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Geologic Time
Earth Science
John Wesley Powell
• “The canyons of this region
would be a Book of
Revelations in the rock-
leaved Bible of geology”
Geologic Time Scale
It helps us understand the Earth’s exceedingly long
history
A Brief History of Geology
• James Ussher, Anglican
Archbishop of Armagh, Primate of
all Ireland, constructed a
chronology of human and Earth
history in the mid 1600s in which
he determined that Earth was
only a few thousand years old,
having been created in 4004 B.C.
A Brief History
of Geology
• Catastrophism, a
philosophy that
believed that Earth’s
landscapes had been
developed primarily by
great catastrophes
Birth of Modern
Geology
• James Hutton, published his Theory
of the Earth in the late 1700s
• Uniformitarianism, the physical,
chemical, and biological laws that
operate today have also operated in
the geologic past
Relative Dating: Key
Principles
Relative Dating
• placing rocks in their proper
sequence of formation
Law of
Superposition
• Nicolaus Steno, (1636–1686), is
credited with being the first to
recognize a sequence of
historical events in an outcrop of
sedimentary rock layers.
• in an undeformed sequence of
sedimentary rocks, each bed is
older than the one above it and
younger than the one below.
Principle of
Original
Horizontality
• layers of sediment
are generally
deposited in a
horizontal position
Principle of
Cross-Cutting
Relationship
• An intrusive rock
body is younger
than the rocks it
intrudes. A fault is
younger than the
rock layers it cuts.
Inclusions
• pieces of one rock unit
that are contained
within another
Unconformities
• Conformable, rock that have been deposited without
interruption
• Unconformity, breaks in the rock record
• Three Types:
• Angular Unconformity
• Disconformity
• Nonconformity
Angular
Unconformity
• It consists of tilted or folded
sedimentary rocks that are
overlain by younger, more flat
lying strata
Disconformity
• an unconformity
between parallel
layers of
sedimentary rocks
which represents a
period of erosion
or non-deposition
Nonconformity
• the break
separates older
metamorphic or
intrusive igneous
rocks from younger
sedimentary strata.
Test Your Understanding
Correlation
of Rock
Layers
Correlation
• Rocks of the same
region are concluded
to be around the
same age.
Principle of
Original Lateral
Continuity
• all rock layers are laterally continuous
and may be broken up or displaced by
later events
Fossils: Evidence of Past Life
Fossils
Types of
Fossils
Petrification
• turned into stone
• the small internal
cavities and pores are
filled with precipitated
mineral matter
Types of
Fossils
Molds and Cast
• Mold is a fossilized
imprint
• Cast are hardened
mineral matter that
forms in the shape of
the mold
Types of
Fossils
Carbonization
• The process of
transforming organic
material into a carbon
residue through a
combination of heat,
pressure, and time.
Types of
Fossils
Impression
• The organism’s original
bone or tissue is
removed by processes
after burial, such as
ground water flow
Types of
Fossils
Amber
• Hardened resin of
ancient trees that traps
insects
Other Types
of Fossils
An indirect evidence of
prehistoric life
Tracks
Animal footprints
Burrows
• Tubes in sediment, wood,
or rock made by an
animal
Coprolites
• Fossil dung and
stomach contents
Gastroliths
• Highly polished stomach
stones
Fossils and
Correlation
Principle of Fossil
Succession
• Fossil organisms
succeed one another in
a definite and
determinable order,
and therefore any time
period can be
recognized by its fossil
content.
Index Fossil
• Fossils that are
widespread
geographically and are
limited to a short span
of geologic time.
• Provides an important
method of matching
rocks of the same age.
Index Fossils
Criteria
•Easily recognized
•Geographically widespread
•Have lived for only a short time
Importance of
Fossils
• Can be an indicator of the
age of the rock
• Can be used as an
environmental indicator
• Can indicate the former
temperature of the water
Importance of Fossils
•Can be an indicator of the age of
the rock
•Can be used as an environmental
indicator
•Can indicate the former
temperature of the water
Dating with
Radioactivity
Reviewing the Basic
Atomic Structure
Subatomic Particles
• Neutron
• Electrons
• Protons
Reviewing Basic
Atomic Structure
•Atomic Number
•Mass Number
•Isotopes
92
234
𝑈
92
235
𝑈
92
238
𝑈
Radioactivity
•A spontaneous
emission or decay
of the nuclei of an
atom
3 Common
Types
Alpha Emission, 2
4
𝐻𝑒
• the emission of an alpha particle means
that the mass number of the isotope is
reduced by four and the atomic number
is decreased by two
Alpha Emission, 2
4
𝐻𝑒
•the emission of an alpha particle means
that the mass number of the isotope is
reduced by four and the atomic number is
decreased by two
3 Common
Types
Beta Emission, −1
0
𝑒
• Because the electron has come from a
neutron, the nucleus contains one more
proton than before. Therefore, the
atomic number increases by one.
Beta Emission, −1
0
𝑒
•Because the electron has come from a
neutron, the nucleus contains one more
proton than before. Therefore, the atomic
number increases by one.
3 Common
Types
Electron Capture
• the nucleus now contains one less
proton, the atomic number decreases
by one
Electron Capture
•the nucleus now contains one less proton,
the atomic number decreases by one
Radiometric Dating
•a reliable means of calculating the ages of
rocks and minerals that contain particular
radioactive isotopes
Half-life
•The time
required for one
half of the nuclei
in a sample to
decay
Dating with Carbon – 14
• Used to date recent events
• Half-life: 5,730 years
Geologic Time Scale
•A system of chronological
measurement that relates
stratigraphy to time
•Divides the geologic history into units
Subdivisions
•Eon – greatest expansion of time
•4 Eons
•Phanerozoic – “visible life”, the most
recent
•Proterozoic
•Archean
•Hadean – the oldest
Subdivisions
•Era – subdivision of an eon
•Eras of the Phanerozoic Eon
•Cenozoic – recent life
•Mesozoic – middle life
•Paleozoic – ancient life
Subdivisions
•Period – subdivisions of era
•Epoch – subdivisions of periods
Precambrian Eon
•Comprises about 88% of the geologic
timescale
Age of Invertebrates
•Cambrian Period and Ordovician
Period
Age of Fishes
•Silurian Period and Devonian Period
Age of Amphibians
•Mississippian Period, Pennsylvanian
Period, and Permian Period
Age of Reptiles
•Mesozoic Era
Age of Mammals
•Cenozoic Era
Earth Science Geologic Time and Fossils.pptx

