Answer:
Except in the crust, the interior of the Earth cannot be studied by drilling holes to take samples. Instead, scientists map the interior by watching how seismic waves from earthquakes are bent, reflected, sped up, or delayed by the various layers.
Explanation:
Answer: the one spinnin
There is nothing faster then light
l.j
yep
g / 16
T = 2π
angular frequency ω = 2π /T
=
ω₁ /ω₂ =
Putting the values
ω₁ = ω , ω₂ = ω / 4
ω₁ /ω₂ = 4
4 =
g₂ = g / 16
option d is correct.