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Retrieved January 19, 2023 (English)

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The passenger ship, which travels between the lake centers throughout the season, can also 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 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, part of Franconia. From right here the Altmühl is half 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-Fundamental Canal, some of which 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 circulation around the Altmühlsee. Section also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee in 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 under 418 m above sea level. 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 round 414 m above sea level. This floodplain ditch is the proper branch of the previous one at around 414 m above sea stage. Drains in an identical meandering course because the Fallach talked about above to under 414 m above sea degree. Arises beneath 420 m above sea stage. Arises at around 420 m above sea degree. Flows at about 420 m above sea level. Wieseth, from the precise and southeast or southwest to under 416 m above sea degree. Roßbachgraben, from the suitable and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at below 414.9 m above sea degree. Northeast at underneath 418 m above sea degree. Arises at around 418 m above sea stage. 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 right; The last one arises instantly on the Altmühl feeder and appears to be the decrease reaches of an previous proper estuary of the Wieseth, which is not steady due to 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.

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 main branch north of the mill, the secondary department about 500 meters west of it. The 2 upper reaches up to the Heidweiher are additionally known as Wiesengraben. There are additionally two moats in the route of the tip of the mountain spur, one in all which continues to be six meters deep. NN at a dirt street 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 where supply from sinkholes has been confirmed. Generally karstification additionally leads to the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea stage. 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 level.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea level. NN on the northwest seashore of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Center and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely because the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The list of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. 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 building to 415.3 m above sea stage. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Upper 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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