Gespeichert in:
| Titel: | The continental drift controversy |
|---|---|
| Unterteilung: | Introduction of seafloor spreading Volume 3 |
| Von: |
Henry R. Frankel, University of Missouri - Kansas City
|
| Person: |
Frankel, Henry R.
1944-2019 Verfasser aut |
| Hauptverfasser: | |
| Format: | Buch |
| Sprache: | Englisch |
| Veröffentlicht: |
Cambridge
Cambridge University Press
2016
|
| Schlagworte: | |
| Online-Zugang: | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029844136&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029844136&sequence=000002&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA |
| Beschreibung: | xvi, 476 Seiten Diagramme, Karten |
| ISBN: | 9781316616123 9780521875066 |
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Datensatz im Suchindex
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|---|---|
| adam_text | Contents
Foreword by Robert L. Fisher page x
Acknowledgments xii
List of abbreviations xiv
Introduction xv
1 Extension and reception of paleomagnetic/paleoclimatic support
for mobilism: 1960-1966 1
1.1 Introduction 1
1.2 Dott reexamines the Squantum Tillite 1
1.3 Comparisons of paleomagnetic and paleoclimatic evidence:
the 1959 Newcastle symposium and its 1961 publication
Descriptive Palaeociimatology 1
1.4 Reviews of Descriptive Palaeociimatology 13
1.5 Speculations on mechanism in the early 1960s 18
1.6 The 1962 anthology Continental Drift and MacDonald’s review of it 25
1.7 Blackett turns to paleoclimatology 31
1.8 Deutsch proposes continental drift without polar wandering 33
1.9 The 1963 Newcastle NATO conference 36
1.10 Bucher continues to criticize mobilism at the NATO conference 41
1.11 Harland and Rudwick link mobilism, the Great Infra-Cambrian
Ice Age and the burgeoning of Cambrian fauna 47
1.12 Responses of some biogeographers to the paleomagnetic case for
continental drift 52
1.13 Hamilton welcomes paleomagnetism’s support of mobilism 65
1.14 Kay and Colbert reassess mobilism because of its
paleomagnetic support 67
1.15 Japanese rock magnetists avoid accepting the paleomagnetic
case for mobilism 76
1.16 Further poles from Australia, 1958-1964 81
v
VI
Contents
1.17 Further poles from Africa: the Salisbury (Harare) Group and
further work at the Bernard Price Institute, Johannesburg,
1959-1964 85
1.18 Convergence of paleomagnetism and paleoclimatology
at Canberra, 1959-1966 92
2 Reception of the paleomagnetic case for mobilism by several
notables: 1957-1965 115
2.1 Introduction 115
2.2 Gutenberg’s career 115
2.3 Gutenberg supports mobilism during the 1920s and 1930s 117
2.4 In the 1950s Gutenberg reconsiders mobilism and appeals
to paleomagnetism 121
2.5 Vening Meinesz reconsiders mobilism 123
2.6 Vening Meinesz becomes favorably inclined toward mobilism
because of its paleomagnetic support 126
2.7 MacDonald denies mantle convection and Runcorn responds 129
2.8 MacDonald renews his attack on the paleomagnetic case
for mobilism 136
2.9 Harold Jeffreys, his career 137
2.10 Jeffreys renews his attack on mobilism in the first Harold
Jeffreys Lecture 140
2.11 Bullard’s journey to mobilism: his early career 143
2.12 Bullard considers mantle convection and measures ocean floor
heat flow 147
2.13 Bullard begins to consider mobilism seriously 152
2.14 Bullard recognizes that all obstacles to the paleomagnetic case
had been removed and becomes a mobilist 157
2.15 Bullard squabbles with geologists about the contributions of
geology and geophysics to the mobilism debate 165
2.16 Arthur Holmes’attitude to the paleomagnetic case for mobilism 173
2.17 Mobilism’s solution to divergent APW paths, its difficulty-free
status 178
2.18 On the general failure to recognize the difficulty-free status of the
paleomagnetic case for mobilism 181
2.19 Unreasonableness of fixist responses 185
2.20 Telling it like it was not, revisionist accounts of the paleomagnetic
case for mobilism 186
2.21 Presentation of the mobilist interpretation of the paleomagnetic
results, Runcorn’s tactical error 188
2.22 Waiters and actors: taking the paleomagnetic support
for mobilism seriously 194
Contents
