Chapter 11 - ESC1000 Flashcards

1
Q

What is the principle of uniformitarianism?

A

Concept that the processes that have shaped the Earth in the past are essentially the same as those operating today.

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2
Q

What is catastrophism?

A

Concept that Earth was shaped by catastrophic events of a short-term nature.

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3
Q

What is numerical dating?

A

Date that specifies the actual number of years that have passed since the event occurred.

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4
Q

What is relative dating?

A

Date that results from placing the rocks in their proper sequence or order to determine the chronological order of events.

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5
Q

Who was James Hutton?

A

Famous Scottish physician from the 1700s who published his Theory of Earth that puts forward the fundamental principle of uniformitarianism.

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6
Q

Who was James Ussher?

A

Anglican archbishop from the mid 1600s who constructed a chronology of human and Earth history based on the bible in which he determined that Earth was only a few thousand years old.

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7
Q

Explain the difference between catastrophism and uniformitarianism.

A

Catastrophism views the processes that shape the Earth as short-term events while uniformitarianism views the processes that shape the Earth as slow and acting over long spans of time.

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8
Q

List the principles of relative dating.

A

Superposition, Original Horizontality, Lateral Continuity, Cross-Cutting Relationships, and Inclusions.

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9
Q

What is the principle of superposition?

A

States that in any undeformed sequence of sedimentary rocks, each bed is older than the one above and younger than the one below.

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10
Q

Who is Nicholas Steno?

A

Danish geologist from the 1600s that proposed the principles of superposition and original horizontality.

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11
Q

What is the principle of original horizontality?

A

Principle by which layers of sediment are generally deposited in horizontal position.

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12
Q

What is the principle of lateral continuity?

A

Principle which states that sedimentary beds originate as continuous layers that extend in all directions until they grade into a different type of sediment or thin out at the edge of a sedimentary basin.

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13
Q

What is the principle of cross-cutting relationships?

A

Principle which states that a rock or fault is younger than any rock or fault through which it cuts.

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14
Q

What is the principle of inclusion?

A

Principle which states that the rock mass that provided the inclusion is older than the rock mass containing the inclusion.

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15
Q

What are unconformities?

A

A surface that represents a break in the rock record, caused by erosion or nondeposition.

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16
Q

What is conformable?

A

Layers of rock that were deposited without interruption.

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17
Q

List the 3 types of unconformities.

A

Angular, Disconformity, and Nonconformity.

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18
Q

What is angular unconformity?

A

Unconformity in which strata below dip at an angle different from that of the beds above.

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19
Q

What does an angular unconformity indicates?

A

Indicates that during a pause in deposition, a period of deformation (folding or tilting), and erosion occurred.

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20
Q

What is a disconformity?

A

Is a gap in the rock record that represents a period during which erosion rather than deposition occurred. Beds above and below are parallel.

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21
Q

What is nonconformity?

A

An unconformity in which older metamorphic or intrusive igneous rocks are overlain by younger sedimentary strata.

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22
Q

How does a nonconformity form?

A

Older metamorphic and igneous rocks that originate deep below must experience a period of uplift. Once exposed at the surface the rocks are subject to erosion and undergo a renewed period of sedimentation.

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23
Q

What are fossils?

A

Remains and traces of organisms preserved from the geologic past.

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24
Q

What is paleontology?

A

Systematic study of the fossils and the history of life on Earth.

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25
Q

Why are fossils important in geology?

A

They can serve as tools for interpreting the geologic past. They can indicate past environmental conditions and help correlate rocks of similar ages that are in different places.

26
Q

List the 5 types of fossils.

A

Permineralization, Molds and Casts, Carbonization and Impressions, Amber, and Trace Fossils.

27
Q

Describe the process of permineralization.

A

Mineral-rich groundwater permeates porous tissue such as bone or wood, minerals precipitate out of the solution and fill pores and empty spaces.

28
Q

Describe the process of a mold and a cast.

A

A structure is buried in sediment and then dissolved by underground water forming a mold. If the hollow spaces of the structure are filled with mineral matter, casts are created.

29
Q

Describe the process of carbonization.

