sea stage. Roßbachgraben, from the appropriate and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at under 414.9 m above sea stage. Northeast at beneath 418 m above sea stage. 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 degree. Betzengraben, from the left and north to over 416 m above sea level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the fitting; The last one arises instantly on the Altmühl feeder and seems to be the lower reaches of an old right estuary of the Wieseth, which is now not steady ensuing from the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite facet of the feeder, which now flows is initiated into this.

In 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 principle department north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches as much as the Heidweiher are additionally known as Wiesengraben. There are also two moats in path of the top of the mountain spur, certainly one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the native area, slightly offset in entrance of a dry valley mouth from the route of Riedenburg–Perletzhofen, from the place provide from sinkholes has been proven. Typically karstification also results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea stage. 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 degree.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seaside of Unterwurmbach solely a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because 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 relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally called Schambach, from left and east to lower than 410 m above sea stage. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.3 m above sea level. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Upper Kuhgraben → Lower 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.

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