vii
3 Harry Hess develops seafloor spreading 198
3.1 Harry Hess, seafloor spreading, and revisionist history 198
3.2 Harry Hess, the man 199
3.3 Hess’s early career, 1932-1950: a preview 202
3.4 Hess views island arcs as evolving into mountain belts 203
3.5 Hess discovers guyots and explains their origin 212
3.6 Hess adopts mantle convection and rejects mobilism during his
early career 217
3.7 Hess’s middle career, 1950-1959: a preamble 220
3.8 Hess on mantle convection, oceanic crust and upper mantle,
and mid-ocean ridges, early 1950s 221
3.9 In the early 1950s Hess applies the olivine-serpentine
transformation to formation of guyots and mid-ocean ridges 225
3.10 Hess (1955) revises his theory of mountain formation from
island arcs 229
3.11 Hess (1955) continues to oppose mobilism 232
3.12 Hess (1959) switches to mobilism because of its paleomagnetic
support 233
3.13 Hess (1959, 1960) reevaluates his views about ocean basins 237
3.14 Hess (1960) comes up with seafloor spreading 243
3.15 Hess (1960) explains how seafloor spreading solves many problems 247
3.16 Fisher’s work on trenches; he teams up with Hess 254
3.17 Lamont’s view of trenches, 1954-1959 259
3.18 Fisher’s Ph.D. dissertation (1952-1956) and his continued work
on trenches 261
3.19 C. B. Officer and company’s solution to the origin of trenches 263
3.20 Fisher and Hess’s joint paper 265
3.21 Hess, the scientist 271
4 Another version of seafloor spreading: Robert Dietz 280
4.1 Introduction 280
4.2 Robert Dietz, the man 280
4.3 Dietz argues for meteorite and asteroid impacts, 1946-1964 284
4.4 Dietz recalls his pre-1954 attitude toward mobilism:
a 1987 interview 289
4.5 Dietz’s marine geological work before going to London in 1954
and his later recollections compared 290
4.6 In London, Dietz (1956) learns about mobilism’s paleomagnetic
support 296
4.7 Dietz proposes ocean basin formation by asteroid impact 298
4.8 Dietz (1959) invokes continental drift and motions of seafloor
to explain absence of pre-Cretaceous seamounts 300
Contents
viii
4.9 Presentation and defense of seafloor spreading by Dietz, 1961-1962 302
4.10 The priority muddle over seafloor spreading 310
4.11 Dietz, the scientist 316
5 The Pacific as seen from San Diego and Menard’s changing views about
the origin and evolution of the ocean floor 320
5.1 Introduction 320
5.2 H. W. Menard, the man 321
5.3 Menard’s pre-1950 views about mobilism before arriving
at NEL 322
5.4 Menard and Dietz’s collaborative work, 1949-1954 323
5.5 From the Mendocino Escarpment to fracture zones: Menard’s
1953 solution 326
5.6 Menard’s 1955 theory of fracture zones 329
5.7 Menard’s 1958 solution to the origin of mid-oceanic elevations 333
5.8 Menard provides Exists with isthmian connections and rejects
mobilism, 1958 337
5.9 The discovery of magnetic lineations in the northeastern Pacific,
1952-1961 338
5.10 Menard’s views in flux, 1959 343
5.11 Key factors behind Menard’s shift in attitude about ridges and
fracture zones 346
5.12 Menard’s seafloor stretching hypothesis, 1960 348
5.13 Menard, the scientist 352
6 Fixism and Earth expansion at Lamont Geological Observatory 358
6.1 Introduction 358
6.2 William Maurice Ewing, the man 359
6.3 Ewing’s anti-mobilist attitude at the beginning of the 1950s 364
6.4 Ewing and Tolstoy’s views about the origin of the Mid-Atlantic
Ridge 366
6.5 Bruce Heezen, the making of a marine geologist 374
6.6 Marie Tharp, the making of an oceanographic cartographer 378
6.7 The discovery of the median rift valley 380
6.8 Lamont’s “4500 mile undersea crack,” is it continuous? 390
6.9 Heezen’s Earth expansion, 1957-1959 393
6.10 Holmes and Heezen correspond about Earth expansion 397
6.11 Heezen comes to rely on paleomagnetism as support for Earth
expansion, 1959-1960 400
6.12 Maurice and John Ewing’s 1959 explanation of ocean ridges 408
6.13 Maurice Ewing’s 1960 Vetlesen Prize talk: his Exist explanation
of the Atlantic Basin 410
6.14 Responses to Ewing’s Vetlesen Prize talk 413
Contents
ix
6.15 Heezen’s continued defense and later abandonment of Earth
expansion, 1960-1966 418
