The passenger ship, which travels between the lake centers during the season, can also be appropriate 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 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 part of the principle-Danube Canal, which is accompanied on this route on the left and right by a number of remnants of its predecessor, the Ludwig-Donau-Principal Canal, some of which are also related to it. From right here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the jap movement around the Altmühlsee. Section also 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 below 418 m above sea level.
Hesselbach, from the left and north-northeast to below 418 m above sea level. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea degree. This floodplain ditch is the fitting department of the earlier one at round 414 m above sea level. Drains in a similar meandering course because the Fallach talked about above to below 414 m above sea stage. Arises beneath 420 m above sea level. Arises at around 420 m above sea stage. Flows at about 420 m above sea level. Wieseth, from the suitable and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the suitable and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at beneath 414.9 m above sea degree. Northeast at beneath 418 m above sea degree. 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 level. 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 precise; The final one arises immediately on the Altmühl feeder and seems to be the decrease reaches of an previous right estuary of the Wieseth, which is not continuous due to the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other facet 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 main branch north of the mill, the secondary branch about 500 meters west of it. The two higher reaches up to the Heidweiher are also referred to as Wiesengraben. There are additionally two moats in the route of the end of the mountain spur, one among which is still six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the local space, barely offset in front of a dry valley mouth from the course of Riedenburg–Perletzhofen, from where provide from sinkholes has been proven. Typically karstification also results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea degree. North at over 405 m above sea level. 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 level.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea level. NN on the northwest seaside of Unterwurmbach solely a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Middle and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as effectively as the Birkenmühle and the Langweidmühle in 1806 handed to the brand 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 constructing to 415.3 m above sea degree. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises beneath 365 m above sea degree.
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