Overview - Timescale, Physical Landscapes
GEOL.3310 :: Phanerozoic Eon (538.8 ± 0.2 – 0 Ma) :: Paleozoic Era (538.8 ± 0.2 – 251.902 ± 0.024) :: Paleozoic Era (538.8 ± 0.2 – 251.902 ± 0.024) :: Devonian Period (419.2 ± 3.2 – 358.9 ± 0.4 Ma)
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Overview - Timescale, Physical Landscapes
Phanerozoic Eon
The modern southern continents were united into the supercontinent Gondwana during the Devonian period, roughly along the modern continental shelf boundary. The development of reefs in Western Australia in the Late Devonian indicates that parts of this southern continent were close to tropics.
- Paleozoic Era
- Devonian Period
- Lower
- Lochkovian
- Pragian
- Emsian
- Middle
- Eifelian
- Givetian
- Upper
- Frasnian
- Famennian
The modern southern continents were united into the supercontinent Gondwana during the Devonian period, roughly along the modern continental shelf boundary. The development of reefs in Western Australia in the Late Devonian indicates that parts of this southern continent were close to tropics.
GEOL.3310 :: Phanerozoic Eon (538.8 ± 0.2 – 0 Ma) :: Paleozoic Era (538.8 ± 0.2 – 251.902 ± 0.024) :: Paleozoic Era (538.8 ± 0.2 – 251.902 ± 0.024) :: Devonian Period (419.2 ± 3.2 – 358.9 ± 0.4 Ma)
Page 1 of 1
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