Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers during the season, is also suitable for exploring Lake Altmühlsee (hop over to here) 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 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 part of the primary-Danube Canal, which is accompanied on this route on the left and proper by quite a few remnants of its predecessor, the Ludwig-Donau-Most important Canal, a number of of which are additionally related to it. From here, the Altmühl flows in an synthetic course on a larger scale approximately east-southeast to the eastern movement around the Altmühlsee. Section additionally runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment area. Schafgraben, from the left and northwest to below 418 m above sea level.

Hesselbach, from the left and north-northeast to below 418 m above sea degree. The lower Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to under 414.9 m above sea stage. Judengraben, from the left and northwest at around 414 m above sea degree. This floodplain ditch is the appropriate department of the earlier one at around 414 m above sea degree. Drains in the same meandering course because the Fallach talked about above to under 414 m above sea degree. Arises beneath 420 m above sea degree. Arises at around 420 m above sea stage. Flows at about 420 m above sea level. Wieseth, from the correct 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 proper and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at below 414.9 m above sea stage. Northeast at beneath 418 m above sea level. 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 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 appropriate; The last one arises instantly on the Altmühl feeder and appears to be the decrease reaches of an previous right estuary of the Wieseth, which is no longer steady due to the construction 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 additionally referred to as Wiesengraben. There are additionally two moats towards the end 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 native space, barely offset in front of a dry valley mouth from the course of Riedenburg--Perletzhofen, from the place provide from sinkholes has been proven. Generally karstification additionally leads to the formation of a lake district, such because 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 level. North at over 405 m above sea level. 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 stage. NN on the northwest seashore of Unterwurmbach solely 100 meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Heart 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 handed to the brand new Kingdom of Bavaria. The list of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also referred to 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. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Upper Kuhgraben → Lower 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 stage.