Relative Dating Flashcards

1
Q

What are the two classifications of Geologic Dating?

A

Absolute and Relative Dating

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2
Q

It means placing rocks in their proper sequence of formation, first, second, third, and so on.

____________ ____________ cannot tell us how long ago something took place, only that it followed one event and preceded another.

A

Relative Dating

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3
Q

What are the six key principles of relative dating?

A

Law of Superposition, Law of Original Horizontality, Law of Lateral Continuity, Law of Cross-Cutting Relationships, Law of Inclusions, Principle of Fossil Succession

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4
Q

The law simply states that in an underformed sequence of sedimentary rocks, each bed is older than the one above it and younger than the one below.

A

Law of Superposition

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5
Q

This law states that layers of sediment are generally deposited in a horizontal position.

A

Law of Original Horizontality

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6
Q

By using the law of original horizontality, any tilting or deformation must have occurred ____________ the deposition.

A

After

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7
Q

This law states that sediments extend laterally in all directions until terminating against the edge of a basin or thinning and pinching out (as in a facies change).

A

Law of Lateral Continuity

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8
Q

This law states that intrusions or faults are younger than the rocks that they intruded or displaced.

A

Law of Cross-Cutting Relationships

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9
Q

This law states that inclusions, or fragments of rock, contained within a rock layer are older than the rock layer itself.

A

Law of Inclusion

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10
Q

This principle states that fossil organisms succeed one another in a definite and determinable order, and therefore any time period can be recognized by its fossil content.

A

Principle of Fossil Succession

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11
Q

These fossils are widespread geographically and are limited to a short span of geologic time.

A

Index Fossils

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12
Q

The presence of ________ _________ provides an important method of matching rocks of the same age rock formations.

A

Index Fossils

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13
Q
A
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14
Q

It is essential to know the direction of younging, that is, the direction through the layers towards younger rocks. The direction of younging can be determined by small-scale features that indicate the way-up of the beds or by using other stratigraphic techniques to determine the order of formation.

A

Deformed Strata

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15
Q

Are those that have been deposited essentially without interruption or no gap in the rock record.

A

Conformable beds/strata

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16
Q

True or False:

There are places on Earth that has a complete set of conformable strata.

A

False, there are no place on Earth that has a complete set of conformable strata.

17
Q

An ______________ represents a long period during which deposition ceased, erosion removed previously formed rocks, and then deposition resumed. In each case, uplift and erosion are followed by subsidence andrenewed sedimentation.

A

Unconformity

18
Q

It is the interval of geologic time not represented by strata.

19
Q

A short interruption in deposition with little or no erosion before resumption of sedimentation.

20
Q

What are the three types of unconformities?

A

Disconformities, Angular Unconformities, and Nonconformity

21
Q

A surface of erosion or non-deposition between younger and older beds that are parallel to each other (may be difficult to recognize; gaps in fossil record can be a clue.)

A

Disconformities

22
Q

An unconformity in which the beds are at an angle to each other (one or both may be tilted, but they are not parallel to each other).

A

Angular Unconformities

23
Q

Are eroded metamorphic or igneous rocks are covered by sedimentary rocks (if intrusion, sed rocks older, if non conformity, ig/met rocks older).

A

Nonconformity