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The epicenter does not recive seismic waves.

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When part of earth's crust breaks what waves pass through the earth?

When part of the Earth's crust breaks, seismic waves pass through the Earth. These waves include primary (P) waves, secondary (S) waves, and surface waves. P waves are the fastest and can travel through both solids and liquids, while S waves are slower and can only travel through solids. Surface waves cause the most damage during an earthquake.


Why don't we call tsunamis ''seismic waves''?

Because a seismic wave is something else. Seismic waves are waves sent through the earth as part of the earthquake itself. A tsunami is an ocean wave generated by water being displaced.


The part of the Earth that stops or slows down seismic waves?

The outer core is the part of the Earth that slows down or stops seismic waves due to the change in density and composition from the mantle. Seismic waves travel faster through solid materials like the mantle and crust, but slow down when they reach the liquid outer core.


How we can be confident that part of the Earth's core is liquid when we cannot see it or directly sample it?

Scientists use seismic waves from earthquakes to study the interior of the Earth. The behavior of these waves shows that a portion of the Earth's core is liquid. Additionally, experiments under extreme pressure and temperature conditions in laboratories support the idea of a liquid outer core based on the properties of iron and other materials under those conditions.


P waves and S waves are two kinds of seismic waves.?

P waves are primary waves that are the fastest seismic waves and can travel through both solids and liquids. S waves are secondary waves that are slower than P waves and can only travel through solids. These waves are used by seismologists to study the interior of the Earth and to detect and locate earthquakes.


What is the study of the waves of movement in the crust of the earth called?

Plate Tectonics


What is a vibration caused by an earthquake called?

seismic waves


3 How do earthquakes help us learn about the interior of the earth?

Earthquakes explain and support tectonic plate theory and show the movements of the plates over time. Fault lines also expose rock layers and allow geologists to study the rocks and the changes in the environment over time.An Earthquake gives out Seismic waves which. There are Primary Waves (P-Wave) and Secondary waves (S-Wave) The Secondary Seismic wave can't travel through liquid so when the sensors detect a wave and sees that some part the S-wave isn't going through a layer of the earth they know that that layer of the earth is Liquid.


What part of earth core is liquid?

Scientists suspect that the outer core is liquid because of its interaction with seismic waves. Actually, only one segment of inner earth is theorized to be liquid. This segment is known as the outer core


Are earthquakes real?

Yes, earthquakes are real. They are caused by the sudden release of energy in the Earth's crust, resulting in seismic waves that shake the ground. Earthquakes can cause significant damage and are a natural part of the Earth's geologic processes.


What is the part of an earthquake that is directly above the focus?

The part of an earthquake that is directly above the focus is called the epicenter. It is the point on the Earth's surface vertically above the earthquake's point of origin, where the seismic waves are most strongly felt.


What part of the earth does not receive direct p waves from a quake?

The outer core of the Earth does not receive direct P waves from a quake due to the difference in density between the outer core and the inner core. P waves can only travel through solid material, so they are refracted when they reach the outer core, creating a shadow zone where they are not detected.