Geologic time, Lectures 2 & 3 Flashcards

1
Q

Pinatubo, Phillippines

when, what, causes

A
  • 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
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2
Q

Charleston earthquake 1886

where, deaths, spatial scale, timescale

A

South Carolina, USA
60 deaths
spatial scale: 100-1000km2
timescale: seconds/minutes

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3
Q

How has the relative geologic timescale been constructed?

4 principles

A
  1. principle of original horizontality
  2. principle of superposition
  3. principle of cross-current relationships
  4. principle of faunal success
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4
Q

Principle of original horizontality

A

sediments are deposited as horizontal beds

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5
Q

Principle of superposition

A

Each layer of sedimentary rock in a tectonically undisturbed sequence is younger than the one beneath it.

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6
Q

Principle of cross-current relationships

A

An igneous intrusion or fault must be younger than the rocks it intrudes or cuts.

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7
Q

Principle of faunal succession

A

The sedimentary strata in an outcrop contain fossil in a definite sequence.

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8
Q

Fossils

A

Remains of ancient organisms

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9
Q

Palaeontology

A

the study of ancient life and Earth’s history from the fossil record

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10
Q

Body fossils

4

A

shells, teeth, bomes, impressions of plants

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11
Q

Trace fossils

4

A
records of biological activity:
burrows
footprints
feeding trails
coprolites
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12
Q

Another name for trace fossils

A

ichnofossils

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13
Q

Coprolites

A

Pieces of fossilised dung

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14
Q

Who came up with the principle of faunal succesion

A

William Smith (1769 - 1839)
‘Father of English Geology’
surveyor at coalfield and coal canal in Somerset
published first geologic map in 1815

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15
Q

Absolute ages (of rocks and sediments)

A

dates in years

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16
Q

When was radioactivity discovered?

17
Q

Isotopic dating

A

the use of naturally occurring radioactive elements to determine rock ages

18
Q

Who introduced isotopic dating and when?

A

1905, Ernest Rutherford

19
Q

All matter is made up of…

A

elements which are composed of atoms

20
Q

Every atom has a…

A

nucleus containing most of the mass of the atom, surrunded by a negative cloud of electrons

21
Q

Isotopes

A

Atoms of the same element with different numbers of neutrons but the same number of protons.

22
Q

Difference between isotopes of the same element?

A

atomic mass

23
Q

Similarity between isotopes of the same element?

A

chemical properties

24
Q

Are isotopes unstable or stable?

A

some are stable but some are unstable and radioactively decay

25
What is used for radioactive/isotopic dating?
radioactive decay
26
What happens to atoms of radioactive elements?
they spontaneouly disintergrate (radioactively decay) to form atoms of a different element
27
Radioactive parent elements...
decompose to form radioactive daughter elements
28
Half-life
the time for one half of the original number of radioactive atoms to decay
29
Why is radioactive decay used as a clock?
- decay rates/half lives of radioactive atoms known and do not vary with changes in T or P - can measure the ratio of parent to daughter atoms in a rock samples
30
Use of a mass spectrometer when carrying out isotopic dating in a lab
1. count the daughter element atoms 2. know the rate of decay 3. calculate the time when there were no daughters (only parents) = time of rock formation
31
The isotopic age of a rock/sediment/fossil?
time since the isotopic clock was 'reset' when the isotopes were locked into the minerals, eg: crystallisation from melt or during metamorphism
32
Radioactive isotopes are used to date | 3
1. time of death of organisms (fossils in sedimentary rocks) 2. time of cooling and crystallisation of magma (igneous rocks) 3. time elapsed since metamorphism (metamorphic rocks)
33
Age of the Earth | and how was this calculated?
4.6 billion years | relative and absolute dating techniques
34
Relative vs absolute dating
``` relative = no specific dates, to determine if one object is older than another absolute = origin dates, time ranges, age range in years ```