The passenger ship, which travels between the lake centers through the season, can also be appropriate for exploring Lake Altmühlsee in a relaxed method. 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: Historic Atlas of Bavaria, part of Franconia. From here the Altmühl is an element 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-Major Canal, a number of of that are additionally linked to it. From here, the Altmühl flows in an artificial course on a bigger scale roughly east-southeast to the japanese move around 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 under 418 m above sea stage. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to below 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the fitting branch of the earlier one at around 414 m above sea stage. Drains in an analogous meandering course because the Fallach talked about above to under 414 m above sea degree. Arises below 420 m above sea stage. Arises at round 420 m above sea stage. Flows at about 420 m above sea level. Wieseth, from the correct and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the precise and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at beneath 414.9 m above sea degree. Northeast at beneath 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 stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the right; The final one arises straight on the Altmühl feeder and seems to be the lower reaches of an previous right estuary of the Wieseth, which is now not continuous because of 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.
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 principle department north of the mill, the secondary department about 500 meters west of it. The 2 upper reaches as much as the Heidweiher are also referred to as Wiesengraben. There are additionally two moats in the course of the end of the mountain spur, one in every of which is still six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the local space, slightly offset in front of a dry valley mouth from the course of Riedenburg–Perletzhofen, from the place provide from sinkholes has been confirmed. Generally karstification additionally 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 stage. Raingraben, from the left and north at over 416 m above sea level. North at over 405 m above sea stage. 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 stage.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest beach of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Middle and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly 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 additionally called 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 degree. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises under 365 m above sea stage.
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