The passenger ship, which travels between the lake centers throughout the season, can be 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, a 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 a lot of remnants of its predecessor, the Ludwig-Donau-Predominant Canal, just a few of that are also connected to it. From here, the Altmühl flows in an artificial course on a larger scale approximately east-southeast to the eastern circulate across the Altmühlsee. Part additionally runs underground under 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 stage.
Hesselbach, from the left and north-northeast to beneath 418 m above sea degree. The lower Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to under 414.9 m above sea degree. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the right department of the previous one at around 414 m above sea level. Drains in a similar meandering course because the Fallach mentioned above to beneath 414 m above sea degree. Arises below 420 m above sea stage. Arises at around 420 m above sea stage. Flows at about 420 m above sea stage. Wieseth, from the proper and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the fitting and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at under 414.9 m above sea degree. Northeast at under 418 m above sea level. Arises at round 418 m above sea level. 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 level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the right; The last one arises straight on the Altmühl feeder and appears to be the decrease reaches of an outdated right estuary of the Wieseth, which is not steady as a result of the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite facet 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 main department north of the mill, the secondary branch about 500 meters west of it. The 2 upper reaches up to the Heidweiher are additionally referred to as Wiesengraben. There are additionally two moats in the path of the tip of the mountain spur, certainly one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the native space, slightly offset in front of a dry valley mouth from the direction of Riedenburg–Perletzhofen, from where supply from sinkholes has been confirmed. Typically karstification also results in the formation of a lake district, such because 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 level. North at over 405 m above sea degree. 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 level. NN on the northwest seaside of Unterwurmbach only 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Center and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely because the Birkenmühle and the Langweidmühle in 1806 passed 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 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 name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify 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 below 365 m above sea stage.
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