The passenger ship, which travels between the lake centers throughout the season, is also appropriate for exploring Lake Altmühlsee (read this blog post from sangjin.recossia.gethompy.com) 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 here the Altmühl is a part of the primary-Danube Canal, which is accompanied on this route on the left and right by quite a lot of remnants of its predecessor, the Ludwig-Donau-Most important Canal, a few of that are also related to it. From right here, the Altmühl flows in an synthetic course on a larger scale approximately east-southeast to the japanese circulation around the Altmühlsee. Part also 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 beneath 418 m above sea degree.

Hesselbach, from the left and north-northeast to under 418 m above sea degree. The lower Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to under 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea degree. This floodplain ditch is the best department of the previous one at around 414 m above sea stage. Drains in an identical meandering course as the Fallach mentioned above to under 414 m above sea degree. Arises under 420 m above sea level. Arises at round 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the precise and southeast or southwest to beneath 416 m above sea stage. 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 degree. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at below 414.9 m above sea level. Northeast at beneath 418 m above sea degree. 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 level. 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 best; The last one arises straight on the Altmühl feeder and appears to be the lower reaches of an old right estuary of the Wieseth, which is now not steady because of the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other 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 higher reaches as much as the Heidweiher are additionally called Wiesengraben. There are also two moats in path of the end of the mountain spur, certainly one of which continues to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the native space, barely offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where supply from sinkholes has been proven. Typically karstification also results in the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 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 level. 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 stage. NN on the northwest seashore of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Center and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly as the Birkenmühle and the Langweidmühle in 1806 passed 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 called Schambach, from left and east to less than 410 m above sea stage. → 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 identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Upper 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 stage.