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NARROW
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all geography including DSDP/ODP Sites and Legs
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North Pole
“THE SEA FRYSETH NOT”: SCIENCE AND THE OPEN POLAR SEA IN THE NINETEENTH CENTURY
FROM INTERWAR TO COLD WAR: SELLING FIELD SCIENCE IN THE UNITED STATES, 1920s THROUGH 1950s
Late Quaternary coccoliths at the North Pole: Evidence of ice-free conditions and rapid sedimentation in the central Arctic Ocean
Paleobotanical evidence for cool north polar climates in middle Cretaceous (Albian-Cenomanian) time
Sediments of the Lomonosov Ridge and Makarov Basin: A Pleistocene stratigraphy for the North Pole
Comment and Reply on ‘Impacts and evolution conference’: REPLY
Contents Page Table 8 1. Figure of the Earth’s surface 104 2. Gravity at the surface; mass, mean density, moment of inertia 104 3. Pressure, density, acceleration of gravity and ellipticity of layers of equal density in the Earth 105 4. The Earth’s core 106 1. Benfield, Z. f. Geophys. 13, 157, 1937. 2. Birch, Bull. Seism. Soc. Amer. 29, 463, 1939. 3. Bullen, M. N. R. A. S. Geophys. Supp. 3, 395, 1936. 4. Bullen, Trans. Roy. Soc. New Zealand, 67, 122, 1937. 5. Bullen, idem, 69, 188, 1939. 6. Bullen, Bull. Seism. Soc. Amer. 30, 235, 1940. 7. Gutenberg and Richter, Beitr. z. Geophys. 54, 94, 1939. 8. Gutenberg and Richter, M. N. R. A. S. Geophys. Supp. 4, 363, 1938. 9. Jeffreys, M. N. R. A. S. Geophys. Supp. 4, 537, 548 and 594, 1939. 10. Lambert, The Internal Constitution of the Earth, Chap. 13, McGraw-Hill, New York, 1939. 11. Olczak, Acta Astron. 3, 81, 1938. 12. Williamson and Adams, J. Washington Acad. Sci. 13, 413, 1923. T able 8–1.—F igure of the E arth’s S urface (Ref. 10) Semi-axes of International Ellipsoid of Reference (1924): Equatorial, a = 6378.388 km. Polar, c = 6356.912 km. Radius of sphere of equal volume, α 0 = 6371 km. Ellipticity of surface, ( a – c )/ a = 1/297 = 0.00337. (For ellipticity of internal levels, see Table 8–3.) Quadrant of a meridian = 10,002.288 km. Quadrant of the equator = 10,019.148 km. Area of surface = 5.101 × 10 18 cm. 2 Volume = 1.083 2