EarthSci_6.1 Estimating Earth's Age and Principles
Interactive Video
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History
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9th - 12th Grade
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Practice Problem
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Medium
Georgianna Allen
Used 6+ times
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10 questions
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1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the current scientific estimate for the age of Earth?
6,000 years
75,000 years
100 million years
4.54 billion years
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What was Greek philosopher Aristotle's theory regarding the age of the Earth?
It was 6,000 years old.
It was eternal, having existed forever.
It was 100 million years old.
It was created entirely separate from the rest of the universe.
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How did James Ussher, a 17th-century Irish Archbishop, calculate his estimate for the Earth's age?
By examining layers of rock and fossils.
By measuring the cooling rate of a globe.
By analyzing genealogical tables in the Book of Genesis.
By observing the formation of limestone in warm, shallow seas.
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What principle did naturalist Nicolas Steno propose regarding rock layers?
The Earth was created entirely separate from the rest of the universe.
Deeper rock layers are older than shallower ones.
Layers with the same fossils are likely the same age.
The Earth's age can be determined by its cooling rate.
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What experimental method did Georges-Louis Leclerc use to estimate the Earth's age?
Analyzing the rate of erosion of coastlines.
Studying the fossil record in different geological strata.
Measuring the cooling rate of a small globe resembling Earth's composition.
Calculating the accumulation of salt in the oceans.
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
William Thomson's 1862 calculations for Earth's age were based on what principle?
Salt accumulation in oceans
Radioactive decay
Cooling of a fully molten mass
Erosion rates of land materials
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What was a key factor William Thomson failed to acknowledge in his Earth age calculations?
Ocean salinity
Volcanic activity
Radioactive decay and mantle convection
Solar radiation
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