What Are Minerals? - Types, Properties & Examples

An error occurred trying to load this video.

Try refreshing the page, or contact customer support.

Coming up next: Mineral Consumption: How Developed and Developing Nations Consume Minerals Differently

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

Take Quiz Watch Next Lesson
Your next lesson will play in 10 seconds
  • 0:06 What Are Minerals?
  • 0:27 What Makes a Mineral a…
  • 1:19 Properties of Minerals
  • 4:20 The Importance of Minerals
  • 5:11 Lesson Summary
Save Save Save

Want to watch this again later?

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

Log in or Sign up

Speed Speed

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 lesson, you will learn about minerals and their properties. You will also understand the importance and everyday use of different types of minerals found on Earth.

What Are Minerals?

Can you name some minerals off the top of your head? You likely came up with things like gold, silver and copper. These are all correct, but there are many more minerals on Earth - over 4,000 in fact! To understand what makes a mineral a mineral, we need to understand the basic requirements that categorize them, as well as their properties.

What Makes a Mineral a Mineral?

In order for something to be a mineral, it must first meet four criteria:

  1. First, all minerals are solid. So, while water may contain minerals, water itself can't be a mineral because it's liquid.
  2. Minerals are all naturally formed. This means they can't be manufactured in a lab. Synthetic gems, like cubic zirconia, are therefore not minerals.
  3. All minerals have a unique and specific chemical composition. This is like the DNA of the mineral - it's what makes the mineral different from other minerals.
  4. Lastly, all minerals have a crystalline structure. Minerals are some of the most beautiful substances on Earth, because they are always arranged in an orderly geometric pattern. Minerals of the same type always have the same geometric arrangement of their atoms.

Properties of Minerals

Minerals are classified by their chemical composition and crystalline structure. These two features occur on a microscopic level, but we can see them in other ways because they determine a mineral's observable physical properties. In other words, what appears to us on the outside is determined by what's on the inside.

The seven physical properties of minerals are:

  1. Crystal form
  2. Hardness
  3. Fracture or cleavage
  4. Luster
  5. Color
  6. Streak
  7. Density

Let's see how each one helps identify a mineral.

Crystal form is the outward expression of the orderly arrangement of atoms inside the mineral. What you are seeing is the actual arrangement and structure of the atoms in that mineral. For example, look at some everyday table salt, which is a combination of sodium and chlorine. Normally, what you see is a salt cube, but if you were to break this cube down into smaller parts, it would simply break into smaller and smaller cubes because that is how the atoms are arranged.

Hardness is how resistant a mineral is to scratching, not how easily it breaks. Hardness depends on the bonds within the mineral, so the stronger the bonds, the harder the mineral. Mineral hardness is measured on the Mohs scale of hardness, which compares the hardness of different minerals.

Diamond is considered the hardest mineral, so it's a 10 on the Mohs scale of hardness. Talc has a very weak bond between its atoms, and so it's a 1 on the Mohs scale of hardness. If it helps, you can think of the hardness of talc in relation to the hardness of your fingernail, which is about a 2.5.

Fracture and cleavage describe how a mineral breaks. Some minerals break very nicely along smooth planes, and this is called cleavage. Minerals that break this way do so because their atoms are arranged so that they break apart from each other along these planes. Mica is an example of a mineral that has cleavage. If a mineral fractures, it breaks in uneven ways that are not flat or parallel. Again, these minerals break like this because that's how their atoms are arranged.

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

Register to view this lesson

Are you a student or 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
What teachers are saying about Study.com
Try it risk-free for 30 days

Earning College Credit

Did you know… We have over 200 college courses that prepare you to earn credit by exam that is accepted by over 1,500 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 risk-free for 30 days!
Create an account