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The passenger ship, which travels between the lake centers through 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 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 right here the Altmühl is a part of the primary-Danube Canal, which is accompanied on this route on the left and right by a number of remnants of its predecessor, the Ludwig-Donau-Principal Canal, some of that are also connected to it. From here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the jap flow around the Altmühlsee. Part additionally runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. Schafgraben, from the left and northwest to beneath 418 m above sea stage.

Hesselbach, from the left and north-northeast to beneath 418 m above sea degree. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to under 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea level. This floodplain ditch is the best branch of the earlier one at around 414 m above sea stage. Drains in the same meandering course because the Fallach mentioned above to below 414 m above sea level. Arises below 420 m above sea stage. Arises at round 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the proper and southeast or southwest to under 416 m above sea stage. Roßbachgraben, from the fitting and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the proper 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 underneath 418 m above sea level. Arises at round 418 m above sea stage. Arises at over 418 m above sea level. 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 proper; The final one arises immediately on the Altmühl feeder and seems to be the lower reaches of an previous right estuary of the Wieseth, which is no longer steady on account of the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other 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 primary department north of the mill, the secondary department about 500 meters west of it. The two upper reaches as much as the Heidweiher are additionally known as Wiesengraben. There are also two moats in course of the top of the mountain spur, certainly one of which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the native area, barely offset in front of a dry valley mouth from the route of Riedenburg--Perletzhofen, from the place provide from sinkholes has been proven. Sometimes 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 level. 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 stage. 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 degree. NN on the northwest seaside of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Center and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as effectively as the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The checklist of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally known as 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. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of 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 beneath 365 m above sea stage.



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