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 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: Historic Atlas of Bavaria, a part of Franconia. From right here the Altmühl is part of the primary-Danube Canal, which is accompanied on this route on the left and right by numerous remnants of its predecessor, the Ludwig-Donau-Predominant Canal, a number of 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 jap movement across the Altmühlsee. Part also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee (Full Document) in the Rednitz catchment space. 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 level. 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 level. This floodplain ditch is the correct department of the earlier one at around 414 m above sea stage. Drains in an analogous meandering course as the Fallach talked about above to below 414 m above sea stage. Arises beneath 420 m above sea stage. Arises at round 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the precise and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the proper and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at under 414.9 m above sea stage. Northeast at beneath 418 m above sea stage. Arises at round 418 m above sea level. Arises at over 418 m above sea degree. Ant ditch, from the left and north-northwest at 418 m above sea degree. 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 proper; The final one arises immediately on the Altmühl feeder and appears to be the lower reaches of an old right estuary of the Wieseth, which is no longer steady attributable 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.
Within 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 department north of the mill, the secondary branch about 500 meters west of it. The two higher reaches up to the Heidweiher are additionally called Wiesengraben. There are additionally two moats inside the course of the top of the mountain spur, one in every of which continues to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the local area, barely offset in entrance of a dry valley mouth from the route of Riedenburg–Perletzhofen, from where supply from sinkholes has been proven. Sometimes 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 level. Raingraben, from the left and north at over 416 m above sea stage. 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 stage.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest beach 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 Middle and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well as the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The listing of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally referred to as 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 building to 415.3 m above sea stage. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Higher Kuhgraben → Decrease 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 stage.