The passenger ship, which travels between the lake centers during the season, is also appropriate for exploring Lake Altmühlsee in a relaxed method. 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 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 a component of the primary-Danube Canal, which is accompanied on this route on the left and proper by quite a few remnants of its predecessor, the Ludwig-Donau-Principal Canal, a number of of which are additionally related to it. From here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the japanese move across the Altmühlsee. Part additionally runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to under 418 m above sea degree.

Hesselbach, from the left and north-northeast to beneath 418 m above sea level. The lower Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to beneath 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the right department of the previous one at around 414 m above sea degree. Drains in an analogous meandering course as the Fallach mentioned above to beneath 414 m above sea stage. Arises below 420 m above sea stage. Arises at round 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 right and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at beneath 414.9 m above sea level. Northeast at underneath 418 m above sea level. Arises at round 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 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 fitting; The final one arises instantly on the Altmühl feeder and seems to be the decrease reaches of an previous proper estuary of the Wieseth, which is not steady due to the construction 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 branch north of the mill, the secondary branch about 500 meters west of it. The 2 upper reaches up to the Heidweiher are additionally called Wiesengraben. There are also two moats in direction of the top of the mountain spur, one in all which is still six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the local space, barely offset in front of a dry valley mouth from the route of Riedenburg--Perletzhofen, from where supply from sinkholes has been proven. Typically karstification additionally results in the formation of a lake district, such as 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 level. North at over 405 m above sea degree. 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 seashore of Unterwurmbach only 100 meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Heart and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely as the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The listing of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally referred to as Schambach, from left and east to less than 410 m above sea level. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn constructing to 415.Three m above sea level. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of Esbach) → Birkengraben → Upper 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 stage.