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Phase 2: During subsequent ice ages, other glaciers were created and hollowed out the valley. In warmer periods, the material was eroded by
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Phase 3: After the removal of rocks from the fault, erosion of a stronger layer from a different age was much slower.
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278:(1,382 m), a few minutes walk away from the summit of the rocky cirque. Some hiking paths are signposted, via
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The ground beneath the Creux du Van remains permanently frozen to this day (
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approximately 1,400 metres wide and 150 metres deep, on the north side of
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Wild Alpine Ibex and Swiss Alps at Creux du Van with snow during sunset
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The summit area can be reached on foot or by car. A paved road from
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420:"Three Top Excursions To The Creux Du Van You Don't Want To Miss"
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were introduced in the area in 1965. As of 2009, there are 17.
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A picture of sunset taken at the summit of the Creux du Van.
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The rocky arc of Creux du Van was created in three phases:
438:"A practical guide to hiking the Creux du Van rock arena"
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Other unmarked paths allow access to the summit via
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109:Learn how and when to remove this message
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287:Notable trails in the areas include:
511:Mountains of the canton of Neuchâtel
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47:adding citations to reliable sources
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506:Tourist attractions in Switzerland
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448:from the original on 2021-10-07
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442:Newly Swissed Online Magazine
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357:Panoramic view from the top
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209:around 140,000 years ago (
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521:Mountains of Switzerland
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362:1467 Montagne de Bounty
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482:46.93250°N 6.72361°E
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444:. 6 October 2021.
332:le Pertuis de Bise
326:la Fontaine Froide
275:la ferme du Soliat
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372:Creux du Van
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41:Please help
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201:Phase 1: A
500:Categories
470:46°55′57″N
404:8 February
366:References
241:Attraction
235:permafrost
69:newspapers
473:6°43′25″E
452:7 October
399:Swisstopo
298:Noiraigue
218:meltwater
188:Neuchâtel
175:, in the
173:Le Soliat
446:Archived
340:Panorama
397:(Map).
203:glacier
194:Geology
83:scholar
266:Couvet
252:Access
228:cirque
184:canton
169:cirque
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379:Notes
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454:2021
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