MODULE 4 Flashcards

1
Q

This is the study of fossils.

A

Paleontology is the branch of geology that studies fossils, which are the preserved remains or traces of ancient organisms.

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2
Q

The approximate age of the Earth.

A

The Earth is estimated to be about 4.54 billion years old. This age has been determined through various dating methods, including radiometric dating of meteorites and lunar samples.

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3
Q

It is the other name for trace fossils.

A

Ichnofossils are traces of the activities of ancient organisms, such as footprints, burrows, and feeding marks.

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4
Q

He is referred to as “Father of Modern Geology.”

A

James Hutton

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5
Q

These are preserved remains or traces of organisms.

A

Fossils

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6
Q

It is the point or orbit of a planet farthest from the sun.

A

Aphelion

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7
Q

It states that fault cut through rocks is always younger than the rocks it cuts.

A

Principle of Cross-Cutting Relationships

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8
Q

It is the current period of geologic time, also known as Anthropocene epoch.

A

Holocene

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9
Q

It presents the evidences that land masses move and were once together.

A

Plate Tectonics

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10
Q

It states that sediments will assume a horizontal manner due to gravity and will assume such orientation until lithification or diagenesis preserves it.

A

Principle of Original Horizontality

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11
Q

This era tells the extinction of dinosaurs which gave way to the age of mammals including man.

A

Cretaceous Period

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12
Q

It is a hierarchical set of divisions describing geologic time in which units of time include the Eon, Era, Period, Epoch, and Age.

A

The geologic time scale is a system of chronological dating that divides Earth’s history into a series of time units, from the largest (eons) to the smallest (ages).

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13
Q

It states that layers near the bottom of an undistributed basin are older than the ones above them.

A

Principle of Superposition

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14
Q

It is used to find the absolute age of a sample by comparing the parent isotopes to the daughter isotopes.

A

Radiometric Dating

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15
Q

observed geological processes like erosion, wind, and tides, concluding that these forces, acting over vast periods, shaped the Earth. This led him to believe the planet was much older than the biblical account.

A

Bernard Palissy

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16
Q

used biblical genealogies to calculate the Earth’s creation date as October 26, 4004 BC, 9:00 am (PST). This influenced the theory of catastrophism, which proposed that Earth’s features were shaped by sudden, catastrophic events.

A

James Ussher

17
Q

known as the “Father of Modern Geology,” observed geological processes and their rates of change. He proposed uniformitarianism, suggesting that the same processes shaping the Earth today have been active throughout its history. This led him to conclude that Earth was much older than the biblical estimate of 6000 years.

A

James Hutton

18
Q

built upon Hutton’s uniformitarianism, emphasizing gradualism, the idea that geological changes happen slowly and steadily over long periods. His work solidified the understanding of Earth’s vast age and established the foundation for modern geology.

A

Charles Lyell

19
Q

calculated Earth’s age by studying its cooling rate, assuming it was initially molten. His estimates, ranging from 20 to 100 million years, were significantly younger than modern estimates, but they spurred further research into Earth’s age.

A

Lord Kelvin

20
Q

estimated Earth’s age by studying the rate of salt accumulation in the ocean. He calculated an age of 90 to 100 million years, but his method was flawed due to factors like salt recycling and removal.

A

John Joly

21
Q

discovery of radioactivity revolutionized our understanding of Earth’s age. It provided a new tool for dating rocks and minerals, leading to much more accurate estimates.

A

Henri Becquerel’s

22
Q

pioneered radiometric dating, using the decay of radioactive elements to determine the age of rocks and minerals. This led to the first accurate estimates of Earth’s age, which have been refined over time.

A

Ernest Rutherford and Bertram Boltwood