Fossilizing the shells

Bentonite, charcoal, common clay or diatomaceous earth are the most important examples. In this case we will use the Diatomeas land as an important intestinal parasitic destructive agent Detoxant Review.

Diatoms are unicellular plants that lived in the oceans by trillions about 300 million years ago. They formed a small shell composed of the same silicates extracted from the water. When the diatoms died, this microscopic coating was deposited at the bottom of the oceans.

Through the eras they accumulated in deposits forming thicknesses of thousands of meters. Over time the oceans receded and these deposits were eventually covered Detoxant Review. Fossilizing the shells and compressing, they give rise to a rock chalk powder called diatomaceous earth.

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