Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers in the course of the season, is also suitable 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 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: Historical Atlas of Bavaria, a part of Franconia. From here the Altmühl is a component of the main-Danube Canal, which is accompanied on this route on the left and proper by plenty of remnants of its predecessor, the Ludwig-Donau-Predominant Canal, just a few of which are additionally related to it. From right here, the Altmühl flows in an artificial course on a larger scale approximately east-southeast to the eastern move around the Altmühlsee. Section also runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. Schafgraben, from the left and northwest to under 418 m above sea level.

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 around 414 m above sea level. This floodplain ditch is the appropriate department of the earlier one at around 414 m above sea level. Drains in an analogous meandering course because the Fallach mentioned above to below 414 m above sea level. Arises under 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the fitting and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the appropriate and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at under 414.9 m above sea degree. Northeast at beneath 418 m above sea degree. Arises at around 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 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 precise; The last one arises straight on the Altmühl feeder and appears to be the decrease reaches of an previous right estuary of the Wieseth, which is now not continuous because of the construction 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 trail continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the main branch north of the mill, the secondary department about 500 meters west of it. The 2 upper reaches up to the Heidweiher are additionally called Wiesengraben. There are additionally two moats in the path of the tip of the mountain spur, certainly one of which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the native area, barely offset in entrance of a dry valley mouth from the course of Riedenburg--Perletzhofen, from where supply from sinkholes has been confirmed. Generally karstification also leads to the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 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 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 level.

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 previous one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Center and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as effectively because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The listing of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally known as Schambach, from left and east to less 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 degree. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Higher Kuhgraben → Lower Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises beneath 365 m above sea level.

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