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Forggensee

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either new farms could be found nearby or new houses were built. Above all, many of the farmers and their descendants who lived in what is now the Forggensee area can still be found in the surrounding communities today. Construction of the dam began in early 1951 after new access roads and a residential camp for up to 1,000 workers had been built. To ensure the dam structure was watertight, the entire dam and its associated structures were built directly on rock; For geological reasons, this did not happen directly at the breakthrough of the Lech through the Illa's Gorge as originally planned, but about a kilometre downstream, so that the ecologically valuable gorge was lost in the process. On the lakeside, a five-meter-thick concrete apron was installed up to 20 meters deep into the rock. In the spring of 1952, the Lech was dammed here and diverted through a tunnel that had been built in the meantime. In the remaining two years until its completion at the end of 1954, the remaining structures were built and the dam was flooded. The building materials were largely obtained from the reservoir itself.
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BAWAG, meanwhile only responsible for expanding the Lech dams, began building the Lech Reservoir in 1950. This led to strong protests from the residents, who founded a protective association and reached a largely satisfactory agreement with BAWAG in the 1952 Schwangau Agreement. For those affected,
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near today's Füssen district of Weidach was completely relocated, 32 families having to leave their homes. Of the affected buildings, only 14 houses from Deutenhausen survived: They were bought by Bavarian Hydropower in 1952 from
391:), from south to north these are the strata of the Deutenhausen Formation, the clay marl strata, the rock strata and in particular the Weißach strata of the Lower Freshwater Molasse (Illasberg, Zwieselberg, Senkele). 354:
This lake may be viewed as the forerunner of the Forggensee and the smaller Pre-Alpine lakes in this region, most of which have survived. The foothills of the Alps were finally free of ice around 14,500 years ago.
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The increasing demand for electricity in the interwar period aroused renewed interest in building a Lech storage reservoir. A draft paper from 1936/37 envisaged a storage target of
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flows through it. The Forggensee is known primarily as a tourist destination for aquatic sports and recreation. Besides Füssen, other settlements on the lake include
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would have resulted in larger resettlements of 1,500 to 2,000 people and, especially in the area around Schwangau, significant loss of agricultural land. The
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Even though the Forggensee is not a natural lake today, it is located in a basin that was filled by a much larger lake after the last ice age: when after the
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A few hundred metres from today's shore, on the former path from Brunnen to Forggen, you will come across the foundation walls and brick remains of a Roman
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to Forggen in 1644, was probably the most important building among the larger individual farms; today its foundation walls are crumbling on the lake bed.
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in the south could be a Roman road that has fallen into oblivion, which perhaps represents a connection from the Roman settlement of Tegelberg to
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The Roßhaupten Dam was renovated in 2018, which is why the lake was not filled in 2018 (as it is every spring). In 2019 the lake was reflooded.
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castles. With a surface area of 15.2 km, it is the fifth-largest lake in Bavaria and the largest reservoir in Germany by area. The
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zone adjoining them to the south) at the southern end of the Murnau Depression at the northern end of the present-day Forggensee.
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whenever the glacier halted temporarily or advanced briefly again. These ridges can still be seen in today's landscape.
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local researcher Sigulf Guggenmos (1941–2018) discovered various important archaeological sites, including traces of
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with a height of 34 m, a crown length of 140 m and a total capacity of 65 million m was to be built. The
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ridges were formed from the masses of debris carried by the ice from the mountains piled up at the edge of the
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near Roßhaupten and received a licence to build a hydroelectric power plant, which, however, expired in 1907.
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Official Settlement Register for Bavaria, based on the census of 13 September 1950, Munich, 1952, column 1288
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gradually carved out through the southern wing of the Murnau Depression near today's barrage no. 1 at
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The lake provides ideal conditions for surfing, sailing, fishing, and boating. The lake is stocked with
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that were cleared in 1974. Such manor houses supplied travellers on the Roman roads. According to the
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in a relatively short time. Lake Füssen also visibly silted up, but it also flowed out through the
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Altogether 32 residential buildings with 256 inhabitants (1950) from the Schwangau villages
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and its trading station at Osterreinen. It is, therefore, possible that an additional
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could be built in the years 1940 to 1950 - the smaller plants could be built faster.
