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The passenger ship, which travels between the lake centers during the season, is also appropriate 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 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, part of Franconia. From right here the Altmühl is half of the main-Danube Canal, which is accompanied on this route on the left and proper by plenty of remnants of its predecessor, the Ludwig-Donau-Main Canal, some of that are additionally linked to it. From right here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the japanese circulation across the Altmühlsee. Section also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee 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 beneath 418 m above sea level. 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 round 414 m above sea degree. This floodplain ditch is the correct department of the earlier one at round 414 m above sea level. Drains in an identical meandering course because the Fallach mentioned above to below 414 m above sea degree. Arises under 420 m above sea level. Arises at round 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the proper and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the fitting and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at beneath 414.9 m above sea level. Northeast at underneath 418 m above sea degree. Arises at round 418 m above sea degree. 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 correct; The last one arises immediately on the Altmühl feeder and seems to be the decrease reaches of an outdated proper estuary of the Wieseth, which is not steady as a result 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 trail 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 branch about 500 meters west of it. The two higher reaches as much as the Heidweiher are also referred to as Wiesengraben. There are additionally two moats inside the course of the top of the mountain spur, one among which is still six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the native area, slightly offset in front of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from where provide from sinkholes has been proven. Sometimes karstification additionally results in the formation of a lake district, such because 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 degree. North at over 405 m above sea stage. 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 level.

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Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. 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. Because of the Reich Deputation Heart and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely as the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also called 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.Three m above sea degree. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Higher Kuhgraben → Lower 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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