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The passenger ship, which travels between the lake centers in the course of the season, is also 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, a part of Franconia. From here the Altmühl is half of the principle-Danube Canal, which is accompanied on this route on the left and right by numerous remnants of its predecessor, the Ludwig-Donau-Fundamental Canal, a number of of which are additionally connected to it. From right here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the jap circulation across the Altmühlsee. Section also runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee (Get More Information) within the Rednitz catchment space. Schafgraben, from the left and northwest to beneath 418 m above sea level.

Hesselbach, from the left and north-northeast to below 418 m above sea degree. The lower Schlegelsbühlgraben takes the higher 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 level. This floodplain ditch is the right branch of the earlier one at round 414 m above sea degree. Drains in the same meandering course as the Fallach talked about above to under 414 m above sea level. Arises beneath 420 m above sea level. Arises at round 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the best and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the appropriate and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at below 414.9 m above sea degree. Northeast at underneath 418 m above sea level. Arises at around 418 m above sea level. Arises at over 418 m above sea stage. 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 best; The final one arises immediately on the Altmühl feeder and appears to be the lower reaches of an old right estuary of the Wieseth, which is now not continuous due to the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite 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 branch north of the mill, the secondary branch about 500 meters west of it. The 2 upper reaches as much as the Heidweiher are additionally called Wiesengraben. There are also two moats inside the course of the top of the mountain spur, considered one of which continues to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN within the local area, slightly offset in entrance of a dry valley mouth from the path of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Sometimes karstification also leads to the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea degree. North at over 405 m above sea level. 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 seaside of Unterwurmbach solely 100 meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Center and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely as the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The record of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally referred to as Schambach, from left and east to lower 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 stage. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means 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 beneath 365 m above sea degree.