140:. When such rock solidifies, the magnetite aligns itself with the prevailing magnetic field at the time, thus providing a sort of "fossil" magnetic record. If new crust were being formed at the ridges and moving away, as Hess theorized, then reversals in the Earth's magnetic polarity would result in just the kind of parallel, symmetrical anomalies that Matthews' survey had found. The ocean crust would in effect act as a kind of giant tape recorder of magnetic anomalies over time.
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activity. Hess hypothesized that new ocean crust was being formed at the ocean ridges by extrusions of magma from the Earth's mantle, and that convection currents within the mantle were continuously carrying the newly formed crust away from the ridge, widening the ocean basin and pushing the continents apart.
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in 1963. From then on, rapid progress was made both in terms of acceptance of Hess's theory and of further verification. Subsequent surveys of other ocean ridges showed similar and correlatable anomalies in every case. Confirmation of the Earth's polarity reversals a few years later not only further
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had never gained much scientific support due to its lack of any satisfactory mechanism to drive the process. During the 1950s, however, extensive surveys of the ocean floor revealed a global, linked system of mid-ocean ridges, all of which exhibited high thermal flow and considerable seismic
128:. This revealed a pattern of magnetic anomalies running in parallel stripes and virtually symmetrically on either side of the ridge. The most plausible explanation for these anomalies required the assumption (already in circulation at the time, but not yet proven) that the
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but provided a timescale allowing the rate of spreading to be estimated for each section of ocean ridge. The contribution of
Matthews and Vine proved to be an essential element in the development and acceptance of plate tectonics theory.
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50:(5 February 1931 – 20 July 1997), known as "Drum", was a British marine geologist and geophysicist and a key contributor to the theory of
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Matthews and his research student, Fred Vine, published these ideas in the article "Magnetic
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White, R. S. (1999). "Drummond Hoyle
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had reversed its polarity repeatedly over time. Ocean crust consists of basic
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In 1982 Matthews became the first scientific director of the
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Biographical
Memoirs of Fellows of the Royal Society
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305:(1963). "Magnetic Anomalies over Oceanic Ridges".
240:(online ed.). Oxford University Press. 2004.
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234:"The Oxford Dictionary of National Biography".
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89:During World War II he went to school at
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73:. In 1989 he was awarded the
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272:Award Winners since 1831
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77:'s highest honour, the
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18:Drummond Hoyle Matthews
246:10.1093/ref:odnb/64976
210:10.1098/rsbm.1999.0019
130:Earth's magnetic field
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703:British geophysicists
470:David Roderick Curtis
160:Chree medal and prize
93:in Malvern, and then
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723:Marine geophysicists
632:Renato Dulbecco
387:at Wikimedia Commons
642:Giuseppe Occhialini
637:George H. Hitchings
475:John Frank Davidson
348:Gates A.E. (2009).
319:1963Natur.199..947V
158:In 1977 he won the
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71:seafloor spreading
69:'s 1962 theory of
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555:John Polkinghorne
535:Peter D. Mitchell
530:Drummond Matthews
495:Jack Halpern
485:Pehr Victor Edman
385:Drummond Matthews
383:Media related to
282:on 19 August 2010
268:"Wollaston Medal"
252:(Subscription or
110:continental drift
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673:1997 deaths
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286:25 February
662:Categories
609:Statute 12
256:required.)
181:References
85:Early life
585:John Vane
138:magnetite
122:Cambridge
91:The Downs
56:Fred Vine
428:elected
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60:Canadian
625:Foreign
437:Fellows
430:in 1974
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315:Bibcode
204:: 275.
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307:Nature
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146:Nature
101:Career
40:, 1981
331:S2CID
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356:ISBN
288:2009
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.