Geological Time: Lesson 1 Review
Question 1
Principle of Superposition
Principle of Uniformitarianism
Principle of Lateral Continuity
Principle of Original Horizontality
Question 2
Earth's history is shaped by catastrophic events.
Geological processes today are similar to those in the past.
Earth's surface remains unchanged over time.
The age of rocks can be determined by their position in the rock layers.
Question 3
By comparing the age of rocks to other rocks nearby.
By studying the composition of rocks.
By analyzing the fossils found in the rocks.
By measuring the radioactive decay of rocks.
Question 4
At the top
In the middle
At the bottom
Throughout the layers
Question 5
Erosion
Deposition
Tectonic activity
Weathering
Question 6
It helps determine the relative ages of rock layers.
It explains how fossils are formed.
It shows how rocks are eroded over time.
It helps identify the boundaries of different rock formations.
Question 7
Older
Younger
Unrelated
Fossilized
Question 8
Pieces of one rock found within another indicate the inclusion is younger.
Pieces of one rock found within another indicate the inclusion is older.
The age of rocks can be determined by their color.
The age of rocks can be determined by their size.
Question 9
Preserved remains and evidence of ancient life
Ancient artifacts left by humans
Rock formations found in caves
Natural minerals formed over time
Question 10
By providing information about ancient climates
By showing the progression from simple to complex organisms
By explaining the formation of rock layers
By revealing the age of the Earth
Question 11
The temperature of the water
The depth of the water
The presence of other organisms
The salinity of the water
Question 12
By providing information about the climate
By showing the types of plants and animals present
By indicating the presence of water
By revealing the location of ancient cities
Question 13
Ancient mountains
Ancient forests
Ancient seafloors
Ancient deserts
Question 14
By analyzing the size of the fossils
By studying the composition of the fossils
By comparing the fossils to modern organisms
By measuring the radioactive decay of the fossils
Question 15
Warmer climate in the past
Colder climate in the past
No change in climate over time
Tropical climate in the past
Question 16
1 million years
10 million years
100 million years
1 billion years
Question 17
Principle of Superposition
Principle of Uniformitarianism
Principle of Lateral Continuity
Principle of Original Horizontality
Question 18
It helps determine the absolute age of rocks.
It helps determine the order of geologic events.
It helps identify the types of fossils present.
It helps determine the climate at the time of rock formation.
Question 19
By revealing the age of the Earth
By showing the progression of life forms
By indicating changes in biodiversity
By preserving ancient organisms
Question 20
The history of Earth's climate
The age of the Earth
The types of organisms that lived in the past
The composition of ancient oceans
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