The Sands of Time (L13) Flashcards

1
Q

What are the 2 concepts of time used in geology?

A

relative time - based on relative timing of geological events

Absolute time - involves the determination of age in years before present, based on decay of radioactive isotopes

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2
Q

How is relative time organized and structured?

A

earliest event at the bottom of the list and the most recent at the top

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3
Q

What is the principal of original horizontality?

A

an important principle when dealing with layered rocks or “strata”

states that layers of sediment are generally deposited in a horizontal bed

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4
Q

What does it mean when strata are flat and horizontal

A

means it has not been disturbed

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5
Q

what does it mean when strata are deformed and/ot not horizontal?

A

been disturbed by tectonic activity and not in their original state

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6
Q

Law of Superposition

A

states that in an undeformed sequence of sedimentary rocks, YOUNGER strata progressively overlie OLDER strata

basically the youngest rock layer would be at the top of hte stack whereas the oldest rock would be at the bottom

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7
Q

What does it reflect that we can use fossils as markers of time intervals?

A

the useage of fossils as markers of time intervals reflects the fact that evolution is irreversible

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8
Q

what does it mean that organisms can’t de-evolve to an earlier form?

A

means that the range of time a fossil is represented in the rock record is unique to that particular fossil

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9
Q

Index Fossils?

A

fossils that are best suited as indiciators of specific time intervals

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10
Q

what are the 4 things that the best index fossils have?

A

a short time range

well-preserved

easily collected

widely distributed geographically

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11
Q

the Law of Cross-cutting Relationships states?

A

states that a fault or intrusive igneous body must be younger than the rock through which it has cut

fault is younger than the layers

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12
Q

What is an inclusion and what do we know about it?

A

inclusion is a piece of rock that is enclosed within another rock

rock containing the inclusion is YOUNGER than the inclusion itself

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13
Q

Law of Inclusions

A

states that if a rock body (B) contains fragments of another rocky body (A), it must be YOUNGER than the fragments of rock it contains

Rock A must have been there first to provide the fragments

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14
Q

What do inclusions in igneous rock bodies tend to be?

A

tend to be rock fragments dislodged from walls of magma chamber

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15
Q

What do inclusions in sedimentary rocks tend to be?

A

rock fragments eroded from underlying rocks

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16
Q

the rate of sediment deposition is _____ through time

A

not uniform

17
Q

How does a deposition become not uniform?

A

when there are significant pauses in sediment deposition, or in extreme cases, rocks can be removed by erosion

“time” in the form of rock goes missing

18
Q

What happens when deposition resumes after the interruption?

A

a distinct (and often irregular) surface is produced

19
Q

Uncomformity

A

a break in the rock record produced by erosion and/or nondeposition of rock units.

its a surface, not a unit of rock

20
Q

3 types of unconformities

A

Angular unconformity – surface underlain by tilted strata and overlain by flat-lying strata

A disconformity – surface underlain by flat-lying strata and overlain by flat-lying strata

Noncomformity – surface underlain by metamorphic or plutonic igneous rocks and overlain by flat-lying strata

21
Q

What happens when land is uplifted above sea level or if the sea level falls? Why?

A

the exposed land will eventually erode to a flat surface

Because land above sea level tends to wear down while ocean basins tend to be filled up with sediment

22
Q

Where is a good place where you can see all three types of unconformity?

A

Grand Canyon

23
Q

What does the principle of relative time allow us to do?

A

deduce the order in which such events have occured

24
Q

atoms of the same element with differing atomic weights are called

A

isotopes

25
Q

What is the process called where certain isotopes (parent isotopes) will lose particles to form isotopes of new elements (daughter isotopes)

A

radioactive decay

26
Q

Rates of decay are commonly expressed in terms of

A

Half-life

27
Q

Half-life?

A

the time required for half of the atoms in a sample to decay to daughter products

28
Q

How do half-life’s work?

A

it represents the “halving” of the preceding amount of parent isotope

29
Q

How would you date minerals in a clastic sedimentary rock?

A

you would obtain the age the particles came from and NOT the sedimentary rock body itself

30
Q

The “Master Timetable”for the Earth

A

Geologic Time Scale - born from concepts of relative time with emphasis on time slices represented by distinctive fossil forms

31
Q

3 reasons why geologic time scale is important?

A

serves as a framework for the timing of geological events

makes scientific communication more efficient

comprises a hierarchy of time units similar to a regular calendar

32
Q

What are the 3 main time scales focused on in this course?

A

Eon - Largest
Era
Periods

33
Q

What are Earth’s history divided into? (Oldest to Youngest)

A

Hadeon Eon - hellish world
Archean Eon - rocks
Proterozoic Eon - “earlier life”
Phanerozoic Eon - “visible life”

34
Q

What are the 3 eras? (Pahenrozoic Eon focused) Oldest to Youngest

A

Paleozoic (ancient life)
Mesozoic (middle life)
Cenozoic (recent life)

35
Q

What are the order of Periods? Oldest to Youngest

A

Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian, Triassic, Jurassic, Cretaceous, Paleogene, Neogene, Quaternary

36
Q

Where are the names of Periods derived from?

A

“Type” localities
Rock characteristics
Various whim