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Retrieved January 19, 2023 (English)

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작성자 Wade 작성일24-04-02 07:19 조회30회 댓글0건

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The passenger ship, which travels between the lake centers in the course of the season, can be appropriate for exploring Lake Altmühlsee in a relaxed manner. 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 here the Altmühl is half of the main-Danube Canal, which is accompanied on this route on the left and right by a variety of remnants of its predecessor, the Ludwig-Donau-Essential Canal, some of which are also connected to it. From right here, the Altmühl flows in an artificial course on a bigger scale approximately east-southeast to the eastern move across 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 below 418 m above sea stage.

Hesselbach, from the left and north-northeast to beneath 418 m above sea stage. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to beneath 414.9 m above sea level. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the fitting department of the earlier one at around 414 m above sea level. Drains in the same meandering course because the Fallach mentioned 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 correct and southeast or southwest to under 416 m above sea stage. Roßbachgraben, from the right and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the suitable and south to 414.7 m above sea degree. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at under 414.9 m above sea degree. Northeast at under 418 m above sea level. Arises at around 418 m above sea level. Arises at over 418 m above sea level. 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 decrease reaches of an previous right estuary of the Wieseth, which is not steady as a result of the development of the Altmühl feeder, because the Zeckl, Zegel or Leugraben flows to the opposite side 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 department north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches up to the Heidweiher are also called Wiesengraben. There are additionally two moats in route of the tip of the mountain spur, one of which remains to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN inside the local space, barely offset in entrance of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from the place supply from sinkholes has been proven. Generally karstification also results in the formation of a lake district, such as 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 stage. 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 stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. NN on the northwest seaside of Unterwurmbach solely 100 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 properly as the Birkenmühle and the Langweidmühle in 1806 passed to the brand new Kingdom of Bavaria. The checklist of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally called 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 building to 415.3 m above sea level. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through 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 below 365 m above sea stage.



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