The passenger ship, which travels between the lake centers through 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 a component of the primary-Danube Canal, which is accompanied on this route on the left and right by various remnants of its predecessor, the Ludwig-Donau-Foremost Canal, some of which are additionally related to it. From right here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the eastern move around the Altmühlsee. Part additionally runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. Schafgraben, from the left and northwest to below 418 m above sea level.
Hesselbach, from the left and north-northeast to under 418 m above sea stage. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea stage. Judengraben, from the left and northwest at around 414 m above sea degree. This floodplain ditch is the proper department of the earlier one at round 414 m above sea stage. Drains in a similar meandering course as the Fallach talked about above to beneath 414 m above sea stage. Arises beneath 420 m above sea stage. Arises at round 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the suitable and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the right and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at under 414.9 m above sea degree. Northeast at under 418 m above sea stage. Arises at around 418 m above sea level. Arises at over 418 m above sea level. Ant ditch, from the left and north-northwest at 418 m above sea stage. Betzengraben, from the left and north to over 416 m above sea degree. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the appropriate; 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 not steady because of the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite side 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 principle department north of the mill, the secondary branch about 500 meters west of it. The two higher reaches up to the Heidweiher are additionally referred to as Wiesengraben. There are also two moats towards the tip of the mountain spur, considered one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the local space, barely offset in front of a dry valley mouth from the direction of Riedenburg–Perletzhofen, from the place provide from sinkholes has been confirmed. Typically karstification also 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 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 level. NN on the northwest beach of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. As a result 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 checklist of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also known as Schambach, from left and east to less than 410 m above sea degree. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.Three m above sea level. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name 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 below 365 m above sea degree.
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