1. Geologic Time
Chapter
12

2. Outline
• Geologic time: perspective & a bit of history
• Dating geologic materials
-General: relative & absolute dating
-Relative dating:
-7 Principals & their application to a geologic history
-Fossil successions
• Gaps in the geologic record (unconformity)
-3 types of unconformities
-Stratigraphic correlation & the global geologic column
• Numerical (absolute) dating
-Radioactive decay
-Meaning of a radiometric date
-Other numerical dating methods
-Dating the geologic column, geologic time scale, & age of Earth
Chapter 12

3. Geologic Time
• Magnitude of Earth’s past is amazing.
• Discovering this forever altered our perception of
ourselves within nature & the Universe.
Chapter
12

4. Geologic Time
• Understanding time permits assigning ages to…
• Rocks.
• Fossils.
• Geologic structures.
• Landscapes.
• Tectonic events.
Chapter
12

5. Geologic Time
• Prior to late 1600s, geologic time was thought to =
historical time.
• Archbishop James Ussher, Ireland, 1654.
• He added up generations from Old Testament.
• Determined Earth formed on Oct 23, 4004 BCE.
Chapter
12

6. Geologic Time
• Scientists began to find clues to a more ancient Earth…
• Nicolaus Steno (1638–1686; danish physician).
• Observed marine fossils high in mountains.
• Deduced they were ancient animals.
• Processes of lithification & uplift suggested long time periods.
fossil
shark
tooth
Chapter
12

7. Outline
• Geologic time: perspective & a bit of history
• Dating geologic materials
-General: relative & absolute dating
-Relative dating:
-7 Principals & their application to a geologic history
-Fossil successions
• Gaps in the geologic record (unconformity)
-3 types of unconformities
-Stratigraphic correlation & the global geologic column
• Numerical (absolute) dating
-Radioactive decay
-Meaning of a radiometric date
-Other numerical dating methods
-Dating the geologic column, geologic time scale, & age of Earth
Chapter 12

8. Geologic Time
2 ways to date geological materials:
1. Relative age – Based on order of formation.
• Qualitative method developed 100s of yrs ago.
• Determine older vs. younger relationships.
Chapter
12

9. Geologic Time
2 ways to date geological materials:
1. Relative age – Based on order of formation.
• Qualitative method developed 100s of yrs ago.
• Determine older vs. younger relationships.
2. Numerical (absolute) age – # of yrs since an event.
• Quantitative method developed recently.
• Numerical age assigned.
Chapter
12

10. Relative vs. Absolute
1. Relative ages
assign event
order.
2. Numerical ages
assign dates to
events.
Chapter
12

11. Relative Age
• Logical tools are useful for defining relative age.
• Principles of:
1. Uniformitarianism
2. Superposition
3. Original horizontality
4. Original continuity
5. Cross-cutting relations
6. Inclusions
7. Baked contacts.
Chapter
12

12. Geologic Time
1. Uniformitarianism – “The present is key to the past”.
• Physical processes we observe today have always
operated the same way (ie. in the geological past).
• Modern processes help us understand ancient
events.
Chapter
12

13. Defining Relative Age
2. Superposition.
• In an undeformed sequence of layered sed. rocks…
• Younger rocks on top; older rocks below.
Chapter
12

14. Relative Age
3 & 4. Horizontality and continuity.
• Seds deposited in horizontally extensive layers.
• Erosion then dissects once-continuous layers.
• Flat-lying layers unlikely to have been disturbed.
Chapter
12

15. Relative Age
5. Cross-cutting relations.
• Younger features cut across older features.
• Faults, dikes, erosion etc., must be younger than the
material that is faulted, intruded, or eroded.
• E.g. a volcano cannot intrude rocks that aren’t there yet.
Chapter
12

16. Relative Age
6. Inclusions – a rock fragment within another.
• Inclusion is older than surrounding material.
• Eg.:
• Igneous xenoliths – Country rock that fell into magma.
Chapter
12

17. Relative Age
7. Baked contacts.
• Thermal (contact) metamorphism occurs when
country rock is intruded by igneous rock.
• Baked rock is older than the intruded rock.
Chapter
12

18. Relative Age
• Determining relative ages empowers geologists to
unravel complicated geologic histories.
Chapter
12

19. Geologic History
• Deposition of horizontal strata below sea level in order
1 8 (old to young). *Horizontality & continuity*
Chapter
12

