The passenger ship, which travels between the lake centers through the season, can be appropriate for exploring Lake Altmühlsee in a relaxed method. 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: Historic Atlas of Bavaria, a part of Franconia. From right here the Altmühl is an element of the principle-Danube Canal, which is accompanied on this route on the left and right by plenty of remnants of its predecessor, the Ludwig-Donau-Principal Canal, some of which are also related to it. From here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the eastern stream across 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 below 418 m above sea level.

Hesselbach, from the left and north-northeast to below 418 m above sea stage. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to below 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea stage. This floodplain ditch is the fitting branch of the earlier one at around 414 m above sea degree. Drains in an identical meandering course as the Fallach mentioned above to under 414 m above sea degree. Arises below 420 m above sea level. Arises at round 420 m above sea degree. Flows at about 420 m above sea level. Wieseth, from the right and southeast or southwest to beneath 416 m above sea degree. Roßbachgraben, from the best and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the correct 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 stage. Northeast at underneath 418 m above sea stage. Arises at around 418 m above sea level. Arises at over 418 m above sea degree. 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 stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the right; The final one arises straight on the Altmühl feeder and seems to be the lower reaches of an outdated proper estuary of the Wieseth, which is no longer continuous as a consequence of the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other aspect 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 department north of the mill, the secondary branch about 500 meters west of it. The two higher reaches as much as the Heidweiher are additionally called Wiesengraben. There are also two moats towards the top of the mountain spur, considered one of which remains to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the local area, slightly offset in entrance of a dry valley mouth from the path of Riedenburg–Perletzhofen, from where provide from sinkholes has been proven. Typically karstification additionally results in 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 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 level.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea level. NN on the northwest seaside of Unterwurmbach only a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Heart and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely because 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 Research. Kästleinsmühlbach, partly also referred to as Schambach, from left and east to lower than 410 m above sea degree. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.3 m above sea stage. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Higher Kuhgraben → Lower 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 degree.

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