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The Age of Enlightenment
Late 18th
century
Tremendous advances in science, politics,
philosophy, economics, etc.
Thomas Jefferson – an American member of the
Enlightenment
The Scientific Method
Inductive phase : reasoning from the specific to the genera
(Formulate the hypothesis)
deductive phase: reasoning from the general to the specific
(test the hypothesis)
Example: formulation of the hypothesis
of spontaneous generation; Its testing by Louis Pasteur
Hypothesis:
An explanation that accounts for a set of observations
and can be tested by further investigation
Observation v.s. fact
A fact is a “cooked” observation
Lawyers talk about “facts”
Scientist are more conservative-
talk only about observations
Theory
A system of ideas used to explain
observations
Paradigm
A shared perspective within a scientific community
Usually expresses as a set of related theories
James Hutton
A “gentleman farmer”
Associate of James Watt
and other members of
the “Oyster Club”
The Scottish
Enlightenment –
centered in Edinburgh
(home of Hume, Smith)
Hutton and Deism
Hutton was a Deist
Deism held that one could gain greater
understanding of God by understanding nature –
his creation
The “Denudation Dilemma - a theological
conundrum
Denudation Dilemma
Rock and soil are essential to life
Rock is the foundation for where we live
Soil is the foundation of agriculture – sustains
life
To the Deists, this was evidence of God’s
beneficence
Denudation Dilemma
Rocks decay at Earth’s surface – weathering
Soil is washed away from farmlands – erosion
Weathering and erosion indicate destruction of
the land
Martin Luther predicted that the world would end
as a result of erosion
The Dilemma
How can one reconcile God’s beneficence with
the destruction of the land, which is essential for
life?
Hutton’s Observations
Processes of weathering and erosion are slow
Many rocks visible on the land are made up of
the products of weathering and erosion
These rocks are Sedimentary Rocks
Sediments accumulate in the ocean, so these
rocks originally formed in the ocean
The Riddle
How can rocks that formed below sea level be
found on land?
More of Hutton’s Observations
Not all rocks form by accumulation of sediment
Some rocks are made of crystals
These rocks show signs of having formed at
very high temperatures from molten material
These are Igneous Rocks
Arthur’s Seat and Salisbury Crags
Hutton’s Solution
Igneous rocks provide evidence for heat within
the Earth
Heat is capable of work (Watt’s influence)
Heat within the Earth lifts rocks from the sea and
creates new land
The dilemma is solved because as erosion
destroys land, heat uplifts new land
Implications of Hutton’s Solution
Earth processes are slow
Great changes can be accomplished with great
amounts of time
Evidence of great expanses of time recorded by
the rocks
Conclusion: the Earth must be extremely old
Evidence for Deep Time –
Hutton’s Unconformity
Sedimentary Rocks
reflect change in environment on the Earth’s
surface.
Rises and falls in sea level
Climate
Change in life forms
UNCONFORMITIES
Angular Unconformity
a) deposit of sediments
b) tectonic event
c) erosion
d) deposition
Historical Geology
Founders of Historical Geology
Nicolaus Steno (1638-1687)
fossil descriptions
first stratigrapher
Steno's Laws
Superposition
Original Horizontality
Original Lateral Continuity
Historical Geology
Steno's Laws
Superposition
Why the law of superposition is
necessary-
overturned strata in the hamalayas
Steno's Laws
Original Horizontality
Steno’s Laws:
original Horizontality
Steeply dipping sandstone and shale in the
Oachita Mountains, Arkansas
Original Continuity
Steno’s law of
Neptunism vs. Plutonism
Neptunism
Plutonism
the theory that the rocks of the
Earth's crust all consist of material deposited from,
or crystallized out of the ocean.
Abraham Gottlob Werner (1749-1817)
the concept of the formation of crystalline rocks by
solidification from a melt.
James Hutton (1726-1797)
Founders of Historical Geology
James Hutton (1726-1797)
dynamic/cyclic concept of Earth history-
“no vestige of a beginning, no prospect of an end”
recognized significance of unconformities
deep time
Uniformitarianism:
“ The present is the key to the past”
Hutton’s “Great unconformity” at Siccar point,
eastern Scotland
Hutton’s “Great
unconformity”
at Siccar point,
eastern Scotland
Historical Geology
Founders of Historical Geology
Catastrophism vs. Uniformitarianism
catastrophism
uniformitarianism
the doctrine that sudden violent, short-lived, more
or less worldwide events outside our present
experience or knowledge have greatly modified the
Earth's crust accounting for its present configuration
as well as for the observed distribution of life forms
James Ussher (1581-1656)
the fundamental principle that geological processes
and natural laws now operating to modify the Earth's
crust have acted in much the same manner and with
essentially the same intensity throughout geologic
time, and that past geologic events can be explained
by forces observable today;
"The present is the key to the past."
James Hutton (1726-1797)
Uniformitarianism: The present is the key to the past
(Hutton, 1788)
The basic physical, chemical and biological
laws of the present-day world also operated in the
Earth’s past.
Implications:
1. Present day geological processes acting at slow
rates, but over long time periods, can produce
dramatic results.
