تخطى إلى المحتوى الرئيسي

المشاركات المكتوبة بواسطة Eve Scales

Retrieved January 19, 2023 (English)

Retrieved January 19, 2023 (English)

The passenger ship, which travels between the lake centers throughout the season, is also appropriate for exploring Lake Altmühlsee in a relaxed method. A transport 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, part of Franconia. From here the Altmühl is part of the main-Danube Canal, which is accompanied on this route on the left and right by plenty of remnants of its predecessor, the Ludwig-Donau-Fundamental Canal, some of which are additionally linked to it. From here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the eastern circulate around the Altmühlsee. Section also runs underground under 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 level.

Hesselbach, from the left and north-northeast to under 418 m above sea level. The lower Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to under 414.9 m above sea degree. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the appropriate branch of the earlier one at round 414 m above sea stage. Drains in a similar meandering course as the Fallach mentioned above to under 414 m above sea level. Arises beneath 420 m above sea stage. Arises at around 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the best and southeast or southwest to below 416 m above sea stage. Roßbachgraben, from the precise and west at 416.7 m above sea degree. → Exit of the Kaltenlachgraben, to the proper and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also known as Häfelesgraben, at under 414.9 m above sea level. Northeast at underneath 418 m above sea degree. Arises at around 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 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 seems to be the decrease reaches of an previous right estuary of the Wieseth, which is no longer 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.

lost in the sky

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 department north of the mill, the secondary branch about 500 meters west of it. The 2 upper reaches up to the Heidweiher are additionally called Wiesengraben. There are also two moats towards the tip of the mountain spur, certainly one of which remains to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN in the native area, barely offset in entrance of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from where provide from sinkholes has been confirmed. 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 degree. Raingraben, from the left and north at over 416 m above sea degree. North at over 405 m above sea degree. 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 stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea degree. NN on the northwest seashore of Unterwurmbach solely a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Middle and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as well as the Birkenmühle and the Langweidmühle in 1806 passed to the brand 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 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 constructing to 415.3 m above sea stage. Section name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the identify Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (via Esbach) → Birkengraben → Upper Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Higher course and approx. 3.2 km². Arises beneath 365 m above sea stage.

  • مشاركة