The passenger ship, which travels between the lake centers through the season, can be 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 a 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: Historical Atlas of Bavaria, part of Franconia. From here the Altmühl is a part of the main-Danube Canal, which is accompanied on this route on the left and right by quite a few remnants of its predecessor, the Ludwig-Donau-Predominant Canal, some of which are additionally related to it. From right here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the jap move across the Altmühlsee. Section also runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment space. Schafgraben, from the left and northwest to under 418 m above sea level.

Hesselbach, from the left and north-northeast to under 418 m above sea degree. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to below 414.9 m above sea stage. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the appropriate department of the earlier one at round 414 m above sea level. Drains in an identical meandering course as the Fallach talked about above to below 414 m above sea degree. Arises under 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the proper and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the fitting and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at under 414.9 m above sea level. Northeast at underneath 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 stage. 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 appropriate; The final one arises immediately on the Altmühl feeder and appears to be the decrease reaches of an old right estuary of the Wieseth, which is not steady on account of the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite aspect of the feeder, which now flows is initiated into this.

In the Franconian Lake District the path continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the primary department north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches up to the Heidweiher are additionally called Wiesengraben. There are additionally two moats in course of the tip of the mountain spur, one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the local space, barely offset in front of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from where supply from sinkholes has been proven. Typically karstification also leads to the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea degree. North at over 405 m above sea stage. 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 seashore of Unterwurmbach only a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Middle and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly as the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The listing of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally called Schambach, from left and east to less than 410 m above sea level. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.3 m above sea degree. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Upper Kuhgraben → Lower Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises below 365 m above sea degree.