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Charles Lyell profoundly influenced Charles Darwin with his pioneering geological research, which here focuses on periodising rock formations.
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Charles Lyell profoundly influenced Charles Darwin with his pioneering geological research, which here focuses on periodising rock formations.
Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.
Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.
Produktdetails
- Produktdetails
- Verlag: Cambridge University Press
- Seitenzahl: 556
- Erscheinungstermin: 8. Juli 2009
- Englisch
- Abmessung: 216mm x 140mm x 32mm
- Gewicht: 775g
- ISBN-13: 9781108001373
- ISBN-10: 1108001378
- Artikelnr.: 26823560
- Herstellerkennzeichnung
- Libri GmbH
- Europaallee 1
- 36244 Bad Hersfeld
- gpsr@libri.de
- Verlag: Cambridge University Press
- Seitenzahl: 556
- Erscheinungstermin: 8. Juli 2009
- Englisch
- Abmessung: 216mm x 140mm x 32mm
- Gewicht: 775g
- ISBN-13: 9781108001373
- ISBN-10: 1108001378
- Artikelnr.: 26823560
- Herstellerkennzeichnung
- Libri GmbH
- Europaallee 1
- 36244 Bad Hersfeld
- gpsr@libri.de
1. Connexion between the subjects treated of in the former parts of this work and those to be discussed in the present volume
2. Arrangement of the materials composing the earth's crust
3. Different circumstances under which the secondary and tertiary formations may have originated
4. Chronological relations of mineral masses the first object in geological classification
5. Classification of tertiary formations in chronological order
6. Newer Pliocene formations
7. Marine and volcanic formations at the base of Etna
8. Speculations on the origin of the Val del Bove on Etna
9. Origin of the newer Pliocene strata of Sicily
10. Tertiary formations of Campania
11. Newer Pliocene freshwater formations
12. Geological monuments of the older Pliocene period
13. Crag of Norfolk and Suffolk
14. Volcanic rocks of the older Pliocene period
15. Miocene period
16. Miocene alluviums
17. Eocene period
18. Marine formations of the Eocene period
19. Volcanic rocks of the Eocene period
20. Eocene formations, continued
21. Denudation of secondary strata during the deposition of the English Eocene formations
22. Denudation of the Valley of the Weald, continued
23. Secondary formations
24. On the relative antiquity of different mountain-chains
25. On the rocks usually termed 'primary'
26. On the stratified rocks usually called 'primary'.
2. Arrangement of the materials composing the earth's crust
3. Different circumstances under which the secondary and tertiary formations may have originated
4. Chronological relations of mineral masses the first object in geological classification
5. Classification of tertiary formations in chronological order
6. Newer Pliocene formations
7. Marine and volcanic formations at the base of Etna
8. Speculations on the origin of the Val del Bove on Etna
9. Origin of the newer Pliocene strata of Sicily
10. Tertiary formations of Campania
11. Newer Pliocene freshwater formations
12. Geological monuments of the older Pliocene period
13. Crag of Norfolk and Suffolk
14. Volcanic rocks of the older Pliocene period
15. Miocene period
16. Miocene alluviums
17. Eocene period
18. Marine formations of the Eocene period
19. Volcanic rocks of the Eocene period
20. Eocene formations, continued
21. Denudation of secondary strata during the deposition of the English Eocene formations
22. Denudation of the Valley of the Weald, continued
23. Secondary formations
24. On the relative antiquity of different mountain-chains
25. On the rocks usually termed 'primary'
26. On the stratified rocks usually called 'primary'.
1. Connexion between the subjects treated of in the former parts of this work and those to be discussed in the present volume
2. Arrangement of the materials composing the earth's crust
3. Different circumstances under which the secondary and tertiary formations may have originated
4. Chronological relations of mineral masses the first object in geological classification
5. Classification of tertiary formations in chronological order
6. Newer Pliocene formations
7. Marine and volcanic formations at the base of Etna
8. Speculations on the origin of the Val del Bove on Etna
9. Origin of the newer Pliocene strata of Sicily
10. Tertiary formations of Campania
11. Newer Pliocene freshwater formations
12. Geological monuments of the older Pliocene period
13. Crag of Norfolk and Suffolk
14. Volcanic rocks of the older Pliocene period
15. Miocene period
16. Miocene alluviums
17. Eocene period
18. Marine formations of the Eocene period
19. Volcanic rocks of the Eocene period
20. Eocene formations, continued
21. Denudation of secondary strata during the deposition of the English Eocene formations
22. Denudation of the Valley of the Weald, continued
23. Secondary formations
24. On the relative antiquity of different mountain-chains
25. On the rocks usually termed 'primary'
26. On the stratified rocks usually called 'primary'.
2. Arrangement of the materials composing the earth's crust
3. Different circumstances under which the secondary and tertiary formations may have originated
4. Chronological relations of mineral masses the first object in geological classification
5. Classification of tertiary formations in chronological order
6. Newer Pliocene formations
7. Marine and volcanic formations at the base of Etna
8. Speculations on the origin of the Val del Bove on Etna
9. Origin of the newer Pliocene strata of Sicily
10. Tertiary formations of Campania
11. Newer Pliocene freshwater formations
12. Geological monuments of the older Pliocene period
13. Crag of Norfolk and Suffolk
14. Volcanic rocks of the older Pliocene period
15. Miocene period
16. Miocene alluviums
17. Eocene period
18. Marine formations of the Eocene period
19. Volcanic rocks of the Eocene period
20. Eocene formations, continued
21. Denudation of secondary strata during the deposition of the English Eocene formations
22. Denudation of the Valley of the Weald, continued
23. Secondary formations
24. On the relative antiquity of different mountain-chains
25. On the rocks usually termed 'primary'
26. On the stratified rocks usually called 'primary'.