The passenger ship, which travels between the lake centers during the season, can also 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 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: Historical Atlas of Bavaria, a 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 proper by numerous remnants of its predecessor, the Ludwig-Donau-Main Canal, just a few of that are additionally linked to it. From right here, the Altmühl flows in an artificial course on a larger scale approximately east-southeast to the japanese circulate across the Altmühlsee. Part also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment space. Schafgraben, from the left and northwest to below 418 m above sea stage.
Hesselbach, from the left and north-northeast to beneath 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to under 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the correct department of the previous one at around 414 m above sea level. Drains in an identical meandering course because the Fallach mentioned above to below 414 m above sea stage. Arises beneath 420 m above sea degree. Arises at round 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the suitable and southeast or southwest to beneath 416 m above sea stage. Roßbachgraben, from the precise and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the suitable 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 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 precise; The final one arises immediately on the Altmühl feeder and appears to be the decrease reaches of an old proper estuary of the Wieseth, which is now not continuous resulting from the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other aspect 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 primary branch north of the mill, the secondary department about 500 meters west of it. The 2 upper reaches as much as the Heidweiher are additionally called Wiesengraben. There are additionally two moats towards 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 inside the native space, slightly offset in front of a dry valley mouth from the route of Riedenburg--Perletzhofen, from the place provide from sinkholes has been confirmed. Generally karstification also leads to the formation of a lake district, such because 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 stage. 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 degree.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seaside of Unterwurmbach only 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Center and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The list of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally called Schambach, from left and east to lower than 410 m above sea degree. → 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 identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Upper 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 degree.
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