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and economically difficult post-war years prevented the realisation of this project.
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on the old road was demolished as were individual buildings near Dürracker and
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The resulting lake basins were filled with clay and silt deposits from glacial
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gave an impression of the scale of this when the lake level on 22 May 1999 at
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or BAWAG) was founded to build hydropower stations on the Lech, the Lower
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Only small lakes in the hollows of the former lake bed have survived: the
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Aerial photograph of the Forggensee at low water from the SE (March 2020)
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was just over a metre lower than the originally planned water level.
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Northern end of the Forggensee with a view of the Illasberg Gorge
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may be seen in the foothills to the left; to the right is
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View from the terrace of the Neuschwanstein Music Theatre
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The Forggensee from the north. In the background are the
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Boat landing stage at Füssen for the Forggen Navigation
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bought the first plots of land in the area of the Lech
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The Via Claudia Augusta between Rieden and Roßhaupten
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In 1910, the "Royal Supreme Construction Authority" (
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continued to melt, initially forming large masses of
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Southern end of the Forggensee with a view of Füssen
273:. The lake takes its name from the former hamlet of 454:were made at the end of the 19th century. In 1898, 179: 171: 163: 155: 145: 137: 132: 124: 116: 103: 95: 83: 75: 64: 59: 51: 41: 24: 794:Remains of the hamlet of Forggen in the Forggensee 430:that came down from the mountains wintered there. 293:. In the course of its retreat, as in the entire 635:The former episcopal mill, which was moved from 921:Armin Guggenmos, Birgit Gehlen (January 2019), 564:Forggensee Dam from the east aerial view (2019) 552:Forggensee Dam from the west aerial view (2019) 865:"Der Forggensee bleibt diesen Sommer trocken" 671:Bavarian State Office for Monument Protection 332:was one of these glacial lakes, Lake Füssen ( 8: 806:Tiefental Bridge of the former Bundesstraße 522:- the originally planned storage height of 277:which has been submerged by the reservoir. 249:and one of many lakes in the region around 325:, after which lakes formed in the basins. 