L5.2 FAULTS AND FOLDS Flashcards

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1
Q

It is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks.

A

Stratigraphy

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2
Q

He presented four basic principles that govern the way that sedimentary rocks are deposited and layered.

A

Nicholas Steno

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3
Q

These are the four basic principles that govern the way that sedimentary rocks are deposited and layered.

A

Steno’s Principles of Stratigraphy

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4
Q

When did Nicholas Steno present his four basic principles?

A

17th Century

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5
Q

STENO’S PRINCIPLES OF STRATIGRAPHY

This law states that younger layers of rock sit atop older layers.

A

Law of Superposition

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6
Q

STENO’S PRINCIPLES OF STRATIGRAPHY

This law states that layers of sedimentary rock are originally deposited flat.

A

Law of Original Horizontality

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7
Q

STENO’S PRINCIPLES OF STRATIGRAPHY

This law states that rock layers A and B must be older than the intrusion (C) that disturbs them.

A

Law of Cross-Cutting Relationships

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8
Q

The Law of Cross-Cutting Relationships is later reinforced by who?

A

James Hutton

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9
Q

STENO’S PRINCIPLES OF STRATIGRAPHY

This law states that layers of rock are continuous until they encounter other solid bodies that block their deposition or until they are acted upon by agents that appeared after deposition took place.

A

Law of Lateral Continuity

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10
Q

These are surfaces within rock sequences that represent gaps in the geologic record, due to periods of erosion or non-deposition, meaning some rock layers are missing, representing a “break” in time.

A

Unconformities

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11
Q

TYPES OF UNCONFORMITIES

These are between parallel layers of sedimentary rock. The rock layers on both sides of this unconformity are generally horizontal and have similar orientations.

A

Disconformity

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12
Q

TYPES OF UNCONFORMITIES

These are horizontally deposited sedimentary rock layers that are uplifted, tilted, or folded, eroded, and then covered by new, horizontally deposited layers

A

Angular unconformity

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13
Q

TYPES OF UNCONFORMITIES

An unconformity between younger sedimentary rocks and older igneous or metamorphic rocks.

A

Nonconformity

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