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The passenger ship, which travels between the lake centers in the course of 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 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, a part of Franconia. From right here the Altmühl is half of the primary-Danube Canal, which is accompanied on this route on the left and proper by plenty of remnants of its predecessor, the Ludwig-Donau-Foremost Canal, some of which are also related to it. From right here, the Altmühl flows in an artificial course on a larger scale approximately east-southeast to the jap flow around the Altmühlsee. Section also runs underground below 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 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 beneath 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 degree. Drains in an identical meandering course because the Fallach talked about above to below 414 m above sea level. Arises below 420 m above sea level. Arises at round 420 m above sea level. Flows at about 420 m above sea level. Wieseth, from the appropriate and southeast or southwest to beneath 416 m above sea degree. Roßbachgraben, from the fitting and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the correct and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at under 414.9 m above sea level. Northeast at under 418 m above sea degree. Arises at around 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 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 fitting; The final one arises immediately on the Altmühl feeder and seems to be the lower reaches of an old proper estuary of the Wieseth, which is not continuous as a consequence of the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite facet of the feeder, which now flows is initiated into this.

Within 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 primary department 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 also two moats towards the top of the mountain spur, certainly one of which is still six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the native space, slightly offset in entrance of a dry valley mouth from the course of Riedenburg–Perletzhofen, from the place supply from sinkholes has been proven. Typically karstification additionally 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 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 stage. 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 level. NN on the northwest seaside of Unterwurmbach only a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Heart 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 list of landscapes in Bavaria relies 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.Three m above sea stage. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by 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 under 365 m above sea level.

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