The passenger ship, which travels between the lake centers throughout 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 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 half of the principle-Danube Canal, which is accompanied on this route on the left and proper by quite a lot of remnants of its predecessor, the Ludwig-Donau-Essential Canal, a couple of of which are also linked to it. From here, the Altmühl flows in an synthetic course on a larger scale approximately east-southeast to the jap circulate around the Altmühlsee. Section also runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee within the Rednitz catchment space. Schafgraben, from the left and northwest to beneath 418 m above sea degree.
Hesselbach, from the left and north-northeast to beneath 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to under 414.9 m above sea level. Judengraben, from the left and northwest at round 414 m above sea level. This floodplain ditch is the fitting branch of the previous one at around 414 m above sea degree. Drains in the same meandering course because the Fallach talked about above to under 414 m above sea stage. Arises under 420 m above sea level. Arises at around 420 m above sea stage. Flows at about 420 m above sea degree. Wieseth, from the right and southeast or southwest to below 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 degree. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at under 414.9 m above sea stage. Northeast at underneath 418 m above sea degree. Arises at round 418 m above sea degree. Arises at over 418 m above sea level. Ant ditch, from the left and north-northwest at 418 m above sea level. Betzengraben, from the left and north to over 416 m above sea stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the best; The last one arises instantly on the Altmühl feeder and appears to be the lower 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 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 branch north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches up to the Heidweiher are also referred to as Wiesengraben. There are additionally two moats towards the top of the mountain spur, one of which is still six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the native area, barely offset in front of a dry valley mouth from the course of Riedenburg–Perletzhofen, from where provide from sinkholes has been confirmed. Generally karstification additionally 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 degree. North at over 405 m above sea level. 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 stage. NN on the northwest seashore of Unterwurmbach only 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 Middle and on account of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as effectively as the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The record of landscapes in Bavaria relies on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally known as Schambach, from left and east to less than 410 m above sea degree. → 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 title sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Upper Kuhgraben → Lower Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises under 365 m above sea stage.
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