The passenger ship, which travels between the lake centers throughout the season, can also be suitable 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 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, a 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 a variety of remnants of its predecessor, the Ludwig-Donau-Main Canal, some of that are additionally related to it. From right here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the jap movement across the Altmühlsee. Part additionally runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee within 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 beneath 418 m above sea degree. The lower Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to under 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the suitable department of the earlier one at round 414 m above sea level. Drains in an identical meandering course as the Fallach mentioned above to below 414 m above sea stage. Arises below 420 m above sea stage. Arises at round 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the proper and southeast or southwest to beneath 416 m above sea stage. Roßbachgraben, from the appropriate and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at below 414.9 m above sea degree. Northeast at under 418 m above sea level. 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 suitable; The final one arises straight on the Altmühl feeder and seems to be the decrease reaches of an previous right estuary of the Wieseth, which is now not steady as a result of the construction of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other facet 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 principle branch north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches as much as the Heidweiher are additionally referred to as Wiesengraben. There are also two moats within the path of the tip of the mountain spur, one among which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the native area, barely offset in entrance of a dry valley mouth from the course of Riedenburg–Perletzhofen, from where provide from sinkholes has been confirmed. Generally karstification also 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 degree. 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 stage. Inlet of the Heidental dry valley, from the left and north at 338.2 m above sea stage.

    Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea level. NN on the northwest beach of Unterwurmbach only 100 meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Heart and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well as the Birkenmühle and the Langweidmühle in 1806 handed 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 known as 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 415.3 m above sea stage. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher 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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