957 resultados para Assyrian Church of the East
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[Conceptual Sketch of Elevation], untitled. Ink sketch on tracing paper with marker coloring, 12x32 inches [from photographic copy by Lance Burgharrdt]
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[Conceptual Representation of Tree of Life Motif on Door], untitled. Cut-out cardboard pieces on mat board, initialed, 18x23 inches [from photographic copy by Lance Burgharrdt]
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Mode of access: Internet.
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Cover title: Rev. J. Adams' convention sermon on the relation of Christianity to civil government in the United States of America.
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Mode of access: Internet.
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owing to the loss of the volume containing the entries for that period."--Pref.
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Colored plates accompanied by guard sheets with descriptive letterpress.
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v. 1. Arabian nights' entertainments [from the French version of A. Galland] New Arabian nights [from the French version of D. Chavis and J. Cazotte]--v. 2. Continuation of the New Arabian nights. Persian tales [from the translation of F. Pétis de la Croix] Persian tales of Inatulla of Delhi [tr. by A. Dow] Oriental tales [by A. C. P., comte de Caylus] The history of Nourjahad [by Mrs. Frances Sheridan] Additional tales from the Arabian nights.--v. 3. Mogul tales [by T. S. Gueulette] Turkish tales [from the translation of F. Pétis de la Croix] Tartarian tales; Chinese tales [by T. S. Gueulette] Tales of the genii [by J. Ridley] The history of Abdalla, the son of Hanif [by J. P. Bignon]
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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During the expeditions ARK-VII/1, ARK-VII/3 and ARK-Xl2 sediment cores were taken by "RV Polarstern" from the shelf and the fjords of East Greenland and the Greenland Sea. The magnetic susceptibility and heavy mineral were determined at 48 surface sediment samples from undisturbed box cores. The main objective of this study was the identification of source areas and transport processes of terrigenous sediments at the East Greenland continental margin. The results can be summarized as lollows: 1a) Magnetic susceptibility in the North Atlantic is useful to detect delivery regions of the material transported by currents. b) The magnetic susceptibility is controlled by the ferromagnetic particles of the silt fraction. c) There are four important source areas: . The ferromagnetic particles of the box core PS2644-2 are transported from the Iceland Archipelago. . The material from the Geiki-Plateau effects the magnetic susceptibility in the Scoresby Sund Basin. . The magnetic susceptibility in the shelf regions in the North are produced by material from the fjords. . The ferromagnetic particles in the Greenland Sea are derived from the Mid Atlantic Ridges in the east. d) It is possible to determine the rock type, which delivers the ferromagnetic material because of differences in magnetic susceptibility of different intensity. . The erosion of the basalts of the Geiki-Plateau and the basalts of the Mid Atlantic ridges produce the high magnetic susceptibility in the south. . The magnetic susceptibility on the shelf in the north are probably produced by erosionproducts of the gneises of East Greenland. (2a) Heavy mineral assemblages show a significant difference between material transported by the Transpolar Drift from the Eurasian shelf regions (amphiboles, clinopyroxene, orthopyroxene) and material derived from East Greenland (garnets and opaque minerals). Transport via ice is dominant. b) lt is also possible to show different petrographic provenances (volcanic and metamorphic provenances). These associations verify the source areas. c) The information of heavy mineral composition gives no more detailed hint on the rock type or rock formation in the source area, due to mixing processes, large area of investigation and the sample quantity.