The passenger ship, which travels between the lake centers through the season, is also suitable for exploring Lake Altmühlsee in a relaxed manner. 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 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 primary-Danube Canal, which is accompanied on this route on the left and right by a lot of remnants of its predecessor, the Ludwig-Donau-Fundamental Canal, some of which are also related to it. From here, the Altmühl flows in an synthetic course on a bigger scale roughly east-southeast to the japanese circulate around the Altmühlsee. Section also runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. Schafgraben, from the left and northwest to beneath 418 m above sea stage.

Hesselbach, from the left and north-northeast to below 418 m above sea degree. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the precise branch of the previous one at round 414 m above sea stage. Drains in the same meandering course because the Fallach mentioned above to under 414 m above sea level. Arises below 420 m above sea degree. Arises at round 420 m above sea stage. Flows at about 420 m above sea level. Wieseth, from the appropriate and southeast or southwest to under 416 m above sea degree. Roßbachgraben, from the fitting and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at below 414.9 m above sea degree. Northeast at underneath 418 m above sea stage. Arises at around 418 m above sea stage. Arises at over 418 m above sea stage. 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 right; The final one arises instantly on the Altmühl feeder and appears to be the decrease reaches of an outdated right estuary of the Wieseth, which is now not continuous as a result of the development of the Altmühl feeder, because 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 trail 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 additionally referred to as Wiesengraben. There are additionally two moats towards the end of the mountain spur, considered one of which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the local area, barely offset in front of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from the place provide from sinkholes has been confirmed. Generally karstification additionally results in the formation of a lake district, such as 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 degree. North at over 405 m above sea stage. 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 level. NN on the northwest seaside 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 Middle and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely as the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The record of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also called 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 building to 415.3 m above sea level. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part 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 beneath 365 m above sea degree.