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12 Cards in this Set

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  • Back
  • 3rd side (hint)
The youngest rocks on the ocean floor are located __________.
a. near continents
b. at mid-ocean ridges
c. far from mid-ocean ridges
d. near Asia
b. at mid-ocean ridges
The crust and upper mantle make up Earth's __________.
a. lithosphere
b. asthenosphere
c. core
d. continents
a. lithosphere
Scientists have observed that the plates move at rates ranging from 1 cm to 12 cm per __________.
a. century
b. decade
c. day
d. year
d. year
Plates of the lithosphere float on the __________.
a. crust
b. asthenosphere
c. core
d.atmosphere
b. asthenosphere
The result of plate movement can be seen at __________.
a. abyssal plains
b. ocean margins
c. plate centers
d. plate boundaries
d. plate boundaries
The __________ are mountains formed by the collision of the Indo-Australian Plate and the Eurasian Plate.
a. Alps
b. Rockies
c. Himalaya
d. Appalachians
c. Himalaya
The presence of the same __________ on several continents supports the hypothesis of continental drift.
a. fossils
b. rocks
c. neither a nor b
d. both a and b
d. both a and b
The hypothesis that continents have slowly moved to their current locations is called __________.
a. continental drift
b. continental slope
c. magnetic pole
d. convection
a. continental drift
Plates move apart at __________ boundaries.
a. convergent
b. stable
c. divergent
d. transform
c. divergent
The alignment of iron minerals in rocks when they are formed reflects the fact that Earth's __________ has reversed itself several times in the past.
a. magnetic field
b. core
c. asthenosphere
d. gravity
a. magnetic field
A lack of explanation for continental drift prevented many scientists from accepting that a single supercontinent called __________ once existed.
a. Glomar
b. Glossopteris
c. Pangaea
d. Wegener
c. Pangaea
The Glomar Challenger provided support for the theory of plate tectonics by providing __________.
a. high-altitude photos of existing continents
b. samples of plant life from mid-ocean ridges
c. samples of older rock found far from mid-ocean ridges
d. direct measurements of the movement of continents
c. samples of older rock found far from mid-ocean ridges