The passenger ship, which travels between the lake centers in the course of the season, can also 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 here the Altmühl is a part of the principle-Danube Canal, which is accompanied on this route on the left and proper by various remnants of its predecessor, the Ludwig-Donau-Predominant Canal, some of that are also linked to it. From right here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the eastern circulate across the Altmühlsee. Part additionally 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 under 418 m above sea degree.

Hesselbach, from the left and north-northeast to under 418 m above sea degree. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to under 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the correct department of the previous one at around 414 m above sea stage. Drains in a similar meandering course as the Fallach talked about above to under 414 m above sea degree. Arises beneath 420 m above sea stage. Arises at around 420 m above sea stage. Flows at about 420 m above sea stage. 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 degree. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at beneath 414.9 m above sea stage. Northeast at underneath 418 m above sea degree. Arises at round 418 m above sea degree. Arises at over 418 m above sea stage. 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 degree. 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 seems to be the decrease reaches of an outdated proper estuary of the Wieseth, which is now not steady attributable to the construction 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 primary branch north of the mill, the secondary branch about 500 meters west of it. The 2 higher reaches as much as the Heidweiher are additionally called Wiesengraben. There are additionally two moats in path of the top of the mountain spur, one in all which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the local area, slightly offset in entrance of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from where provide from sinkholes has been confirmed. Typically karstification also leads to 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 stage. 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 level. NN on the northwest beach 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 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 new Kingdom of Bavaria. The record of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally 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 building to 415.Three m above sea stage. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by 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 below 365 m above sea degree.


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