The passenger ship, which travels between the lake centers throughout 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, a part of Franconia. From here the Altmühl is a part of the primary-Danube Canal, which is accompanied on this route on the left and right by a number of remnants of its predecessor, the Ludwig-Donau-Essential 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 japanese flow across the Altmühlsee (recent xn--e1ane2e.xn--82-6kc3btf8dtc.xn--p1ai blog post). Part also runs underground below 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 beneath 418 m above sea degree. The lower 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 level. This floodplain ditch is the best branch of the earlier one at around 414 m above sea stage. Drains in an analogous meandering course as the Fallach mentioned above to beneath 414 m above sea level. Arises beneath 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea level. Wieseth, from the correct and southeast or southwest to below 416 m above sea stage. Roßbachgraben, from the right and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at below 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 degree. 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 correct; The final one arises straight on the Altmühl feeder and appears to be the lower reaches of an outdated right estuary of the Wieseth, which is not steady on account of the construction of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite 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 branch north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches up to the Heidweiher are also called Wiesengraben. There are also two moats in the path of the tip of the mountain spur, considered one of which is still six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN within the local area, slightly offset in front of a dry valley mouth from the route of Riedenburg–Perletzhofen, from the place supply from sinkholes has been confirmed. Generally karstification also leads to 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 stage. 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 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. Because of the Reich Deputation Middle and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely because the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The list of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. 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 degree. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises under 365 m above sea level.