
AIR test prep

Flashcard
•
Other Sciences
•
6th - 8th Grade
•
Hard
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10 questions
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1.
FLASHCARD QUESTION
Front
What are the two sources of thermal energy in Earth’s interior? Options: solar heater and gravity, combustion and solar heating, gravity and radioactive decay, radioactive decay and combustion
Back
gravity and radioactive decay
2.
FLASHCARD QUESTION
Front
One bar magnet sits on a table, and a rubber band suspends another magnet above it. In the view on the left, the upper magnet is held in place and cannot move. In the view on the right, the upper magnet has been released. What happens to the energies?
Back
Magnetic and gravitational potential energy decreased, and elastic potential energy increased.
3.
FLASHCARD QUESTION
Front
An engineer is collecting data on four different satellites orbiting Earth. The engineer records the satellites’ distances from Earth in kilometers (km) and their forces due to gravity in Newtons (N). Estimate the values for the two missing quantities.
Back
16000, 6000
4.
FLASHCARD QUESTION
Front
Which term is an example of force? Options: Energy, Mass, Weight, Work
Back
Weight
5.
FLASHCARD QUESTION
Front
Instruments located around Earth record seismic wave activity during an earthquake. The epicenter of the earthquake and locations of four instrument stations around Earth are shown. Which stations will record fewer waves than the others?
Back
Station 2 and 3
6.
FLASHCARD QUESTION
Front
Select the one of statements that explain why fewer waves were recorded at some stations: Part of Earth's interior bent some of the waves.
Different materials in earth reflect some of the waves., Some waves are blocked by the water on the Earth's surface.
Weather events near the station can prevent waves from being recorded.
Back
Part of Earth's interior bent some of the waves.
Different materials in earth reflect some of the waves.
7.
FLASHCARD QUESTION
Front
How can scientists tell when the reversals of the magnetic field occurred? Options: by measuring the thickness of the different bands of the oceanic crust, by measuring the distance between the mid-ocean ridge and the ocean flood band, by measuring the amount of minerals that aligned to Earth's magnetic field in the different bands, by measuring the strength of Earth's magnetic field recorded in the solidified magma of the oceanic crust
Back
by measuring the distance between the mid-ocean ridge and the ocean flood band
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