The passenger ship, which travels between the lake centers throughout the season, can also be suitable for exploring Lake Altmühlsee in a relaxed manner. A delivery 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 a part of the main-Danube Canal, which is accompanied on this route on the left and right by plenty of remnants of its predecessor, the Ludwig-Donau-Most important 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 japanese flow across the Altmühlsee. Part additionally runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. Schafgraben, from the left and northwest to below 418 m above sea stage.

Hesselbach, from the left and north-northeast to below 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea level. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the correct branch of the previous one at round 414 m above sea degree. Drains in an identical meandering course because the Fallach mentioned above to below 414 m above sea degree. Arises beneath 420 m above sea degree. Arises at round 420 m above sea degree. Flows at about 420 m above sea level. Wieseth, from the appropriate and southeast or southwest to beneath 416 m above sea degree. Roßbachgraben, from the fitting and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the fitting and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at below 414.9 m above sea level. Northeast at beneath 418 m above sea stage. Arises at round 418 m above sea level. Arises at over 418 m above sea level. 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 immediately on the Altmühl feeder and appears to be the lower reaches of an old proper estuary of the Wieseth, which is no longer continuous as a consequence 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.

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 branch about 500 meters west of it. The two upper reaches up to the Heidweiher are also referred to as Wiesengraben. There are additionally two moats inside the route of the end of the mountain spur, considered one of which continues to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the local area, slightly offset in front of a dry valley mouth from the path of Riedenburg–Perletzhofen, from where provide from sinkholes has been proven. Typically 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 stage. North at over 405 m above sea level. Heglauer Mühlbach, from the left and north at over 414.7 m above sea level. 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 seashore of Unterwurmbach solely 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 Center 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 passed to the brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally known as Schambach, from left and east to less than 410 m above sea degree. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn constructing to 415.3 m above sea level. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of Esbach) → Birkengraben → Upper Kuhgraben → Lower Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises below 365 m above sea level.

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