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Tuesday, July 21, 2020 | History

3 edition of Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, 1975-1979 found in the catalog.

Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, 1975-1979

Charles D. Whiteman

Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, 1975-1979

by Charles D. Whiteman

  • 121 Want to read
  • 31 Currently reading

Published by Louisiana Dept. of Transportation and Development, Office of Public Works in Baton Rouge, La .
Written in English

    Places:
  • Louisiana,
  • Baton Rouge region.
    • Subjects:
    • Subsidences (Earth movements) -- Louisiana -- Baton Rouge region.

    • Edition Notes

      Bibliography: p. 13.

      Statementby C. D. Whiteman, Jr.
      SeriesWater resources technical report ;, no. 20
      ContributionsLouisiana. Office of Public Works.
      Classifications
      LC ClassificationsQE600.3.U6 W48
      The Physical Object
      Paginationiv, 18 p. :
      Number of Pages18
      ID Numbers
      Open LibraryOL4241115M
      LC Control Number80621814

      Flood insurance study East Baton Rouge Parish, Louisiana, (Baton Rouge and vicinity) (SuDoc FEM /) Unknown Binding – January 1, Manufacturer: Federal Emergency Management Agency. Historic Crests (1) ft on 05/18/ (2) ft on 01/18/ (3) ft on 04/25/ (4) ft on 06/01/ (5) ft on 01/20/

      louisiana department of wildlife and fisheries po box quail drive baton rouge, la search the site.   Recent U.S. Geological Survey research focused on better understanding the physical processes that contributed to historical wetland loss in coastal Louisiana and the spatial and temporal trends of that loss. The results of this study provide the first comprehensive analyses of the three-dimensional aspects of historical wetland loss in coastal Louisiana and .

      images. Since , the emergent land area at the five study areas in south-central Louisiana has decreased by about 50%. Comparison of the water-area curve derived from the 29 TM images with water-level records from the nearby Grand Isle, Louisiana tide gauge (NOS #) clearly shows that changes in land and water areas fluctuate in. Louisiana must obtain a certificate of authority to transact business in Louisiana from the Louisiana Secretary of State, Corporations Division, Essen Lane, Baton Rouge, Louis iana , telephone number ()


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Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, 1975-1979 by Charles D. Whiteman Download PDF EPUB FB2

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measuring local subsidence with extensometers in the baton rouge area, louisiana, prepared by united states department of the interior geological survey in cooperation with louisiana department of transportation and development office of public works Buy Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, (Water resources technical report) by Charles D Whiteman (ISBN:) from Amazon's Book Store.

Everyday low prices and free delivery on eligible : Charles D Whiteman. Whiteman, C.D., Jr.,Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, Louisiana Department of Transportation and Development, Office of Public Works Water Resources Technical Report no. 20, 18 p.

Whiteman, C.D., Jr.,Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, Louisiana Department of Transportation and Development, Office of Public Works Water Resources Technical Report no. 20, 18. Whiteman CD () Measuring local subsidence with extensometers in the Baton Rouge area, Louisiana, – Office of Public Works Water Resources technical report no.

20, Louisiana Department of Transportation and Development, Baton Rouge, LA, 18 pp. the Baton Rouge area, Louisiana,including a discussion of saltwater in other sands: Louisiana Department of Transportation and Development, Office of Public Works Water Resources Technical Report no. 19, 49 p. Whiteman, C.D., Jr.,Measuring local subsidence with extensometers in the Baton Rouge.

Subsidence of South Louisiana: Measurement, Causes, and Human Implications Roy K. Dokka Department of Civil & Environmental Engineering Center for GeoInformatics Louisiana State University, Baton Rouge, LA The book was.

Tides • Diurnal = Gulf of Mexico northern coast – One high/low tide cycle per day • Semidiurnal = East & West U.S. coasts – Two high/lot tide cycles per day • High tide is 11 minutes later each day • Affected by storms, geology, variation of the Earth’s density, wobble of Earth & Moon, and the planet Venus (and currents).

Understanding Subsidence. in Coastal Louisiana. Prepared by: Denise J. Reed. Brendan Yuill. Pontchartrain Institute for Environmental Sciences.

University of New Orleans. New Orleans, LA. For the Louisiana Coastal Area Science and Technology Program. Barbara Kleiss, Director. Febru Contract # WHZ iii. LONG-TERM SUBSIDENCE AND COMPACTION RATES: A NEW MODEL FOR THE MICHOUD AREA, SOUTH LOUISIANA A Thesis Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Master of Science In The Department of Geology By Clint H.

Edrington. For example, the MARY station in Michoud records mm/yr subsidence at a depth of m (Table 1 and Figure S4 in the supporting information), which would imply that in the same general area. P.O. Box ( North Third Street) Baton Rouge, Louisiana Bill Info - SB27 Login Sign-Up.

Present subsidence rates from tide gauge records exceed 40 mm/yr at the modern Mississippi River Delta and approximate I 0 mm/yr in wetlands near the gulf coast. Subsidence rates over the last I, years appear to have. Request PDF | Resolving the contributing factors to Mississippi Delta subsidence: Past and Present | To date, quantification of individual components that.

Two regional releveling profiles and six tide gauges provide a basis for evaluating recent rates of delta plain subsidence in southcentral Louisiana. Analyses of these records demonstrate close correlations among highest historical rates of subsidence, rapid wetland losses, large volume hydrocarbon production, and probable reactivation of deep subsurface faults.

• Where and at what volumes water moves underground from one part of the area to the next – information important to storm-water drainage plans. • The effects changing groundwater levels and subsidence are having on the wooden pilings supporting many of the city’s buildings and homes – an issue brought to light in other cities.

Business First Bank Baton Rouge, East Baton Rouge Parish, LA, proposes to relocate its MAIN OFFICE from Jefferson Highway, Suite [] to Laurel Street [] (a distance of approximately 7 miles), both locations within Baton Rouge, East Baton Rouge Parish, LA. LOAN or TRUST PRODUCTION OFFICES Filed/Approved Aug Rainfall Frequency/Magnitude Atlas for the Louisiana State University Baton Rouge, LA SRCC Technical Report 97­1 southeastern Texas into southwestern Louisiana.

Another area with relatively large storm magnitudes occurs over the coastal areas of southeastern Louisiana and coastal Mississippi.

Created Date: Z. Louisiana State University Baton Rouge, Louisiana ABSTRACT / Annual coastal land loss in the sedimentary deltaic plain of southern Louisiana is km 2, which is correlated with man- made canal surface area. The relationships between land loss and.The main components of sediment budget include relative sea-level rise, local subsidence, human activities, oxidation and decomposition of surface peat, tides and winds.

Recent estimates of relative sea-level rise in Louisiana are cm/year (Turner, ). The rate of subsidence, due to the compaction of coastal.Household Types by Place in the Baton Rouge Area There are 53 places that are fully or partially contained within the Baton Rouge Area (52 fully and 1 partially).

This section compares all 53 of those to each other, the Baton Rouge Area, and other entities that contain or substantially overlap with the Baton Rouge Area.