
THE FACE OF THE EARTH
(DAS ANTLITZ DER ERDE)
BY
EDUARD SUESS
Professor of Geology in the University of Vienna
Foreign Member of the Royal Society of London
Translated by
Hertha B. C. Sollas
Ph. D. Heidelberg; of Newnham College, Cambridge
under the direction of
W. J. Sollas
Sc. D. (Cantab.), LL. D. (Dublin), M.A. (Oxon.), F.R.S.
Fellow of University College, Oxford
Professor of Geology in the University of Oxford
VOL. I
OXFORD
AT THE CLARENDON PRESS
1904
This electronic edition prepared by Dr. David C. Bossard
from original documents in his personal library.
December, 2005.
Copyright © 2005 by David C. Bossard.
CONTENTS.
Preface by the Author iii
iv
v
vi
vii
Introduction 1 001
002
003
004
005
006
007
008
009
010
011
012
013
014
015 016
Wedge-like form of the
continents. Great depth of the oceans. Difference between
the Pacific and the Atlantic regions. Subsidence. 'What is a geological
formation?' Cycles of development. The stratigraphical
terminology of Europe applicable to the whole world. Extent of
transgressions. Independence of ancient coast-lines and mountain
structure. Contents of the following parts.
[001] If we imagine an observer to
approach our planet from outer space, and, pushing aside the belts of
red-brown clouds which obscure our atmosphere, to gaze for a whole day
on the surface of the earth as it rotates beneath him, the feature
beyond all others most likely to arrest his attention would be the
wedge-like outlines of the continents as they narrow away to the South.
...
Such forms must have been determined by the structure of the outer
parts of the planet itself. Our observer would have no doubt on
this point, if, as he had previously pushed aside the clouds, he were
now to remove the sea, so that he could gaze directly on the rocky
crust of the globe thus laid bare. The remarkable depth of the ocean
basins as opposed to the trifling height of the continents, and the
steep slope of a great part of the coasts, would then become apparent
to him.
[006] The mightiest mountain chains of the earth are themselves only
subordinate members of far greater structural features which dominate
the whole globe.
[011] More than forty years have passed since the publication of
Darwin's book.... The continuity of life is more and more clearly
illustrated by the results of Palaeontology; yet the fact remains that
we do not find species varying gradually within the limits of single
families or genera, and at different times, but that whole groups,
entire animal and vegetable populations, or, if I may so express
myself, complete economic unities of Nature appear together, and
together disappear.
PART I
The Movements in the Outer Crust of the Earth
Chapter I. The Deluge 17 017
018
019 020
021
022
023
024
025
026
027 028
029
030
031
032
033
034
035
036
037
038
039
040
041
042
043
044
045
046
047
048
049
050
051
052
053
054
055
056
057
058
059
060
061
062
063
064
065
066
067
068 069
070
071
072
Oceanic floods. In the biblical
story two accounts combined. Berosus: the Izdubar epic.
Locality. Use of Asphalt. Warnings. The
catastrophe. Stranding. Conclusion of the event. More
recent events in the lower courses of the rivers of India.
Indus. rann of Cutch. Ganges and Brahmaputra.
Cyclones. Nature and extent of the Deluge. Classification
of accounts. Berosus and Izdubar epic. Biblical
accounts. Egypt. Hellenic-Syrian group. India.
China. Conclusion.
Chapter II. Some Seismic Areas. 73 073
074
075
076
077
078
079
080
081
082 083
084
085
086
087
088
089
090
091
092
093
094 095
096
097
098
099
100
101
102
103
104
105
106
Various branches of research. The
north-eastern Alps. South Italy. The continent of Central America.
Alleged spasmodic elevation of Chili. Rebounding of objects. Movement
of
submarine sediment. Valparaiso, 1822. Concepcion, 1835. Valdivia,
1837. Elevation of the land not proved.
Chapter III. Dislocations 106 106
107
108
109
110
111
112
113
114
115 116
117
118
119 120
121
122
123
124
125
126
127 128
129
130
131
132
133
134
135
136
137
138
139
140
141
142
143
Resolution of stresses. Dislocation by
tangential movement. Folding. Imbricated structure. Overthrusts or Wechsel. Dislocation on flaw (Blatt) planes. Torsion. Dislocation
by radial movement. Subsidence on a yielding base. Flexures and faults.
Networks of fracture. Caldron subsidences. Dislocation by combined
radial and tangential movement. Backfolding and squeezing in.
Forefolding.
Chapter IV.
Volcanos. 144 144
145
146
147
148
149
150
151
152
153
154
155
156
157
158
159
160
161
162
163
164
165
166
167
168 169
170
171
172
Stages of denudation. Vesuvius and
Monte Nuovo. Monte Venda. Laccolites. Palandocan and Dary-dagh. The
Whin Sill. The Hebrides. Predazzo. The Fissure of the Banat. Syenite
cicatrice of Brünn. Elk mountains and the Harz. Batholites;
Drammen granite; Vosges; Erzgebirge. Maculae. Invagination. The
denudation series.
Chapter V. Diversity of
the Movements. 173 173
174
175
176
177
178
179
Attempts to classify earthquakes.
