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The passenger ship, which travels between the lake centers through the season, is also suitable 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 here the Altmühl is an element of the principle-Danube Canal, which is accompanied on this route on the left and right by a variety of remnants of its predecessor, the Ludwig-Donau-Essential Canal, some of which are also related to it. From right here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the jap move across the Altmühlsee. Section additionally runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment area. Schafgraben, from the left and northwest to below 418 m above sea degree.

Hesselbach, from the left and north-northeast to under 418 m above sea level. 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 stage. This floodplain ditch is the best department of the previous one at round 414 m above sea degree. Drains in a similar meandering course because the Fallach talked about above to below 414 m above sea level. Arises beneath 420 m above sea degree. Arises at around 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the proper and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the right and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at beneath 414.9 m above sea level. Northeast at under 418 m above sea stage. Arises at round 418 m above sea degree. Arises at over 418 m above sea level. 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 level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the best; The last one arises directly on the Altmühl feeder and seems to be the decrease reaches of an old proper estuary of the Wieseth, which is now not continuous due to 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.

Within 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 principle branch 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 towards the tip of the mountain spur, one in every of which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the local space, barely offset in entrance of a dry valley mouth from the path of Riedenburg--Perletzhofen, from the place 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 level. Raingraben, from the left and north at over 416 m above sea level. North at over 405 m above sea level. 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 stage. NN on the northwest seaside of Unterwurmbach only 100 meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Middle and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well as the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The listing of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also 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.Three m above sea level. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify 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 beneath 365 m above sea stage.

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