The passenger ship, which travels between the lake centers throughout the season, is also 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: Historical 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 various remnants of its predecessor, the Ludwig-Donau-Main Canal, some of which 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 movement across the Altmühlsee. Section additionally runs underground below 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 level.

Hesselbach, from the left and north-northeast to below 418 m above sea stage. The decrease 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 best department of the earlier one at round 414 m above sea degree. Drains in the same meandering course as the Fallach talked about above to beneath 414 m above sea stage. Arises under 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the correct and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the precise and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the fitting and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at beneath 414.9 m above sea stage. Northeast at below 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 degree. Betzengraben, from the left and north to over 416 m above sea stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the right; The last one arises immediately on the Altmühl feeder and seems to be the decrease reaches of an previous right estuary of the Wieseth, which is not continuous as a consequence of the construction of the Altmühl feeder, because 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 principle branch north of the mill, the secondary branch about 500 meters west of it. The two upper reaches as much as the Heidweiher are also called Wiesengraben. There are additionally two moats in the direction of the end of the mountain spur, certainly one of which is still six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the native area, barely offset in entrance of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where supply from sinkholes has been confirmed. Typically karstification additionally results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 416 m above sea level. 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 level.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea level. NN on the northwest seaside of Unterwurmbach solely 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 effectively as the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The record of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also called Schambach, from left and east to lower than 410 m above sea level. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.3 m above sea stage. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises under 365 m above sea stage.

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