Answer the following questions to the best of your ability. You will have only 1 chance to take this test so PLEASE use any resources available to help you - your notes, the internet and DEFINITELY your ESRT!
Your final score will automatically be submitted to your teacher BUT. . . . If you print out your score and See morehand it in, you will automatically receive 5% BONUS added to your score on this test.
PLEASE MAKE SURE YOU HAVE YOUR ESRT (Earth Science Reference Table) BEFORE YOUR BEGIN! Page 10 will be invaluable!
Good Luck!
Layer A
Layer B
Layer C
Layer D
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Layer A
Layer B
Layer C
Layer D
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Crust
Mantle
Inner Core
Outer Core
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Crust
Mantle
Inner Core
Outer Core
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Crust
Mantle
Inner Core
Outer Core
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Crust
Mantle
Inner Core
Outer Core
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Albert Lovera
Albert Einstein
Alfred Wegener
Mrs. Marquart
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A large pancake
The landmasses of today
The super-continent of the past
The super-ocean of the past
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It broke apart over millions of years
It broke apart in a couple of years
It was destroyed by an asteroid
It sunk into the ocean
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South America and Asia
South America and North America
South America and Africa
Europe and Australia
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Obsenterius
Glossopteris
Mesosaurus
Fernatius
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Mesosaurus
Lystrosaurus
Glaciers
Meteors
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Islands in the Bahamas
Islands in the Arctic ocean
Hawaii
Bermuda
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It states that pieces of the Earth's crust are moving very slowly
It states that pieces of the Earth's crust are moving quickly
It states that the Earth's crust is solid and unbroken
It states that pieces of the Earth's crust are shaped like puzzle pieces
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Thicker and heavier
Thicker and lighter
Thinner and heavier
Thinner and lighter
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Mantle
Inner core
Crust
Outer core
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Crust
Inner core
Mantle
Outer core
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It decreases
It stay the same
In increases
No one knows
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In decreases
In increases
It stays the same
It varies
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Mantle
Outer core
Crust
Inner core
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Pangaea
Plate tectonics
Continental drift
Landmass movement
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Earthquakes
A land bridge
The Mesosaurus swimming across the ocean
The movement of tectonic plates
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He did not give any evidence
He did not provide an explanation for the force that moved the continents
He was not well liked by people
His ideas were false
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Continental crust
Oceanic crust
Both continental and oceanic crust
Mesosphere
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Eurasia
Gondwana
Pangaea
Laurasia
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Serveral layers
Solid rock
Hollow space
One layer
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Convergent theory
Plate tectonics
Plate theory
Tectonic theory
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Like a layer cake
Like a jigsaw puzzle
Like a stack of books
Like a model car
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As warm, dense water sinks and flows beneath cold ocean water.
As cold, dense water sinks and flows beneath warm ocean water.
As warm, dense water sinks and flows with other warm ocean water.
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True
False
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Coriolis effect
Salinity
Density current
Surface current
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Wind that blows every now and then
Wind that blows in regular directions
The moon's gravitational pull
Differences in salinity and temperature
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A) Salt was always present in Oceans.
B) Acid rain falls into the Ocean. It contains Salts.
C) Volcanoes let out salt when they erupt.
D) Over millions of years, rains, rivers and streams have washed over rocks carrying away salt into the Ocean
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Inner core, outer core, crust, mantle
Outer core, inner core, mantle, crust
Crust, mantle, outer core, inner core
Crust, mantle, inner core, outer core
Each layer has approximately the same density
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The present climates at locations X and Y are similar
Mesosaurus migrated across the ocean from location X to location Y.
Mesosaurus came into existence on several widely separated continents at different times.
The continents of South America and Africa were joined when Mesosaurus lived.
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crust
mantle
Inner core
outer core
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That the landmasses have always been in the same places
That the landmasses had been joined together, and have since drifted apart
That the continents do not move
That earthquakes have caused the landmasses to move
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Lower saltinity
Higher salinity.
Same amount of salt as water on the surface.
No salt at all.
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Oxygen and silicon
Aluminum and oxygen
Aluminum and iron
iron and nickel
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Warm, cold
Cold, warm
None of the above
All of the above
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A) Sea
B) Land
C) Water
D) Acid rain
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600°C
1000°C
2600°C
3,000°C
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Wind
Convection currents
Ocean currents
Temperature changes
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Oceanic
Continental
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Rocks of the ocean ridges are older than those of the adjacent sea floor.
Rock and fossil correlation can be made where the continents appear to fit together.
Marine fossils can be found at high elevations above sea level on all continents
Great thicknesses of shallow-water sediments are found at interior locations on some continents
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1,500°C
4,500°C
5,000ºC
7,000ºC
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Continental crust
Asthenosphere (plastic mantle)
Stiffer mantle
Outer core
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1000 km
2000 km
5800 km
6400 km
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