The passenger ship, which travels between the lake centers during the season, can be appropriate for exploring Lake Altmühlsee in a relaxed method. 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 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: Historic Atlas of Bavaria, a 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 quite a lot of remnants of its predecessor, the Ludwig-Donau-Major Canal, some of that are also connected to it. From here, the Altmühl flows in an synthetic course on a larger scale approximately east-southeast to the jap circulation around the Altmühlsee. Section additionally runs underground below the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment area. Schafgraben, from the left and northwest to beneath 418 m above sea level.

Hesselbach, from the left and north-northeast to under 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to beneath 414.9 m above sea stage. Judengraben, from the left and northwest at round 414 m above sea stage. This floodplain ditch is the precise department of the earlier one at around 414 m above sea degree. Drains in a similar meandering course because the Fallach talked about above to under 414 m above sea level. Arises under 420 m above sea level. Arises at around 420 m above sea degree. Flows at about 420 m above sea level. Wieseth, from the fitting and southeast or southwest to under 416 m above sea stage. Roßbachgraben, from the right and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the precise and south to 414.7 m above sea stage. → 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 level. 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 level. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the correct; The last one arises directly on the Altmühl feeder and seems to be the decrease reaches of an outdated proper estuary of the Wieseth, which is no longer continuous as a result of the construction of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite facet of the feeder, which now flows is initiated into this.

In 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 primary branch north of the mill, the secondary branch about 500 meters west of it. The two higher reaches as much as the Heidweiher are also called Wiesengraben. There are also two moats within the route of the top of the mountain spur, one in every of which is still six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN in the local area, slightly offset in entrance of a dry valley mouth from the route of Riedenburg--Perletzhofen, from where provide 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 beneath 416 m above sea level. 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 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 stage. NN on the northwest beach of Unterwurmbach solely 100 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 nicely because the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The listing 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 stage. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Upper Kuhgraben → Lower Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises under 365 m above sea degree.

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