The passenger ship, which travels between the lake centers through the season, can be appropriate for exploring Lake Altmühlsee in a relaxed method. A shipping 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 primary-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 which are additionally connected to it. From right here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the eastern move around the Altmühlsee; visit the next website page,. Section also runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to beneath 418 m above sea level.

Hesselbach, from the left and north-northeast to below 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the proper branch of the previous one at around 414 m above sea degree. Drains in an analogous meandering course as the Fallach talked about above to under 414 m above sea degree. Arises beneath 420 m above sea degree. Arises at round 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the right and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the correct 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 known as Häfelesgraben, at beneath 414.9 m above sea degree. Northeast at underneath 418 m above sea stage. Arises at around 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 degree. 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 immediately on the Altmühl feeder and appears to be the lower reaches of an previous proper estuary of the Wieseth, which is no longer steady 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.

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 department north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches up to the Heidweiher are additionally referred to as Wiesengraben. There are also two moats in route of the end of the mountain spur, one among which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN within the local area, barely offset in front of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from the place provide from sinkholes has been confirmed. Sometimes karstification additionally 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 degree. Raingraben, from the left and north at over 416 m above sea degree. 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 stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seaside of Unterwurmbach solely 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Heart and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely because the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The checklist of landscapes in Bavaria relies 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 stage. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.Three m above sea degree. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the title 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 beneath 365 m above sea level.