2. The two groups of
minerals .
• The most common
classification of minerals
is based on chemical
composition.
• Minerals are divided into
two groups based on their
chemical composition.
• These groups are the
silicate minerals and the
nonsilicate minerals.
3. http://www.youtube.com/watc
h?v=a335mLdMsZM
What’s Silicate
minerals?
• Minerals that contain a
combination with two
elements are called
Silicate minerals.
• Silicate minerals make
up more than 90% of the
crust.
• The rest of the crust is
made out of nonsilicate.
4. The common silicate
minerals .
Quartz = is the basic building block of minerals
Feldspar = minerals are the main component of
most rock on the earth surface.
Mica = minerals separate easily into sheets when
they break.
5. How do silicate form?
The silicate minerals make up the great majority
of rocks. Silicate is a chemical term for the
group of a single atom of silicon surrounded by
four atoms of oxygen.
Most silicate minerals are formed when molten
rock cools at either the earths surface, or deep
underground.
6. Nonsilicate minerals.
Non-silicates are
minerals that do not
include the silicon-
oxygen units
characteristic of silicates.
They may contain oxygen,
but not in combination
with silicon
7. Nonsilicate minerals.
Some minerals do not contain a
combination of Silicon and
Oxygen, as silicate minerals do.
This group of minerals, called
nonsilicates, are found in only
8% of the Earth's crust.
Nonsilicate minerals include
very valuable resources to
humans, such as the precious
metals gold, silver, and
platinum, useful metals like iron,
aluminium and lead, and the
precious gems diamond and
ruby.
8. Why nonsilicate is so
important?
Nonsilicate minerals are not
nearly as common as silicate
minerals, they are a big part
of our everyday life.
Since these minerals are so
important to humans, we
need to use them carefully.
Many of these minerals can
be reused or recycled into
new products.