Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers through the season, is also suitable for exploring Lake Altmühlsee in a relaxed manner. A transport 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, part of Franconia. From right here the Altmühl is an element of the principle-Danube Canal, which is accompanied on this route on the left and right by plenty of remnants of its predecessor, the Ludwig-Donau-Most important Canal, some of which are also linked to it. From right here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the japanese circulation around the Altmühlsee. Section 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 beneath 418 m above sea level.

Hesselbach, from the left and north-northeast to under 418 m above sea degree. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to beneath 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the suitable branch of the earlier one at round 414 m above sea stage. Drains in an analogous meandering course as the Fallach talked about above to under 414 m above sea degree. Arises beneath 420 m above sea stage. Arises at around 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the appropriate and southeast or southwest to beneath 416 m above sea stage. Roßbachgraben, from the appropriate and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at below 414.9 m above sea stage. Northeast at under 418 m above sea stage. Arises at around 418 m above sea degree. 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 degree. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the suitable; The last one arises immediately on the Altmühl feeder and appears to be the lower reaches of an previous proper estuary of the Wieseth, which is now not continuous because of the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite side 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 department north of the mill, the secondary department about 500 meters west of it. The 2 upper reaches up to the Heidweiher are also referred to as Wiesengraben. There are additionally two moats towards the tip of the mountain spur, considered one of which is still six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the native space, barely offset in entrance of a dry valley mouth from the course of Riedenburg–Perletzhofen, from where provide from sinkholes has been confirmed. Sometimes karstification additionally leads to 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 level. North at over 405 m above sea degree. 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 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 properly because the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The checklist of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also called 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 name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Higher Kuhgraben → Decrease 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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