Abstract
The sea has repeatedly invaded large portions of the continents and then subsequently retreated. This part of the earth’s history is an extremely monotonous one, but this very monotony, this continuous recurrence of the same events, constitutes one of its most important aspects. Why does the sea invade the continents, and why does the water later withdraw to the oceanic receptacles, only to advance again afterwards? In other words, in geological terminology, — what is the origin of the periodic trans- and regressions?
“We have to account for periodic transgressional seas and orogenesis upon an enormous scale and clearly associated with vertical continental movements”. (J. Jolv)
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References
Barrell, J., The strength of the Earth’s Crust (Journal of Geology 22, 1914 ).
Barrell, J., Rhythms and the measurement of geologic time (Bull. Geol. Soc. of America 1917 ).
Born, A., Periodizität epirogener Krustenbewegungen (Rep. 16th Intern. Geol. Congress Washington 1933, 1, 1936 ).
Bucher, W. H., The deformation of the Earth’s Crust (1933).
Daly, R. A., The changing world of the ice age (1934).
Grabau, A. W., Oscillation or pulsation (Rep. 16th Intern. Geol. Congress Washington 1933, 1, 1936 ).
Grabau, A. W., Palaeozoic formations in the light of the pulsation theory (1936).
Haug, E., Les géosynclinaux et les aires continentales; contribution a l’étude des transgressions et regressions (Bull. Soc. Géol. de France, 3e sera 18, 1900 ).
Joly, J., The surface history of the Earth (Oxford Univ. Press. 1925 ).
Kuenen, PH. H., Quantitative estimations relating to eustatic movements (Geologie en Mijnbouw 1, 1939 ).
Kijenen, PH. H., Causes of ecstatic movements (Proceed. sixth Pac. Sci. Congress I I, 1940 ).
Penck, A., Theorie der Bewegung der Strandlinie (Sitzungsber. Preuss. Akad. Wiss. 1934 ).
Schuchert, Cu., Correlation and chronology on the basis of paleogeography (Bull. Geol. Soc. of America 26, 1916 ).
Stille, H., Studienfiber Meeres- und Bodenschwankungen (Nachr. K. Ges. Wiss. Göttingen. Mat. -phys. Kl. 1922 ).
Stille, H., Grundfragen der Vergleichenden Tektonik (1924).
Suess, ED., The face of the Earth (transl. Sollas) 2, 1906.
Umbgrove, J. H. F., The amount of the maximal lowering of the sea-level in the pleistocene (Proc. Fourth Pacific Science Congress, vol. 2, 1930).
Umbgrove, J. H. F., On rhythms in the history of the Earth (Geol. Magazine 76, 1939).
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© 1942 Springer Science+Business Media Dordrecht
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Umbgrove, J.H.F. (1942). Oscillations of the Sea-Level. In: The Pulse of the Earth. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-6568-8_5
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DOI: https://doi.org/10.1007/978-94-017-6568-8_5
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