The passenger ship, which travels between the lake centers during the season, can 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 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 main-Danube Canal, which is accompanied on this route on the left and proper by numerous remnants of its predecessor, the Ludwig-Donau-Essential Canal, a few of which are also linked to it. From here, the Altmühl flows in an synthetic course on a bigger scale roughly east-southeast to the jap stream across the Altmühlsee. Section also runs underground beneath 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 higher Bankertsgraben from the left and northwest to beneath 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the best branch of the previous one at round 414 m above sea degree. Drains in a similar meandering course because the Fallach mentioned above to beneath 414 m above sea stage. Arises under 420 m above sea stage. Arises at around 420 m above sea stage. Flows at about 420 m above sea stage. Wieseth, from the fitting and southeast or southwest to below 416 m above sea degree. Roßbachgraben, from the fitting and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at below 414.9 m above sea stage. Northeast at under 418 m above sea stage. Arises at around 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 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 proper; The last one arises straight on the Altmühl feeder and seems to be the lower reaches of an previous proper estuary of the Wieseth, which is not continuous on account of the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite side of the feeder, which now flows is initiated into this.

In 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 2 higher reaches up to the Heidweiher are also known as Wiesengraben. There are additionally two moats towards the end 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 native space, slightly offset in entrance of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from where provide from sinkholes has been confirmed. Generally karstification additionally 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 level. Raingraben, from the left and north at over 416 m above sea degree. North at over 405 m above sea level. 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 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 solely a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Heart and on account 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 brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also referred to as Schambach, from left and east to less than 410 m above sea degree. → 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 title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Higher Kuhgraben → Lower 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 degree.