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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 method. 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: Historic Atlas of Bavaria, a part of Franconia. From here the Altmühl is half of the primary-Danube Canal, which is accompanied on this route on the left and proper by numerous remnants of its predecessor, the Ludwig-Donau-Important Canal, some of that are also connected to it. From here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the japanese circulate around the Altmühlsee. Section additionally runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment area. Schafgraben, from the left and northwest to beneath 418 m above sea degree.

Hesselbach, from the left and north-northeast to beneath 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the suitable branch of the earlier one at round 414 m above sea degree. Drains in the same meandering course as the Fallach mentioned above to below 414 m above sea degree. Arises below 420 m above sea stage. Arises at around 420 m above sea level. Flows at about 420 m above sea degree. Wieseth, from the fitting and southeast or southwest to under 416 m above sea degree. Roßbachgraben, from the precise and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the fitting and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at beneath 414.9 m above sea stage. Northeast at below 418 m above sea level. Arises at around 418 m above sea level. Arises at over 418 m above sea level. 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 degree. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the best; The last one arises immediately on the Altmühl feeder and seems to be the decrease reaches of an outdated right estuary of the Wieseth, which is no longer steady because of the construction of the Altmühl feeder, as a result of 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 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 2 upper reaches as much as the Heidweiher are also known as Wiesengraben. There are additionally two moats towards the end of the mountain spur, considered one of which is still six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the local space, barely offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where provide from sinkholes has been proven. Typically karstification also leads to 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 degree. 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 level. NN on the northwest beach 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 Center and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well because the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The checklist of landscapes in Bavaria is based 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 constructing to 415.Three m above sea degree. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises below 365 m above sea level.

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