Ivory - Limestone
Quarry Location: Middle Mississippian;southern Indiana, Florida
Recommended Usage: Building stone, pool coping, sills, ornamental stone, interior, exterior design
Finishing Surface: Bush Hammered, Tumbled, Brushed, Honed, Split, Machine Cut, Natural Surface, Sandblasted, Combed, Filled, Chiseled, Pickling
Additional Names: Egg Stone, Oolitic Limestone, Oolite Shellstone, Oolite Stone Standard Buff, Salem Limestone, Oolite Shell Limestone, Oolite Stone
Oolite stone is a unique type of sedimentary limestone characterized by the presence of small spherical structures known as ooids or ooliths. These ooliths are composed of concentric layers of calcium carbonate that accumulate around a central nucleus. Oolite stone forms when these ooids are stuck together by lime mud, creating a distinctive and attractive texture.
The formation of oolite stone begins in shallow marine environments, particularly on the sea floor. Here's how the process typically occurs:
Calcium Carbonate Deposition: In a shallow sea, calcium carbonate is abundant in the water. This mineral can come from various sources, such as the shells of marine organisms or chemical precipitation from the water itself.
Nucleation: The process starts when a small particle, often a sand grain or shell fragment, serves as a nucleus for the ooid formation. This nucleus becomes coated with layers of calcium carbonate as it rolls around on the seafloor, moved by the action of waves.
Accretion: Layers of calcium carbonate continually deposit on the nucleus, forming concentric layers. The growth of these layers results in the creation of ooids, which are small, rounded, and usually between 0.25 to 2.0 millimeters in diameter.
Lime Mud Cementation: Lime mud, which is primarily composed of fine-grained carbonate particles, surrounds the ooids. This mud acts as a binding agent, cementing the ooids together over time.
Oolite stone is known for its attractive appearance, characterized by the multitude of small, rounded ooids that are tightly packed together. The stone can vary in color, often reflecting the local geology and the types of sediments and minerals present in the region where it forms.
Oolite stone is commonly quarried in various locations, including southern Indiana and parts of Florida. Its unique appearance and durability make it a desirable material for construction and ornamental use. It is often used in architectural and landscaping projects, as well as for decorative features such as façades, flooring, and countertops. The combination of the distinctive oolitic texture and the enduring nature of limestone makes oolite stone a popular choice for both aesthetic and functional purposes in construction and design.