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The shores of the bay are shaped by the tides and the surf as during high winds from the northeast and southwest, heavy sea might build up. When the water level is 0.75 m (2.5 ft) higher than usual, sand and gravel is being eroded from the cliff coast. In some places, the coastline recedes
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and
Eckernförde Bay, which was later converted into a dam. The dam was badly damaged in the 1872 flood of the Baltic Sea, as the road built in the 17th century was no longer functional. The road was rebuilt and the dam was raised. The modern road was built in 1965.
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The
Eckernförde Bay is a popular holiday destination. The seaside resort Eckernförde registers around 135,000 overnight stays a year. There are eleven campsites scattered around the bay. The waters of the bay are also the starting point for the ancient
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was subsequently used. However, Danish also remained in widespread use in
Schwansen until the 19th century. Both Schwansen and the Danish Wahld retained their feudal character until the Early Modern Period.
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As Danish tribes had settled in
Schwansen since around 700 CE. and German settlers had arrived at Danish Wahld around 1260, the Eckernförde Bay became the linguistic border between
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376:, that had formed during the last Ice Age in the southeast are hollowed out and a 30 m (98 ft) high and 3.6 km (2.2 mi) long cliff has formed in front of
587:"Physical and Biological Influences on the Formation of Sedimentary Fabric in an Oxygen-Restricted Depositional Environment: Eckernförde Bay, Southwestern Baltic Sea"
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266:. The bay extends around 17 km (11 mi) deep into the land and is 10 km (6.2 mi) wide at its entrance where
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from the
Eckernförde Bay. Several sand banks run parallel to the beach. The banks are mainly forested with deciduous trees.
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eventually exploded and the crewv of the frigate surrendered and the ship was taken over by the
Schleswig-Holstein army.
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caused severe damage to the coastal towns of
Eckernförde Bay. The town of Eckernförde in particular suffered the most.
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of the
Eckernförde Bay had already formed before the Ice Age and contributed to the fact that the
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peninsula between Kiel Fjord and
Eckernförde Bay constituted the borderland between the
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380:. The steadily eroded material is partly deposited further west and has separated the
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between 120,000 to 10,000 years ago from a glacier. According to some geologists, the
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282:) mark the endpoints. The bay is up to 28 m (92 ft) deep. The border to the
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15 to 20 cm (5.9 to 7.9 in) every year. As a result the hills of the
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565:"Effects of the Temporal Variability of Storm Surges on Coastal Flooding"
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operates several bases and facilities at
Eckernförde Bay, such as the
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in the north. The divide is still noticeable in the Danish-Nordic
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Since the 15th century a road on the beach wall (near the modern
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were shot at by beach batteries from Schleswig-Holstein troops.
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364:. There are plans to establish a canal between the Bay and the
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network. The region is thus connected with Kiel, Lübeck and
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Kiel-Eckernförde-Flensburger Eisenbahn-Gesellschaft - KEFE
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The original post-glacial end of Eckernförde Bay, today's
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traverses around the Baltic Sea as part of the European
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Ortsnamen und Ortsgeschichten aus Schleswig-Holstein
503:) runs parallel to the road that is operated by the
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585:Samuel J. Bentley, Charles A. Nittrouer (1999).
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543:"Spannende Radrouten in der Eckernförder Bucht"
306:. At the inner end of the bay lies the town of
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758:"AALREGATTA ZUR KIELER WOCHE FÜR JEDERMANN"
642:A History of the Church in the Middle Ages
514:criss-cross the Eckernförde Bay area. The
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666:Haefs, Hanswilhelm (March 11, 2004).
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456:Economy, infrastructure and transport
510:Numerous bicycle paths, such as the
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505:Schleswig-Holstein Regional Railway
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639:F Donald Logan (2 October 2012).
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782:. Ostsee-Holstein-Tourismus e.V
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236:Egernførde Fjord or Egernfjord
73:Show map of Schleswig-Holstein
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711:. archive org. Archived from
709:"Katastrofen ved Eckernførde"
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329:municipality, Eckernförde Bay
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645:. Routledge. pp. 71–.
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844:Bays of Schleswig-Holstein
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333:The bay formed during the
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802:"Baltic Sea Cycle Route"
545:. Ostseebad Eckernfoerde
200:10 km (6.2 mi)
736:"Sturmflut Ostsee 1872"
448:A few years later, the
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854:Bays of the Baltic Sea
516:Baltic Sea Cycle Route
512:Baltic Sea Cycle Route
497:Kiel–Flensburg railway
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208:28 m (92 ft)
780:"Ostseeküsten-Radweg"
597:(6). jstor: 585–600.
450:1872 Baltic Sea flood
425:Battle of Eckernförde
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325:tree forest in rural
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696:– via Ernster.
427:in 1849, the Danish
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147:54.47806°N 9.94500°E
679:] (in German).
603:1999Palai..14..585B
343:Eckernförde glacier
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103:Show map of Germany
676:Schleswig-Holstein
487:) existed between
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260:Schleswig-Holstein
228:Eckernförder Bucht
117:Schleswig-Holstein
18:Bay of Eckernförde
849:Förden of Germany
652:978-1-134-78669-5
407:in the south and
374:Terminal moraines
351:Wittensee-Goossee
349:and the southern
278:(municipality of
270:(municipality of
258:off the lands of
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246:between the
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175:Part of
829:(in German)
465:during the
423:During the
308:Eckernförde
304:Middle Ages
280:Schwedeneck
268:Booknis-Eck
244:Bay of Kiel
189:Max. length
179:Bay of Kiel
150: /
125:Coordinates
838:Categories
808:January 5,
786:January 6,
764:January 5,
742:January 5,
719:January 5,
692:January 6,
624:January 5,
570:January 5,
549:January 4,
530:References
524:Copenhagen
474:Bundeswehr
463:Aalregatta
405:Low German
302:until the
284:Kiel Fjord
256:Baltic Sea
205:Max. depth
197:Max. width
135:54°28′41″N
467:Kiel Week
314:Geography
252:Schwansen
220:‹See Tfd›
138:9°56′42″E
119:, Germany
520:EuroVelo
413:toponyms
378:Altenhof
298:and the
113:Location
619:3515315
599:Bibcode
591:PALAIOS
489:Goossee
436:frigate
388:History
382:Goossee
264:Germany
238:) is a
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478:WTD 71
439:Gefion
409:Danish
399:, 1849
296:Saxons
274:) and
232:Danish
224:German
804:. ECF
672:[
615:JSTOR
323:Beech
300:Danes
272:Waabs
240:firth
169:firth
810:2021
788:2021
766:2021
744:2021
721:2021
694:2021
681:ISBN
647:ISBN
626:2021
572:2021
551:2021
495:The
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362:Noor
327:Noer
164:Type
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