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Miami Rock Ridge
from Wikipedia
Rock outcrop closeup

The Miami Rock Ridge is an oolitic, continuous outcrop of limestone, part of the Miami Formation, which formerly covered a large extent of southernmost South Florida; as part of an ecosystem it formed portions of the Everglades. Rising 7 to 8.6 m (23 to 28 ft) above sea level, it ranges from northern Miami-Dade County—the approximate latitude of North Miami Beach—southward to the upper Florida Keys and southwestward into Everglades National Park, creating a karst-dominated landscape.[1] The ridge is of Late Pleistocene origin. A series of tidal channels, dubbed transverse glades, formed within valleys in the ridge and acted as outlets for freshwater from the Everglades, thereby modifying the estuarine environment of Biscayne Bay.[2][a] One of the few areas above pre-drainage sea level, the Miami Rock Ridge was heavily exploited for agriculture and real estate.[5][6]

Ecology

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The coastal ridge was traditionally a component of the endangered pine rocklands, which grew upon its length.[7] Globally imperiled today, the environmental community consisted of a large, unbroken expanse of South Florida slash pines (Pinus elliottii var. densa), interspersed by tropical hardwood hammocks; related to the Bahamian pineyards, it also occupied the Florida Keys.[8][7] The communities of the Miami Rock Ridge are sustained by wildfires, including those caused by lightning strikes, which affect the vegetation and its associates, maintaining biodiversity,[9][10] with a 20% floristic endemism rate.[7] Climate and an often-marly substrate limit the growth of vegetation, such that a mature subtropical hammock on the ridge typically is no taller than 59 feet (18 m).[11][12] Development has largely removed the original communities, which have fragmented into tiny parts of their original range;[7] remnants include Vizcaya Museum and Gardens, Simpson Park Hammock, and Alice Wainwright Park, which form part of Brickell Hammock, underlain by a large oolite outcrop, Silver Bluff.[13][14][b]

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See also

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Notes

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References

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Sources

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