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The passenger ship, which travels between the lake centers through the season, is also suitable for exploring Lake Altmühlsee in a relaxed method. 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 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 part of the principle-Danube Canal, which is accompanied on this route on the left and right by quite a lot of remnants of its predecessor, the Ludwig-Donau-Main Canal, just a few of which are additionally connected to it. From here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the eastern move around the Altmühlsee. Section additionally runs underground underneath 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 degree.

Hesselbach, from the left and north-northeast to beneath 418 m above sea stage. The decrease Schlegelsbühlgraben takes the higher 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 degree. This floodplain ditch is the precise branch of the previous one at around 414 m above sea level. Drains in an analogous meandering course because the Fallach mentioned above to under 414 m above sea degree. Arises beneath 420 m above sea level. Arises at round 420 m above sea level. Flows at about 420 m above sea degree. Wieseth, from the appropriate and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the precise and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the right 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 stage. Northeast at below 418 m above sea level. 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 proper; The final one arises instantly on the Altmühl feeder and seems to be the lower reaches of an previous right estuary of the Wieseth, which is not continuous attributable to 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 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 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 known as Wiesengraben. There are additionally two moats towards the tip of the mountain spur, one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the local space, barely offset in front of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Generally karstification also 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 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 level.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seaside of Unterwurmbach only 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 Center and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly as the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The list of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also referred to 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 building to 415.Three m above sea level. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Higher Kuhgraben → Lower Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises beneath 365 m above sea level.


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