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?

A

1985

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
Q

What is used for radioactive/isotopic dating?

A

radioactive decay

26
Q

What happens to atoms of radioactive elements?

A

they spontaneouly disintergrate (radioactively decay) to form atoms of a different element

27
Q

Radioactive parent elements…

A

decompose to form radioactive daughter elements

28
Q

Half-life

A

the time for one half of the original number of radioactive atoms to decay

29
Q

Why is radioactive decay used as a clock?

A
  • 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
Q

Use of a mass spectrometer when carrying out isotopic dating in a lab

A
  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
Q

The isotopic age of a rock/sediment/fossil?

A

time since the isotopic clock was ‘reset’ when the isotopes were locked into the minerals, eg: crystallisation from melt or during metamorphism

32
Q

Radioactive isotopes are used to date

3

A
  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
Q

Age of the Earth

and how was this calculated?

A

4.6 billion years

relative and absolute dating techniques

34
Q

Relative vs absolute dating

A
relative = no specific dates, to determine if one object is older than another
absolute = origin dates, time ranges, age range in years