Oolitic aragonite sand

From Wikipedia, the free encyclopedia
Jump to: navigation, search

Oolitic aragonite sand forms in tropical waters. Most of the topography of the Bahama Banks is composed of calcium carbonate oolitic aragonite sand material.

The natural formation through precipitation and sedimentation of aragonite sand in the Bahamas surpasses anyplace else in the world.[citation needed] There are billions of tons of this type of sand material in reserve and millions of tons more created annually.[citation needed]

Commercial uses[edit]

Commercial uses are similar to limestone and other high calcium carbonate materials.

References[edit]

See also[edit]