crust and upper mantle
because it's denser
transform, divergent, convergent
convergent boundary
continental-continental
divergent boundary
convection current
earthquake
transform
surface wave
by oceaning-oceaning convergent boundary
concentrated in narrow zones
triangulation method
the outer core is liquid
seismic waves
p waves are refracted and s waves are absorbed
ocean ridges
ocean ridge
asthenosphere
no
divergent
gondwana
laurasia?