Earthquakes of volcanic origin, and those caused by dislocation.
Earthquakes associated with flaws. Earthquakes associated with
over-riding. Earthquakes caused by subsidence. Aetna, 1780, and 1874 to
1883. Different nature of volcanic earthquakes. The denudation series
PART II
The Mountain Ranges of the Earth
Chapter I. The Northern
Foreland of the Alpine System. 180 180
181
182 183
184
185
186
187
188
189
190
191
192
193
194 195
196
197
198
199
200
201
202
203
204
205
206
207
208
209
210
211
212
213
214
215
The Russian Platform. The Sudetes. The
Franconian-Swabian area of subsidence. Ries and Höhgau. The
horsts. Quartz dykes in the horsts. Zigzag outlines. Jurassic relicts
of the Sudetes. Relation of the Alpine system to its foreland.
Chapter II. The
Trend-lines of the Alpine system. 216 216
217
218
219 220
221
222
223
224
225
226
227 228
229
230
231
232
233
234
23
The northern border of the Alps and the
Carpathians. Local overthrusting of the outer border. Curvature of the
extremity of the Carpathians. Curvature of the mountains of Western
Transylvania. Curvature of the Apennines. Sicily. Mountains of North
Africa. Gibraltar. The Betic Cordillera. Spiral arrangement of the
trend-lines.
Chapter III. The Basin of te Adriatic. 236 236
237
238
239
240
241
242
243
244
245
246
247
248
249
250
251
252
253
254
255
256
257
258
259
260
261
262
263
264
265
266
267
268 269
270
271
272
273 274
275
276
Significance of the Adamello. The
Judicarian line. Fractures of the Cima d' Asta. Region between the
Judicaria and the fracture of Schio. Dislocations on the north of the
fractures of the Cima d' Asta. Fractures of the Drau and the Gail.
Dinaric fractures or fractures of the Karst. Recent extension of the
Adriatic sea. Summary.
Chapter IV. The
Mediterranean. 277 277
278
279
280
281
282 283
284
285
286
287
288
289
290
291
292
293
294 295
296
297
298
299
300
301
302
303
304
305
306
307
308
309
310
311
312
313
314
315 316
317
318
319 320
321
322
323
324
325
326
327 328
329
330
331
332
333
334
335
336
337
338
339
340
341
342
343
344
345
346
347
348
349
350
351
352
353
354
355
Five historical phases of unequal
value. Relations to America. The Atlantic Ocean. Guadalquivir, Gironde,
Rhone. First Mediterranean stage. The Schlier. Second Mediterranean
stage. The Sarmatian inland sea. The Pontic lakes. More recent times.
Northern immigrants. The latest subsidences. Summary.
Chapter V. The Great
Deseert Plateau. 356 356
357
358
359
360
361
362
363
364
365
366
367
368 369
370
371
372
373 374
375
376
377
378
379
380
381
382 383
384
385
386
The Sahara and Egypt. South Arabia and
Abyssinia. Sinai, Syria, and north Arabia. Suez and the Nile.
Chapter VI. The
Fragments of the Indian Continent. 387 387
388
389
390
391
392
393
394 395
396
397
398
399
400
401
402
403
404
405
406
407
408
409
410
411
412
413
414
415 416
417
418
419 420
South Africa. The East Indian
peninsula. Madagascar. Summary.
Chapter VII. The Syntaxis of the Mountains of
India. 421 421
422
423
424
425
426
427 428
429
430
431
432
433
434
435
436
437
438
439
440
441
442
443
444
445
446
447
448
449
450
451
452
453
454
455
456
457
458
459
460
461
462
The exterior chains of Iran. The Salt
range. The Tertiary chains. The western Himalaya. Mustágh and
Kuen-luen. Hindu Kush and Púmir. The eastern Himalaya. Burma,
Malacca, Sumatra. Summary.
Chapter VIII.
The Relation of the Alps to the Mountains of Asia. 463 463
464
465
466
467
468 469
470
471
472
473 474
475
476
477
478
479
480
481
482 483
484
485
486
487
488
489
490
491
492
493
494 495
496
497
498
499
500
501
502
503
504
505
506
507
The object of this chapter. Thian-shan
by J. Muschketoff. Western branches of the Thianshan. Nuru-tau,
Scheich-Djeli, Mangischlik, Coal-field of the Donetz. Paropamisus,
Khorassan, Kopet-dagh, Balkan, Caucasus, Crimea. Matschin. Balkans and
Carpathians. Albourz, Iranian-Tauric syntaxis. Dinaric chain.
Explanation of the vortical arrangement of the Alps. Ural, Pae-khoi,
and Timan. Summary.
Chapter IX. South
America. 508 508
509
510
511
512
513
514
515 516
517
518
519 520
521
522
523
524
525
526
527 528
529
530
531
532
533
534
535
536
537
538
539
540
541
The Argentine chains. The Andes of
Bolivia and Chili. The coast Cordilleras and Patagonia. Peru. Ecuador.
North Granada and Venezuela. Summary.
