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The passenger ship, which travels between the lake centers during the season, is also 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: Historic Atlas of Bavaria, part of Franconia. From right here the Altmühl is a part of the primary-Danube Canal, which is accompanied on this route on the left and proper by quite a few remnants of its predecessor, the Ludwig-Donau-Predominant Canal, a number of of that are also related to it. From here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the eastern movement around the Altmühlsee. Part 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 degree.

Hesselbach, from the left and north-northeast to below 418 m above sea degree. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to beneath 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the correct department of the previous one at round 414 m above sea level. Drains in an identical meandering course because the Fallach talked about above to beneath 414 m above sea level. Arises beneath 420 m above sea stage. Arises at around 420 m above sea level. Flows at about 420 m above sea level. Wieseth, from the right and southeast or southwest to below 416 m above sea stage. Roßbachgraben, from the right and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at under 414.9 m above sea level. Northeast at beneath 418 m above sea degree. Arises at around 418 m above sea degree. 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 correct; The final one arises straight on the Altmühl feeder and appears to be the decrease reaches of an outdated proper estuary of the Wieseth, which is not continuous due to the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other aspect 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 branch about 500 meters west of it. The 2 higher reaches up to the Heidweiher are also called Wiesengraben. There are additionally two moats towards the end 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 within the local space, barely offset in front of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from the place supply 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 below 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea level. 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 degree. NN on the northwest beach of Unterwurmbach only 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 because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The record of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also called 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 stage. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea level.


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