The passenger ship, which travels between the lake centers through the season, can be suitable for exploring Lake Altmühlsee in a relaxed manner. 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 a 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 an element of the main-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-Important Canal, some of which are also connected to it. From here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the jap circulate around the Altmühlsee. Section additionally runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee (Highly recommended Reading) in 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 under 418 m above sea level. The decrease 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 around 414 m above sea degree. This floodplain ditch is the precise department of the earlier one at round 414 m above sea level. Drains in an analogous meandering course as the Fallach mentioned above to beneath 414 m above sea level. Arises below 420 m above sea stage. Arises at round 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the precise and southeast or southwest to beneath 416 m above sea degree. Roßbachgraben, from the suitable and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at below 414.9 m above sea degree. Northeast at below 418 m above sea degree. Arises at round 418 m above sea level. 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 degree. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the precise; The last one arises immediately on the Altmühl feeder and appears to be the decrease reaches of an previous proper estuary of the Wieseth, which is now not steady on account of the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite aspect 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 branch north of the mill, the secondary department about 500 meters west of it. The two upper reaches as much as the Heidweiher are also known as Wiesengraben. There are also two moats towards 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 inside the local area, slightly offset in entrance of a dry valley mouth from the route of Riedenburg–Perletzhofen, from the place provide from sinkholes has been proven. Generally karstification also results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 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 level.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. 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. As a result of the Reich Deputation Center and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as effectively because the Birkenmühle and the Langweidmühle in 1806 passed to the new Kingdom of Bavaria. The record of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally called Schambach, from left and east to lower than 410 m above sea stage. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn constructing to 415.3 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 → Lower Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises below 365 m above sea stage.
