937 resultados para North Carolina--Church history--Colonial period, ca. 1600-1775


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A comprehensive engineering analysis of the coastal sediment transport processes along a 42-kilometer segment of the North Carolina shoreline from Wrightsville Beach to Fort Fisher is presented. Included in the analysis is an interpretation of the littoral processes, longshore transport, and the behavior and success of beach nourishment projects at Wrightsville Beach and Carolina Beach, North Carolina. The historical position of the MLW, MSL, and MHW contours, relative to a fixed base line, is plotted for the period between 1964 and 1975. An equivalent volumetric erosion or accretion between successive surveys is determined by multiplying the average excursion distance of the contours by a constant of proportionality. The plots of excursion distance versus time for the MLW, MSL, and MHW contours also show the time response of the beach fills. This response is described by a mathematical function. The alongshore components of wave-induced energy flux are also determined within the study area through wave refraction analysis. This information, together with the information on volumetric change, is used in a sediment budget analysis to determine the coefficient of alongshore sediment transport and the inlet trapping characteristics. (Author).

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Beach profile lines at 21 near-evenly spaced intervals along Holden Beach, North Carolina, between Lockwoods Folly and Shallotte Inlets, were measured from November 1970 to December 1974. These have been analyzed to determine the spatial and temporal variabilities on long-term, seasonal, and short-term scales. Profile lines near the inlets showed the greatest variability in mean sea level (MSL) position, above MSL volume, foreshore slope, and profile envelope. This variability near Lockwoods Folly Inlet was partly enhanced by artificial nourishment at profile line 2. Temporary, low-cost shore protection devices (e.g., sandbag groins) were constructed near that inlet during part of the study. No other modifications or activities that affected beach processes were known to occur during the study period. The central part of Holden Beach was studied separately because of the high variability of the inlet sections at either end of the island. Foreshore slopes along this reach increased from an average of 1:30 at the east end to 1:17 at the west. A seasonal change in above MSL volume indicates loss of sand during autumn and winter, and gain during spring and summer. Changes in MSL shoreline intercept and above MSL volume were highly variable during the study.

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National Highway Traffic Safety Administration, Washington, D.C.

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National Highway Traffic Safety Administration, Washington, D.C.

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Contents: v. 1. Early Period, from the Ascencion of Our Lord to the Conversion of Constantine -- v. 2. Early Middle Period, from the Edict of Milan to the establishments of the new Western Empire under the Carlovingians, the temporal power of the Popes, and the coming into being of the States of the Church (1931) -- v. 3. To the s-called Reformation -- v. 4. Reformation to the triumph of the Papcy in the restoration of the temporal power in 1929 under Pope Pius XI.

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Vol.1 includes section "Recent publications on North Carolina".

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"Roster of the continental line from North Carolina, 1783": v. 16, p. [1002]-1197. Other rosters and lists of revolutionary soldiers in the collection are noted in the Index, v. 4 (Historical review, p. 95-96)

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The colonial and state records of North Carolina. vol. [XXVII]-XXX.

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Vols. for 1909-33 issued as Publications of the Historical Commission; 1935-39 as Publications of the Legislative Reference Librarian.

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Title varies slightly.