The passenger ship, which travels between the lake centers in the course of the season, can be appropriate for exploring Lake Altmühlsee in a relaxed manner. 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 here the Altmühl is half of the principle-Danube Canal, which is accompanied on this route on the left and right by a lot of remnants of its predecessor, the Ludwig-Donau-Major Canal, a couple of of which are additionally connected to it. From right here, the Altmühl flows in an synthetic course on a bigger scale roughly east-southeast to the eastern circulate across the Altmühlsee. Part additionally runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. Schafgraben, from the left and northwest to beneath 418 m above sea degree.
Hesselbach, from the left and north-northeast to under 418 m above sea degree. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 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 branch of the earlier one at around 414 m above sea degree. Drains in an analogous meandering course because the Fallach mentioned above to under 414 m above sea level. Arises below 420 m above sea level. Arises at round 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the fitting and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the correct and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at under 414.9 m above sea degree. Northeast at beneath 418 m above sea degree. Arises at around 418 m above sea stage. Arises at over 418 m above sea stage. 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 suitable; The final one arises immediately on the Altmühl feeder and seems to be the decrease reaches of an old right estuary of the Wieseth, which is not continuous as a result of the development 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 primary department north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches up to the Heidweiher are additionally referred to as Wiesengraben. There are additionally two moats in direction of the end of the mountain spur, certainly one of which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the native space, slightly offset in entrance of a dry valley mouth from the route of Riedenburg–Perletzhofen, from where provide from sinkholes has been confirmed. Generally karstification additionally results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 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 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. 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 effectively as the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The checklist of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally known as 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 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 beneath 365 m above sea stage.
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