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Earth Structures Study Guide

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Name: ____________________________________________
Date: __________
Period: _____
Earth Structures Study Guide - Comp Sci 2
DUE ON: ____________________
1. Review all vocabulary terms. You may use Quizlet to study the vocabulary terms for this unit. There are 3 study sets:
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Dating Relative-Age & Absolute Age
Earth's Interior & The Rock Cycle
Plate Tectonics
2. Name and describe the 4 layers of Earth (list from outermost layer to innermost layer).
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3. Describe the lithosphere.
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4. What are the 3 types of rocks?
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5. Which crust is more dense? Underline one:
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continental crust
oceanic crust
6. Explain how each rock is formed in the rock cycle. Using the word bank provided, place each word in its correct
location on the diagram. Some terms may be used more than once.
cementation
compaction
cooling
erosion
melting
pressure
weathering
heat
7. How is sediment formed?
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8. Which events of the rock cycle occur on Earth’s surface?
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9. Which events of the rock cycle occur under Earth’s surface?
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10. Using the word bank provided, place each word in its correct location on the diagram of Earth’s layers.
asthenosphere
continental crust
crust
inner core
lithosphere
lower mantle
mantle
oceanic crust
outer core
upper mantle
11. Draw a line to match the plate boundary with the type of stress that occurs at the boundary?
Convergent boundary
Shear
Divergent boundary
Tension
Transform boundary
Compression
12. Explain the Theory of Continental Drift.
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13. At what plate boundaries can volcanoes form?
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14. Describe the plate boundaries that form mountains.
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15. Identify and describe the movement of each plate boundary shown above.
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C. _____________________________________________________________________________________________
16. Explain how a mid-ocean rift is formed.
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17. Explain convection currents in Earth’s mantle and how they move the tectonic plates.
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18. Define deforestation.
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19. Define Urbanization.
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20. Define desertification.
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21. What is erosion?
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22. What are the two ways that scientists determine the age of the earth?
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23. Explain how scientists determine the relative ages of rocks.
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24. What is the law of superposition?
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25. Explain how scientists find the absolute age of the earth?
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This study guide is a grade! When is this study guide due? _________________________
26. Using the word bank provided, place each answer in its correct location on the concept map.
absolute age
correlation
half-life
inclusion
index fossils
isotopes
radioactive decay
relative age
superposition
unconformity
uniformitarianism
27. Which layer(s) experienced erosion?
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28. Which layers are folded?
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29. Where is the fault line?
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Additional Notes:
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Dating Relative-Age & Absolute Age
geologic time scale
a chart representing all of the individual time periods in Earth’s history divided into units
called eons, eras, periods, and epochs
Law of Superposition
the principle that in undisturbed rock layers, the oldest rocks are on the bottom
fault
a fracture line between two blocks of rock
intrusion
igneous rock, formed from magma that cools and solidifies under Earth's surface
extrusion
extrusive rock, formed above the surface of the crust
relative age
the age of rocks and geologic features compared with other rocks and features nearby
radioactive dating
scientists measure the ratio of radioactive isotopes in a mineral to determine how much
time has passed since the mineral formed
uniformitarianism
processes we see acting today acted in the past, and explain what we see in the
geologic record
deforestation
the purposeful clearing of forested land
urbanization
the redistribution of populations from rural (farming or country life) to urban (town and
city) life
desertification
the spread or encroachment of a desert environment into a non desert region
weathering
a natural process that slowly breaks apart or changes rock
correlation
matching rocks and fossils from separate locations
inclusion
a piece of an older rock that becomes part of a new rock
fossil
the preserved remains or evidence of ancient living things
index fossil
a fossil that represents a species that existed on Earth for a short length of time, was
abundant, and inhabited many locations
unconformity
a surface where rock has eroded away, producing a break, or gap, in the rock record
Earth's Interior & The Rock Cycle
sediment
rock and mineral fragments that are loose or suspended in water
magma
molten rock when it is inside Earth
rock
a naturally occurring solid mixture of minerals or grains
erosion
break down exposed rocks by water, wind, or ice
rock cycle
the series of processes that continually change one rock type into another
sedimentary rock
type of rock made of layers that are pressed or cemented together
metamorphic rock
type of rock that forms when a parent rock is squeezed, heated, or exposed to hot fluids
igneous rock
type of rock that forms when magma or lava cools and hardens
Earth's layers
crust, mantle, outer core, inner core
core
the dense metallic center of Earth
crust
rocky, outermost layer of Earth
mantle
thick middle layer in the solid part of Earth
inner core
a dense ball of solid iron crystals
outer core
the liquid metallic center of Earth
lithosphere
rigid layer that includes the crust and uppermost mantle
asthenosphere
the plastic layer within the mantle
convection currents
the cycle of heating, rising, cooling, and sinking of fluids
oceanic crust
crust under oceans, more dense than continental crust
continental crust
crust on land, less dense than oceanic crust
plastic
capable of being molded
Plate Tectonics
tectonic plate
rigid plates that make up Earth's crust
convergent boundary
where two plates move toward each other
divergent boundary
where two plates move apart from each other
transform boundary
where plates slide horizontally past each other
subduction
where one plate slides under another
sea floor spreading
new oceanic crust forms along a mid-ocean ridge and older oceanic crust moves away
from the ridge
Theory of Plate Tectonics
states that Earth’s crust is broken into rigid plates that move slowly over Earth’s surface
Pangaea
a former “supercontinent” that included all the present continents in one large landmass
compression
stress resulting from squeezing
shear
stress resulting from parallel forces acting in opposite directions
tension
stress that pulls something apart
continental drift
the hypothesis that continents are in constant motion on the surface of Earth
subduction zone
the area where one plate slides under another
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