2. Based on the study of changes that are known to
occur gradually (e.g. wearing down of mountains),
the Earth must be very old.
Misconception:
All geologic processes are slow and gradual.
Historical Geology
Founders of Historical Geology
William Smith (1769-1839)
first geologic map
Principle of Faunal Succession
Historical Geology
Founders of Historical Geology
Charles Lyell (1797-1875)
first geologic time scale
relative time
Principle of Cross-cutting Relationships
Principle of Inclusions
Historical Geology
Lyell's Principles of Relative Time
Cross-cutting Relationships
Nonconformity
Unconformity separating younger rocks from distinctly
older, metamorphosed rocks
a) tectonic event produces some sort of crystalline
rock
b) uplift with erosion
c) deposition
Disconformity
Unconformity in which beds on opposite sides are
parallel
a) deposition
b) erosion
c) deposition
Paraconformity
Deposition
Erosion
Deposition
Uniformitarianism
the laws of nature do not change with time.
Hutton- first to discover geological time, and the first to
state that the Earth is much older than 6000 years.
Before Hutton, everyone believed in catastrophism,
which states that the shape of the Earth came to be
quickly and violently.
Catastrophism was a by-product of the fact that religion
was in control of most governments.
An old Earth
Recycling of Earth materials
Evidence for earlier episodes of recycling
“No vestige of a beginning… no prospect of an
end.”
Hutton’s “Theory of the Earth” - 1785
Playfair’s Commentary
“The mind seemed to grow giddy looking so far
into the abyss of time…”
Example of Slow Change: Green River, Utah
1871
1968
Catastrophism: Changes in the Earth are sudden and violent
Major changes in the Earth’s state tend to occur
in short bursts of activity.
Implication:
Geologic changes tend to occur as rare events that
are short-lived with little change occurring between
these events.
Misconceptions:
1. All changes that occur on the Earth are catastrophic
2. The Earth and its present day features were produced
during a single event, and therefore the Earth must be
very young
Catastrophic Event: Eruption of Mount Vesuvius, Italy, 79 AD
Effects: Mass human mortality in Pompeii and Herculaneum
volcanic
ash
layerexcavated ruins
Catastrophic Event: Chicxulub Crater, Yucutan, Mexico
Impact event: 65 million years ago
Crater size: 180-280 km dia.
Profoundly affected global climate due to atmospheric dust
Possible cause of mass extinction
What’s so remarkable about Hutton’s Ideas?
Contrary to prevailing views of the time
Based on observation – what he saw
Hutton drew inferences from his observations
Inferences are hypotheses
Hypotheses are testable
This is an application of the scientific method
to study of the Earth
Hutton solution
Hutton solution

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Hutton solution

  • 1. The Age of Enlightenment Late 18th century Tremendous advances in science, politics, philosophy, economics, etc. Thomas Jefferson – an American member of the Enlightenment
  • 2. The Scientific Method Inductive phase : reasoning from the specific to the genera (Formulate the hypothesis) deductive phase: reasoning from the general to the specific (test the hypothesis) Example: formulation of the hypothesis of spontaneous generation; Its testing by Louis Pasteur
  • 3. Hypothesis: An explanation that accounts for a set of observations and can be tested by further investigation
  • 4. Observation v.s. fact A fact is a “cooked” observation Lawyers talk about “facts” Scientist are more conservative- talk only about observations
  • 5. Theory A system of ideas used to explain observations
  • 6. Paradigm A shared perspective within a scientific community Usually expresses as a set of related theories
  • 7. James Hutton A “gentleman farmer” Associate of James Watt and other members of the “Oyster Club” The Scottish Enlightenment – centered in Edinburgh (home of Hume, Smith)
  • 8. Hutton and Deism Hutton was a Deist Deism held that one could gain greater understanding of God by understanding nature – his creation The “Denudation Dilemma - a theological conundrum
  • 9. Denudation Dilemma Rock and soil are essential to life Rock is the foundation for where we live Soil is the foundation of agriculture – sustains life To the Deists, this was evidence of God’s beneficence
  • 10. Denudation Dilemma Rocks decay at Earth’s surface – weathering Soil is washed away from farmlands – erosion Weathering and erosion indicate destruction of the land Martin Luther predicted that the world would end as a result of erosion
  • 11. The Dilemma How can one reconcile God’s beneficence with the destruction of the land, which is essential for life?
  • 12. Hutton’s Observations Processes of weathering and erosion are slow Many rocks visible on the land are made up of the products of weathering and erosion These rocks are Sedimentary Rocks Sediments accumulate in the ocean, so these rocks originally formed in the ocean
  • 13. The Riddle How can rocks that formed below sea level be found on land?
  • 14. More of Hutton’s Observations Not all rocks form by accumulation of sediment Some rocks are made of crystals These rocks show signs of having formed at very high temperatures from molten material These are Igneous Rocks
  • 15. Arthur’s Seat and Salisbury Crags
  • 16. Hutton’s Solution Igneous rocks provide evidence for heat within the Earth Heat is capable of work (Watt’s influence) Heat within the Earth lifts rocks from the sea and creates new land The dilemma is solved because as erosion destroys land, heat uplifts new land
  • 17. Implications of Hutton’s Solution Earth processes are slow Great changes can be accomplished with great amounts of time Evidence of great expanses of time recorded by the rocks Conclusion: the Earth must be extremely old
  • 18. Evidence for Deep Time – Hutton’s Unconformity
  • 19. Sedimentary Rocks reflect change in environment on the Earth’s surface. Rises and falls in sea level Climate Change in life forms
  • 20.
