Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers through the season, can be appropriate for exploring Lake Altmühlsee in a relaxed method. A transport 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, a part of Franconia. From right here the Altmühl is a component of the main-Danube Canal, which is accompanied on this route on the left and right by various remnants of its predecessor, the Ludwig-Donau-Primary Canal, some of that are additionally connected to it. From right here, the Altmühl flows in an artificial course on a larger scale approximately east-southeast to the jap circulate around the Altmühlsee. Part additionally runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment space. 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 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 proper department of the earlier one at around 414 m above sea degree. Drains in a similar meandering course because the Fallach mentioned above to beneath 414 m above sea degree. Arises under 420 m above sea stage. Arises at round 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the correct and southeast or southwest to below 416 m above sea level. Roßbachgraben, from the fitting and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at under 414.9 m above sea degree. Northeast at underneath 418 m above sea level. Arises at round 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 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 directly on the Altmühl feeder and seems to be the lower reaches of an outdated right estuary of the Wieseth, which is not continuous due to the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the other side 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 department north of the mill, the secondary department about 500 meters west of it. The two higher reaches as much as the Heidweiher are also known as Wiesengraben. There are additionally two moats in course of 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, slightly offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from where provide from sinkholes has been proven. Sometimes karstification also results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 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 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 stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. NN on the northwest beach of Unterwurmbach solely a hundred meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Middle and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly as 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 also known as Schambach, from left and east to lower than 410 m above sea level. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn constructing to 415.3 m above sea level. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via 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 stage.

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