Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers throughout the season, is also suitable 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 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, a part of Franconia. From here the Altmühl is half of the primary-Danube Canal, which is accompanied on this route on the left and right by plenty of remnants of its predecessor, the Ludwig-Donau-Most important Canal, some of that are also related to it. From right here, the Altmühl flows in an artificial course on a larger scale approximately east-southeast to the jap flow across the Altmühlsee (https://sttimothysignal.org/). 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 under 418 m above sea stage.

Hesselbach, from the left and north-northeast to below 418 m above sea level. The lower 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 around 414 m above sea stage. This floodplain ditch is the proper department of the previous one at around 414 m above sea level. Drains in a similar meandering course because the Fallach talked about above to below 414 m above sea degree. Arises under 420 m above sea level. Arises at around 420 m above sea degree. Flows at about 420 m above sea stage. Wieseth, from the suitable and southeast or southwest to below 416 m above sea degree. Roßbachgraben, from the appropriate and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at below 414.9 m above sea degree. Northeast at under 418 m above sea level. Arises at around 418 m above sea degree. 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 stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the precise; The final 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 construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite facet of the feeder, which now flows is initiated into this.

Within the Franconian Lake District the path continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the principle department north of the mill, the secondary branch about 500 meters west of it. The 2 higher reaches up to the Heidweiher are additionally called Wiesengraben. There are additionally two moats in the route of the end of the mountain spur, one among which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the native area, slightly offset in entrance of a dry valley mouth from the route of Riedenburg--Perletzhofen, from the place supply from sinkholes has been proven. Generally karstification additionally results in the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 416 m above sea level. Raingraben, from the left and north at over 416 m above sea stage. North at over 405 m above sea level. 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 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 nicely as the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The listing 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 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 415.3 m above sea degree. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title 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 beneath 365 m above sea degree.