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The passenger ship, which travels between the lake centers during the season, can be 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 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, part of Franconia. From right here the Altmühl is half of the main-Danube Canal, which is accompanied on this route on the left and right by a variety of remnants of its predecessor, the Ludwig-Donau-Fundamental Canal, some of which are also connected to it. From here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the japanese move around the Altmühlsee. Part additionally runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment space. Schafgraben, from the left and northwest to below 418 m above sea level.

Hesselbach, from the left and north-northeast to beneath 418 m above sea degree. The decrease 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 branch of the earlier one at round 414 m above sea level. Drains in an analogous meandering course as the Fallach talked about above to under 414 m above sea stage. Arises under 420 m above sea level. Arises at round 420 m above sea stage. Flows at about 420 m above sea level. Wieseth, from the correct and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the suitable and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at under 414.9 m above sea level. Northeast at beneath 418 m above sea degree. 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 stage. Betzengraben, from the left and north to over 416 m above sea stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the appropriate; The last one arises instantly on the Altmühl feeder and seems to be the decrease reaches of an old right estuary of the Wieseth, which is not continuous as a result of the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other facet 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 department about 500 meters west of it. The two higher reaches up to the Heidweiher are also called Wiesengraben. There are additionally two moats in path of the top of the mountain spur, one in every of which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the native space, slightly offset in entrance of a dry valley mouth from the route 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 below 416 m above sea level. 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 degree. 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 degree. NN on the northwest seaside of Unterwurmbach solely 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Center and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally 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 415.3 m above sea level. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of Esbach) → Birkengraben → Upper Kuhgraben → Lower Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea stage.

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