P waves (primary waves) are compressional seismic waves that can travel through both solids and liquids, while S waves (secondary waves) are shear waves that can only move through solids. When an earthquake occurs, P waves arrive at seismic stations before S waves, allowing scientists to analyze their travel times. The absence of S waves in certain areas indicates that the material in those regions is liquid, leading to the conclusion that the outer core of the Earth is liquid, while the presence of both P and S waves in the inner core suggests it is solid. This distinction helps geologists understand the physical state of Earth's core.
body waves
Scientists use seismic waves from earthquakes to study the Earth's interior. By analyzing how these waves travel through the layers of the Earth, they can determine the composition and structure of the planet without physically reaching the core.
Seismic waves
no
Yes, P-waves (primary waves) can travel through the Earth's mantle. P-waves are a type of seismic wave that is capable of propagating through solid, liquid, and gaseous materials. They are the fastest seismic waves and can travel through the mantle, which is the layer between the Earth's crust and core.
Shooting seismic waves into the planet
making inferences based on data from seismic waves.
body waves
body waves
Primary Waves(P-Waves)
By the earths atmosphere
when the crust breacks apart it reveles objects beneth earths iner crust.
the lenght of the waves , strenght of the waves and the duration o the high waves determine how high the waves in a place will be
they can learn about earthquakes before there about to happen and they can learn also about the layers of the earth when the wave goes through the earth.
In physical science, a medium is a substance or material through which a wave can propagate. It can be solid, liquid, or gas, and its properties determine how fast and in what manner the wave travels through it. Examples include air for sound waves, water for ocean waves, and glass for light waves.
earthquake waves travel through the earths crust.
The force and speed of wind will determine how little and big the waves are.