The passenger ship, which travels between the lake centers during the season, can also 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 here the Altmühl is an element of the principle-Danube Canal, which is accompanied on this route on the left and proper by numerous remnants of its predecessor, the Ludwig-Donau-Foremost Canal, some of which are also linked to it. From here, the Altmühl flows in an synthetic course on a bigger scale roughly east-southeast to the japanese stream across the Altmühlsee. Part additionally runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee within 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 below 418 m above sea stage. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to below 414.9 m above sea level. Judengraben, from the left and northwest at round 414 m above sea level. This floodplain ditch is the proper department of the earlier one at around 414 m above sea stage. Drains in the same meandering course because the Fallach talked about above to below 414 m above sea degree. Arises below 420 m above sea stage. Arises at round 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the right and southeast or southwest to under 416 m above sea degree. Roßbachgraben, from the appropriate and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at beneath 414.9 m above sea level. Northeast at below 418 m above sea stage. Arises at round 418 m above sea level. Arises at over 418 m above sea degree. 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 level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the best; The final one arises directly on the Altmühl feeder and appears to be the lower reaches of an previous proper estuary of the Wieseth, which is not continuous due to the development 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 path continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the main department north of the mill, the secondary department about 500 meters west of it. The two higher reaches as much as the Heidweiher are additionally called Wiesengraben. There are additionally two moats towards the tip of the mountain spur, considered one of which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN inside the local area, slightly offset in entrance of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where provide from sinkholes has been confirmed. Generally karstification also results in the formation of a lake district, such because 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 level. North at over 405 m above sea degree. Heglauer Mühlbach, from the left and north at over 414.7 m above sea degree. 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 degree. 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 because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly as the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The listing of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally called 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 constructing to 415.Three m above sea stage. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title 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. Upper course and approx. 3.2 km². Arises below 365 m above sea level.

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