Geologic time, Lectures 2 & 3 Flashcards
Pinatubo, Phillippines
when, what, causes
- June 1991,
- one of the largest eruptions of the 20th century
- Rich in SO2
- Aerosol dispersed globally in both hemispheres
- cooling of 0.2 degrees C for 1-2 years
Charleston earthquake 1886
where, deaths, spatial scale, timescale
South Carolina, USA
60 deaths
spatial scale: 100-1000km2
timescale: seconds/minutes
How has the relative geologic timescale been constructed?
4 principles
- principle of original horizontality
- principle of superposition
- principle of cross-current relationships
- principle of faunal success
Principle of original horizontality
sediments are deposited as horizontal beds
Principle of superposition
Each layer of sedimentary rock in a tectonically undisturbed sequence is younger than the one beneath it.
Principle of cross-current relationships
An igneous intrusion or fault must be younger than the rocks it intrudes or cuts.
Principle of faunal succession
The sedimentary strata in an outcrop contain fossil in a definite sequence.
Fossils
Remains of ancient organisms
Palaeontology
the study of ancient life and Earth’s history from the fossil record
Body fossils
4
shells, teeth, bomes, impressions of plants
Trace fossils
4
records of biological activity: burrows footprints feeding trails coprolites
Another name for trace fossils
ichnofossils
Coprolites
Pieces of fossilised dung
Who came up with the principle of faunal succesion
William Smith (1769 - 1839)
‘Father of English Geology’
surveyor at coalfield and coal canal in Somerset
published first geologic map in 1815
Absolute ages (of rocks and sediments)
dates in years