The Earth Structures Retake Test-Part One examines key geological concepts including rock transformation, tectonic movements, and mineral composition. It assesses understanding of Earth's structure and geological processes, crucial for learners in Earth science and geology.
Luster
Streak
Hardness
Color
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Increase in size
Become more complex
Increase in number
Change over time
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Continental Drift
Continental Movement
Continental Shelf
Continental Rise
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Mantle
Crust
Lithosphere
Core
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Mantle
Asthenosphere
Lithosphere
Core
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Both processes involve repeating the experiment.
They are characteristics of a good experiment.
None of the Above
Both A and B
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Two plates slide or glide past each other.
Two plates collide.
Two plates move away from each other.
Two plates move in the same direction.
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Divergent Boundary
Convergent Boundary
Transform Boundary
Uplift
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The weight of the fish.
The day on which the fish was fed.
The type of food given to the fish.
The amount food given to the fish.
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Erosion
Deposition
Weathering
Subsidence
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Naturally occurring
Inorganic or non-living
Have a crystalline structure
All of the Above
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How they are formed
The layers present
Where they are found
The elements they contain
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Sedimentary Rock
Igneous Rock
A Fossil
Metamorphic Rock
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Sedimentary
Igneous
Metamorphic
All the above
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The transfer of energy due to the movement of matter.
The transfer of energy through materials in direct contact.
The transfer of energy as earthquake waves.
The process that breaks down rocks.
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Movement in Earth’s core
Gravity
Convection in the mantle
Volcanic Activity
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They are made up of only one kind of atom.
They melt at very low temperatures.
They are made up of compounds.
They are pure elements.
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The coastlines of the continents fit together like a puzzle.
Fossils of the same species are found on continents on different sides of the Atlantic ocean.
Minerals and Igenous rocks are found on all seven continents.
Matching mountain and rock formation on the coastlines.
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Scientific laws are frequently modified, but scientific theories are rarely changed as new information becomes available.
Scientific theories are based on observation and scientific laws are based on opinions.
Scientific theories require scientific evidence and scientific laws do not.
Scientific theories explain why something happens, and scientific laws describe what happens.
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By their structural features
By their physical properties
By their chemical composition
By their plate tectonics
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Fieldwork
Independent Variable
Scientific Theory
Empirical Evidence
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The transport of rocks and the scratching of the bedrock are both examples of weathering.
The transport of rocks and the scratching of the bedrock are both examples of erosion.
The transport of rocks is an example of weathering, and the scratching of the bedrock is an example of erosion.
The transport of rocks is an example of erosion and the scratching of the bedrock is an example of weathering.
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Metamorphic rock changes into igneous rock
Sedimentary rock changes into igneous rock
Sedimentary rock changes into metamorphic rock
Igneous rock changes into metamorphic rock
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Layer B
Layer C
Layer D
Layer E
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