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of the entire west beach of the island and this has proved an important protection against the loss of land. However this has also resulted in the Rotes Kliff in the municipality of
Wenningstedt becoming largely invisible from the sea, because it is now hidden behind
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For centuries these striking cliffs have acted as an unmistakable recognition mark of the island for ships. Nowhere on the German and Dutch North Sea shores is there such a striking
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have a similar coloration but are considerably older and have a different genesis. The rocks that break off the Rotes Kliff - such as
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facing the open sea, beginning in the south at the car park of "Risgap" in
Wenningstedt and ending in the north at
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debris in the region of the present-day island of Sylt. As a result of rising
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231:- still enable an accurate determination of their origin to be made.
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Rotes Kliff, seen from the beach between
Wenningstedt and Kampen
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measures have been taken, however, in the shape of extensive
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suspected there was a geological connexion between Sylt and
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234:The Rotes Kliff has always been at great risk from
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192:in the post-glacial period, these formed an
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158:. It is located on the west side of the
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48:adding citations to reliable sources
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138:is a around 30-metre high line of
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328:Landforms of Schleswig-Holstein
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207:Even in the 19th century,
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176:About 120,000 years ago,
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204:of ferrous elements.
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294:54.95083°N 8.32417°E
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248:sand replenishment
194:abrasion coastline
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323:Cliffs of Germany
299:54.95083; 8.32417
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63:"Rotes Kliff"
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59:Find sources:
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29:This article
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236:storm surges
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198:glacial till
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144:Wenningstedt
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104:January 2012
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42:Please help
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253:beach grass
136:Rotes Kliff
312:Categories
282:54°57′03″N
257:sand dunes
213:Heligoland
209:geologists
190:sea levels
154:island of
140:sea cliffs
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285:8°19′27″E
255:-covered
202:oxidation
152:North Sea
31:does not
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178:glaciers
240:erosion
180:of the
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52:removed
37:sources
160:island
148:Kampen
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221:flint
217:rocks
95:JSTOR
81:books
238:and
186:rock
156:Sylt
146:and
134:The
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35:any
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