P-Waves.
A seismic body wave that can penetrate the Earth's core is called a P wave (Primary wave). P waves are the fastest seismic waves and they can travel through both solid and liquid layers of the Earth, including the core.
A body earthquake wave that cannot penetrate the Earth's core is called a P-wave. P-waves are the fastest seismic waves and travel through the Earth by compressing and expanding the rock. While they can travel through the Earth's core, their speed and path are altered, causing them to refract instead of penetrate it.
A body wave that doesn't penetrate the Earth's core is a type of seismic wave known as a S wave. S waves, also called secondary waves, are slower than P waves and only travel through solids. They cannot pass through the liquid outer core of the Earth.
A body wave that does not penetrate the Earth's core is a compressional wave or P-wave. P-waves travel through the Earth by compressing and expanding the material they pass through, but they do not travel through the outer core because the outer core is liquid.
The composition of Earth's interior affects earthquakes by influencing the propagation of seismic waves. The different layers, such as the crust, mantle, and core, have varying densities and properties that impact how seismic waves travel through them. This influences the speed, direction, and intensity of seismic waves during an earthquake.
A seismic body wave that can penetrate the Earth's core is called a P wave (Primary wave). P waves are the fastest seismic waves and they can travel through both solid and liquid layers of the Earth, including the core.
s waves
It's called a P-wave
S-Wave. They are not able to travel through the liquid outer core.
Body earthquake waves that can penetrate the Earth's core are known as primary waves, or P-waves. They are the fastest seismic waves and can travel through both solid and liquid materials, including the Earth's inner core.
the outer core is liquid; the inner core is solid
A body earthquake wave that cannot penetrate the Earth's core is called a P-wave. P-waves are the fastest seismic waves and travel through the Earth by compressing and expanding the rock. While they can travel through the Earth's core, their speed and path are altered, causing them to refract instead of penetrate it.
A body wave that doesn't penetrate the Earth's core is a type of seismic wave known as a S wave. S waves, also called secondary waves, are slower than P waves and only travel through solids. They cannot pass through the liquid outer core of the Earth.
They go faster through the inner core than the liquid outer core
Surface waves such as Love waves and Rayleigh waves refract when they encounter the core beneath the Earth's surface. These waves cannot penetrate the core due to the difference in density and composition between the core and the surrounding layers of the Earth.
there are convection currents in the upper core.
p wave