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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
After a description of the various types of limestone around the world, the author lays out four problems with the standard theory of how limestone formed in warm, shallow seas. The rest of the book describes an alternative theory for the formation of limestone, suggesting that most limestone came from inorganic sources, possibly from mineral-saturated water that had been under the crust of the earth since its creation. In a global flooding event, this mineral water came to the surface, was sorted into layers by liquefaction, and formed a large portion of the world's sedimentary rock layers.
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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
After a description of the various types of limestone around the world, the author lays out four problems with the standard theory of how limestone formed in warm, shallow seas. The rest of the book describes an alternative theory for the formation of limestone, suggesting that most limestone came from inorganic sources, possibly from mineral-saturated water that had been under the crust of the earth since its creation. In a global flooding event, this mineral water came to the surface, was sorted into layers by liquefaction, and formed a large portion of the world's sedimentary rock layers.