Great Blue Hole: Perbedaan antara revisi
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Baris 1:
|title=The Great Blue Hole of Lighthouse Reef Atoll, Belize, Central America: Deep Technical Diving to Collect Sea-Level Records
|publisher=Transactions of the Fifteenth Caribbean Geological Conference
|url=http://books.google.lv/books?id=RZbjcQEvfN4C&pg=PA190&lpg=PA190&dq=dEAN'S+bLUE+hOLE+geology&source=bl&ots=Xdmi64cZ_L&sig=BnSHUtiUb7YIYxhGMV4uUCRYj6w&hl=lv&ei=LPNBTPrPNomCOPKbmOsM&sa=X&oi=book_result&ct=result&resnum=3&ved=0CCEQ6AEwAg#v=onepage&q=dEAN'S%20bLUE%20hOLE%20geology&f=false
}}</ref> Hal ini terbentuk selama beberapa episode [[glasiasi Kuarter]] ketika permukaan air laut jauh lebih rendah - analisa penemuan stalaktit di Great Blue Hole menunjukkan formasi yang telah terjadi 153.000, 66.000, 60.000, dan 15.000 tahun yang lalu.<ref name="Wondermondo" >{{cite web
|title=Great Blue Hole
|publisher=Wondermondo
|url=http://www.wondermondo.com/Countries/NA/Belize/Belize/GreatBlueHole.htm}}</ref> As the ocean began to rise again, the caves were flooded.<ref name="NASA" >{{cite web
|title=Belize Blue Hole reef
|publisher=NASA
|url=http://earthobservatory.nasa.gov/IOTD/view.php?id=37741&src=iotdrss
}}</ref>
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