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Published: 2012-08-02 15:09:12 +0000 UTC; Views: 395; Favourites: 35; Downloads: 0
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Description
The famous red and white striped cliffs at Hunstanton in Norfolk, UK, are an eye-catching attraction:The stripes in the cliffs are caused by layers of different-coloured rock. The main layers are:
Carrstone. This is the brown layer and consists of sandstone - sand cemented together by iron oxide (rust). In places where the cement is stronger, the rock is darker and less crumbly. There are no fossils in this layer apart from a little fossilised wood.
Chalk. The red and white chalk is made of limestone. Limestone forms in warm tropical climates, which suggests that Hunstanton's climate was once warmer than it is today! The colour of the red chalk is due to iron staining
Taken at Hunstanton, Norfolk, England. UK
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Dawn Quadling, in-the-picture, © 2011
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Comments: 6
AmandaDrage [2012-08-04 17:04:53 +0000 UTC]
Ah the umistakeable Hunstanton! I was there a couple of months ago, I loved the fulmars nesting on the cliff face!
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In-the-picture In reply to AmandaDrage [2012-08-06 16:46:45 +0000 UTC]
Its a great place to bird watch - amazing what you can observe, whilst others just walk by unseeing
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In-the-picture In reply to Speck2 [2012-08-03 19:26:10 +0000 UTC]
Thanks, I used to spend a lot of time there when I was little - great rock pools to play in
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Speck2 In reply to In-the-picture [2012-08-03 20:29:53 +0000 UTC]
Aww, memories!! So very welcome !!
Cindy
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