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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 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: Historic Atlas of Bavaria, part of Franconia. From right here the Altmühl is part of the main-Danube Canal, which is accompanied on this route on the left and proper by a lot of remnants of its predecessor, the Ludwig-Donau-Predominant Canal, a few of that are additionally connected to it. From right here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the jap circulation around the Altmühlsee (http://cskfloor.com/gnuboard5/bbs/board.php?bo_table=inquiry&wr_id=23295). Section also runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to under 418 m above sea degree.

Hesselbach, from the left and north-northeast to under 418 m above sea level. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea degree. Judengraben, from the left and northwest at around 414 m above sea degree. This floodplain ditch is the correct department of the earlier one at round 414 m above sea stage. Drains in the same meandering course as the Fallach talked about above to below 414 m above sea stage. Arises beneath 420 m above sea level. Arises at round 420 m above sea stage. Flows at about 420 m above sea level. Wieseth, from the fitting and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the correct and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at under 414.9 m above sea level. Northeast at beneath 418 m above sea stage. Arises at around 418 m above sea level. Arises at over 418 m above sea stage. 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 last one arises immediately on the Altmühl feeder and seems to be the lower reaches of an previous proper estuary of the Wieseth, which is no longer steady as a result of the development 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.

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 department north of the mill, the secondary department about 500 meters west of it. The two upper reaches as much as the Heidweiher are also known as Wiesengraben. There are additionally two moats in the course of the top of the mountain spur, one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the native area, 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 leads to 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 level. North at over 405 m above sea degree. Heglauer Mühlbach, from the left and north at over 414.7 m above sea stage. 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 stage. NN on the northwest seaside of Unterwurmbach only 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 because the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The listing of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also referred to as Schambach, from left and east to less than 410 m above sea stage. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn constructing to 415.3 m above sea level. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Higher Kuhgraben → Lower 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 degree.