Cannabaceae

Ocala Platform
Stratigraphic range: Miocene
TypeGeological structure
Lithology
PrimaryCarbonate
Location
RegionNorth Florida
Country United States
ExtentWakulla to Pasco County
Type section
Named forOcala, Florida
Named byT. M. Scott, 1988
Location of the Ocala Platform within Florida (in red).

The Ocala Platform or Ocala Uplift is a geologic feature, a structural high, and a northwest-trending uplift paralleling the Peninsular Arch along the west coast of Florida.

Age

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Period: Neogene
Epoch: Early Late Oligocene through Pliocene
Faunal stage: Chattian through early Blancan ~23.03 to ~2.588 mya, calculates to a period of 20.442 million years

Origin

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The Ocala Platform was originally named by Hopkins in 1920. Due to the uncertainty of its creation, T. M. Scott[1] used the term "platform" in place of "uplift" or "arch". This geologic feature was described as a gentle flexure developed in Tertiary sediments with a northwest–southeast trending crest by Vernon in 1951.

The Ocala Platform was created during two episodes. The first occurred during the Late Oligocene through Early Miocene and the second episode occurred in Early Pliocene and into Late Pleistocene according to Williams et al. This movement created the feature referred to as the Ocala Uplift. It has been suggested that the uplift was a pre-Hawthorn Group occurrence (Pirkle & Brooks 1959a).[2]

Sediments of the Hawthorn Group are thought to have been deposited across the Ocala Platform (Scott, 1981a; Scott, 1988). Erosion after the Miocene has removed sediments of the Hawthorn Group from much of the crest of the Ocala Platform. This has exposed Eocene carbonates which could confuse dating. (Cooke, 1945; Espenshade and Spencer, 1963; Brooks, 1966; and Scott, 1981b).

Structure

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Fluctuating sea levels during the Neogene has created three marine terraces.

  • Wicomico terrace (70–100 feet)
  • Sunderland/Okefenokee terrace (100–175 feet)
  • Coharie terrace (170–215 feet)

References

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  1. ^ Scott, T.M., 1988, The lithostratigraphy of the Hawthorn Group (Miocene) of Florida: Florida Geological Survey Bulletin 59, 148 p.
  2. ^ USGS: Seismic Reflection Surveys Regional Geology

One thought on “Cannabaceae

  1. Well, that’s interesting to know that Psilotum nudum are known as whisk ferns. Psilotum nudum is the commoner species of the two. While the P. flaccidum is a rare species and is found in the tropical islands. Both the species are usually epiphytic in habit and grow upon tree ferns. These species may also be terrestrial and grow in humus or in the crevices of the rocks.
    View the detailed Guide of Psilotum nudum: Detailed Study Of Psilotum Nudum (Whisk Fern), Classification, Anatomy, Reproduction

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