20. Geologic History
• Igneous intrusion of a sill. *baked contact*
Chapter
12

21. Geologic History
• Intrusion solidified into sill
• Tectonic compression
Chapter
12

22. Geologic History
• Compression results:
• Folding (inference: layers had to exist to be folded).
• Uplift (above sea level) & erosion.
• Intrusion of a pluton. *baked contact/cross-cutting*
Chapter
12

23. Geologic History
• Extension -> normal faulting.
• Faulting cross-cuts pluton & rock layers.
Chapter
12

24. Geologic History
• Dike intrusion.
• Dike cross-cuts everything (even normal fault).
Chapter
12

25. Geologic History
• Erosion to present landscape.
• Removed volcano and cuts down the dike top.
Chapter
12

26. Geologic History
• Relative ages help to unravel a complicated history.
• Those rules permit one to decipher this diagram!
Chapter
12

27. Geologic History
• Test yourself at home:
Chapter
12

28. Geologic History
Geologic History
A cross-section through the earth reveals the variety of
geologic features. View 1 of this animation identifies a
variety of geologic features; View 2 animates the sequence
of events that produced these features, and demonstrates
how geologists apply established principles to deduce
geologic history. For more information, see Section 12.4
Principles for Defining Relative Age starting on p.418 and
Figure 12.5 in your textbook.
Chapter
12

29. Fossil Succession
• Fossils (organism traces) can be preserved in
sedimentary rocks.
• Useful for relative age determination.
• Several fossil types will occur as an assemblage.
• Fossils are time markers.
Chapter
12

30. Fossil Succession
• Species evolve, exist, and then go extinct.
• 1st appearance to extinction dates rocks.
• Fossils succeed one another in a known order.
• A time period is recognized by fossil assemblage.
Chapter
12

31. Fossil Succession
• Fossil range – first to last appearance.
• Each fossil has a unique time range.
• Overlapping ranges provide
distinctive time markers.
• Also index fossils (unique).
• Permit correlation of strata.
• Locally to globally.
Chapter
12

32. Outline
• Geologic time: perspective & a bit of history
• Dating geologic materials
-General: relative & absolute dating
-Relative dating:
-7 Principals & their application to a geologic history
-Fossil successions
• Gaps in the geologic record (unconformity)
-3 types of unconformities
-Stratigraphic correlation & the global geologic column
• Numerical (absolute) dating
-Radioactive decay
-Meaning of a radiometric date
-Other numerical dating methods
-Dating the geologic column, geologic time scale, & age of Earth
Chapter 12

33. Unconformity
• An unconformity is a time gap in the rock record.
• Causes: non-deposition or erosion.
Chapter
12

34. Unconformities
3 Types:
1. Disconformity – parallel strata bracketing non-deposition.
• Due to an interruption in sedimentation.
• Can be difficult to recognize.
Chapter
12

35. Disconformities
Chapter
12

36. Unconformities
3 Types:
2. Nonconformity – Metamorphic/igneous rocks overlain by
sedimentary strata.
• Igneous/metamorphic rocks exposed by erosion.
• Sediment deposited on eroded surface.
Chapter
12

37. Nonconformity
Chapter
12

38. Unconformities
3 Types:
3. Angular unconformity – represents a big gap in time.
• Horizontal rocks deposited, then deformed (i.e. titled/folded).
• Then eroded.
• Then sediments horizontally deposited on erosion surface.
Chapter
12

39. Types of Unconformity
Types of Unconformity
This animation shows the stages in the development of
three main types of unconformity in cross-section, and
explains how an incomplete succession of strata provides a
record of Earth history. View 1 shows a disconformity, View
2 shows a nonconformity and View 3 shows an angular
unconformity.
Chapter
12

40. Unconformities
• Earth history is in
strata.
• Missing strata =
missing history.
• The Grand Canyon:
• Thick strata.
• Many gaps (red).
• Partial record of
geologic past.
Chapter
12

41. Stratigraphic Correlation
• In 1793, William “Strata” Smith noted strata could be
matched across distances.
• Similar rock types in a similar order.
• Rock layers contained same distinctive fossils.
• He made the 1st geologic map (of the UK).
Chapter
12

42. Stratigraphic Correlation
• Stratigraphic columns depict strata in a region.
• Drawn to portray relative thicknesses.
• Rock types depicted by fill patterns.
• Divided into formations (mapable rock units).
• Formations separated by contacts.
Chapter
12

43. Stratigraphic Correlation
• National Parks of Arizona & Utah.
• Formations can be traced long distances.
• Overlap in rock type sequences.
• Overlapping rock columns are used to build a composite.
Chapter
12