A

Fine sediment encases the remains of an organism. As time passes, pressure squeezes out the liquid and gaseous components and leaves behind a thin residue of carbon.

30
Q

Describe the process of impressions.

A

If the film of carbon created in carbonization is lost, a replica of the surface may still show.

31
Q

Describe the process of amber fossils.

A

Organism is trapped in tree resin and then it hardens over time.

32
Q

Describe what are trace fossils.

A

They are traces of prehistoric life and they can be tracks (footprints), burrows, and gastroliths (stomach stones from dinosaurs).

33
Q

What conditions favor preservation of an organism as a fossil?

A

Rapid burial where remains are protected from the surface environment and hard parts have better chance of preservation.

34
Q

What is correlation?

A

The process of establishing the equivalence of rocks of similar age in different areas.

35
Q

What is the principle of fossil succession?

A

Principle by which fossil organisms succeed one another in a definite and determinable order, and any time period can be recognized by its fossil content.

36
Q

What is the difference between index fossils and fossil assemblages?

A

One is limited to a short period of time so they help matching rocks of the same age and the other requires a variety of fossils to establish the age of the bed.

37
Q

What is an index fossil?

A

A fossil that is associated with a particular span of geologic time.

38
Q

What is a fossil assemblage?

A

The overlapping ranges of a group of fossils collected from a layer.

39
Q

What is nuclear decay?

A

Spontaneous decay of certain unstable atomic nuclei.

40
Q

What are the 3 types of nuclear decay?

A

Alpha emission, Beta emission, and Electron capture.

41
Q

Describe the alpha emission.

A

A particle composed of 2 protons and 2 neutrons is emitted from the nucleus. The atomic number drops by 2 and the mass number diminishes by 4.

42
Q

Describe the beta emission.

A

A neutron decays to produce an electron plus a proton and then the electron is emitted. The atomic number increases by 1 and there is no change in mass number.

43
Q

Describe the electron capture.

A

An electron is captured by the nucleus and combines with a proton and forms an additional neutron. The change in the atomic number drops by 1 and there is no change in mass number.

44
Q

What is a parent isotope?

A

An unstable isotope.

45
Q

What is a daughter isotope?

A

Isotopes resulting from the decay of the parent isotope.

46
Q

What is radiometric dating?

A

Procedure of calculating the absolute ages of rocks and minerals that contain radioactive isotopes.

47
Q

What is the half-life?

A

Time required for one-half of the atoms of a radioactive substance to decay.

48
Q

What is radiocarbon dating?

A

Radiometric dating using carbon-14, a radioactive isotope of carbon that is produced in the atmosphere.

49
Q

Explain how the carbon-14 dating works.

A

Carbon-14is produced in the atmosphere and absorbed by every living organism. As long the as the organism is alive it will continue to absorb and replace carbon-14. Carbon-12 is the most common and stable type of carbon and when an animal dies, gradually the carbon-14 decays by beta emission into nitrogen-14. By comparing the proportions of carbon-14 and carbon-12 in an organism, a radiocarbon date can be determined.

50
Q

How far can radiocarbon dating be used?

A

As far as 70,000 years.

51
Q

Why it is difficult to assign a reliable numerical date to a sample of sedimentary rock?

A

The rocks composing sedimentary strata are not the same age as they are the result of weathered down rocks from different ages.

52
Q

How might a numerical date for a layer of sedimentary rock be determined?

A

Geologists must relate the strata to datable igneous masses.

53
Q

What is the geologic time scale?

A

The division of Earth history into blocks of time.

54
Q

What are the blocks of time of a geologic time scale?

A

Eon, Eras, Periods, and Epochs.

55
Q

What are the 2 eons?

A

Phanerozoic and Precambrian.

56
Q

What is the phanerozoic?

A

Eon containing abundant fossil evidence and it extended from the end of the Proterozoic eon (540 million years ago) to present.

57
Q

How can the Precambrian be divided?

A

In Archean and Proterozoic.

58
Q

What are the 3 eras of the Phanerozoic?

A

Paleozoic, Mesozoic, and Cenozoic.

59
Q

How long does the Precambrian lasts?

A

From 541 million years ago to 4.6 billion years ago.

60
Q

What does “zoic” means?