↑ Jürgen Eisenbrand: Sediments from Altmühlsee end up in artificial basins. These sediments have been removed since September 2015, every autumn and winter. This web page was last edited on September 1, 2021 at 11:Forty am. This page was last edited on August 30, 2022 at 10:37 am. This web page was final edited on March 25, 2023 at 4:Forty six a.m. This page was last edited on August 3, 2023 at 10:55 am. This page was last edited on June 26, 2023 at 2:17 am. After it was dismantled because of dilapidation, it’s now related to the trail by a connecting causeway. The prices of constructing the system, the detailed planning of which started in 1971 by the Nuremberg Dam Construction Authority, which existed until 2000, amounted to approx. The Großer Brombachsee, dammed by the primary dam, serves as a reservoir and the water level can fluctuate by as much as seven meters throughout common operation because of the irregular inflow and outflow. The Birkenhof north of Absberg between the 2 our bodies of water Igelsbach and Gänsbach, whose corridor additionally sank into the Großer Brombachsee, only existed as a barn by 1962. By 1962, just one barn was left standing at the Birkenhof north of Absberg between the 2 bodies of water, Igelsbach and Gänsbach, whose land additionally sank into the Großer Brombachsee.
When water is low, water can also be released from the lake back into the Altmühl, however as a rule it’s initially transported from the Altmühlsee through the 8.7 km long Altmühl overpass, which crosses below the watershed in a tunnel over a distance of 2.7 km the Kleiner Brombachsee and from there into the instantly adjoining Großer Brombachsee. The Dennenloher See is positioned at Dennenlohe within the Ansbach district in Dennenloher Forst, a big forest and heath area. The trail extends over the districts of Weißenburg-Gunzenhausen, Ansbach and Roth. The Mandlesmühle, which is now abandoned as a result of resident, now a district of Pleinfeld situated east of the large Brombachsee, is now residence to the information heart “Seenland – Water for Franconia” of the Ansbach Water Management Office. In Might 1964, the area of today’s Brombachsee was considered appropriate, a valley lock was taken into account to type the Altmühlwasser. November 6, 2018, archived from the unique (not obtainable on-line) on May 20, 2019; accessed on May 20, 2019 (German). ↑ Absberg municipality in the local database of the Bavarian State Library Online. W. Lux: Streudorf municipality. In this manner, water that may usually flow into the Danube via the Altmühl might be redirected into the river system of the Rhine-Primary space over the European important water sheath.
With the Donau-Predominant Transfer, the water management authorities of the Free State of Bavaria lead water from the river system of the Danube to the REGNITZ and MAINE, which is threatened by temporary drought and threatened. While within the designation Main-Donau-Canal the rivers in the word of the geographical association correspond to the common map, the term Danube-Primary override displays the circulation direction of the water pumped from the Danube. The water release from the Rothsee of a maximum of 15 m³/s takes place partly into the decrease reaches of the Kleine Roth, from the place the water flows into the primary by way of Roth, Rednitz and Regnitz, and partly into the underwater of the canal lock, where it flows by means of another barrage the Schwarzach is diverted, which also flows into the Rednitz. This amount of water flows into the principle via the Swabian Rezat, Rednitz and Regnitz. Within the years 1995-2013, a mean of 27.9 million m³ of water was transferred yearly throughout the watershed in this manner; after the top of the impoundment, an average of 26.5 million m³ was transferred in 1999-2013 and 28.7 million m³ from the watershed Brombachsee, with eleven million m³ of additional inflow from the Brombach catchment area expected every year. A complete of three lakes, together with the Altmühlsee with Ringdamm and with Brombach- and Rothsee, include two dams, which embrace 5 dams, three hydropower plants on the dam and the Hilpoltstein lock, the channel routes to the Altmühlsee and with Brombach- and Rothsee. From there to the Brombachsee and 27 other weirs to a few of the watercourses developed for the upper water routing.
To the construction of the three reservoirs of the Brombachsee, the wastelands had to be torn milling mills, Birkenmühle, Furthmühle, Grafenmühle, Griesmühle, Rooster Mill, Langweidmühle, Neumühle, Scheermühle, Spagenhof, Sägmühle, Ziegelhütte, Öfelinsmühle and a concrete plant. The center of the Franconian lake country varieties the Große Brombachsee, the Little Brombachsee and the Igelsbachsee, three straight subsequent to one another, that are solely separated from one another by 2 dams, as well because the Altmühlsee, which is around 10 km west, and the 20 kilometer northeastern Rothsee. The great Brombachsee is round 37 kilometers as the crow flies south of Nuremberg and thirteen kilometers east of Gunzenhausen. An authority was created for the development in 1971, the Nuremberg dam. On July 16, 1970, the construction mission was decided on July 16, 1970 by the Bavarian state parliament and carried out by the Nuremberg Verwördern new constructing office in several construction levels. The Franconian Seenland is an area with artificially created lakes in Bavaria, almost 50 km southwest of Nuremberg in the Middle Franconia region. The lakes had been essentially created with the Danube-Primary bridge, which was built to stability the water distribution between water-rich southern and water-poor northern Bavaria; This is completed by transferring water from the Altmühl and Danube valleys across the main European watershed into the Regnitz-Major space. Along with their water management capabilities, the lakes with a complete of 20 km² of water surface and 80 km of public paths also serve for native recreation.
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