The passenger ship, which travels between the lake centers through the season, can also be 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, 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 proper by numerous remnants of its predecessor, the Ludwig-Donau-Important Canal, some of that are additionally related to it. From here, the Altmühl flows in an synthetic course on a bigger scale roughly east-southeast to the jap stream across the Altmühlsee (http://forum.prolifeclinics.ro). Part additionally 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 below 418 m above sea degree.
Hesselbach, from the left and north-northeast to beneath 418 m above sea stage. The lower Schlegelsbühlgraben takes the higher 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 level. This floodplain ditch is the suitable department of the previous one at around 414 m above sea stage. Drains in an analogous meandering course as the Fallach talked about above to under 414 m above sea degree. Arises beneath 420 m above sea level. Arises at round 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the proper and southeast or southwest to below 416 m above sea stage. Roßbachgraben, from the suitable 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, also called Häfelesgraben, at beneath 414.9 m above sea stage. Northeast at under 418 m above sea level. Arises at around 418 m above sea degree. Arises at over 418 m above sea degree. Ant ditch, from the left and north-northwest at 418 m above sea stage. 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 correct; The last one arises immediately on the Altmühl feeder and seems to be the lower reaches of an previous right 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 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 primary branch north of the mill, the secondary branch 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 course of the end of the mountain spur, certainly one of which is still six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN within the local area, barely offset in front of a dry valley mouth from the path of Riedenburg--Perletzhofen, from the place supply from sinkholes has been proven. Typically karstification also 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 degree. Raingraben, from the left and north at over 416 m above sea stage. North at over 405 m above sea degree. 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 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. As a result of the Reich Deputation Heart and as a result of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly as the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The list of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally known as 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 constructing to 415.Three m above sea degree. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Higher Kuhgraben → Lower Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises under 365 m above sea degree.