Rock Deformation: Causes and Types

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  • 0:06 Rocks Are Stressed
  • 1:11 Stages of Rock Deformation
  • 2:21 How Rocks Handle Stress
  • 4:39 Lesson Summary
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Lesson Transcript
Instructor: Sarah Friedl

Sarah has two Master's, one in Zoology and one in GIS, a Bachelor's in Biology, and has taught college level Physical Science and Biology.

In this video lesson, you will learn about how rock can be deformed from stress and the effect this has on the rock. You will identify different types of deformation based on the composition of the rock as well as external stress factors.

Rocks Are Stressed

Did you know that rocks experience stress? While not the same kind of stress that you might experience on a bad day, the stress rocks are subjected to still has quite an impact. Stress causes rocks to deform, meaning the rocks change size or shape.

There are different kinds of stress that rocks experience, and these determine how the rocks deform. Tensional stress is when rock is stretched apart. This is similar to pulling on a string from both ends after the string has already been fully extended. Compressional stress is when rock is pressed together. Here, rocks are squeezed together, like a car caught in the middle of a long pile-up on the highway.

Shear stress is when rock slips in a horizontal direction. With shear stress, the rock is being pulled in opposite directions but on different ends. To understand this, try putting your palms together and then rubbing them back and forth. Now imagine that there is a rock in the middle and you can see how one end goes forward while the other end gets pulled backward.

Stages of Rock Deformation

As rocks are stressed, they go through stages of deformation. At first, the rock is strained enough that its shape or size may change, but the change is reversible. This is the first stage, called elastic deformation. Think of this 'elastic' change like the elastic in your waistband. If you pull it and then let it go, the stretch is reversible because it can go back to its original shape.

Rocks may also become so deformed that the change is not reversible, which we call ductile deformation. Ductile means that something can be changed into a new shape, but once this happens, it stays that way. This is like the copper wiring in your house. Copper is ductile, meaning you can stretch it into long, thin wires. However, once you've made this change, you can't 'unstretch' it, and the same is true for rocks in this stage of deformation.

Finally, if rocks are stressed enough, they fracture, which is when the change is irreversible and the rock breaks. If you fall down hard enough, you may fracture a bone in your body, and rocks experience the same thing when the stress is great enough.

How Rocks Handle Stress

Some people handle stress better than others, and rocks are the same way. So, just like there are various types of rock stress, there are also different responses to the stress for different types of rock material. The ability of a rock to handle stress depends on its elasticity, or the flexibility of the rock.

You might be surprised to learn that rocks are flexible. Under the right conditions, they can 'flow' very slowly. This movement is similar to silly putty. Push on silly putty very hard and it feels like a solid, but pull it apart and it moves like a liquid. Rocks are not quite as fluid as silly putty, but sometimes they can act similarly.

Do you remember from before that ductile materials like copper can be reshaped? The same is true for rocks. Ductile rock is rock that flows in response to stress. These rocks are more flexible than not. Things like clay and mica minerals are ductile materials, which you've experienced if you've ever played with clay to mold it into different shapes.

Alternately, there is also brittle rock, which breaks or fractures in response to stress. This type of rock is less flexible and therefore cracks under pressure more easily than ductile rock. Examples of this type of material are quartz and feldspar minerals, which would break very easily if you dropped them on the ground.

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