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The passenger ship, which travels between the lake centers through the season, can also be suitable 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 a 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 half 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-Principal Canal, some of that are additionally linked to it. From right here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the jap flow across the Altmühlsee. Section also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to beneath 418 m above sea stage.

Hesselbach, from the left and north-northeast to below 418 m above sea level. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to beneath 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea level. This floodplain ditch is the precise branch of the earlier one at around 414 m above sea degree. Drains in an analogous meandering course as the Fallach mentioned above to beneath 414 m above sea level. Arises under 420 m above sea level. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the best and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the precise and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea level. → 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 stage. Arises at round 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 level. 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 fitting; The last one arises directly on the Altmühl feeder and seems to be the lower reaches of an old 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 side of the feeder, which now flows is initiated into this.

Within the Franconian Lake District the trail 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 two higher reaches as much as the Heidweiher are additionally known as Wiesengraben. There are also two moats within the direction of the tip of the mountain spur, one among which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN within the local space, barely offset in entrance of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from where provide from sinkholes has been proven. Generally karstification also leads to 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 stage. 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 degree. NN on the northwest seaside of Unterwurmbach only a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Middle and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as effectively because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also called Schambach, from left and east to lower 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.Three m above sea stage. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises below 365 m above sea stage.

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