The passenger ship, which travels between the lake centers through the season, is also suitable for exploring Lake Altmühlsee in a relaxed method. A shipping 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, part of Franconia. From right here the Altmühl is a part of the primary-Danube Canal, which is accompanied on this route on the left and proper by various remnants of its predecessor, the Ludwig-Donau-Essential Canal, some of which are also related to it. From right here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the jap flow across the Altmühlsee. Part 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 degree.
Hesselbach, from the left and north-northeast to below 418 m above sea level. 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 degree. This floodplain ditch is the precise branch of the earlier one at around 414 m above sea level. Drains in the same meandering course as the Fallach talked about above to below 414 m above sea degree. Arises below 420 m above sea degree. Arises at around 420 m above sea level. 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 correct and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the correct and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at beneath 414.9 m above sea stage. Northeast at beneath 418 m above sea level. Arises at round 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 level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the proper; The final one arises instantly on the Altmühl feeder and seems to be the lower reaches of an old proper estuary of the Wieseth, which is no longer continuous due to 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 trail 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 higher reaches up to the Heidweiher are also known as Wiesengraben. There are additionally two moats in direction of the top of the mountain spur, one in all which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the local space, slightly offset in front of a dry valley mouth from the route of Riedenburg--Perletzhofen, from the place provide from sinkholes has been proven. Sometimes karstification additionally results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 416 m above sea degree. 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 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 seashore of Unterwurmbach only a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Middle and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well as the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The record of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally known as Schambach, from left and east to less than 410 m above sea level. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.3 m above sea degree. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Higher Kuhgraben → Lower Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises below 365 m above sea degree.
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