6.16 The Ewing-Heezen rift 420
6.17 Heezen’s stress on collecting one’s own data and resentment
of Hess 421
6.18 The effect of the Ewing-Heezen split on Heezen 423
6.19 Ewing (1962) assesses the relative merits of mobilism and fixism
in explaining sediments of ocean basins
References 435
Index 461
Resolution of the sixty year debate over continental drift,
culminating in the triumph of plate tectonics, changed
the very fabric of Earth science. This four-volume treatise
on The Continental Drift Controversy is the first complete
history of the origin, debate and gradual acceptance of this
revolutionary explanation of the structure and motion of the
Earth s outer surface. Based on extensive interviews, archival
papers, and original works, Frankel weaves together the lives
and work of the scientists involved, producing an accessible
narrative for scientists and non-scientists alike.
Volume 3 - Introduction of Seafloor Spreading
Every historian of 20th Century
Earth science will need these
volumes close at hand; there is no
substitute.”
EOS
The Continental Drift Controversy
is undoubtedly the definitive
account. It is inconceivable that it
can be bettered or even matched at
any time in the future.”
Isis
This third volume describes the expansion of the land-based
paleomagnetic case for drifting continents and recounts the
golden age of marine geology and geophysics. Fuelled by
the Cold War, US and British workers led the way in making
discoveries and forming new hypotheses, especially about
the origin of oceanic ridges. When first proposed, seafloor
spreading was just one of several competing hypotheses
about the evolution of ocean basins, and every hypothesis left
unexplained the newly discovered and wholly unexpected
magnetic anomalies associated with mid-oceanic ridges and
in the Pacific basin off the western coast of the United States.
This is one of the most remarkable
histories of science to appear in my
lifetime.”
Earth Sciences History
These volumes should be read
by all geoscientists serious about
understanding how we have come
to learn the inner workings of our
planet.”
Preview
Other volumes in The Continental Drift Controversy:
Volume 1 - Wegener and the Early Debate
Volume 2 - Paleomagnetism and Confirmation of Drift
Volume 4 - Evolution into Plate Tectonics
Here we have an unparalleled
study of remarkable depth, detail
and quality of a key development
in our ideas about how the Earth
functions.”
Progress in Physical Geography
Winner of the Sue Tyler Friedman Medal of The Geological
Society of London and the Mary C. Rabbitt History And
Philosophy of Geology Award of the Geological Society of
America
Cover illustration: Lakagigar, Laki crater, Iceland. ©Tokelau /
Shutterstock.com
Cambridge
UNIVERSITY PRESS
www.cambridge.org
ISBN 978-1-316hS1 612-3
Cover design by Hart McLeod Ltd
9 781316 616123
|
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| isbn | 9781316616123 9780521875066 |
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| spellingShingle | Frankel, Henry R. 1944-2019 The continental drift controversy Kontinentalverschiebung (DE-588)4032288-9 gnd Paläomagnetismus (DE-588)4173115-3 gnd Seafloor spreading (DE-588)4332840-4 gnd Meeresgeologie (DE-588)4038316-7 gnd |
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| title | The continental drift controversy |
| title_auth | The continental drift controversy |
| title_exact_search | The continental drift controversy |
| title_full | The continental drift controversy Volume 3 Introduction of seafloor spreading Henry R. Frankel, University of Missouri - Kansas City |
| title_fullStr | The continental drift controversy Volume 3 Introduction of seafloor spreading Henry R. Frankel, University of Missouri - Kansas City |
| title_full_unstemmed | The continental drift controversy Volume 3 Introduction of seafloor spreading Henry R. Frankel, University of Missouri - Kansas City |
| title_short | The continental drift controversy |
| title_sort | the continental drift controversy introduction of seafloor spreading |
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