Q 01/05
A) The lithosphere
B) The inner mantle
C) The outer core
D) The asthenosphere
Answer · why
This rigid outer shell, crust plus upper mantle, rides on the hotter, more ductile asthenosphere beneath.
Q 02/05
A) Three or four
B) Eleven or twelve
C) Twenty or more
D) Seven or eight
Answer · why
The Indo-Australian plate is sometimes split in two, which is why the count wobbles.
Q 03/05
A) Oceanic, continental and mixed
B) Compressive, tensile and shear
C) Convergent, divergent and transform
D) Active, passive and dormant
Answer · why
Where two plates meet decides whether crust is destroyed, created or simply slides past.
Q 04/05
A) About 10 metres
B) About 1 metre
C) About 10 cm
D) About 1 mm
Answer · why
The Mid-Atlantic Ridge spreads at fingernail-growth pace; the Nazca plate races along at hair-growth pace, about 160 mm a year.
Q 05/05
A) Obduction
B) Accretion
C) Subduction
D) Rifting
Answer · why
It shrinks Earth's surface, which is balanced by new crust forming at spreading ridges, a tectonic 'conveyor belt'.
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