Sea levels fell during the last ice age, so that about 20,000 years ago these reefs and ridges were exposed and vegetation grew on the once-submerged areas. At that time the sea was warm enough to allow coral to grow and reefs and sandy bars formed on the shallow shelf. It is these variations in sea level, starting 125,000 years ago when the sea level was about 7m higher than at present, which have been primarily responsible for the geology and topography of the Florida Keys. Modified from Shinn and Lidz, 2018.Ĭarbonate sedimentation continued through the Pleistocene and Holocene and on into the present, interspersed by glacial and interglacial periods and subsequent marine incursions and withdrawals. Sketch cross-section roughly north-west to south-east across the Florida Keys. Subsidence of the passive continental margin resulted in carbonate deposition about 160 million years ago in the late Jurassic, which continued through the Cretaceous and Tertiary to create the Florida Platform, an accumulation of nearly 5,000m of shallow-water carbonates and evaporites with only minor components of terrigenous sediments. Precambrian-Cambrian igneous rocks were overlain by Ordovician-Devonian sediments and Triassic-Jurassic volcanics, deposited as the Florida basement separated from the African plate to join North America. The relatively young Florida Keys have much older foundations. However, this unique environment, the result of repeated episodes of flooding and exposure during the Pleistocene, also allows us an insight into limestone formation throughout the world. Made up of over 800 islands, none more than 5.5m above sea level, and stretching in a gentle arc nearly 200 km from Miami south-westwards into the Gulf of Mexico, the Florida Keys are known for their distinctive ecology, clear waters and beautiful coral reefs a famous playground for fishermen and snorkellers alike. Source: Google Earth.Ī string of pearls in a turquoise sea: as well as being picturesque, the unique Florida Keys offer the petroleum geologist a masterclass on carbonate sedimentary processes. Satellite image of the Florida Keys identifying places mentioned in the text. Sunshine/Oolite is typically “cut to order” with short lead time of 7 to 30 days depending on size, thickness and quantity required.Īn ancient stone, that has stood the test of time in design for today’s residential and commercial markets.The picturesque Florida Keys are not just a favourite holiday destination, they also offer geoscientists a masterclass on carbonate geology and the sedimentary processes associated with creating carbonate reservoirs. Coral Classics recommends 40SK Dry Treat Sealer for this product. If sealed properly after install, this material can be managed and maintained and kept relatively clean. If left exposed to weather and not sealed, this material over time will “Patina” and achieve the “Old World Castle Look”. Wall cladding, flooring, architectural elements, stepping stones, landscape boulders and retaining walls, wall caps, coping, stair treads, fountains, fireplaces and benches are just a few of the examples. Made famous in Coral Gables and South Beach, is has been and is still today, used on luxurious residential homes and estates as well as commercial hotel and retail store applications. Created from water and compression, this material is uniform in color and is available in either a white selection or a gold selection.Ī very porous material with holes throughout, it has been used all over South Florida in all types of applications. This unique material is extracted from underground shallow quarries that are thousands of years old.
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