The passenger ship, which travels between the lake centers through the season, can be appropriate for exploring Lake Altmühlsee in a relaxed manner. A transport 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 part of the primary-Danube Canal, which is accompanied on this route on the left and right by a variety of remnants of its predecessor, the Ludwig-Donau-Primary Canal, some of which are additionally connected to it. From right here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the jap circulation around the Altmühlsee. Section additionally 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 below 418 m above sea level. The decrease 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 around 414 m above sea stage. This floodplain ditch is the correct department of the previous one at round 414 m above sea stage. Drains in a similar meandering course as the Fallach mentioned above to beneath 414 m above sea stage. Arises below 420 m above sea degree. Arises at around 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the fitting and southeast or southwest to under 416 m above sea degree. Roßbachgraben, from the suitable and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at under 414.9 m above sea stage. Northeast at under 418 m above sea stage. 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 stage. 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 suitable; The final one arises straight on the Altmühl feeder and seems to be the decrease reaches of an previous proper estuary of the Wieseth, which is no longer continuous attributable to the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other facet of the feeder, which now flows is initiated into this.

Within 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 upper reaches up to the Heidweiher are also called Wiesengraben. There are also two moats in direction of the tip of the mountain spur, one among which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN within the native area, slightly offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Generally karstification also leads to the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 416 m above sea degree. 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 degree. 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 beach of Unterwurmbach only a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Center 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 brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also 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 constructing to 415.Three m above sea stage. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea level.

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