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 delivery 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 a part of the primary-Danube Canal, which is accompanied on this route on the left and proper by various remnants of its predecessor, the Ludwig-Donau-Important Canal, a couple of of which are additionally linked to it. From right here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the eastern movement around the Altmühlsee. Part also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to under 418 m above sea stage.
Hesselbach, from the left and north-northeast to under 418 m above sea stage. The lower 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 level. This floodplain ditch is the suitable branch of the earlier one at round 414 m above sea level. Drains in an identical meandering course because the Fallach mentioned above to under 414 m above sea stage. Arises below 420 m above sea degree. Arises at round 420 m above sea degree. Flows at about 420 m above sea level. Wieseth, from the correct and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the appropriate and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the right and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at under 414.9 m above sea degree. Northeast at below 418 m above sea level. 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 level. 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 best; The last one arises straight on the Altmühl feeder and seems to be the lower reaches of an outdated proper estuary of the Wieseth, which is not continuous attributable to the construction of the Altmühl feeder, as a result of 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 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 two higher reaches up to the Heidweiher are additionally referred to as Wiesengraben. There are also two moats in course of the tip of the mountain spur, one among which is still six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the local space, barely offset in front of a dry valley mouth from the path of Riedenburg–Perletzhofen, from where supply 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 degree. North at over 405 m above sea stage. 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 degree.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seashore 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 Center and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as effectively because the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The listing of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also called Schambach, from left and east to less than 410 m above sea level. → 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 identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea degree.
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