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What are the three types of stress in plates?

The three types of stress in plates are tensile stress (stretching), compressive stress (compressing), and shear stress (sliding or tearing). These stresses can cause deformation or failure in the material if they exceed its strength.


Where in Seattle can I get grief counseling on a sliding scale fee?

You can try contacting Low Fee Counseling Services at Seattle University or the Seattle Counseling Service which offers sliding scale fees for grief counseling. Additionally, you can check with community health centers like Neighborcare Health or mental health organizations for more resources.


What is the Cause and Effect of something?

The cause is the reason something happens, while the effect is the result of that cause. Cause and effect are linked in that the cause triggers an action or event that leads to the effect. Identifying the cause and effect relationship helps in understanding how events are connected and predicting outcomes.


What is cause ang effect?

Cause and effect is a relationship between events or things, where one event (the cause) leads to the occurrence of another event (the effect). The cause is what makes something happen, while the effect is the result of that cause. Understanding cause and effect helps in analyzing relationships and predicting outcomes in various situations.


Give you an 10 example of cause and effect?

cause_joel kick the balleffect_the ball go near joel's placeSome one smoked all their life (cause).So they got lung cancer(effect).Cause: I punched my friend.Effect: hes not my friend anymore.

Related Questions

Do earthquakes cause sliding plates?

If you mean tetonic plates, then no, sliding tetonic plates cause earthquakes.


Sliding plates cause?

ha


What do sliding plates release that causes earthquakes?

Sliding plates release tension and energy to cause earthquakes.


Why is this movement often described as horizontal sliding?

The movement is described as horizontal sliding because the two tectonic plates are moving past each other horizontally along a fault line. This sliding motion can cause earthquakes as the plates interact and build up pressure along the fault line.


If two geologic plates are sliding past each other they are at what boundary?

Transform boundary is when the plates are sliding past each other: ↑ ↓; Divergent is when plates are sliding away from each other: ← →; and convergent is when plates are sliding towards each other: → ←. Those are the three main plate boundaries.


What layer are the continents and tectonic plates sliding on?

Continents and tectonic plates are sliding on the asthenosphere, which is a ductile layer of the Earth's mantle below the lithosphere. The asthenosphere allows for the movement of tectonic plates due to its semi-fluid properties.


What are underground plates called?

Underground plates are called tectonic plates. These plates are large pieces of the Earth's lithosphere that move and interact with each other, causing phenomena such as earthquakes and volcanic eruptions.


What can be caused by slipping sliding and colliding of the tectonic plates?

Slipping, sliding, and colliding of tectonic plates can cause earthquakes, volcanic eruptions, and the formation of mountain ranges. These movements can also lead to the creation of new landforms, such as rift valleys and trenches, and can impact the distribution of resources and habitats on Earth.


What layer are the plates sliding on?

The worlds tectonic plates slide on the earths mantle.


What layer are the continents sliding plates?

The outer crust.


What volcanoes can cause?

Volcanoes can cause various natural disasters, including eruptions, pyroclastic flows, ash fall, lava flows, lahars (mudflows), and gas emissions. These events can lead to loss of life, property destruction, and environmental impacts.


What layer of the Earth makes up the tectonic plates and what layer are the continents sliding on?

The continents of the Earth are sliding through the asthenosphere. This is the viscous part of the mantle on which the plates of the lithosphere sit.