History of Geologic Thought
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Transcript of History of Geologic Thought
History ofGeologic Thought
Historical Geology – Principles
History of Geologic Thought
Historical Geology – Principles
Myths and Legendsto explain the “unknown”
Creation: every society has a creation myth.
Geologic processes:earthquakes, volcanoes,
History of Geologic Thought
Historical Geology – Principles
Myths and Legendsto explain the “unknown”
Fossils: what are they?
• really organic remains?• how - when did they get there?
• before/after rock formed?
History of Geologic Thought
Historical Geology – Principles
Myths and Legendsto explain the “unknown”
Fossils: what are they?
• animals crawled into cracks • remains of a lost race
• grew from seeds, solution or vapors• "figure stones" by "plastic forces"
History of Geologic Thought
Historical Geology – Principles
Myths and Legendsto explain the “unknown”
Fossils: what are they?
• animals crawled into cracks • remains of a lost race
• grew from seeds, solution or vapors• "figure stones" by "plastic forces"
Fossil Folklore @ Natural History Museum, London
History of Geologic Thought
Historical Geology – Principles
Myths and Legendsto explain the “unknown”
Fossils: what are they?
• Organisms caught in the Biblical deluge
• dominated scientific thought up to mid-19th Century
History of Geologic Thought
Historical Geology – Principles
Scientific Observation:
Leonardo da Vinci: 1500's
Recognized that fossil shells represent ancient marine life, even though they were miles from the nearest shore.
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History of Geologic Thought
Historical Geology – Principles
Scientific Observation:
Rationale
• too fragile to be transported for miles • fossil communities,not jumbled
• distinct fossiliferous layers, multiple events
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da Vinci Geologist @ UCMP
Fundamental Stratigraphic Principles
Historical Geology – Principles
Nicolas Steno:
• 1600’s
• Physician - "amateur scientist"
• Observed sediment and water sorting, and stratification
Steno as Geologist - Theologian
Fundamental Stratigraphic Principles
Historical Geology – Principles
1. Superposition:
in a sequence of undisturbed strata,
oldest layers are on the bottom,
youngest on top.
Historical Geology – Principles
1. Superposition:
Fundamental Stratigraphic Principles
Historical Geology – Principles
2. Original horizontality:
Particles settle from
a fluid under the
influence of gravity
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Fundamental Stratigraphic Principles
Historical Geology – Principles
2. Original horizontality:
Layers must therefore be
parallel and horizontal to
the surface on which particles settle.
Fundamental Stratigraphic Principles
Historical Geology – Principles
2. Original horizontality:
Layers must therefore be
parallel and horizontal to
the surface on which particles settle.
Fundamental Stratigraphic Principles
Historical Geology – Principles
2. Original horizontality:
Layers must therefore be
parallel and horizontal to
the surface on which particles settle.
Fundamental Stratigraphic Principles
Historical Geology – Principles
2. Original horizontality:
Layers must therefore be
parallel and horizontal to
the surface on which particles settle.
Fundamental Stratigraphic Principles
Historical Geology – Principles
2. Original horizontality:
uplifted, butundisturbed beds
Grand Canyon
Fundamental Stratigraphic Principles
Historical Geology – Principles
some tectonic eventtilted these beds
2. Original horizontality:
old on the bottom?
Fundamental Stratigraphic Principles
Historical Geology – Principles
some tectonic eventtilted these beds
2. Original horizontality:
Maybeold on the bottom?
Fundamental Stratigraphic Principles
Historical Geology – Principles
3. Original lateral continuity:
Strata originally extend in all directions until they:
• thin to zero at edge of basin
• end abruptly against some barrier
Fundamental Stratigraphic Principles
Historical Geology – Principles
3. Original lateral continuity:
Strata originally extend in all directions until they:
• change gradationally into some different kind of sediment.
Fundamental Stratigraphic Principles
Historical Geology – Principles
3. Original lateral continuity:
“Old” View of the World
Historical Geology – Principles
Catastrophism:
The belief that geologic features can be
explained by catastrophic events (floods)
on a scale not seen today.
“Old” View of the World
Historical Geology – Principles
Catastrophism:
The belief that geologic features can be
explained by catastrophic events (floods)
on a scale not seen today.
Especially the Noachian, Biblical Flood
“Old” View of the World
Historical Geology – Principles
Catastrophism:
Indirectly linked to interpretation
of a young Earth.
< 10,000 years old
“New” View of the World
Historical Geology – Principles
4. Uniformitarianism:
Uni - form - i - tarian - ism
“New” View of the World
Historical Geology – Principles
4. Uniformitarianism: Uni - form - i - tarian - ism
James Hutton:
"The past history of our globe can be
explained by what can be seen to happen now"
Hutton Bio @
“New” View of the World
Historical Geology – Principles
4. Uniformitarianism: Uni - form - i - tarian - ism
"The present is key to the past"
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Present Day Beach with forming Ripple Marks
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Uniformitarianism
“New” View of the World
Historical Geology – Principles
Strict uniformitarianism: what we see today ...
is exactly the conditions of the past
“New” View of the World
Historical Geology – Principles
Actualism:
"Laws of nature" are inviolable:
gravity, properties of water, chemical reactions
20th C
“New” View of the World
Historical Geology – Principles
Actualism:
But, we now recognize thatintensity and rates may vary:
• climate change • tectonic spreading rates • intensity of volcanism
“New” View of the World
Historical Geology – Principles
Actualism:
• the stray meteor
“New” View of the World
Historical Geology – Principles
With Actualism:
We can account for events that
have not occurred over the course
of human time span.
Deep Geologic Time
Historical Geology – Principles
Hutton: Siccar Point Scotland Recognized significance ofan unconformities.
Deep Geologic Time
Historical Geology – Principles
Hutton: Siccar Point Scotland Recognized the significance
of unconformities.
Deep Geologic Time
Historical Geology – Principles
Hutton: Siccar Point Scotland
Deep Geologic Time
Historical Geology – Principles
Hutton: Siccar Point Scotland
Deep Geologic Time
Historical Geology – Principles
Hutton: Siccar Point Scotland
Deep Geologic Time
Historical Geology – Principles
Hutton: Siccar Point Scotland
Deep Geologic Time
Historical Geology – Principles
Hutton: Siccar Point Scotland
Deep Geologic Time
Historical Geology – Principles
Hutton: • developed a cyclic view of the earth
• earth in a continuous state of fluxold rocks decay,new rocks form (dynamic)
Deep Geologic Time
Historical Geology – Principles
Hutton:
• Did not see the need to
invoke catastrophes to explain
geologic formations.
Deep Geologic Time
Historical Geology – Principles
Hutton:
• Did not see the need to
invoke catastrophes to explain
geologic formations.
• Observable processes and
... Time
Deep Geologic Time
Historical Geology – Principles