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The passenger ship, which travels between the lake centers through the season, is also 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 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 part of the primary-Danube Canal, which is accompanied on this route on the left and proper by a variety of remnants of its predecessor, the Ludwig-Donau-Predominant Canal, just a few of which are also related to it. From right here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the eastern circulation across the Altmühlsee. Part also runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee - click through the next document, 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 decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to below 414.9 m above sea degree. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the best department of the previous one at round 414 m above sea level. Drains in the same meandering course because the Fallach mentioned above to beneath 414 m above sea level. Arises below 420 m above sea stage. Arises at round 420 m above sea degree. Flows at about 420 m above sea level. Wieseth, from the right and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the precise and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the correct and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at below 414.9 m above sea stage. Northeast at beneath 418 m above sea level. Arises at around 418 m above sea stage. Arises at over 418 m above sea degree. 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 level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the best; The last one arises immediately on the Altmühl feeder and seems to be the lower reaches of an previous right estuary of the Wieseth, which is not steady as a consequence 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 path continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the primary branch north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches up to the Heidweiher are additionally called Wiesengraben. There are additionally two moats towards the top of the mountain spur, considered one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the local space, barely offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where supply from sinkholes has been proven. Generally 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 degree. 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 level. 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 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 nicely because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The record of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally referred to as Schambach, from left and east to lower than 410 m above sea level. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.3 m above sea stage. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Higher 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.