44. The Geologic Column
• A composite global stratigraphic column exists.
• Constructed from incomplete sections across the globe.
• It brackets almost all Earth history.
Chapter
12

45. Outline
• Geologic time: perspective & a bit of history
• Dating geologic materials
-General: relative & absolute dating
-Relative dating:
-7 Principals & their application to a geologic history
-Fossil successions
• Gaps in the geologic record (unconformity)
-3 types of unconformities
-Stratigraphic correlation & the global geologic column
• Numerical (absolute) dating
-Radioactive decay
-Meaning of a radiometric date
-Other numerical dating methods
-Dating the geologic column, geologic time scale, & age of Earth
Chapter 12

46. Numerical (Absolute) Dating
• Based on radioactive decay of atoms in minerals.
• Radioactive decay proceeds at a known, fixed rate.
• Radioactive elements act as internal clocks.
• Numerical dating is called geochronology.
Chapter
12

47. Radioactive Decay
Isotopes
• Atoms with same # of protons, different # of neutrons.
• Have similar, but different mass numbers.
Some are stable – never change (i.e., 13C).
Some are unstable (radioactive) – Spontaneously change to
something else (decay) at a fixed rate (i.e., 14C).
Chapter
12

48. Radioactive Decay
• Decay process has 2 main components:
• Parent – isotope that decays.
• Daughter – decay product isotope.
• Decay process can:
• Have 1 step (parent -> daughter)
• Have many steps (parent -> daughter -> etc…)
• Decay product is also unstable and hence also decays.
• Eventually proceeds to a stable endpoint.
Chapter
12

49. Radioactive Decay Time
• Half-life (t½) – time for ½ unstable parent to decay.
• t½ is unique for each isotope.
• After one t½ - ½ original parent remains.
• After three t½ - 1/8th original parent remains.
• Parent disappears (nonlinear), daughter accumulates.
Chapter
12

50. Radiometric Dating
• Mineral age can be determined by:
• Measuring parent/daughter isotope ratio.
• Calculating time by using the known t½.
• Must pick the right mineral & isotope.
• Geochronology requires analytical precision.
Chapter
12

51. Chapter
12

52. What Is a Radiometric Date?
• Time since a mineral began to retain all parent &
daughter isotopes.
• Requires cooling below “closure (blocking) temperature.”
• Daughter retained only below closure T.
• Daughter leaks out above closure T.
• Thus, if rock is reheated above closure T, the radiometric clock
can be reset to zero.
Chapter
12

53. Other Numerical Ages
• Numerical ages are possible without isotopes.
• Growth rings – Annual layers from trees or shells.
• Rhythmic layering – Annual layers in seds or ice.
Chapter
12

54. Other Numerical Ages
• Magnetostratigraphy – Magnetic signatures in strata
are compared to global reference column.
Chapter
12

55. Other Numerical Ages
• Decay process can cause scars (tracks) in minerals.
• Decay by fission (explosion) produces scar (track).
• Daughter isn’t another isotope, it’s a damage zone.
• Fission Tracks!
• Track density (daughter) is proportional to age.
Chapter
12

56. Dating the Geologic Column
• Use geochronology to:
• Date specific strata OR
• Bracket those that can’t be dated directly.
Chapter
12

57. The Geologic Time
Scale
Chapter
12

58. Age of the Earth
• Oldest rocks are 3.96 Ga.
• Zircon minerals in some sandstones are 4.1-4.2 Ga.
• Earth is ~4.57 Ga based on correlation with…
• Meteorites, moon rocks.
Chapter
12

59. End
Chapter
12

60. Geologic Time
• Deep time – The immense span of geologic time.
• So vast, difficult to grasp.
• We think of time in terms of our lives…
• The lives of our parents and grandparents.
• The lives of our children or grandchildren.
• Human history is tiny compared to geologic time.
Chapter
12

61. Geologic Time
• James Hutton (1726-1797) – Scottish physician.
• Called “the Father of Modern Geology.”
• Stated the Principle of Uniformitarianism.
• Of time, He wrote: “we find no vestige of a beginning;
no prospect of an end.”
Chapter
12

62. Geologic Time
• Principle of Uniformitarianism:
• “The present is the key to the past.”
• Processes seen today are same as in the past.
e.g. Old mudcracks formed as mudcracks do today.
• Geologic change = slow; large changes = long time.
Chapter
12