Chapter X. The
Antilles. 542 542
543
544
545
546
547
548
549
550
551
552
The three series of islands. Cuba.
Haiti. Jamaica. Puerto Rico to Barbados. The Cordillera of the
Antilles. Comparison with the border of the western Mediterranean.
Earthquakes.
Chapter XI. North
America. 553 553
554
555
556
557
558
559
560
561
562
563
564
565
566
567
568 569
570
571
572
573 574
575
576
577
578
579
580
581
582 583
584
585
586
587
588
589
590
591
592
The foldings in the east.. Prairies and
Black hills. Division of the mountain ranges of the west. Rocky
mountains. Uinta mountains. Wahsatch and mountain chains on the Snake
river. Colorado plateau. The table-land of Utah and the grand canyon of
Colorado. Basin ranges. Sierra Nevada. The Coast Cordilleras and lower
California. The west of Canada. Summary.
Chapter XII. The
Continents. 593 593
594 595
596
597
598
599
600
601
602
603
604
These expressions untenable. Age of the
continents. America. Separation of Indo-Africa and Eurasia. Folding of
Eurasia. The Han-hai and the depression of Turkestan. The Mediterranean
seas. The Indian Ocean. The great units. Multiformity of the mountains.
Collapse of the lithosphere.
NOTE: High resolution images (400 ppi) of the text illustrations are
available here.
1. Fissures and Funnel-shaped Apertures produced by the
Earthquake of
Cachar on January 10, 1869 51
2. The Path of some Indian Cyclones 54
3. Recent Earthquakes in the North-east of the Alps and West of the
Carpathians 78
4. The Peripheral Line of the Lipari Islands 83
5. The Western Part of the Volcanos of Central
America 93
6. Scene of the Earthquake of February 20, 1835 99
7. Folded Menilite Shales. Wolfsgraben near Nikolschitz,
Moravia 108
8. Reversed Fold on the Summit of the Mamrang Pass,
Himalaya 109
9. Summit of the Gstelli-Horn, Mass of the Finster-Aarhorn, seen from
the Laucherli 110
10. The Botzberg Tunnel 113
11. The Habsburg 114
12. The System of Fractures of St. Andreasberg 123
13. The Faults of the High Plateaux of Utah 130
14. Stereogram of a Part of the 'Musinia Zone of Diverse
Displacement' 132
15. Prattigau and Rhaeticon 140
16. Foot of the Heiigenstein at the Hohe-Wand near Wiener-Neustadt
(Lower Austria) 141
17. Disturbances in the Belgian Coal-fields 142
18. The Mount Hillers Group of Laccolites 150
19. The Volcanos of the Inner Hebrides 156
20. Predazzo (South Tyrol) 158
21. The Volcanic Line of the Banat 162
22. Sections to correspond to Fig. 23 164
23. Arrangement of the Lowest Parts of the Cretaceous Formation around
Snow Mass and White Rock in the
Elk Mountains 165
24. The Foreland of the Western Carpathians. 186
25. The Foreland of the Eastern Carpathians 187
26. Diagram of the Trend-lines of the Alpine System 232
27. Monte Doja. Mass of the Re di Castello 239
28. Cima delle Casinelle. (South Part of the Adamello
Mass.) 241
29. Approximate Arrangement of the Principal Fractures and Flexures
which surround the Cima d' Asta
245
30. Seilspitz, Ascent to the Penserjoch (West of the Brenner
Road) 247
31. Trias Limestone overthrust by Phyllite, in the Limestone Wedge of
the Seilspitz 248
32. Entrance to the Gorge of Torrente Maso, South Side of the Cima d'
Asta 250
33. The Torrente Silano (Val Rovina) entering the Plain (West of the
Brenta) 252
34. Castles of the Montagues and Capulets to the West of Vicenza
257
85. Northern Border of the Palaeozoic Zone to the South of
Hermagor 265
36. South Side of the Palaeozoic Zone South of Hermagor 266
37. The Tertiary Deposits on the North Side of the Gulf of Mexico
284
38. Suderöe, the most southerly of the Faeröe Islands
287
39. The Trough-subsidence of Malta and Gozzo 348
40. View of the Fault of Malak on the South Coast of the Island of
Malta 349
41. Sketch-map showing the Distribution of the Formations in the Desert
of Sahara 360
42. Morbat on the South Coast of Arabia 365
43. Jebel Atáqa near Suez 371
44. South Africa 388
45. The Salt Range near Kálabágh 430
46. View of the Silakank 437
47. Diagram of the Trend-lines of the Carpathians and the Balkans
480
48. The Curvature of the Strike on the Lower Danube 482
PLATES
Plate
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Click for plate at 100 ppi
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DESCRIPTION
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I
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Folding of Strata on one Side of a
Tributary
to the Bambadhura Glacier, Lissar Valley,
Dharma Valley, Kumann
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II
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Lago di Campo and Passo della
Forceffina,
Adamello, South Tyrol
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III
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The System of the Alps
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IV
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The Syntaxis at the Foot of the
Hindu Kush
and the Himalaya
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V
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The Relation of Europe to Asia
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VI
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The Virgation of the Rocky Mountains
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