Last edited by Milkis
Friday, July 17, 2020 | History

2 edition of Facies and genesis of a hurricane-washover fan, St. Joseph Island, Central Texas Coast. found in the catalog.

Facies and genesis of a hurricane-washover fan, St. Joseph Island, Central Texas Coast.

Peter B. Andrews

Facies and genesis of a hurricane-washover fan, St. Joseph Island, Central Texas Coast.

by Peter B. Andrews

  • 238 Want to read
  • 38 Currently reading

Published by University of Texas in Austin, Tx .
Written in English


Edition Notes

SeriesReport of Investigations -- no 67
ContributionsUniversity of Texas. Bureau of Economic Geology.
ID Numbers
Open LibraryOL15636625M

The island is situated in the only major gap of this barrier chain, between Anclote Key to the north and Honeymoon Island to the south. St. Joseph Sound, a relatively shallow back barrier bay, bounds the island to the east, and 3-meter-deep channels, both north and south of the island, allow essentially unrestricted tidal flow between the Gulf   Identification of such a trend will require extensive and very deep drilling. References Cited Allen, stratified units, with notes on their origin: Sedimentology, v. 2, pp. Andrews, P. B. () Facies and genesis of a hurricane washover fan, St. Joseph  › 百度文库 › 行业资料.

Stratigraphic and Sedimentological Evidence for Accelerated Washover Rates: Case Study of Follets Island, Texas. Christopher I. Odezulu, Jorge Lorenzo-Trueba, Davin J. Wallace, John B. Anderson. Effects of Highstand Mud Accumulation on the Evolution of the Central Texas Coast. Christopher I. Odezulu, Travis Swanson, John B. Deep-water processes and facies models (7) High Island, late Pliocene, conventional core, Gulf of Mexico, U.S. (8) East Breaks, late Pliocene-Holocene, conventional and piston cores, Gulf of Mexico, U.S. (9) Midway Sunset Field, upper Miocene, conventional core, onshore California, U.S. (10) Jackfork Group, Pennsylvanian, outcrop, Ouachita

ABSTRACT Barrier islands developed on the southeastern flanks of a volcanic terrain during the Lower Silurian transgression of southwest Wales. The barriers are preserved in transgressive sequences overlying basalts and comprising from base upwards: lagoon→barrier island→offshore marine sediments. The thickness of the barrier island sediments varies from 5 m to 28 m. Comparison with modern   ABSTRACT: Bunces Key, a narrow, linear, barrier island on the west-central coast of Florida, was formed in Its growth and development since that time is well documented by aerial photography. Cores taken from the Key and surrounding areas reveal a stratigraphic succession of facies reflecting rapid vertical ://


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Facies and genesis of a hurricane-washover fan, St. Joseph Island, Central Texas Coast by Peter B. Andrews Download PDF EPUB FB2

RID. Facies and Genesis of a Hurricane-Washover Fan, St. Joseph Island, Central Texas Coast - Downloadable PDF. Part Number RID Facies and genesis of a hurricane-washover fan, St. Joseph Island, Central Texas Coast. View/ Open. txu-oclcpdf (Mb) Date Author. Andrews, Peter B.

Share Facebook Twitter LinkedIn. Metadata Show full item record. Department. UT Libraries. :// Get this from a library. Facies and genesis of a hurricane-washover fan, St. Joseph Island, Central Texas Coast. [Peter B Andrews]   Facies and Genesis of a Hurricane-Washover Fan, St.

Joseph Island, Central Texas Coast Abstract Two distinctive subaerial physiographic features that form a substantial portion, by area, of most barrier islands along the Texas coast are the washover fan and the tidal Facies and genesis of a hurricane-washover fan, St.

Joseph Island, Central Texas Coast. By Peter B. Andrews. Cite. BibTex; Full citation; Abstract. This report formed the basis of a Ph.D. dissertation concluded at the University of Texas at Austin in UT Librarie RI Facies and Genesis of a Hurricane-Washover Fan, St. Joseph Island, Central Texas Coast, by P.