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Earth Science Geologic Time and Fossils.pptx

Editor's Notes

  1. * Powell realized that the evidence for an ancient Earth is concealed in its rocks * Interpreting Earth history is a prime goal of the science of geology
  2. *today’s geological processes are the same in the past *geological processes occur over a long period of time *cited verifiable observations
  3. To say that geological processes in the past were the same as those occurring today is not to suggest that they always had the same relative importance or that they operated at precisely the same rate
  4. To establish a relative time scale, a few basic principles or rules had to be discovered and applied.
  5. *Danish anatomist, geologist, and priest
  6. Beneath the ocean, beds A, B, C, and E were deposited in that order (law of superposition).
  7. Uplift and intrusion of a sill (layer D). We know that sill D is younger than beds C and E because of the inclusions in the sill of fragments from beds C and E.
  8. Next is the intrusion of dike F. Because the dike cuts through layers A through E, it must be younger (principle of cross-cutting relationships).
  9. Layers A through F were tilted and exposed layers were eroded.
  10. Next, beds, G, H, I, J, and K were deposited in that order atop the erosion surface to produce an angular unconformity. Because layer H is a lava flow, superposition applies to it as well as the surrounding sedimentary beds.
  11. An English engineer and canal builder
  12. For example, an Age of Trilobites is recognized quite early in the fossil record. Then, in succession, paleontologists recognize an Age of Fishes, an Age of Coal Swamps, an Age of Reptiles, and an Age of Mammals
  13. *Origin of the Earth *First one-celled organism *First multicelled organism
  14. *First Organism with shells *Trilobites dominant (Cambrian) *Cephalopods dominant (Ordovician) *First Fishes
  15. *First Land Plants (Silurian) *Fishes Dominant (Ordovician) *First insect fossils
  16. *Amphibians abundant (Mississippian) *Large coal swamps *First reptiles (Pennsylvanian) *Extinction of Trilobites and other marine animals (the Permian extinction 250 yago)
  17. *Dinosaurs dominant (Triassic) *First birds (Jurassic) *First flowering plants *Extinction of dinosaurs (end of Cretaceous)
  18. *Mammals (tertiary period – Miocene Epoch) *Evolution of humans (Pleistocene Epoch)