The passenger ship, which travels between the lake centers throughout the season, can also be appropriate for exploring Lake Altmühlsee in a relaxed method. A shipping line on which the MS Altmühlsee (redirected here) 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 an element of the principle-Danube Canal, which is accompanied on this route on the left and right by a lot of remnants of its predecessor, the Ludwig-Donau-Essential Canal, a few of that are also related to it. From right here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the eastern circulation around the Altmühlsee. Section also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment area. Schafgraben, from the left and northwest to under 418 m above sea stage.
Hesselbach, from the left and north-northeast to beneath 418 m above sea level. The lower 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 appropriate branch of the previous one at around 414 m above sea level. Drains in an identical meandering course because the Fallach mentioned above to below 414 m above sea stage. Arises below 420 m above sea degree. Arises at round 420 m above sea level. Flows at about 420 m above sea level. Wieseth, from the proper and southeast or southwest to under 416 m above sea stage. Roßbachgraben, from the precise and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at beneath 414.9 m above sea degree. Northeast at below 418 m above sea degree. Arises at around 418 m above sea stage. 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 fitting; The last one arises straight on the Altmühl feeder and seems to be the decrease reaches of an outdated right estuary of the Wieseth, which is not steady as a result of the construction of the Altmühl feeder, as a result of 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 trail continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the principle branch north of the mill, the secondary branch about 500 meters west of it. The 2 higher reaches as much as the Heidweiher are additionally known as Wiesengraben. There are also two moats inside the route of the tip of the mountain spur, one in all which is still six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN within the local space, slightly offset in front of a dry valley mouth from the route 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 below 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 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 stage.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. 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 Middle and because 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 Studies. Kästleinsmühlbach, partly additionally referred to as Schambach, from left and east to less 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.Three 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 Esbach) → Birkengraben → Higher 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.
