M2 Subtopic 5 Flashcards

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1
Q

As sediments accumulate, they form distinct layers, each representing a different period in Earth’s history; are like pages in a book, with each layer telling a different part of Earth’s story

A

Stratification

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2
Q

are like pages in a book, with each layer telling a different part of Earth’s story

A

Stratified Rocks

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3
Q

Two Dating Methods

A

Relative and Absolute Dating

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4
Q

Establishes the sequence of events without determining their exact age. Used to understand the order in which layers and geological events occurred.

A

Relative Dating

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5
Q

In an undisturbed sequence of rock layers, the oldest layers are at the bottom, and the youngest are at the top.
This principle helps geologists identify the relative ages of different layers.

A

Principle of Superposition

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6
Q

Sedimentary layers are originally deposited in a horizontal position.
If layers are found tilted or folded, these changes occurred after deposition.

A

Principle of Original Horizontality

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7
Q

A rock or fault that cuts across other layers is younger than the layers it disrupts.
This principle is crucial for understanding the sequence of events that have affected rock formations.

A

Principle of Cross-Cutting Relationships

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8
Q

Fossils of organisms that lived during a specific, relatively short time frame.
Widely distributed and easily recognizable, making them ideal for correlating the age of rock layers across different regions.

A

Index Fossils

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9
Q

provides a precise numerical age for rocks and fossils.
This method is essential for calibrating the geological time scale and understanding the timing of specific events in Earth’s history.

A

Absolute Dating

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10
Q

measures the decay of radioactive isotopes within minerals to determine the exact age of rocks.
Widely used for dating igneous and metamorphic rocks and is key to determining the ages of ancient geological formations.

A

Radiometric Dating

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11
Q

the time it takes for half of the radioactive isotopes in a sample to decay

A

Half life

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12
Q

specific form of radiometric dating used to date organic materials, such as wood, bones, and shells.
Effective for dating materials up to about 50,000 years old.

A

Carbon Dating

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13
Q

organizes Earth’s history into a series of time intervals.
These subdivisions are based on significant events such as mass extinctions, major climate shifts, and the emergence of new life forms.

A

Geologic Time Scale

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14
Q

Subdivisions of Geologic Time

A

Eons, Eras, Periods, Epochs

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15
Q

The largest time units, encompassing billions of years. (Precambrian and Phanerozoic)

A

Eons

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16
Q

Subdivisions of eons, marked by significant changes in Earth’s biosphere (Paleozoic, Mesozoic, Cenozoic)

A

Eras

17
Q

Smaller time units within eras, often defined by the types of life that dominated (Jurassic, Devonian)

A

Periods

18
Q

The smallest divisions, representing specific changes in climate and life within periods (Holocene, Pleistocene)

A

Epochs

19
Q

Covers over 4 billion years of Earth’s history, including the formation of Earth and the emergence of early life.

A

Precambrian

20
Q

The current eon, starting around 541 million years ago, marked by abundant fossil evidence and the rise of complex life.

A

Phanerozoic

21
Q

Known as the “Age of Fishes,” it saw the development of complex life in the oceans and the colonization of land by plants and animals

A

Paleozoic Era

22
Q

The “Age of Reptiles,” dominated by dinosaurs, and the breakup of the supercontinent Pangaea

A

Mesozoic Era

23
Q

The “Age of Mammals,” characterized by the rise of mammals and, eventually, humans

A

Cenozoic Era

24
Q

Part of the Mesozoic Era, famous for the dominance of dinosaurs and the evolution of birds

A

Jurassic Period

25
Q

The current epoch, which began approximately 11,700 years ago, marked by the development of human civilizations.

A

Holocene Epoch

26
Q

also known as guide fossils, are the remains of organisms that were widespread geographically but lived during a relatively short and specific time period.
These fossils are crucial for identifying and correlating the ages of rock layers across different regions.

A

Marker Fossils

27
Q

Characteristics of an Effective Marker Fossil

A

Widespread Distribution
Short Time Range
Abundant Fossil Record

28
Q

The organism must have lived in various locations around the world, making its fossils common in many areas.

A

Widespread Distribution

29
Q

The species must have existed for a brief period, allowing for precise dating of the layers in which its fossils are found.

A

Short Time Range

30
Q

The organism should have left behind a substantial number of fossils, making it easier to find and identify in different rock layers

A

Abundant Fossil Record

31
Q

Extinct marine arthropods that lived during the Paleozoic Era, particularly useful as marker fossils.
Helps date rock layers from Cambrian to Permian Periods

A

Trilobite

32
Q

Marine mollusks that lived during the Mesozoic Era, particularly during the Jurassic and Cretaceous periods.
Their rapid evolution and wide distribution make them valuable for dating and correlating rock layers from these periods.
Defines Jurassic and Cretaceous periods on Geologic Time Scale

A

Ammonites