Quiz 10 Flashcards

1
Q

Absolute Geologic Age

A

precise dates of many types of geologic events

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2
Q

Relative Geologic Age

A

the age of one event relative to another

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3
Q

Principle of Original Horizontality

A

-sediments are deposited in horizontal or near-horizontal layers
-therefore, non horizontal layers have generally been folded or tilted from their original positions

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4
Q

Principle of Superposition

A

-in any given succession of sedimentary rock layers lying in their original horizontal position the rocks at the bottom of the sequence are older than those lying above

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5
Q

Principle of Original Lateral Continuity

A

-sediments are deposited in layers that continue laterally in all directions until they thin out as a result of nondeposition
-or until they reach the edge of the basin in which they are deposited
-therefore, if you find a layer that abruptly ends, something has cut this layer after it was deposited (faults, dikes, and erosion) can truncate otherwise laterally continuous layers

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6
Q

Principle of Cross-Cutting Relations

A

any geologic feature is younger than any feature that it cuts

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7
Q

Principle of Inclusions

A

an inclusion in a rock is older than the rock containing it

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8
Q

Compressive stress

A

causes shortening and is an important type of stress at convergent tectonic plate boundaries

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9
Q

Tensional stress

A

the principal stress at divergent boundaries, causes stretching

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10
Q

Shear stress

A

causes one side of a body to slide past the other, and is the principal type of stress along transform-fault plate boundaries

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11
Q

Elastic strain

A

temporary; if the stress is removed, the object snaps back to its original shape (think stretched rubber band)

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12
Q

Plastic strain

A

permanent; if the stress is removed, the original size or shape is not restored (bending a piece of soft wire)

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13
Q

Brittle deformation

A

a rock undergoing elastic strain which can suddenly break (a dry stick)

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14
Q

Ductile

A

a rock that undergoes much plastic strain without rupturing (bent wire)

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15
Q

Outcrop

A

visible exposures of bedrock or other geologic formations at the surface of the earth

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16
Q

Contacts

A

surfaces separating adjacent bodies of rock of different types or ages

17
Q

Geologic maps

A

show the distribution of rock units at or very near the surface of the earth

18
Q

Geologic cross sections

A

vertical slices that show how the rocks would appear if they could be viewed on a cliff face

19
Q

Principle of Fossil Succession

A

fossil organisms succeed one another in time in a definite and recognizable order

20
Q

Principle of Fossil Assemblages

A

characteristic groups of fossil organisms also define unique geologic ages

21
Q

Unconformity

A

the erosion of a surface that represents a substantial gap in the geologic record

22
Q

Angular unconformity

A

-an erosion surface separating rocks whose layers are not parallel
-layers above and below meet at an angle
-underlying rocks were folded or tilted and eroded before the overlying layers were deposited

23
Q

Disconformity

A

-an erosion surface or a surface of nondeposition separating rocks whose layers are parallel
-an erosion surface is uneven and cuts layers of underlying rocks

24
Q

Nonconformity

A

-an erosion surface separating sedimentary rocks from older plutonic or massive metamorphic rocks

25
Q

Concordant

A

intrusive contacts parallel to layers in the intruded rock

26
Q

Discordant

A

intrusive contacts cut across layers in the intruded rock

27
Q

Anticlines

A

upward bends, or upfolds, with older rocks in the center

28
Q

Syncline

A

upward bends, or upfolds, with younger rocks in the center

29
Q

Upright fold

A

has a vertical or nearly vertical axial surface

30
Q

Inclined fold

A

has an axial surface that is not vertical or horizontal

31
Q

Overturned

A

beds on opposite limbs dip in the same direction

32
Q

Recumbent fold

A

has an approximately horizontal axial surface