  • 21. UNCONFORMITIES Angular Unconformity a) deposit of sediments b) tectonic event c) erosion d) deposition
  • 22. Historical Geology Founders of Historical Geology Nicolaus Steno (1638-1687) fossil descriptions first stratigrapher Steno's Laws Superposition Original Horizontality Original Lateral Continuity
  • 24. Why the law of superposition is necessary- overturned strata in the hamalayas
  • 25. Steno's Laws Original Horizontality Steno’s Laws: original Horizontality Steeply dipping sandstone and shale in the Oachita Mountains, Arkansas
  • 27. Neptunism vs. Plutonism Neptunism Plutonism the theory that the rocks of the Earth's crust all consist of material deposited from, or crystallized out of the ocean. Abraham Gottlob Werner (1749-1817) the concept of the formation of crystalline rocks by solidification from a melt. James Hutton (1726-1797)
  • 28. Founders of Historical Geology James Hutton (1726-1797) dynamic/cyclic concept of Earth history- “no vestige of a beginning, no prospect of an end” recognized significance of unconformities deep time Uniformitarianism: “ The present is the key to the past”
  • 29. Hutton’s “Great unconformity” at Siccar point, eastern Scotland Hutton’s “Great unconformity” at Siccar point, eastern Scotland
  • 30. Historical Geology Founders of Historical Geology Catastrophism vs. Uniformitarianism catastrophism uniformitarianism the doctrine that sudden violent, short-lived, more or less worldwide events outside our present experience or knowledge have greatly modified the Earth's crust accounting for its present configuration as well as for the observed distribution of life forms James Ussher (1581-1656) the fundamental principle that geological processes and natural laws now operating to modify the Earth's crust have acted in much the same manner and with essentially the same intensity throughout geologic time, and that past geologic events can be explained by forces observable today; "The present is the key to the past." James Hutton (1726-1797)
  • 31. Uniformitarianism: The present is the key to the past (Hutton, 1788) The basic physical, chemical and biological laws of the present-day world also operated in the Earth’s past. Implications: 1. Present day geological processes acting at slow rates, but over long time periods, can produce dramatic results. 2. Based on the study of changes that are known to occur gradually (e.g. wearing down of mountains), the Earth must be very old. Misconception: All geologic processes are slow and gradual.
  • 32. Historical Geology Founders of Historical Geology William Smith (1769-1839) first geologic map Principle of Faunal Succession
  • 33. Historical Geology Founders of Historical Geology Charles Lyell (1797-1875) first geologic time scale relative time Principle of Cross-cutting Relationships Principle of Inclusions
  • 34. Historical Geology Lyell's Principles of Relative Time Cross-cutting Relationships
  • 35. Nonconformity Unconformity separating younger rocks from distinctly older, metamorphosed rocks a) tectonic event produces some sort of crystalline rock b) uplift with erosion c) deposition
  • 36. Disconformity Unconformity in which beds on opposite sides are parallel a) deposition b) erosion c) deposition
  • 37.
  • 39. Uniformitarianism the laws of nature do not change with time. Hutton- first to discover geological time, and the first to state that the Earth is much older than 6000 years. Before Hutton, everyone believed in catastrophism, which states that the shape of the Earth came to be quickly and violently. Catastrophism was a by-product of the fact that religion was in control of most governments.
  • 40. An old Earth Recycling of Earth materials Evidence for earlier episodes of recycling “No vestige of a beginning… no prospect of an end.” Hutton’s “Theory of the Earth” - 1785
  • 41. Playfair’s Commentary “The mind seemed to grow giddy looking so far into the abyss of time…”
  • 42. Example of Slow Change: Green River, Utah 1871 1968
  • 43. Catastrophism: Changes in the Earth are sudden and violent Major changes in the Earth’s state tend to occur in short bursts of activity. Implication: Geologic changes tend to occur as rare events that are short-lived with little change occurring between these events. Misconceptions: 1. All changes that occur on the Earth are catastrophic 2. The Earth and its present day features were produced during a single event, and therefore the Earth must be very young
  • 44. Catastrophic Event: Eruption of Mount Vesuvius, Italy, 79 AD Effects: Mass human mortality in Pompeii and Herculaneum volcanic ash layerexcavated ruins
  • 45. Catastrophic Event: Chicxulub Crater, Yucutan, Mexico Impact event: 65 million years ago Crater size: 180-280 km dia. Profoundly affected global climate due to atmospheric dust Possible cause of mass extinction
  • 46. What’s so remarkable about Hutton’s Ideas? Contrary to prevailing views of the time Based on observation – what he saw Hutton drew inferences from his observations Inferences are hypotheses Hypotheses are testable This is an application of the scientific method to study of the Earth