Colorful White-Red Cliffs In Hunstanton Uk,Interesting For Biologists And Geologists. Eroding Cliffs Expose A Mid-Cretaceous Sequence From The Albian To The Succeeding Cenomanian Around 100 Million Years Ago, With Exceptionally Rich Albian Ammonite Fossils, The Main Layers Are Carstone And Chalk. Carstone Is The Brown Sand Cemented Together By Iron Oxide Rust.

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100 ago albian ammonite biologists brown carr carstone cemented cenomanian chalk cliffs colorful eroding exceptionally expose fossils geologists hunstanton iron layers main midcretaceous million oxide rich rust sand sequence stone succeeding together ukinteresting whitered years