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The passenger ship, which travels between the lake centers in the course of the season, is also appropriate for exploring Lake Altmühlsee in a relaxed manner. A shipping line on which the MS Altmühlsee (Read A great deal more) 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: Historic Atlas of Bavaria, a part of Franconia. From here the Altmühl is part of the principle-Danube Canal, which is accompanied on this route on the left and proper by a variety of remnants of its predecessor, the Ludwig-Donau-Major Canal, a number of of that are also related to it. From right here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the eastern flow across the Altmühlsee. Part also runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. 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 under 414.9 m above sea degree. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the precise branch of the previous one at round 414 m above sea degree. Drains in an identical meandering course because the Fallach mentioned above to under 414 m above sea level. Arises beneath 420 m above sea degree. Arises at around 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the proper and southeast or southwest to below 416 m above sea stage. Roßbachgraben, from the precise and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the fitting and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at below 414.9 m above sea stage. Northeast at under 418 m above sea degree. Arises at around 418 m above sea level. 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 degree. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the appropriate; The last 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 continuous as a result of the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite facet 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 department north of the mill, the secondary branch about 500 meters west of it. The 2 upper reaches up to the Heidweiher are also known as Wiesengraben. There are additionally two moats inside the path of the tip of the mountain spur, one among which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN within the native area, barely offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where supply from sinkholes has been proven. Generally karstification also leads to the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 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 stage. Heglauer Mühlbach, from the left and north at over 414.7 m above sea degree. 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 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 Middle and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well because the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The record of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also known as 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. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises below 365 m above sea degree.