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المشاركات المكتوبة بواسطة Harris Probert

Retrieved January 19, 2023 (English)

Retrieved January 19, 2023 (English)

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The passenger ship, which travels between the lake centers through 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 here the Altmühl is an element of the principle-Danube Canal, which is accompanied on this route on the left and proper by a number of remnants of its predecessor, the Ludwig-Donau-Principal 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 japanese stream around the Altmühlsee. Section additionally runs underground beneath 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 stage.

Hesselbach, from the left and north-northeast to under 418 m above sea stage. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to below 414.9 m above sea stage. Judengraben, from the left and northwest at around 414 m above sea degree. This floodplain ditch is the fitting department of the earlier one at around 414 m above sea stage. Drains in the same meandering course because the Fallach mentioned above to beneath 414 m above sea stage. Arises beneath 420 m above sea degree. Arises at round 420 m above sea level. Flows at about 420 m above sea degree. Wieseth, from the best and southeast or southwest to under 416 m above sea level. Roßbachgraben, from the right and west at 416.7 m above sea stage. → Exit of the Kaltenlachgraben, to the fitting and south to 414.7 m above sea stage. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at under 414.9 m above sea degree. Northeast at under 418 m above sea stage. Arises at round 418 m above sea stage. 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 right; The last one arises instantly on the Altmühl feeder and appears to be the lower reaches of an previous proper estuary of the Wieseth, which is no longer continuous ensuing from the development 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 principle department north of the mill, the secondary department about 500 meters west of it. The 2 higher reaches as much as the Heidweiher are additionally known as Wiesengraben. There are also two moats inside the direction of the top of the mountain spur, one of which remains to be six meters deep. NN at a dirt road junction west of Dittenheim-Sammenheim. NN inside the local space, barely offset in front of a dry valley mouth from the route of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Typically 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 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 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 100 meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. Because of the Reich Deputation Middle 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 new Kingdom of Bavaria. The list of landscapes in Bavaria is based on the numbering of the Federal Institute for Regional Research. Kästleinsmühlbach, partly additionally referred to 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 level. Section identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (through Esbach) → Birkengraben → Higher 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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