The passenger ship, which travels between the lake centers through the season, can be suitable for exploring Lake Altmühlsee in a relaxed manner. 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 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 here the Altmühl is half of the primary-Danube Canal, which is accompanied on this route on the left and proper by a number of remnants of its predecessor, the Ludwig-Donau-Primary Canal, some of which are also related to it. From here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the jap stream around 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 degree.
Hesselbach, from the left and north-northeast to below 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 suitable branch of the previous one at around 414 m above sea level. Drains in an analogous meandering course as the Fallach talked about above to beneath 414 m above sea level. Arises under 420 m above sea level. Arises at round 420 m above sea stage. Flows at about 420 m above sea stage. Wieseth, from the correct and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the suitable 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, also known as Häfelesgraben, at below 414.9 m above sea degree. Northeast at beneath 418 m above sea level. 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 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 seems to be the decrease reaches of an outdated proper estuary of the Wieseth, which is no longer steady because of the construction of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other facet of the feeder, which now flows is initiated into this.
Within 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 branch north of the mill, the secondary branch 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 route of the tip 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 in the native space, barely offset in entrance of a dry valley mouth from the route of Riedenburg–Perletzhofen, from where 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 beneath 416 m above sea degree. Raingraben, from the left and north at over 416 m above sea level. North at over 405 m above sea degree. Heglauer Mühlbach, from the left and north at over 414.7 m above sea stage. 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 solely a hundred meters from the run of the previous 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 nicely because the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The listing of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also known 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.Three m above sea degree. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Higher Kuhgraben → Lower Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises under 365 m above sea degree.
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