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 right here the Altmühl is an element of the primary-Danube Canal, which is accompanied on this route on the left and right by numerous remnants of its predecessor, the Ludwig-Donau-Main Canal, just a few of that are also linked to it. From here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the jap circulation around the Altmühlsee. Section 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 beneath 418 m above sea stage. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to below 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the precise department of the earlier one at round 414 m above sea stage. Drains in an identical meandering course as the Fallach talked about above to beneath 414 m above sea degree. Arises below 420 m above sea degree. Arises at around 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the precise and southeast or southwest to below 416 m above sea degree. Roßbachgraben, from the fitting and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the fitting and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at below 414.9 m above sea stage. Northeast at underneath 418 m above sea degree. 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 degree. 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 suitable; The final one arises directly on the Altmühl feeder and seems to be the decrease reaches of an outdated right estuary of the Wieseth, which is now not continuous as a consequence of the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other 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 department north of the mill, the secondary department about 500 meters west of it. The two upper reaches as much as the Heidweiher are additionally called Wiesengraben. There are additionally two moats inside the course of the top of the mountain spur, one in all which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN in the local space, slightly offset in front of a dry valley mouth from the path of Riedenburg–Perletzhofen, from the place supply from sinkholes has been confirmed. Sometimes karstification additionally 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 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 degree. NN on the northwest seashore of Unterwurmbach solely a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. As a result of the Reich Deputation Heart 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 list of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally known 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 constructing to 415.Three m above sea stage. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of 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 under 365 m above sea level.
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