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Geologic Time Scale
The landscape of the lower Nahe between Bad Sobernheim, Bad Kreuznach, and
Bingen still essentially resembles how it was in the Oligocene period,
35 million years ago. At that time the valley was covered by an ocean, whose
coastline ran along the bay of Kreuznach and the bay of Staudernheim (Bad
Sobernheim) with an island archipelago in the south.
Mio. years |
Cenozoic (Earth Modern Era) |
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Special Events |
0.01 | Holocene (Alluvium) | Quarternary | |
2.4 | Pleistocene (Dilluvium) | | first humans |
5 | Pliocene | Tertiary | |
23 | Miocene | | |
36 | Oligocene | | |
55 | Eocene | | |
65 | Paleocene | | Extinction of the last dinosaurs |
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| Mesozoic (Earth Middle Ages) | | |
100 | Upper Chalk | Cretaceous | |
140 | Lower Chalk | | first flowering plants |
160 | Malm (White Jurassic) | Jurassic | first pterosaurs and birds |
170 | Dogger (Brown Jurassic) | | |
195 | Lias (Black Jurassic) | | Bloom of reptiles |
205 | Keuper | Triassic | |
215 | Shell Limestone | | |
225 | Red Sandstone | | first dinosaurs |
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| Paleozoic (Earth Antiquity) | | |
235 | Zechstein | Permian | highly developed reptiles |
285 | Red-Lying | | first bone fish |
325 | Upper Carboniferous | Carboniferous | first reptiles |
350 | Lower Carboniferous | | |
360 | Upper Devonian | Devonian | first amphibians, wingless insects |
370 | Middle Devon | | |
405 | Lower Devon | | |
440 | Silur | Silurian | first land creatures |
500 | Ordoviz | Ordovician | first fish |
515 | Upper Cambrian | Cambrian | |
540 | Middle Cambrian | | |
570 | Lower Cambrian | | first animals with skeletons |
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| Precambrian (Earth Primeval) | | |
1000 | | Riphaeus | shell-less molluscs, horn shells |
2000 | | Proterozoic | lower aquatic plants |
2800 | | Archean | Oxygen atmosphere |
4000 | | Hadean | Beginning of biological development |
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Literature
R. Hohl: Entwicklungsgeschichte der Erde, Verlag W. Dausien, Hanau 1985
Picture:
A 285 million years old agate mandel with quartz druse from the area of Idar Oberstein (Nahe Valley).
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