The passenger ship, which travels between the lake centers throughout 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 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 half of the principle-Danube Canal, which is accompanied on this route on the left and right by a variety of remnants of its predecessor, the Ludwig-Donau-Predominant Canal, just a few of that are additionally related to it. From here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the eastern flow across the Altmühlsee. Part additionally 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 beneath 418 m above sea level.

Hesselbach, from the left and north-northeast to under 418 m above sea level. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea stage. Judengraben, from the left and northwest at around 414 m above sea stage. This floodplain ditch is the best branch of the previous one at around 414 m above sea degree. Drains in an analogous meandering course as the Fallach talked about above to under 414 m above sea degree. Arises beneath 420 m above sea stage. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the precise and southeast or southwest to below 416 m above sea degree. Roßbachgraben, from the appropriate and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at under 414.9 m above sea level. Northeast at below 418 m above sea stage. Arises at around 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 stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the proper; The final one arises directly on the Altmühl feeder and appears to be the lower reaches of an old proper estuary of the Wieseth, which is no longer steady as a consequence 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.

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 principle department north of the mill, the secondary branch about 500 meters west of it. The 2 upper reaches up to the Heidweiher are additionally called Wiesengraben. There are additionally two moats in the direction of the end of the mountain spur, one in every of which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN inside the local space, slightly offset in entrance of a dry valley mouth from the path of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Typically 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 stage. Raingraben, from the left and north at over 416 m above sea stage. North at over 405 m above sea degree. 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 level. NN on the northwest beach of Unterwurmbach solely 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Heart and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly because the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The list 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 constructing to 415.3 m above sea level. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher 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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