stud
bud
Sign up
Log in
Home
Library
Explore
SAT
More
Beier's 8 Plate Tectonics Review #1 Flashcards | StudBud
Explore
/
Beier's 8 Plate Tectonics Review #1
Beier's 8 Plate Tectonics Review #1
25 terms
·
StudBud Administration
·
247 plays
Plate Tectonics Review #middleschool #earthscience #platetectonics
Flashcards
25 cards
F
Practice quiz
P
Host live
L
Questions
25
Answers
1
One of the main pieces of evidence for sea-floor spreading is
magnetic patterns in rocks
fossils
coal beds
earthquakes
2
As you move from the surface of Earth to the inner core, the temperature of Earth's layers
increase
increase at first, then decrease as you go even deeper
stay the same
decrease
3
Old crust is subducted and consumed at what type of plate boundary?
convergent
lithospheric
transform
divergent
4
The best way to find direction of the movement of Earth's crest along the San Andreas fault is
observe erosion on the continental coastline
study Earth's present magnetic field lines
measure gravitational strength along both sides of the fault
match displaced rock types on both sides of the fault
5
The process that creates new ocean floor is called
subduction
continental drift
convection currents
sea-floor spreading
6
The type of boundary where two plates are moving away from one another is known as
transform
divergent
convergent
subduction
7
The movement of tectonic plates is caused by convection cells in the
outer core
lithosphere
upper mantle
lower mantle
8
Long chains of undersea mountains are known as
hot spots
deep ocean trenches
rift valleys
mid-ocean ridges
9
The scientist who first put forth the idea of continental drift was
Alfred Wegener
Harry Hess
Jules Verne
Charles Richter
10
The primary cause of convection currents in Earth's mantle is believed to be
the sinking of Earth's crust
the rotation of Earth on its axis
the frequency of earthquakes
the difference in densities of Earth's materials
11
The type of boundary associated with the rising part of a lower mantle convection cell is
transform boundary
convergent boundary
divergent boundary
subduction boundary
12
The name of the scientist who first put forth the theory of sea-floor spreading is
Harry Hess
Charles Richter
Jules Verne
Alfred Wegener
13
As you move from the surface of Earth to the inner core, the density of the materials of Earth
decreases
increases
stays the same
increases at first, then decreases as you move higher
14
Which statement is NOT evidence that Wegener used to support his idea of continental drift?
Matching coal beds on different continents
Matching plant fossils on different continents
Matching human fossils found on differennt continents
Matching rock layers on different continents
15
The idea that continents move slowly on Earth's surface is known as
continental drift
sea-floor spreading
convection drifting
subduction shifting
16
The type of boundary formed as two lithospheric plates slide past one another is called a
danger zone boundary
divergent boundary
transform boundary
convergent boundary
17
The type of boundary found along the San Andreas Fault is known as
a transform fault boundary
a convergent boundary
an earthquake boundary
scary
18
Rising magma in the mantle may divide the lithosphere above and form a
mountain range
deep-ocean trench
mid-ocean ridge
subduction zone
19
Of the following options, the best way to detect transform faults is by observing
earthquakes
subdution
convection
volcanic eruptions
20
The name given to the ancient super-continent which was made of our current continents is
Pangaea
Laurasia
Gondwanaland
Pandora
21
Divergent boundaries found on land are known as
rift valleys
volcanic island arcs
mid-continent ridges
trenches
22
Mountain ranges are most often formed at what type of boundary?
divergent
convergent
subduction
transform
23
Large pieces of Earth's crust that move over the asthenosphere are known as
metamorphic plates
lithospheric plates
sea-floor plates
crustal plate
24
Earth's magnetic field is generated by powerful electric waves in the
crust
magnetosphere
mantle
core
25
The sinking of one lithospheric plate under another lithospheric plate is known as
sea-floor rifting
sea-floor spreading
subduction
divergence