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The Brombachsee Marathon began at Lake Brombach and ended in Pleinfeld. The district's respiratory safety center is located on the positioning of the Pleinfeld hearth brigade. The vast majority of the southern a part of the catchment area is located within the adjacent natural space of ​​the southern Franconia alb, including the upper Rezattal and the low hill and mountain country east of it in the sub-area of ​​the Weißenburger Alb, while the areas on the left and west of the valley belong to the underground Weimersheimer Platte. It rises right here in a short side valley within the Narche Altmühlalb natural space of ​​her north -wing principal valley, which also units the Altmühl flowing to the valley axis on the aspect of the valley axis. This is the place the valley begins to deepen. From there up to the mouth, the valley and the rest of the correct-hand catchment area belong to the sub-area Rother Sand Platten, while the left-hand catchment space is distributed over the sub-areas Southern Foreland of the Spalt Hill Nation (with Brombachgrund) within the south, Southern Spalt Hill Nation in the northwest and north and a span of the Jap Foreland of thespalter hill country close to the mouth of the Rezat to the left. It is surrounded by forests in a valley that opens to the east. NHN between Muhr am See within the southeast and Ornbau within the northwest and is bordered within the south by the Altmühlsee, in the east by the Mönchswald, within 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 Volume 4), Weißenburg i. ↑ Ulf Beier: Weißenburg subject name e-book. ↑ Ralph Jätzold: Geographical survey of the nation: The natural spatial models on sheet 172 Nördlingen. ↑ Alexander von Humboldt Professorship|Friedrich Alexander College Erlangen-Nuremberg. ↑ Johann Alexander Döderlein: Schediasma Historicum, IMPP. Johann Kaspar Bundschuh: Retzat. " in a document, they in all probability first sat on the stone home outdoors the village and all through the 12th or 13th 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 leads to the Altmühl. On the locks on the south ramp of the main-Danube Canal - Kelheim, Riedenburg, Dietfurt, Berching and Bachhausen - pumping stations with a supply capability of 35 m³/s are put in, which provide both the canal's water provide and function a transition. → Exit of the Jochsberger Mühlkanal, to the fitting at 426 m above Furthgraben, from the appropriate and west to over 426 m above sea stage. It initially runs via the flat Ried and then passes the core city of Weissenburg within the west. From a natural perspective, the catchment space there shares the eaves of the southern Franconian Alb, and extra precisely, its sub-areas (from southwest to northeast) Weißenburger Alb, Anlauteralb and Anlauter-Braunjuratrichter.

Lastly, the Swabian Rezat unites between the eponymous primary town of the municipality of Georgensgmünd on the left and its district of Petersgmünd on the best opposite at an altitude of 341.7 m with the Franconian Rezat, which comes from the southwest and is for much longer and has a richer catchment area, to form the indirect Essential tributary Rednitz. In response to tradition, Charlemagne already needed to overcome the main European watershed between the catchment areas of the Danube and Rhine, which runs, among other issues, over the mountain ranges between the Swabian Rezat and Altmühl, by means of a canal. Then straight back into open move, it passes the Letzleinsmühle on the correct bank, now flows north between the Galgenberg on the best and the final wasteland of Simonsmühle von Gnotzheim on the left after which modifications to town limits of Gunzenhausen simply under the hamlet of Steinacker on the right slope. After descending from the Alb plateau, the Scheide moves, initially over the Franconian Alb-Zeugenberg Schloßberg (606.7 m), in entrance of, amongst other things, 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 skin. The northern watershed west of the mouth borders the decrease catchment area of ​​the Franconian Rezat, which also competes within the northwest via its proper-hand tributary Erlbach near Höfstetten.

The extra vital tributaries of the Swabian Rezat, listed from origin to confluence. There are several inexperienced areas in Pleinfeld, especially along the Swabian Rezat, that are characterized by broad meadows and small bridges. No federal waterways run by means of Pleinfeld as a result of no river inside the region is appropriate for delivery. ↑ Joshua Sans: Cheers to the area. ↑ Names of our bodies of water within the Weißenburg-Gunzenhausen district, Mfr., in: Sheets for Higher German name analysis. 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 within the Roth district. Massive parts of the southern and jap half of the municipality are occupied by a forestless open panorama. With a vertical Kaplan turbine with a flow fee 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-yr flood on the Swabian Rezat. It belongs to the river system of the Rhine and is the less water -rich of the two source rivers of the Rednitz - its left and western supply movement is the longer and water -rich Franconian recurrence - hydrographically, a tribute to the Rednitz. NHN High summit of the leaf bichel east of the Wülzburg on the southeastern water sheath.

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