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Retrieved January 19, 2023 (English)

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작성자 Drew 댓글 0건 조회 23회 작성일 24-03-21 13:48

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The passenger ship, which travels between the lake centers in the course of the season, can also be appropriate for exploring Lake Altmühlsee in a relaxed method. 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 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, part of Franconia. From right here the Altmühl is part of the main-Danube Canal, which is accompanied on this route on the left and proper by numerous remnants of its predecessor, the Ludwig-Donau-Foremost Canal, some of which are additionally connected to it. From here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the jap move across the Altmühlsee. 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 under 418 m above sea degree.

Hesselbach, from the left and north-northeast to below 418 m above sea stage. The lower Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to under 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the suitable department of the earlier one at around 414 m above sea degree. Drains in an identical meandering course because the Fallach talked about above to under 414 m above sea level. Arises under 420 m above sea degree. Arises at around 420 m above sea degree. Flows at about 420 m above sea level. Wieseth, from the right and southeast or southwest to beneath 416 m above sea stage. Roßbachgraben, from the right and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the appropriate and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, often known as Häfelesgraben, at below 414.9 m above sea level. Northeast at under 418 m above sea degree. Arises at around 418 m above sea stage. Arises at over 418 m above sea stage. 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 final one arises directly on the Altmühl feeder and appears to be the decrease reaches of an previous proper estuary of the Wieseth, which is no longer steady resulting from 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 department about 500 meters west of it. The 2 upper reaches as much as the Heidweiher are additionally called Wiesengraben. There are also two moats inside the course of the tip of the mountain spur, one in every of which remains to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the local area, barely offset in entrance of a dry valley mouth from the route of Riedenburg--Perletzhofen, from where provide from sinkholes has been confirmed. Generally karstification also leads to the formation of a lake district, such because the Plitvice Lake District. Bimswinkelgraben, from the left and west to under 416 m above sea stage. Raingraben, from the left and north at over 416 m above sea stage. North at over 405 m above sea level. Heglauer Mühlbach, from the left and north at over 414.7 m above sea degree. Inlet of the Heidental dry valley, from the left and north at 338.2 m above sea degree.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seaside of Unterwurmbach only 100 meters from the run of the earlier one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Center and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as nicely because the Birkenmühle and the Langweidmühle in 1806 handed to the brand new Kingdom of Bavaria. The listing of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally referred to as Schambach, from left and east to lower 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.Three m above sea degree. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of Esbach) → Birkengraben → Upper Kuhgraben → Lower Kuhgraben → Betzengraben. Upper course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea level.



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