30: 21: 491:In 1940, the Bavarian Hydropower Works ( 855: 697:saddle and via the Roman settlement on 642:At the northern end of the lake, the 7: 16:Lake in Ostallgäu, Bavaria, Germany 233:, is a reservoir located north of 14: 532:782.91 m above NHN 949: 835: 823: 811: 799: 787: 767: 749: 731: 587:Lech-Füssen area in Roman times. 569: 557: 545: 71:, Füssener Ache, Mühlberger Ache 524:784 m above NHN 520:781 m above NHN 486:784 m above NHN 446:The first plans for using the 338:790 m above NHN 1: 863:Christian Rost (2018-04-30). 701:, which was used seasonally. 467:Königliche Oberste Baubehörde 184:780.5 m above  36:Aerial view of the Forggensee 595:Conservation and archaeology 285:Following the climax of the 104:Elevation at crest 493:Bayerische Wasserkraftwerke 108:785 m above  1002: 359:Silting up of Lake Füssen 29: 923:"Nachruf S Guggenmos BA" 385:Lower Freshwater Molasse 76:Height (foundation) 650:hunting stations and a 473:, according to which a 52:Construction began 927:Bayerische Archäologie 588: 443: 222: 867:. Süddeutsche Zeitung 621:Lower Weidachsiedlung 586: 514:After the end of the 441: 216:Neuschwanstein Castle 197: 180:Normal elevation 958:at Wikimedia Commons 528:1999 Pentecost flood 456:Siemens & Halske 381:Lower Marine Molasse 267:Rieden am Forggensee 231:Roßhaupten Reservoir 138:Active capacity 683:Via Claudia Augusta 448:hydroelectric power 164:Maximum length 147:Catchment area 589: 576:Forgensee overflow 444: 229:, also called the 223: 212:Tannheim Mountains 172:Maximum width 117:Width (crest) 954:Media related to 677:in the north and 237:in the county of 192: 191: 156:Surface area 60:Dam and spillways 993: 981:Lakes of Bavaria 953: 937: 936: 935: 934: 918: 912: 907: 901: 900: 898: 897: 882: 876: 875: 873: 872: 860: 839: 827: 815: 803: 791: 771: 753: 735: 632:near Schwangau. 573: 561: 549: 533: 525: 521: 516:Second World War 499:, and the Upper 487: 339: 188: 112: 34: 22: 19:Dam in Ostallgäu 1001: 1000: 996: 995: 994: 992: 991: 990: 971: 970: 946: 941: 940: 932: 930: 920: 919: 915: 908: 904: 895: 893: 884: 883: 879: 870: 868: 862: 861: 857: 852: 847: 846: 845: 844: 843: 840: 832: 831: 828: 820: 819: 816: 808: 807: 804: 796: 795: 792: 781: 780: 779: 777: 772: 763: 762: 761: 759: 754: 745: 744: 743: 741: 736: 727: 707: 597: 581: 580: 579: 578: 577: 574: 566: 565: 562: 554: 553: 550: 531: 523: 519: 485: 479:First World War 450:available near 436: 369:Illasberg Gorge 361: 337: 311: 283: 186:sea level (NHN) 183: 125:Dam volume 110:sea level (NHN) 107: 37: 20: 17: 12: 11: 5: 999: 997: 989: 988: 983: 973: 972: 969: 968: 959: 945: 944:External links 942: 939: 938: 913: 902: 877: 854: 853: 851: 848: 841: 834: 833: 829: 822: 821: 817: 810: 809: 805: 798: 797: 793: 786: 785: 784: 783: 782: 774: 773: 766: 765: 764: 756: 755: 748: 747: 746: 738: 737: 730: 729: 728: 726: 723: 706: 703: 596: 593: 575: 568: 567: 563: 556: 555: 551: 544: 543: 542: 541: 540: 435: 432: 360: 357: 330:Lech Waterfall 310: 307: 303:glacial tongue 282: 279: 255:Neuschwanstein 251:Hohenschwangau 190: 189: 181: 177: 176: 173: 169: 168: 165: 161: 160: 157: 153: 152: 149: 143: 142: 139: 135: 134: 130: 129: 126: 122: 121: 118: 114: 113: 105: 101: 100: 97: 93: 92: 89: 81: 80: 77: 73: 72: 66: 62: 61: 57: 56: 53: 49: 48: 43: 39: 38: 35: 27: 26: 18: 15: 13: 10: 9: 6: 4: 3: 2: 998: 987: 984: 982: 979: 978: 976: 967: 963: 960: 957: 952: 948: 947: 943: 928: 924: 917: 914: 