Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers throughout the season, is also suitable 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: Historic 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 proper by a number of remnants of its predecessor, the Ludwig-Donau-Primary Canal, a couple of of which are additionally related to it. From right here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the jap circulation around the Altmühlsee. Section also runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment space. Schafgraben, from the left and northwest to under 418 m above sea degree.

Triana se quema (XVI Festival Teatro y Danza Las Palmas de G.C.)

Hesselbach, from the left and north-northeast to beneath 418 m above sea level. The lower 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 round 414 m above sea stage. This floodplain ditch is the precise department of the previous one at around 414 m above sea level. Drains in the same meandering course because the Fallach mentioned above to below 414 m above sea level. Arises under 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the suitable and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the best and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the correct and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at below 414.9 m above sea degree. Northeast at beneath 418 m above sea degree. Arises at round 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 stage. 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 correct; The last one arises directly on the Altmühl feeder and appears to be the decrease reaches of an outdated right estuary of the Wieseth, which is not steady because of the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite side 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 referred to as Wiesengraben. There are additionally two moats within the path of the end of the mountain spur, certainly one of which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the native area, barely offset in front of a dry valley mouth from the route of Riedenburg–Perletzhofen, from the place provide from sinkholes has been proven. Typically karstification additionally leads to the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 416 m above sea degree. Raingraben, from the left and north at over 416 m above sea stage. 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 stage. NN on the northwest seaside of Unterwurmbach only a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Heart and as a result 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 new Kingdom of Bavaria. The checklist of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also called Schambach, from left and east to lower 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 stage. Section title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Upper Kuhgraben → Lower 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 level.

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