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The passenger ship, which travels between the lake centers during the season, is also suitable for exploring Lake Altmühlsee in a relaxed method. 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 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 here the Altmühl is an element of the main-Danube Canal, which is accompanied on this route on the left and right by numerous remnants of its predecessor, the Ludwig-Donau-Foremost Canal, just a few of that are also linked to it. From right here, the Altmühl flows in an synthetic course on a larger scale approximately east-southeast to the japanese move around the Altmühlsee. Part also runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee (look at these guys) in the Rednitz catchment space. Schafgraben, from the left and northwest to below 418 m above sea degree.

Hesselbach, from the left and north-northeast to below 418 m above sea stage. The lower Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to under 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the precise department of the earlier one at around 414 m above sea stage. Drains in the same meandering course as the Fallach talked about above to under 414 m above sea level. Arises beneath 420 m above sea degree. Arises at around 420 m above sea degree. 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 fitting and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at beneath 414.9 m above sea level. Northeast at below 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 degree. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the proper; The final one arises directly on the Altmühl feeder and appears to be the lower reaches of an outdated right estuary of the Wieseth, which is not continuous resulting from the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other 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 principle department north of the mill, the secondary branch about 500 meters west of it. The two upper reaches up to the Heidweiher are also known as Wiesengraben. There are additionally two moats in the course of the end of the mountain spur, one in every of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the native area, barely offset in entrance of a dry valley mouth from the route of Riedenburg--Perletzhofen, from where provide from sinkholes has been proven. Sometimes karstification additionally 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 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 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 level. NN on the northwest beach of Unterwurmbach only 100 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 effectively 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 Studies. Kästleinsmühlbach, partly additionally called Schambach, from left and east to lower 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 stage. Section identify 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 → Lower Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises below 365 m above sea degree.

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