Geologic Time Flashcards

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1
Q

means that the forces and processes that we observe today have been at work for a very long time. This means that the forces that keep on changing Earth have been working for very long periods of time since the beginning of Earth’s history.

A

uniformitarianism

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2
Q

a Scottish geologist, proposed the principle of uniformitarianism

A

James Hutton

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3
Q

james hutton quote

A

“the present is the key to the past”

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4
Q

relative dating is determined by

A

stratified rocks
fossils

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5
Q

absolute dating is measured by

A

radioactive dating
fossils

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6
Q

A method of showing the sequence of events; that is, which happened first, next, and so on. For example, the rocks beneath a volcano were formed much ahead of the volcano, which means that a volcano is younger than the rocks beneath it.

A

relative dating

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7
Q

science that deals with the characteristics of layered rocks and how these rocks are used to trace Earth’s history

A

stratigraphy

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8
Q

formed over time by wind, rain and glacial formations. These rocks may be formed by folding and tilting, faulting, and volcanic intrusions.

A

stratified rocks

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9
Q

studied the relative positions of sediments in sedimentary rocks.

A

nicolas steno

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10
Q

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

A

law of superposition

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11
Q

states that sediments are deposited in flat layers. Thus, if the rock still maintains its horizontal layers, it means that it is not yet disturbed and still has its original horizontality.

A

Principle of Original Horizontality

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12
Q

states that when a fault cuts through rock layers, or when magma intrudes other rocks and crystallizes, we can assume that the fault or intrusion is younger than the rocks affected.

A

Principle of Cross-Cutting Relationships

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13
Q

Inclusions are rocks contained within other rocks. Rocks containing inclusions are younger than the inclusions they contain.

A

inclusions principle

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14
Q

rock layers that formed without interruption.

A

conformable

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15
Q

a layer of rock that was deformed or eroded before another layer was deposited, resulting in rock layers that are mismatched.

A

uncomformity

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16
Q

younger sediments rest upon the eroded surface of tilted or folded older rocks.

A

angular uncomformity

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17
Q

contact between younger and older beds is marked by a visible, irregular or uneven erosional surface.

A

disconformity

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18
Q

beds above and below the unconformity are parallel and no erosional surface is evident; but can be recognized based on the gap in the rock record.

A

paraconformity

19
Q

develops between sedimentary rock and older igneous or metamorphic rock that has been exposed to erosion.

A

nonconformity

20
Q

is establishing the equivalence of rocks of similar age in different areas.

A

correlation

21
Q

a system of chronological dating that relates rock strata to time.

A

geologic time scale

22
Q

is the science that deals with the study of fossils.

A

paleontology

23
Q

are the remains or traces of prehistoric life. They are important components of sediment and sedimentary rocks.

A

fossil

24
Q

Some remains of organisms—such as teeth, bones, and shells—may not have been altered, or may have changed hardly at all over time.

A

unaltered remains

25
Q

The remains of an organism are likely to be changed over time.

A

altered remains

26
Q

are the actual remains that did not change through time like teeth, bones, and shells of animals.

A

true form fossil

27
Q

or fossils that turned into stone were formed when all or parts of organisms were replaced by minerals.

A

petrified fossil

28
Q

preserve the form and shape of organisms. Molds are formed when organisms buried in sediments decay or dissolve. When minerals are deposited within the molds, casts can be formed.

A

molds and casts

29
Q

result from a process undergone by leaves and delicate animal forms, through which they are covered with fine sediments.

A

carbonized fossil

30
Q

is the hardened resin of ancient trees where insectsare preserved.

A

amber/preserved

31
Q

states that the fossils of organisms succeed one another in a specific and well-established order, and that any geologic time or period can be recognized by the kind of fossil present.

A

Principle of Fossil Succession

32
Q

The principle of fossil succession was formulated by

A

william smith

33
Q

are fossils of organisms that lived only for a short period of time and are found in most places on the planet.

A

index fossil

34
Q

A methods, sometimes called numerical dating, gives rocks an actual date or date range in number of years.

A

absolute dating

35
Q

are atoms of the same element having the same number of protons but with different numbers of neutrons in their nuclei.

A

isotopes

36
Q

the forces among the particles that makeup the nucleus are balanced.

A

stable

37
Q

these forces are unbalanced; if the nucleus has an excess of either neutrons or protons.

A

unstable

38
Q

is the spontaneous decay of certain unstable atomic nuclei.

A

radioactivity

39
Q

is the amount of time necessary for one-half of the nuclei in a sample to decay to a stable isotope.

A

half life

40
Q

is a type of radioactive disintegration in which some unstable atomic nuclei dissipate excess energy by spontaneously ejecting an alpha particle.

A

alpha emission

41
Q

occurs when the ratio of neutrons to protons in the nucleus is too high. An excess neutron transforms into a proton and an electron. The proton stays in the nucleus and the electron is ejected energetically

A

beta emission

42
Q

occurs when there are too many protons in the nucleus, and there isn’t enough energy to emit a positron.

A

electron capture

43
Q

is the procedure of calculating the absolute ages of rocks and minerals that contain radioactive isotopes.

A

radiometric dating

44
Q

is the method for determining age by comparing the amount of carbon-14 to the amount of carbon-12 in a sample.

A

radiocarbon dating