The passenger ship, which travels between the lake centers during the season, is also suitable for exploring Lake Altmühlsee in a relaxed manner. A delivery 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: Historical Atlas of Bavaria, part of Franconia. From right here the Altmühl is a component 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-Essential Canal, some of which are also connected to it. From here, the Altmühl flows in an artificial course on a larger scale roughly east-southeast to the japanese circulate around the Altmühlsee. Section additionally runs underground beneath the left edge of the Altmühltal, to the Kleiner Brombachsee (just click the following web page) within the Rednitz catchment area. 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 degree. The decrease Schlegelsbühlgraben takes the upper 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 level. This floodplain ditch is the suitable department of the previous one at round 414 m above sea level. Drains in an identical meandering course because the Fallach mentioned above to under 414 m above sea stage. 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 fitting and southeast or southwest to beneath 416 m above sea stage. Roßbachgraben, from the appropriate and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at under 414.9 m above sea stage. Northeast at underneath 418 m above sea level. Arises at round 418 m above sea level. Arises at over 418 m above sea degree. 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 degree. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the appropriate; The final one arises immediately on the Altmühl feeder and appears to be the lower reaches of an previous proper estuary of the Wieseth, which is no longer steady due to the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite side of the feeder, which now flows is initiated into this.
In 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 department about 500 meters west of it. The two upper reaches as much as the Heidweiher are also referred to as Wiesengraben. There are also two moats in route of the top of the mountain spur, one of which continues to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the local area, slightly offset in entrance of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from the place provide from sinkholes has been proven. Typically karstification additionally results in the formation of a lake district, such because 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 degree. 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 degree.
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. On account of the Reich Deputation Center and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well because the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The record of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly also 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 building to 415.3 m above sea level. Part title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea stage.