Rhyacian
From Wikipedia, the free encyclopedia
The Rhyacian (IPA: /rʌɪˈeɪsiən/, Greek: Ρυαξ (rhyax), meaning "stream of lava") is the second geologic period in the Paleoproterozoic Era and lasted from 2300 Ma to 2050 Ma (million years ago). Instead of being based on stratigraphy, these dates are defined chronometrically.
The Bushveld Complex and other similar intrusions formed during this period.
Huronian glaciation period ended in late Rhyacian 2100 Ma.
[edit] References
- Rhyacian Period. GeoWhen Database. Retrieved on January 5, 2006.
- James G. Ogg (2004). "Status on Divisions of the International Geologic Time Scale.". Lethaia 37: 183–199.
| Proterozoic eon | |||||||||
|---|---|---|---|---|---|---|---|---|---|
| Paleoproterozoic era | Mesoproterozoic era | Neoproterozoic era | |||||||
| Siderian | Rhyacian | Orosirian | Statherian | Calymmian | Ectasian | Stenian | Tonian | Cryogenian | Ediacaran |
ca:Rhyacià de:Rhyacium eu:Rhyaciar fr:Rhyacien it:Rhyaciano nl:Rhyacien pt:Rhyaciano sh:Rhyacij zh:层侵纪