Andrews. p., 18 figs., 22 plates, ISSN: X Facies and genesis of a hurricane-washover fan: St. Joseph Island, Central Texas Coast by Peter B. Andrews (Report of investigations, no. 67) Bureau of Economic Geology, University of Texas, Facies and genesis of a hurricane-washover fan: St.

Joseph Island, Central Texas Coast[Bureau of Economic Geology, University of Texas at Austin] in English   Andrews,Facies and genesis Of a hurricane-washover fan.

Joseph Island, central Texas coast: Texas Bureau of Economic Geology Report of Investigati p. Aronow, Saul,Nueces River delta plain of Pleistocene Beaumont Formation, Corpus Christi region. Texas: American Association of Petroleum Geologists Bulletin v.

55,   Landward edge of Matagorda and San Jose Islands includes wash-over fan sediments deposited by hurricane-driven waves that surge over the islands.

Channel sand is interbedded with planar-bedded sand which replaces it landward and in turn merges with lagoonal mud. Facies and genesis of a hurricane-washover fan, St.

Joseph Island, central   Web view. Facies and genesis of a hurricane washover fan, St. Joseph Island, Central Texas Coast Publication Date: Geochemistry, hydrology and mineralogy of the Laguna Madre flats, south Texas Andrews, P.

B.,Facies and genesis of a hurricane-washover St. Joseph Island, Central Texas Coast: Univ. Texas, Austin, Economic Geology Report no. 67, :// Andrews, P.B. Facies and genesis of a hurricane-washover fan, St. Joseph Island, central Texas coast.

Rept and facies of a young hurricane washover fan on southern St. Joseph Island, central south Texas coast. M.S. Thesis, Univ. of Texas, Austin Stoneburner, D.L. Evidence of hurricane influence on barrier island slash pine   Hurricane washover fan, northern St. Joseph Island, Texas.

After Andrews () (slightly modified from McGowen and Scott, ). structures occurred in the fans he studied: (1) flat-bed deposits in the landward and central portions of the fans; and (2) small delta-foreset strata along the landward margins of fans that build into a water ://   Formation and development of a tidal inlet from a washover fan, west-central Florida coast, U.S.A.

Sediment. Geol., A moderate-sized washover fan generated by Hurricane Elena in on the barrier coast of west-central Florida was subsequently cut and reworked into a tidal :// The depositional environment dictates the facies pattern including the size, form and overall context of initially porous and permeable sand-bodies.

ANDREWS, P.B. Facies and genesis of a hurrican washover fan, St. Joseph Island, Central Texas Coast. Rep. Invest. Bur. econ. Geol., 67,Austin, Texas. Google Scholar SWIFT, D.J.P   Facies and Genesis of a Hurricane-Washover Fan, St.

Joseph Island, Central Texas Coast: RI Pre-Chappel Conodonts of the Llano Region, Texas: RI Gum Hollow Fan Delta, Nueces Bay, Texas: RI Palynology of the Eddleman Coal (Pennsylvanian) of North-Central Texas: ?criteria=&items_per_page=50&. MAIN LIBRARY. Perry-Castañeda Library East 21st St.

Austin, TX. Phone: () Facies and genesis of a hurricane-washover fan, St. Joseph Island, Central Texas Coast  Andrews, Peter B.

(University of Texas at Austin. Bureau of Economic Geology, ) Depositional framework, hydrostratigraphy, and uranium mineralization of the Oakville Sandstone (Miocene), Texas Coastal Plain    Andrews, P.B. () Facies and genesis of a hurricane- washover fan, St. Joseph Island, Central Texas Coast.

Bureau of Economic Geology, University of Texas at. Our results indicate that the most commonly used model for a washover fan, the 52 km(2) St. Joseph Island fan, is anomalous and does not reflect the most common sizes or geometries of washover ://Two small mouth-bars are then deposited in the mouths of these channels and the channel continues to split until become too small to carry sediments ().After this, the system becomes chocked and avulsion or lobe switching occ the good example is Mississippi delta system.

The formation of shallow-marine deltaic basins is typically exhibit a lobe shape with multi-scale coeval terminal ?doi=jasPalaeoenvironments and palynofacies of a pulsed transgression: the late Devonian and early Dinantian (Lower Carboniferous) rocks of southeast Wales - Volume Issue 4 -