The passenger ship, which travels between the lake centers throughout the season, can be appropriate 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 a component of the main-Danube Canal, which is accompanied on this route on the left and right by numerous remnants of its predecessor, the Ludwig-Donau-Important Canal, a number of of which are also linked to it. From right here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the jap stream across the Altmühlsee. Section also runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee (click through the next site) within the Rednitz catchment space. 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 level. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea stage. Judengraben, from the left and northwest at around 414 m above sea degree. This floodplain ditch is the precise branch of the previous one at around 414 m above sea degree. Drains in an analogous meandering course as the Fallach talked about above to under 414 m above sea stage. Arises beneath 420 m above sea degree. Arises at around 420 m above sea level. Flows at about 420 m above sea stage. Wieseth, from the correct and southeast or southwest to beneath 416 m above sea degree. Roßbachgraben, from the fitting and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the best and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at under 414.9 m above sea degree. Northeast at underneath 418 m above sea degree. Arises at round 418 m above sea level. Arises at over 418 m above sea level. 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 best; The last one arises straight on the Altmühl feeder and appears to be the decrease reaches of an old right estuary of the Wieseth, which is now not continuous ensuing from 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 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 up to the Heidweiher are also called Wiesengraben. There are also two moats in path of the tip of the mountain spur, one of which is still six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN within the local area, slightly offset in front of a dry valley mouth from the route of Riedenburg--Perletzhofen, from where supply from sinkholes has been proven. Sometimes karstification also leads to the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to below 416 m above sea degree. Raingraben, from the left and north at over 416 m above sea level. North at over 405 m above sea degree. 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 level.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seashore of Unterwurmbach solely a hundred meters from the run of the earlier 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 nicely as the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The record 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 lower than 410 m above sea level. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.Three m above sea degree. Section title 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. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea stage.