The passenger ship, which travels between the lake centers through the season, can be appropriate for exploring Lake Altmühlsee in a relaxed method. 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 right here the Altmühl is part of the main-Danube Canal, which is accompanied on this route on the left and proper by quite a lot of remnants of its predecessor, the Ludwig-Donau-Important Canal, a couple of of which are also linked to it. From here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the jap movement across the Altmühlsee. Part additionally runs underground below 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 stage.

Hesselbach, from the left and north-northeast to below 418 m above sea level. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea level. This floodplain ditch is the best branch of the earlier one at around 414 m above sea degree. Drains in an analogous meandering course as the Fallach talked about above to beneath 414 m above sea level. Arises under 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the appropriate and southeast or southwest to below 416 m above sea degree. Roßbachgraben, from the best 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 known as Häfelesgraben, at under 414.9 m above sea stage. Northeast at underneath 418 m above sea level. Arises at round 418 m above sea degree. Arises at over 418 m above sea degree. 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 correct; The final one arises directly on the Altmühl feeder and seems to be the decrease reaches of an outdated right estuary of the Wieseth, which is now not steady on account of 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.

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 main branch north of the mill, the secondary department about 500 meters west of it. The two higher reaches as much as the Heidweiher are also known as Wiesengraben. There are additionally two moats in direction of the end of the mountain spur, one among which continues to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the native space, slightly offset in entrance of a dry valley mouth from the course of Riedenburg--Perletzhofen, from where provide 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 under 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 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 stage. 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. Because of the Reich Deputation Heart and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly because the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally known 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 415.3 m above sea stage. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Higher Kuhgraben → Lower Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises under 365 m above sea level.