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The passenger ship, which travels between the lake centers in the course of the season, can also be appropriate for exploring Lake Altmühlsee in a relaxed manner. 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 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: Historic Atlas of Bavaria, a part of Franconia. From right here the Altmühl is part of the main-Danube Canal, which is accompanied on this route on the left and right by a lot of remnants of its predecessor, the Ludwig-Donau-Primary Canal, some of that are additionally linked to it. From right here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the japanese stream across the Altmühlsee. Section also runs underground below 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 level.

Hesselbach, from the left and north-northeast to below 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to under 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea stage. This floodplain ditch is the precise department of the earlier one at round 414 m above sea level. Drains in a similar meandering course as the Fallach mentioned above to beneath 414 m above sea degree. Arises under 420 m above sea degree. Arises at around 420 m above sea stage. Flows at about 420 m above sea level. Wieseth, from the precise and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the proper and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the correct and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at below 414.9 m above sea level. Northeast at beneath 418 m above sea degree. 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 level. 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 right; The last one arises immediately on the Altmühl feeder and seems to be the decrease reaches of an old proper estuary of the Wieseth, which is now not continuous because of the construction of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other aspect 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 principle department north of the mill, the secondary department about 500 meters west of it. The two higher reaches up to the Heidweiher are additionally referred to as Wiesengraben. There are additionally two moats in route of the top of the mountain spur, one of which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the native space, slightly offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from the place provide from sinkholes has been confirmed. Sometimes karstification additionally leads to the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 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 level. Heglauer Mühlbach, from the left and north at over 414.7 m above sea degree. 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 earlier one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Middle and because 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 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 additionally 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 building to 415.Three m above sea level. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of 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 below 365 m above sea level.

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