
Earth History EOG Review
Authored by Katherine Cuffe
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12 questions
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1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
1. What types of elements are useful for dating materials?
nonmetals such as chlorine and oxygen
metals such as zinc and copper
radioactive elements such as carbon-14 and uranium-235
noble gases such as neon and xenon
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
2. Which of the following can help scientists estimate geologic time?
comparing fossils
observing rock sequences
radiometric dating
all of these
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
3. What does the process of absolute dating determine
the age of a rock based on what fossils are in it
the age of a rock based on what layer it is in
the order in which rock layers formed
a numerical value for the age of a rock
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
4. It has been theorized that all of today's continents were once part of a single continent. What scientific evidence is used to support this theory?
Fossils of similar life forms have been found on different continents.
The coastlines of some of today's continents have matching shapes.
Some of the different continents that exist today have similar types of rocks.
all of these
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
5. Scientists find a rock that contains a small fish-like creature. Radioactive dating finds that the age of the rock is between 550-450 million years ago. Use the following geologic time table to determine the most likely period in which the fossil lived.
Devonian
Ordovician
Cambrian
Silurian
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
6. What theory explains the formation and movement of the outer surface of the Earth?
the theory of atmospheric layers
the theory of glacier movement
the theory of plate tectonics
the theory of natural selection
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
7. What is Pangaea?
A mid-ocean ridge than runs from north to south along the Atlantic Ocean's floor.
A species whose fossilized remains in Africa led to the hypothesis of continental drift.
A complex theory that explains the motions of continents and many of Earth's features.
A single, large landmass in which all of Earth's continents were once joined.
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