Peninsular Arch

Peninsular Arch
Stratigraphic range: Jurassic
Type Geological formation
Unit of None
Sub-units None
Lithology
Primary Carbonate
Location
Region North Florida to South Florida
Country  United States

The Peninsular Arch is a geologic formation and dominant sub-surface structure of Florida.

Contents

Age

The arch was present from the Jurassic ~199.6—145.5 Ma through the Paleogene geological periods.

Location

The Peninsular Arch extends from southeastern Georgia to just north of Lake Okeechobee in a general northwest to southeast trend. It is highest in Union County and Baker County. Its crest passes beneath Alachua County.

Structure

The Peninsular Arch parallels the Ocala Platform to its west and is the dominant sub-surface feature within Florida. It is a structurally high area which affected deposition of sediments during the Cretaceous to the early Cenozoic. It was a high topographic feature during most of the Cretaceous but was covered with Late Cretaceous sediments and became an ideal base and settling point for carbonate sediments during the Eocene when that portion of land was submerged.[1] According to Williams and T. M. Scott, the arch did not affect sediments from depositing during the Neogene through Halocene.[2][3]

References

  1. ^ Applin, P., 1951, Possible future petroleum provinces of North America - Florida: American Association of Petroleum Geologists Bulletin, v. 35, p. 405-407.
  2. ^ Williams, K.E., Nicol, D., and Randazzo, A.F., 1977, The geology of the western part of Alachua County, Florida: Florida Geological Survey Report of Investigation 85, 97 p.
  3. ^ Scott, T.M., 1997, Miocene to Holocene history of Florida: in Randazzo, A.F., and Jones, D.S., eds., 1997, The Geology of Florida: Gainesville, University Press of Florida, 327 p.