The passenger ship, which travels between the lake centers through the season, is also suitable 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 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, a part of Franconia. From right here the Altmühl is an element of the main-Danube Canal, which is accompanied on this route on the left and proper by various remnants of its predecessor, the Ludwig-Donau-Most important Canal, a few of which are additionally connected to it. From here, the Altmühl flows in an synthetic course on a bigger scale approximately east-southeast to the eastern movement across the Altmühlsee. Part also runs underground underneath the left edge of the Altmühltal, to the Kleiner Brombachsee (Rkhpark Co`s latest blog post) in the Rednitz catchment space. Schafgraben, from the left and northwest to under 418 m above sea stage.
Hesselbach, from the left and north-northeast to below 418 m above sea stage. The decrease Schlegelsbühlgraben takes the upper Bankertsgraben from the left and northwest to below 414.9 m above sea level. Judengraben, from the left and northwest at around 414 m above sea level. This floodplain ditch is the appropriate department of the previous one at around 414 m above sea level. Drains in an analogous meandering course as the Fallach mentioned above to below 414 m above sea stage. Arises beneath 420 m above sea stage. Arises at round 420 m above sea degree. Flows at about 420 m above sea degree. Wieseth, from the precise and southeast or southwest to under 416 m above sea degree. 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 stage. → Departure of the Schlegelsbühlgraben secondary stream, also referred to as Häfelesgraben, at beneath 414.9 m above sea level. Northeast at underneath 418 m above sea stage. Arises at round 418 m above sea degree. Arises at over 418 m above sea degree. 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 fitting; The last one arises directly on the Altmühl feeder and appears to be the decrease reaches of an outdated proper estuary of the Wieseth, which is no longer continuous because of the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the opposite facet 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 main branch north of the mill, the secondary branch about 500 meters west of it. The 2 upper reaches as much as the Heidweiher are also known as Wiesengraben. There are additionally two moats towards the tip of the mountain spur, one among which continues to be six meters deep. NN at a dirt street junction west of Dittenheim-Sammenheim. NN inside the native space, barely offset in front of a dry valley mouth from the direction of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Sometimes 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 level. Raingraben, from the left and north at over 416 m above sea level. North at over 405 m above sea stage. 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 degree.
Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. 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 on account 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 checklist of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly additionally known as 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.Three m above sea degree. Part name sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Section of the title Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by way of Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises beneath 365 m above sea level.