Chapter 8 Flashcards

1
Q

Age of the Earth

A

prior to 19th century age of Earth was based on religious beliefs: bible says approximately 6000 years, and Chinese and Hindu beliefs say its old beyond comprehension

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

James Hutton

A

“father of geology,” realized geologic processes require vast amounts of time

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Charles Lyell

A

popularized Hutton’s concepts in book Principles of Geology

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Relative Age

A

the order of events or objects from oldest to youngest: original horizonality, superposition, lateral continuity,
cross-cutting relationships, inclusions, uncomformities, and correlation

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Numerical Age

A

the age of events or objects expressed as a number or numbers: determined using radiometric dating

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Radiometric Dating

A

determining how much radioactive decay of a specific element has occurred since a rock formed or an event occurred

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Contacts

A

surfaces separating successive rock layers (beds)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Formations

A

bodies of rock of considerable thickness with recognizable characteristics allowing them to be distinguished from adjacent rock layers

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Original Horizonality

A

beds of sediment deposited in water are initially formed as horizontal or nearly horizontal layers

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Superposition

A

within an undisturbed sequence of sedimentary or volcanic rocks, layers get younger from bottom to top

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Lateral Continuity

A

original horizontal layer extends laterally until it tapers or thins at its edges

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Cross Cutting Relationships

A

a disrupted pattern is older than the cause of the disruption: intrusions and faults are younger than the rocks they cut through

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Baked Contacts

A

contacts between igneous intrusions and surrounding rocks, where surrounding rocks have experienced contact metamorphism

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Inclusions

A

fragments embedded in host rock are older than the host rock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Uncomformity

A

a surface (or contact) that represents a gap in the geologic record

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Disconformity

A

an unconformity in which the contact representing missing rock layers separates beds that are parallel to each other

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

Angular Uncomformity

A

an unconformity in which the contact separates overlying younger layers from eroded tilted or folder layers

18
Q

Nonconformity

A

an unconformity in which an erosional surface on plutonic or metamorphic rock has been covered by younger sedimentary or volcanic rock: plutonic and metamorphic rocks exposed by large amounts of erosion, and it typically represents a large gap in the geologic record

19
Q

Correlation

A

The determination of the time-equivalency of rock units, matching of rocks of similar ages in different regions

20
Q

Physical Continuity

A

physically tracing a continuous exposure of a rock unit

21
Q

Similarity of Rock Types

A

assumes similar sequences of rocks formed at same time, and can be inaccurate if very common rock types are involved

22
Q

Correlation by Fossils

A

fossil species succeed one another through the layers in a predictable order

23
Q

Fossils

A

Evidence of past life, traces or remains of prehistoric life now preserved in rock. They are generally found in sediment or sedimentary rock (rarely in metamorphic and never in igneous rock)

24
Q

Paleontology

A

study of fossils

25
Q

Geologic Importance of Fossils

A

They aid in interpretation of the geologic past, serve as important time indicators, and allow for correlation of rocks from different places

26
Q

William Smith

A

noted that sedimentary strata in widely separated area could be identified and correlated by their distinctive fossil content

27
Q

Fossil Succession

A

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

28
Q

Index Fossil

A

geographically widespread fossil that is limited to a short span of geologic time

29
Q

Geologic Time Scale

A

It is a worldwide relative time scale, it subdivides geologic time based on fossil assemblages, and is divided into eons, eras, periods, and epochs

30
Q

Precambrian

A

represents 87% of geologic time

31
Q

Paleozoic Era

A

“Old Life” notes the appearance of complex life

32
Q

Mesozoic Era

A

“Middle Life” dinosaurs were abundant and the era was ended by mass extinction

33
Q

Cenozoic Era

A

“New Life” mammals and birds are abundant, the most recent ice ages occurred during the Pleistocene Epoch of the Quaternary Period

34
Q

Numerical Dating

A

puts absolute values (e.g., millions of years) on the ages of rocks and geologic time periods: it uses radioactive decay of unstable isotopes, and has only possible since radioactivity was discovered in 1896

35
Q

Nucleus

A

made up of protons, positively charged particles with mass, and neutrons, neutral particles with mass

36
Q

Electrons

A

negatively charged particles that orbit the nucleus

37
Q

Atomic Number

A

Element’s identifying number and is equal to the number of protons

38
Q

Mass number

A

Sum of the number of protons and neutrons

39
Q

Isotope

A

variant of the same parent atom, differs in the number of neutrons, results in a different mass number than parent atom

40
Q

Radioactivity

A

Spontaneous changes (decay) in the structure of atomic nuclei