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UNESCO: United Nations Educational, Scientific. Miami limestone or Miami oolites which is deposited during pleistocene. The Miami Oolite, although thin, is a very porous, oolitic limestone that is present at the land surface throughout much of Dade County and parts of Broward and Monroe Counties. Primarily consisting of limestone, the bedrock geology of Everglades National Park has responded over time to the ongoing processes of weathering, erosion, compaction of organic sediments, unique hydrologic conditions, and episodes of sea-level rise and fall to produce the landscapes we see today. These differences are due to the nature of the loading mechanism. Question: Part of Miami is built on a sedimentary rock called oolitic limestone. On much larger orders, the percentage of quantity difference will be reduced. On orders less than 4 tons, please allow for 20% more or less product quantity regarding your ordered amount. The oolitic formation in the lower Florida Keys has less quartz sand and fewer fossils than does the oolitic formation on the mainland. Miami oolite was formed during the Pleistocene era in a high energy, shallow water environment. The part of the Miami Limestone forming the Atlantic Coastal Ridge and the lower Florida Keys is an oolitic grainstone which includes fossils of corals, echinoids, mollusks, and algae. Guiding Volume: On orders of 4 tons or more, please allow for 10% more or less in product quantity regarding your ordered amount. Miami oolite overlays the Key Largo limestone formation. Product Coloration: Product may appear darker or lighter than the picture due to being a natural product. Both stones are generally off white in appearance, but we have found the deposit to contain orange and golden colors as well. Beyond these depths we find a compact limestone called Hemingway stone. This means it is found close to the surface of the ground, and can run as deep as 30 feet. Size Variation: Please allow for up to 10% larger or smaller pieces as well as up to 10% fine material within your product than what is described in the product information. Geologic unit mapped in Florida: The Miami Limestone (formerly the Miami Oolite), named by Sanford (1909), occurs at or near the surface in southeastern. Oolite stone is generally a cap rock material. Common applications: Driveway Gravel RV Pads Drainage Control French Drains Walkways Concrete Mix Disclaimer #57 is one of the most popular and common gravels as it has a wide range of applications. Sizes of #57 Stone range from 1/2" to 1". #57 Stone is a crushed angular Limestone aggregate. The Miami Limestone (formerly the Miami Oolite), named by Sanford (1909), occurs at or near the surface in southeastern peninsular Florida from Palm Beach County to Dade and Monroe Counties.