A boundary called Mohorovicic discontinuity
The sun's radiation heats the Earth's surface through a process called solar radiation. This heat causes water to change states by evaporating into water vapor, condensing into clouds, and eventually returning to the surface as precipitation.
body waves
A seismologist specializes in the study of earthquakes and other movements of the Earth's crust. They analyze seismic waves to understand Earth's internal structure and study the causes and effects of seismic activity.
The immediate result of a sudden slippage of rocks within Earth's crust is an earthquake. This movement along faults causes seismic waves to propagate through the Earth, leading to shaking of the ground surface.
Scientists use seismic waves to study Earth's layers by analyzing how they travel through the different materials that make up the Earth. The speed and direction of seismic waves change as they encounter different densities and compositions in the layers of the Earth, providing valuable information about the structure of the planet's interior. By measuring the arrival times and characteristics of seismic waves at different locations, scientists can infer details about the depth, density, and composition of Earth's layers.
A body wave is a seismic wave that travels through Earths interior.
A body wave is a seismic wave that travels through Earths interior.
body waves
body waves
Seismic waves are the vibrations from earthquakes that travel through the earths surface and is measured bye the shaking you feel.
They can do this by how and how quickly seismic waves can move through the mantle.
I will find the answer lator!
Seismic waves that can pass through the centre of the Earth must be capable of travelling through liquids (as the outer core is molten). As such we know that these waves are longitudinal or compression waves.
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.
By the earths atmosphere
Seismic waves are the types of waves that can travel through the Earth and along its surface. There are two main types of seismic waves: body waves (such as primary and secondary waves) that travel through the Earth's interior, and surface waves (such as Love and Rayleigh waves) that travel along the Earth's surface.
They go faster through the inner core than the liquid outer core