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The passenger ship, which travels between the lake centers throughout the season, can be appropriate for exploring Lake Altmühlsee in a relaxed manner. 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 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 right here the Altmühl is half of the principle-Danube Canal, which is accompanied on this route on the left and proper by numerous remnants of its predecessor, the Ludwig-Donau-Important Canal, some of which are additionally related to it. From here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the eastern circulation around the Altmühlsee. Part also runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment space. Schafgraben, from the left and northwest to beneath 418 m above sea level.

Hesselbach, from the left and north-northeast to beneath 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to under 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea stage. This floodplain ditch is the suitable department of the previous one at round 414 m above sea stage. Drains in an analogous meandering course because the Fallach mentioned above to below 414 m above sea level. Arises below 420 m above sea degree. Arises at round 420 m above sea stage. Flows at about 420 m above sea stage. Wieseth, from the precise and southeast or southwest to beneath 416 m above sea stage. Roßbachgraben, from the suitable and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at under 414.9 m above sea level. Northeast at beneath 418 m above sea stage. Arises at around 418 m above sea stage. 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 last one arises directly on the Altmühl feeder and seems to be the decrease reaches of an outdated proper estuary of the Wieseth, which is no longer steady as a consequence of the construction 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 trail 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 referred to as Wiesengraben. There are also two moats towards the top of the mountain spur, one of which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the local space, barely offset in entrance of a dry valley mouth from the path of Riedenburg--Perletzhofen, from the place supply from sinkholes has been proven. Generally karstification also results in the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea level. North at over 405 m above sea degree. 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 stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. NN on the northwest beach of Unterwurmbach solely 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 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 record of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also known as Schambach, from left and east to lower than 410 m above sea stage. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn constructing to 415.Three m above sea level. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Higher 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 stage.

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