Retrieved January 19, 2023 (English)

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 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 here the Altmühl is part of the main-Danube Canal, which is accompanied on this route on the left and right by various remnants of its predecessor, the Ludwig-Donau-Predominant Canal, just a few of that are additionally related to it. From right here, the Altmühl flows in an synthetic course on a larger scale approximately east-southeast to the eastern flow around the Altmühlsee. Section additionally runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to beneath 418 m above sea stage.

Hesselbach, from the left and north-northeast to under 418 m above sea level. 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 suitable branch of the previous one at around 414 m above sea stage. Drains in an identical meandering course because the Fallach mentioned above to below 414 m above sea stage. Arises beneath 420 m above sea level. Arises at around 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the suitable and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the fitting and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at below 414.9 m above sea stage. Northeast at underneath 418 m above sea level. Arises at round 418 m above sea level. Arises at over 418 m above sea stage. 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 precise; The last one arises immediately on the Altmühl feeder and seems to be the lower reaches of an old right estuary of the Wieseth, which is now not continuous resulting from the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite aspect 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 branch north of the mill, the secondary department about 500 meters west of it. The two upper reaches as much as the Heidweiher are also called Wiesengraben. There are also two moats inside the route of the top of the mountain spur, considered one of which is still six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN within the native area, barely offset in entrance of a dry valley mouth from the route of Riedenburg--Perletzhofen, from the place provide from sinkholes has been proven. Sometimes 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 level. Raingraben, from the left and north at over 416 m above sea level. 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 stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seaside of Unterwurmbach only 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Middle and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely because the Birkenmühle and the Langweidmühle in 1806 handed to the brand 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 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 building to 415.Three m above sea level. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means 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 under 365 m above sea stage.


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