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 shipping 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: Historical Atlas of Bavaria, part of Franconia. From here the Altmühl is a component of the main-Danube Canal, which is accompanied on this route on the left and right by a lot of remnants of its predecessor, the Ludwig-Donau-Major Canal, a number of 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 movement across the Altmühlsee. Part additionally runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee (chat.bomjtrek.site) 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 under 418 m above sea level. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the fitting department of the previous one at round 414 m above sea level. Drains in the same meandering course as the Fallach mentioned above to under 414 m above sea degree. Arises below 420 m above sea level. Arises at around 420 m above sea stage. 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 suitable and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the right and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at beneath 414.9 m above sea level. Northeast at below 418 m above sea degree. Arises at round 418 m above sea degree. Arises at over 418 m above sea level. 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 appropriate; The final one arises straight on the Altmühl feeder and appears to be the lower reaches of an outdated right estuary of the Wieseth, which is now not steady because 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 primary branch north of the mill, the secondary department about 500 meters west of it. The 2 upper reaches as much as the Heidweiher are additionally known as Wiesengraben. There are also two moats towards the tip of the mountain spur, considered one of which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN inside the native area, slightly offset in entrance of a dry valley mouth from the path of Riedenburg–Perletzhofen, from the place provide from sinkholes has been proven. Sometimes karstification additionally 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 degree. 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 level. NN on the northwest seaside of Unterwurmbach only 100 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 as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The record of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also called 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.Three m above sea stage. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by 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 beneath 365 m above sea degree.