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The passenger ship, which travels between the lake centers during the season, can be appropriate 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 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 part of the primary-Danube Canal, which is accompanied on this route on the left and proper by a lot of remnants of its predecessor, the Ludwig-Donau-Main Canal, some of which are also linked to it. From here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the eastern flow across the Altmühlsee. Section also runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee within 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 below 418 m above sea level. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea level. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the best department of the previous one at around 414 m above sea stage. Drains in the same meandering course because the Fallach talked about above to below 414 m above sea stage. Arises beneath 420 m above sea level. Arises at around 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the appropriate and southeast or southwest to below 416 m above sea degree. Roßbachgraben, from the fitting and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at below 414.9 m above sea level. Northeast at underneath 418 m above sea degree. Arises at round 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 degree. 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 right; The final one arises instantly on the Altmühl feeder and appears to be the decrease reaches of an outdated proper estuary of the Wieseth, which is not continuous as a consequence of the construction of the Altmühl feeder, as a result of 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 path 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 branch about 500 meters west of it. The 2 upper reaches up to the Heidweiher are additionally referred to as Wiesengraben. There are also two moats inside the route of the tip of the mountain spur, one in all which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the local space, barely offset in entrance of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where supply 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 beneath 416 m above sea stage. 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 stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. NN on the northwest seaside of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Heart and on account 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 is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also known 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 constructing to 415.3 m above sea level. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify 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. Higher course and approx. 3.2 km². Arises beneath 365 m above sea stage.



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