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Geologist
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An unconformity is a contact between two rock units in which the upper unit is usually much younger than the lower unit. Unconformities are typically buried erosional surfaces that can represent a break in the geologic record of hundreds of millions of years or more.

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Eon Era Period Epochs Start
Phanerozoic Cenozoic Quaternary Holocene 0.0117
Pleistocene 2.558
Neogene Pliocene 5.333*
Miocene 23.030*
Paleogene Oligocene 33.9*
Eocene 56.0*
Paleocene 66.0*
Mesozoic Cretaceous Late Cretaceous 100.5*
Early Cretaceous c. 145.0
Jurassic Late Jurassic 163.5 ± 1.0
Middle Jurassic 174.1 ± 1.0*
Early Jurassic 201.3 ± 0.2*
Triassic Late Triassic c. 235*
Middle Triassic 247.2
Early Triassic 252.2 ± 0.5*
Paleozoic Permian
298.9 ± 0.2*
Carboniferous Pennsylvanian 323.2 ± 0.4*
Mississippian 358.9 ± 0.4*
Devonian
419.2 ± 3.2*
Silurian
443.4 ± 1.5*
Ordovician
485.4 ± 1.9*
Cambrian
541.0 ± 1.0*
Proterozoic Neoproterozoic Ediacaran Precambrian c. 635*
Cryogenian 850
Tonian 1000
Mesoproterozoic Stenian 1200
Ectasian 1400
Calymmian 1600
Paleoproterozoic Statherian 1800
Orosirian 2050
Rhyacian 2300
Siderian 2500
Archean Neoarchean
2800
Mesoarchean 3200
Paleoarchean 3600
Eoarchean 4000
Hadean
4567

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Cambridge scientists and PhD students are at the forefront of monitoring the activity of the Bárðarbunga volcano in Iceland. The research group, led by Professor Bob White of the Department of Earth Sciences, is monitoring the ongoing massive volcanic intrusion through its array of seismic instrumentation - never before has such an intrusion been so well documented. The data they gather is likely to yield considerable new insights into how molten rock moves underground, and whether or not it erupts. Here, Professor White outlines the team’s ongoing work in Iceland...


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