Geological Faults: Definition, Causes & Types

An error occurred trying to load this video.

Try refreshing the page, or contact customer support.

Coming up next: The Processes of Mountain Building

You're on a roll. Keep up the good work!

Take Quiz Watch Next Lesson
Your next lesson will play in 10 seconds
  • 0:07 What Are Faults?
  • 1:02 What Causes Faults?
  • 2:14 Types of Faults
  • 4:19 Lesson Summary
Add to Add to Add to

Want to watch this again later?

Log in or sign up to add this lesson to a Custom Course.

Login or Sign up

Create an account to start this course today
Try it free for 5 days!
Create An Account

Recommended Lessons and Courses for You

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 identify different faults and the types of stress that cause them. You will also see examples of the effects these faults have on the landscape.

What Are Faults?

The surface of Earth is like a giant puzzle, and all the pieces that make up this puzzle are called tectonic plates. Although these giant rock puzzle pieces fit together very nicely, they don't stay in place because they are floating on the layer below us, the mantle. This layer is like the consistency of silly putty - sort of like a liquid and yet sort of solid, too.

The plates float around on the mantle like ice floats on a pond. The movement of the plates is incredibly slow, but since the plates are so big, when they bump into and rub against each other, we get massive events like volcanoes and earthquakes. And along these plate boundaries, we find faults. Faults are cracks in the earth's crust where movement occurs on at least one side. So, in order for a crack in the ground to be a fault, one side or the other has to move, but sometimes both sides move, too!

What Causes Faults?

Faults are classified by how they move, and there are three main types of stress that cause movement along faults. The stress occurs because, as mentioned before, the plates fit together really well, but also float around on the mantle and rub against each other.

Tensional stress is when slabs of rock are pulled apart. Imagine stretching a rope out all the way and then continuing to pull on it from both ends. You're putting tension on the rope because it's being pulled in opposite directions. The same is true for tensional stress in rocks.

Compressional stress is when slabs of rock are pushed together. They are literally being compressed into one another. This is like when two cars crash into each other - they're compressed into smaller, crumpled versions of what they were before.

Shear stress is when slabs of rock slide past each other horizontally in opposite directions. The rocks are not smashed into each other or pulled apart, but their edges slide along each other with a lot of friction. This is like when you rub your hands together to warm them up. One hand goes forward and the other goes backward, rubbing against each other.

Types of Faults

The type of fault we get depends on the type of stress that caused it, which also tells us about how the fault moves. Faults have two sides: the hanging wall and the footwall. These terms were coined by miners because you can stand with your feet on the footwall and hang a lamp on the hanging wall on the opposite side. And the reverse situation would be impossible!

Tensional stress, meaning rocks pulling apart from each other, creates a normal fault. With normal faults, the hanging wall and footwall are pulled apart from each other, and the hanging wall drops down relative to the footwall. Most of the area just west of the Rocky Mountains is affected by normal faults: places like southern Oregon, southwestern Idaho, eastern California, western Utah and the entire state of Nevada.

Compressional stress, meaning rocks pushing into each other, creates a reverse fault. In this type of fault, the hanging wall and footwall are pushed together, and the hanging wall moves upward along the fault relative to the footwall. This is literally the 'reverse' of a normal fault. The Rocky Mountains, the Canadian Rockies and the Appalachian Mountains are all examples of the types of features created by reverse faults.

To unlock this lesson you must be a Study.com Member.
Create your account

Register for a free trial

Are you a student or a teacher?
I am a teacher

Unlock Your Education

See for yourself why 30 million people use Study.com

Become a Study.com member and start learning now.
Become a Member  Back

Earning College Credit

Did you know… We have over 95 college courses that prepare you to earn credit by exam that is accepted by over 2,000 colleges and universities. You can test out of the first two years of college and save thousands off your degree. Anyone can earn credit-by-exam regardless of age or education level.

To learn more, visit our Earning Credit Page

Transferring credit to the school of your choice

Not sure what college you want to attend yet? Study.com has thousands of articles about every imaginable degree, area of study and career path that can help you find the school that's right for you.

Create an account to start this course today
Try it free for 5 days!
Create An Account