63. Chapter
12

64. Stratigraphic Correlation
• Lithologic correlation is based on rock type.
• Sequence – The relative order in which the rocks
occur.
• Limited to correlation between nearby regions.
• Fossil correlation – Based on fossils within rocks.
• Applicable to much broader areas.
Chapter
12

65. Correlation among rock strata in 3 national
parks. Chapter
12

66. Angular Unconformity
• James Hutton - 1st to realize the vast time-significance
of angular unconformities.
• Mountains created, then completely erased.
• Then new sed. deposition.
Chapter
12

67. Angular Unconformity
• “Hutton’s Unconformity” on Siccar Point, Scotland, is a
common destination for geologists.
Chapter
12

68. Geologic Time
• The composite column is divided into time blocks.
• This is the geologic time scale, Earth’s “calendar.”
• The structure of the geologic time scale.
• Eons – The largest subdivision of time (100s to
1000s Ma).
• Eras – Subdivisions of an eon (65 to 100s Ma).
• Periods – Subdivisions of an era (2 to 70 Ma).
• Epochs – Subdivisions of a period (0.011 to 22
Ma).
Chapter
12

69. Geologic Time
• Time scale subdivisions are variously named.
• The nature of life (“zoic” means life); i.e., Proterozoic.
• A characteristic of the time period; i.e.,
Carboniferous.
• A specific locality; i.e., Devonian.
Chapter
12

70. Geologic Time and Life
• Life first appears on Earth ~ 3.8 Ga.
• Early life consisted of anaerobic
single-celled organisms.
• Oxygen from cyanobacteria
built up by 2 Ga.
• ~ 700 Ma, multicellular
life evolved.
• ~ 542 Ma marks the
1st appearance
of hard shells.
 Shells increased fossil
preservation.
 Life diversified rapidly –
the “Cambrian Explosion.”
Chapter
12

71. The Geologic Time Scale
• Names of the eons.
• Phanerozoic – “Visible life” (542 Ma to the present).
• Started 542 Ma at the Precambrian – Cambrian
boundary.
• Marks the 1st appearance of hard shells.
• Life diversified rapidly afterward.
• Proterozoic – “Before life” (2.5 to 0.542 Ga).
• Development of tectonic plates like those of today.
• Buildup of atmospheric O2; multicellular life
appears.
• Archean – “Ancient” (3.8 to 2.5 Ga).
• Birth of continents.
• Appearance of the earliest life forms.
• Hadean – “Hell” (4.6 to 3.8 Ga). Chapter
12

72. The Geologic Time Scale
• Names of the eras.
• Cenozoic – “Recent life.”
• 65.5 Ma to present.
• The “Age of Mammals.”
• Mesozoic – “Middle life.”
• 251 to 65.5 Ma.
• The “Age of Dinosaurs.”
• Paleozoic – “Ancient life.”
• 542 to 251 Ma.
• Life diversified rapidly.
Chapter
12

73. The Age of the Earth
• Before radioactivity-based
dating methods…
• 20 Ma – From Earth
cooling.
• 90 Ma –Ocean salinization.
• Assumed oceans were
initially freshwater.
• Measured the mass of
dissolved material in
rivers.
• Uniformitarianism and
evolution indicated an Earth
older than ~100 Ma. Chapter
12

74. Geologic Time
• The immensity of time is beyond comprehension.
• Metaphors illustrate the scale of time.
• The age of Earth (4.6 Ga) can be compared to
pennies.
• Lined up, 4.6 billion pennies would be 87,400 km
long.
• More than twice around Earth.
Chapter
12

75. Geologic Time
Chapter
12

76. What a Geologist Sees:
Unconformity
The photo shows the Siccar Point unconformity in Scotland,
on the coast about 60 km east of Edinburgh; the sketch
shows a geologist’s interpretation of the unconformity. For
more information, see Section 12.5 Unconformities: Gaps in
the Record starting on p.423 and Figure 12.8 in your
textbook.

77. Zoomable Art:
The Record in Rocks: Reconstructing Geologic History
When geologists examine a sequence of rocks exposed on
a cliff, they see a record of Earth history that can be
interpreted by applying the basic principles of geology,
searching for fossils, and using radiometric dating. For more
information, see the Featured Painting on pp.426-427 in
your textbook.

78. What a Geologist Sees:
Stratigraphic Column
The succession of rocks in the Grand Canyon can be
divided into formations based on notable changes in rock
type and changes in fossil assemblages. For more
information, see Section 12.6 Stratigraphic Formations and
Their Correlation starting on p.424 and Figure 12.11 on p.
429 in your textbook.