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The passenger ship, which travels between the lake centers through the season, can be suitable for exploring Lake Altmühlsee in a relaxed method. 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 right by a number of remnants of its predecessor, the Ludwig-Donau-Important Canal, a couple of of which are additionally linked to it. From right here, the Altmühl flows in an synthetic course on a bigger scale roughly east-southeast to the japanese circulate around the Altmühlsee. Section also runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to below 418 m above sea stage.

Hesselbach, from the left and north-northeast to under 418 m above sea stage. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the fitting branch of the previous one at round 414 m above sea degree. Drains in an identical meandering course as the Fallach mentioned above to beneath 414 m above sea level. Arises below 420 m above sea stage. Arises at around 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the proper and southeast or southwest to beneath 416 m above sea stage. Roßbachgraben, from the suitable and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at under 414.9 m above sea degree. Northeast at underneath 418 m above sea degree. Arises at around 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 level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the suitable; The final one arises immediately on the Altmühl feeder and seems to be the decrease reaches of an previous proper estuary of the Wieseth, which is not steady due to the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other side of the feeder, which now flows is initiated into this.

In 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 2 higher reaches as much as the Heidweiher are also known as Wiesengraben. There are also two moats in direction of the end of the mountain spur, one in all which remains to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN within the native area, barely offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where provide from sinkholes has been confirmed. Typically karstification also results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 416 m above sea level. Raingraben, from the left and north at over 416 m above sea stage. 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 level. NN on the northwest seashore of Unterwurmbach only 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Heart and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly as the Birkenmühle and the Langweidmühle in 1806 passed to the 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 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 415.3 m above sea degree. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises under 365 m above sea level.

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