A seismic station recorded the P-waves, but no S-waves, from an earthquake because S-waves were
(1) absorbed by Earth’s outer core
(2) transmitted only through liquids
(3) weak and detected only at nearby locations
(4) not produced by this earthquake
(1) absorbed by Earth’s outer core
(2) transmitted only through liquids
(3) weak and detected only at nearby locations
(4) not produced by this earthquake