911: 906: 903: 891: 887: 881: 878: 866: 859: 856: 849: 838: 826: 814: 802: 790: 776: 770: 758: 752: 740: 734: 724: 722: 720: 716: 712: 704: 702: 700: 696: 692: 688: 684: 680: 676: 672: 668: 667:villa rustica 663: 661: 657: 653: 649: 645: 640: 638: 633: 631: 627: 622: 618: 614: 610: 606: 602: 594: 592: 585: 572: 560: 548: 539: 535: 529: 517: 512: 510: 506: 502: 498: 494: 489: 482: 480: 476: 472: 468: 463: 461: 457: 453: 449: 440: 433: 431: 429: 425: 421: 417: 413: 409: 405: 401: 397: 392: 390: 386: 382: 378: 374: 370: 366: 358: 356: 352: 350: 347: 343: 335: 331: 328:North of the 326: 324: 320: 319:Lech Glacier 316: 308: 306: 304: 300: 296: 292: 288: 280: 278: 276: 272: 268: 264: 260: 256: 252: 248: 244: 240: 236: 232: 228: 221: 217: 213: 209: 205: 201: 196: 187: 182: 178: 174: 170: 166: 162: 158: 154: 150: 148: 144: 140: 136: 131: 127: 123: 119: 115: 111: 106: 102: 98: 94: 90: 87: 84:Height ( 82: 78: 74: 70: 67: 63: 58: 54: 50: 47: 44: 40: 33: 28: 23: 931:, retrieved 926: 916: 905: 894:. Retrieved 892:. 2019-04-02 880: 869:. Retrieved 858: 708: 693:through the 674: 664: 641: 634: 626:Theodor Momm 625: 620: 605:Deutenhausen 598: 590: 536: 513: 492: 490: 483: 466: 464: 445: 393: 371:, which the 368: 362: 353: 334:Füssener See 333: 327: 315:Würm Ice Age 312: 287:last ice age 284: 230: 226: 224: 964:, lakes in 929:(in German) 652:Late Celtic 637:Waltenhofen 630:St. Coloman 613:Osterreinen 416:Lech Valley 309:Lake Füssen 975:Categories 962:Forggensee 956:Forggensee 933:2019-10-30 896:2019-04-30 871:2018-05-26 850:References 705:Recreation 687:Roman road 648:Mesolithic 452:Roßhaupten 442:Forggensee 377:Roßhaupten 373:River Lech 365:meltwaters 346:Cretaceous 297:area, new 295:Pre-Alpine 291:Kaufbeuren 271:Roßhaupten 259:River Lech 227:Forggensee 25:Forggensee 986:Ostallgäu 699:Tegelberg 689:ran from 660:sacrifice 658:place of 505:Landsberg 460:water gap 434:Reservoir 426:; so the 408:Weißensee 404:Schwansee 396:Bannwald- 239:Ostallgäu 208:Thaneller 200:Tegelberg 133:Reservoir 128:650,000 m 55:1950–1954 46:Ostallgäu 691:Pinswang 675:Auerberg 644:Dösinger 509:Schongau 428:red deer 389:Tertiary 383:and the 323:dead ice 299:morainic 263:Halblech 151:1,594 km 65:Impounds 42:Location 725:Gallery 679:Säuling 609:Forggen 601:Brunnen 400:Hopfen- 342:molasse 275:Forggen 247:Germany 243:Bavaria 204:Säuling 159:15.2 km 86:thalweg 966:Füssen 890:Uniper 695:Alpsee 619:; the 617:Füssen 501:Danube 412:Alpsee 410:. The 349:Flysch 317:, the 281:Origin 235:Füssen 220:Füssen 175:2.8 km 167:8.7 km 141:168 Mm 96:Length 715:trout 656:Roman 424:flora 420:fauna 99:320 m 717:and 711:pike 607:and 507:and 497:Isar 471:Lech 422:and 406:and 269:and 253:and 225:The 210:and 120:10 m 91:37 m 79:41 m 69:Lech 719:eel 654:or 475:dam 241:in 977:: 925:, 888:. 713:, 662:. 603:, 402:, 398:, 265:, 245:, 214:, 206:, 202:, 899:. 874:. 387:( 88:)

Index


Ostallgäu
Lech
thalweg
sea level (NHN)
Catchment area
sea level (NHN)

Tegelberg
Säuling
Thaneller
Tannheim Mountains
Neuschwanstein Castle
Füssen
Füssen
Ostallgäu
Bavaria
Germany
Hohenschwangau
Neuschwanstein
River Lech
Halblech
Rieden am Forggensee
Roßhaupten
Forggen
last ice age
Kaufbeuren
Pre-Alpine
morainic
glacial tongue

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