The Brombachsee Marathon started at Lake Brombach and ended in Pleinfeld. The district’s respiratory protection middle is positioned on the positioning of the Pleinfeld fire brigade. The vast majority of the southern part of the catchment area is positioned within the adjacent natural area of the southern Franconia alb, including the upper Rezattal and the low hill and mountain country east of it in the sub-space of the Weißenburger Alb, while the areas on the left and west of the valley belong to the underground Weimersheimer Platte. It rises here in a short facet valley within the Narche Altmühlalb pure area of her north -wing major valley, which additionally sets the Altmühl flowing to the valley axis on the side of the valley axis. This is where the valley begins to deepen. From there as much as the mouth, the valley and the remainder of the appropriate-hand catchment space belong to the sub-space Rother Sand Platten, while the left-hand catchment area is distributed over the sub-areas Southern Foreland of the Spalt Hill Country (with Brombachgrund) in the south, Southern Spalt Hill Nation within the northwest and north and a span of the Jap Foreland of thespalter hill country near the mouth of the Rezat to the left. It’s surrounded by forests in a valley that opens to the east. NHN between Muhr am See in the southeast and Ornbau within the northwest and is bordered in the south by the Altmühlsee, within the east by the Mönchswald, in the north by the towns of Hirschlach and Heglau and in the west by the Altmühlzuleiter.
Simply behind Weißenburg, its longest tributary, the Felchbach, reaches it from the east. From Galgenberg to the Kingdom of Heaven (Weißenburg Native Historical past Books Quantity 4), Weißenburg i. ↑ Ulf Beier: Weißenburg field title e book. ↑ Ralph Jätzold: Geographical survey of the country: The natural spatial models on sheet 172 Nördlingen. ↑ Alexander von Humboldt Professorship|Friedrich Alexander University Erlangen-Nuremberg. ↑ Johann Alexander Döderlein: Schediasma Historicum, IMPP. Johann Kaspar Bundschuh: Retzat. " in a doc, they in all probability first sat on the stone house outdoors the village and throughout the 12th or thirteenth century they moved their headquarters to the moated castles throughout the village. NN the Hornauer Weiher on the edge of the village of Hornau, approx. The drain from The remains of the canal results in the Altmühl. At the locks on the south ramp of the primary-Danube Canal – Kelheim, Riedenburg, Dietfurt, Berching and Bachhausen – pumping stations with a delivery capacity of 35 m³/s are installed, which provide each the canal's water provide and serve as a transition. → Exit of the Jochsberger Mühlkanal, to the right at 426 m above Furthgraben, from the correct and west to over 426 m above sea degree. It initially runs through the flat Ried and then passes the core city of Weissenburg within the west. From a pure perspective, the catchment area there shares the eaves of the southern Franconian Alb, and more precisely, its sub-areas (from southwest to northeast) Weißenburger Alb, Anlauteralb and Anlauter-Braunjuratrichter.
Lastly, the Swabian Rezat unites between the eponymous essential town of the municipality of Georgensgmünd on the left and its district of Petersgmünd on the suitable reverse at an altitude of 341.7 m with the Franconian Rezat, which comes from the southwest and is much longer and has a richer catchment space, to kind the oblique Fundamental tributary Rednitz. According to tradition, Charlemagne already wanted to overcome the principle European watershed between the catchment areas of the Danube and Rhine, which runs, among different things, over the mountain ranges between the Swabian Rezat and Altmühl, by way of a canal. Then straight again into open movement, it passes the Letzleinsmühle on the correct financial institution, now flows north between the Galgenberg on the precise and the final wasteland of Simonsmühle von Gnotzheim on the left and then changes to the town limits of Gunzenhausen just under the hamlet of Steinacker on the best slope. After descending from the Alb plateau, the Scheide moves, initially over the Franconian Alb-Zeugenberg Schloßberg (606.7 m), in entrance of, among other issues, the tributaries of the upper Roth roughly northwest to the confluence with the Franconian Rezat; Right here the catchment area of the Rednitz borders on the outside. The northern watershed west of the mouth borders the lower catchment area of the Franconian Rezat, which also competes within the northwest via its right-hand tributary Erlbach near Höfstetten.
The more essential tributaries of the Swabian Rezat, listed from origin to confluence. There are a quantity of green areas in Pleinfeld, particularly along the Swabian Rezat, which are characterized by huge meadows and small bridges. No federal waterways run by means of Pleinfeld because no river in the region is appropriate for shipping. ↑ Joshua Sans: Cheers to the region. ↑ Names of our bodies of water within the Weißenburg-Gunzenhausen district, Mfr., in: Sheets for Higher German name research. It then takes up the Brombach coming from the Großer Brombachsee and passes a number of mills and the villages of Mühlstetten and Niedermauk, two districts of the municipality of Röttenbach in the Roth district. Giant elements of the southern and jap half of the municipality are occupied by a forestless open panorama. With a vertical Kaplan turbine with a movement price of 14 m³/s and a head of 7.20 m, an electrical output of 898 kW is achieved; the system has a regular output of 1.8 GWh per 12 months. From 60 m³/s one speaks of a 100-year flood on the Swabian Rezat. It belongs to the river system of the Rhine and is the less water -rich of the 2 supply rivers of the Rednitz – its left and western supply circulation is the longer and water -wealthy Franconian recurrence – hydrographically, a tribute to the Rednitz. NHN Excessive summit of the leaf bichel east of the Wülzburg on the southeastern water sheath.
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