670 resultados para 1340-1416
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This layer is a georeferenced raster image of the historic paper map entitled: Map of the country thirty miles round the city of New York, designed & drawn by I.H. Eddy. It was published by J. Disturnell in 1836. Scale [1:190,080]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Universal Transverse Mercator (UTM) Zone 18N NAD83 projection. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, turnpikes and toll locations, railroads, drainage, canals, selected public buildings (industry locations, taverns, etc.), selected private residences with names of landowners, cities and towns, county and state boundaries, and more. Relief is shown by hachures. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.
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Written in one column, 17 lines per page, in black and red.
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Title from fol. 1r.
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Copy completed on 9 Shawwāl 859 AH [September 21, 1455 AD].
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Laboratory measurements on sediment samples and density well logs run at DSDP Site 534 in the Blake-Bahama Basin were used to establish an in situ velocity and density structure. Synthetic seismograms were generated for comparison to reprocessed seismic reflection data in the vicinity of the Site. Uncertainties in the relative positions of the hole and seismic reflection data, velocity corrections, and the composition of the unrecovered section were evaluated. In light of the errors and compressed section, no unique correlation of the seismic reflection data to the drill hole is completely defensible either in this chapter or elsewhere. The preferred correlation resulting from this exercise is as follows, with the Site 534 report correlation shown in parentheses where different. Horizon beta', 887 m; Horizon beta, 950 m (975 m); Horizon C , 1202 m (1250 m); Horizon C, 1268 m (1340 m); Horizon D', 1342 m (1432 m); Horizon D, 1550 m (1552 m). The major differences in these correlations arise from the use of slightly different velocities and hole location relative to the seismic profiles. The Site 534 report results rely on hole placement on a basement flank, whereas in this chapter we locate it within a basement depression still within the uncertainty of the navigation. The Site 534 report also uses drilling rates, CDP velocity analyses, sonobuoy data, and previous similar drilling correlation methods used at Site 391, along with other geologic considerations in arriving at differing results. Although the correlation method used in this investigation is more objective and the hole location uncertainties better defined, in order to have confidence in any results we will require drilling in areas where reflections are either more widely spaced or where we have better vertical velocity control in the hole.
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Vol. 8, pt. II, to vol. 11, edited by Gaston Raynaud; vol. 12- by Léon Mirot.
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Limbourg Brothers; 9 3/8 in.x 6 11/16 in.; tempera and gold leaf on vellum
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1 ft. 11 5/16 in.x 1 ft. 3 5/8 in.; ink, opaque watercolor and gold on paper
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9 9/16 in.x 7 3/4 in.; ink, opaque watercolor, gold and silver on paper
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Mode of access: Internet.