What Are
Minerals?
Can you name some minerals off the top of your head? You
likely came up with things like gold, silver, copper and coal. 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:
- First, all minerals are solid. So, while water may contain
minerals, water itself can't be a mineral because it's liquid.
- Minerals are all naturally formed. This means they
can't be manufactured in a lab. Synthetic gems, like cubic zirconia, are
therefore not minerals.
- 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.
- 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
crystal 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:
- Crystal form
- Hardness (The Mohs scale of
mineral Hardness)
- Fracture or cleavage
- Luster
- Color
- Streak
- 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.
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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.
Luster is how reflective a mineral is. Minerals are usually either
classified as having metallic
luster, which is very shiny or reflective, or non-metallic luster, which is not shiny and is very
dull.
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