Chapter-2 Historical Geology Flashcards

1
Q

Study of changes to earth and life in time and space.

A

Historical Geology

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2
Q

Types of ages

A
Relative Time (Relative Age)
Absolute Time (Absolute Age)
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3
Q

Measurement of time using comparison methods.

A

Relative Time ( Relative Age )

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4
Q

Measurement of time using actual numbers.

A

Absolute Time ( Absolute Age )

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5
Q

Measuring Earth’s Relative Age

A

Use of Rocks

Use of faults to determine relative rock age layers abd the order in which event happened

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6
Q

Measuring Earth’s Absolute age

A

Radioactive Dating

Half-life

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7
Q

The breaking down of atoms to form different isotopes of the same element or completely new element.

A

Radioactive Dating

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8
Q

The amount of time it takes for half of the original atoms to decay.

A

Half-life

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9
Q

Fundamental Theories of Historical Geology

A

Uniformitarianism

Catastrophism

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10
Q

Suggested that the landscape developed over long periods of time through a variety of slow geologic and geomorphic processes.

A

Theory of Uniformitarianism

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11
Q

Theory proposed by James Huttonin 1785, which was based only on natural history, which was later expanded by Charles Lyell in the 1830s.

A

Theory of Uniformitarianism

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12
Q

Lyell’ uniformitarianism propositions, according to Reijer Hooykas in 1963

A

Uniformity of Law
Uniformity of Methodology
Uniformity of kind
Uniformity of Degree

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13
Q

Laws of nature are constant across time and space.

A

Uniformity of Law

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14
Q

Appropriate hypotheses for explaining the geological past are those with analogy today.

A

Uniformity of Methdology

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15
Q

Past and present causes are all of the same kind, have the same energy, and produce the same effects.

A

Uniformity of Kind

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16
Q

Geological circumstances have remained the same over time.

A

Uniformity of Degree

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17
Q

Theory that says: The idea that the Earth has been affected by sudden, short-lived, violent events that were sometimes worldwide in scope.

A

Theory of Catastrophism

18
Q

First popularized by Georges Cuvier on the 19th century, which proposed that new life forms had moved from other areas after local floods.

A

Theory of Catastrophism

19
Q

Geological epochs had ended woth violent and sudden natural catastrophes such as great floods, formation of major mountain chains or asteroid impact.

A

Theory of Catastrophism

20
Q

formerly Cretaceous-Tertiary (K-T) extinction event, about 66 million years ago

A

Cretaceous-Paleogene Event

21
Q

a large planetismal somehow impacted the early earth, blew out rocky debris, remelted it and formed the moon , about 4.5 billion years ago.

A

Giant Impact Theory

22
Q

distinct surface between two unlike bodies of rocks.

A

Contact

23
Q

single layer/bed of rock

A

Startum

24
Q

multiple layers/beds of rocks

A

Strata

25
Q

Study of Strata

A

Stratigraphy

26
Q

a body of rock with distinctive structure that is bounded by contacts

A

Formation

27
Q

Locations or proportions where rocks are exposed at the earth’s surface

A

Outcrop/Exposure

28
Q

Formulate by Nicolaus Stenoin 1669, a Danish physician, to help him make sense of the rocks of Tuscany, Italy and the various objects contained within them.

A

Fundamental Principles of Historical Geology

29
Q

In any undeformed sequence of sedimentary rocks, each bed is younger than the one below it and older than the one above it.

A

Steno’s Law of Superposition

30
Q

Sedimentary rocks are horizontal because yhe original sediments were horizontal.

A

Steno’s Law of Original Horizontality

31
Q

Starta originally extended in all directions until they thinned to zero at their edges of deposition. Therefore, matching strata on opposite sides of a valley, or continent can be correlated.

A

Steno’s Law of Lateral Continuity

32
Q

Invading igneous rock is always younger than the rock it intrudes.

A

Steno’s Law of Cross-Cutting Relationships

33
Q

Similar to the intrusive relationships, it states that the fault is younger than the rock itself.

A

Steno’s Law of Intrusive Relationships

34
Q

gaps in the geologic taht may indicate episodes of crustal deformation, erosion, and sea level variations.

A

Unconformity

35
Q

Types of Uncoformities

A

Angular Inconformities
Disconformities
Nonconformities

36
Q

are those where an older package of sediments has been tilted, truncatedby erosion, and than a younger package of sediments was deposited on this erosion surface.

A

Angular Unconformity

37
Q

an erosion surface between two packages of sediment, but the lower package of sediments was not tilted prior to deposition of the upper sediment package.

A

Disconformities

38
Q

are unconformities that separate igneous or metamorphic rocks from overlying sedimentary rocks.

A

Nonconformities

39
Q

Paleozoic era – age of invertebrates

A
Cambrian period
Ordovician period
Silurian period
Devonian period
Carboniferous period
Permian period
40
Q

Mesozoic era – age of dinosaurs & reptiles

A

Triassic period
Jurassic period
Cretaceous period

41
Q

Cenozoic era – age of mammals

A

Tertiary period

Quaternary period