The passenger ship, which travels between the lake centers through the season, is also 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: Historical Atlas of Bavaria, part of Franconia. From here the Altmühl is part of the primary-Danube Canal, which is accompanied on this route on the left and right by quite a lot of remnants of its predecessor, the Ludwig-Donau-Essential Canal, a number of of that are additionally related to it. From right here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the japanese move around the Altmühlsee. Part additionally runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee (www.knpe.co.kr) within 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 beneath 418 m above sea degree. The lower 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 round 414 m above sea level. This floodplain ditch is the best department of the earlier one at around 414 m above sea degree. Drains in the same meandering course as the Fallach talked about above to under 414 m above sea stage. Arises beneath 420 m above sea level. Arises at round 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the right and southeast or southwest to beneath 416 m above sea degree. Roßbachgraben, from the right and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the right and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at below 414.9 m above sea level. Northeast at beneath 418 m above sea stage. Arises at round 418 m above sea stage. Arises at over 418 m above sea level. 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 stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the correct; The final one arises directly on the Altmühl feeder and appears to be the lower reaches of an outdated right estuary of the Wieseth, which is not steady as a result 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 branch 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 inside the route of the tip of the mountain spur, one in every of which is still six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the native area, barely offset in entrance of a dry valley mouth from the route of Riedenburg--Perletzhofen, from the place supply from sinkholes has been proven. Typically karstification additionally results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 416 m above sea level. 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 stage. 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 seashore of Unterwurmbach only 100 meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Heart and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely as the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The listing 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 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 415.3 m above sea level. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises under 365 m above sea degree.