Turkey, in the earthquake zone It is a country in the middle of nowhere and therefore regularly witnesses major earthquakes. It is very important to understand both the soil and the fault lines below it, as earthquakes have different structures and different effects occur depending on the terrain type.

To understand earthquakes tension and tension Understanding the concepts is very important. Stress is the force applied to deform or break a material. Stress is the deformation a material undergoes due to applied stress. In the case of earthquakes, these two terms are used to describe changes in the Earth’s crust.

The Earth’s crust is actually made up of interlocking plates called plates.

In recent earthquakes, the Arabian plate has moved north. He pressed the Anatolian plate.

The East Anatolian Fault is a “strike-slip” fault line. In other words, blocks of hard rock exert vertical pressure on each other. When a boulder has no footing and collapses, it moves horizontally. This causes an earthquake.

The Earth’s crust is huge, causing it to deform and break, leading to an earthquake. to tectonic forces exposed. When an earthquake occurs, tectonic stress in the Earth’s crust creates a series of shock waves that can damage structures on the surface. The force of these shock waves is applied to the crust before the earthquake. to the amount of stress and the amount of stress experienced during the earthquake. Understanding the interaction between stress and strain is crucial to predicting and preparing for future earthquakes.

How earthquakes occur is also effective on the resulting waves. Earthquakes move in waves.

The first of these waves is the first wave to reach the surface and is measured first by the seismograph. primary is a wave.

Then comes the wave called the secondary wave. When this wave comes in sturdy materials movement begins. Much faster than the first wave.

Next comes the surface wave called the Longitidunal. It’s a small wave, but much more destructive has effect. The effect is particularly greater if alluvium and groundwater are dense.

Last comes the R wave, in which the Earth’s crust is almost located waves in the sea It starts working like

As the plates repel each other, the effect of the plates grows. to that end tension/stress is called. tension at a given moment to earthquakes why is this happening. The amount of stress affects the size of the earthquake.