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MA. RACHEL B. ESPINO
Buhatan National High School
Purok Marcos, Buhatan, Sorsogon City
 A mineral is a natural inorganic substances
with a definite chemical composition. It is
found in the earth’s crust and does not come
from living things. It is a naturally formed
solid element or compound in which atoms
and molecules are bound in together in a
definite orderly arrangement to form
crystals. Most of these crystals are too small
to be seen even under a microscope. But
some crystals are big enough to be
identified.
 Minerals are found in rocks. They appear like
grains set firmly in a bed of rock. Some are
dark and others are light in color. A rock may
be composed of only one kind of mineral
such as pure limestone, which is composed of
calcite. Others may have more than one
mineral like granite which has 3 very
common minerals – quartz, feldspar and
mica.
 Minerals are most easily identified by their
physical properties. These are:
1. Hardness
2. Color
3. Streak
4. Luster
5. Cleavage and Fracture
 Hardness is the resistance of a mineral to
scratching or abrasion. To test the hardness
of a mineral sample, scratch it against
another. That which can scratch by the other
is softer.
 Diamond is the hardest known mineral and is
industrially used to cut or bore holes into
glass, stone and other hard metals. Talc is
the softest mineral used especially in making
talcum powder.
 Color is one way of telling
one mineral from
another. It is their usually
most noticeable and
interesting property. But
it is not the most
reliable. The outside
color of the mineral may
have been changed by the
atmosphere; hence, it is
safe to examine the color
of a fresh surface by
breaking it apart.
 A mineral may be translucent like mica,
white or pink like quartz or lead gray like
galena. Hematite is dark red while sulfur is
yellow, while silver, tin and magnesium have
almost the same gray-white color.
MICA QUARTZ GALENA
HEMATITE
SULFUR
SILVER
 Streak refers to the
color of the powder
a rock or mineral
leaves behind when
rubbed on a rough
surface. The streak
test consist of
rubbing the mineral
against a hard
surface.
 However, the color of the streak is not
always the same as the color of the mineral.
For example, the mineral pyrite which has
the same color as gold leaves a greenish-
black streak while gold always leaves a gold
streak.
PYRITE
GOLD
 The mineral hematite may be reddish brown
or brownish black when viewed in solid form
but is always cherry red in powder form, that
is why hematite is also called bloodstone.
 Luster is the appearance of the surface of a
mineral in reflected light. A mineral that can
reflect much light appears very shiny. Metals
have metallic luster like silver and gold.
Nonmetals are dull such as quartz, mica or
asbestos.
 Cleavage and fracture
describe the way a mineral
breaks. Any irregular break
is termed a fracture while
the tendency of a certain
minerals to break along
one or more planes when
put under pressure is
called cleavage. Minerals
split horizontally into thin
sheets. Feldspar splits at
nearly right angles in
different directions.
FELDSPAR COPPER
SULFUR
SALT
 The richness of the Philippines in terms of
mineral resources is being attributed to its
location at the western fringes of so called
Pacific Ring of Fire – a ground found to be
superloaded with mineral deposits. Globally,
we are rankes 5th as most mineralized
country in the world.
 The Philippines is situated along the circum
Pacific Ring of Fire where the processes of
volcanism and plate convergence caused the
deposition of minerals, both metallic and
non-metallic. In fact, the large reserves of
various kind of minerals beneath our ground
has put the country in the world mineral map
as 5th mineral country in the world, 3rd in
gold reserves, 4th in copper and 5th in nickel.
 Around 9 million hectares or 30% of the
country’s total land area of 30 million
hectares are believed to contain important
metallic mineral deposits; while 5 million are
also known to be potential site for
nonmetallic reserves.
 Among our important metallic minerals found
in abundance in various parts of the country
include gold, copper, iron, chromite, nickel,
cobalt and platinum while our non-metallic
resources include sand and gravel,
limestone, marble, clay and other quarry
materials.
 The most prolific copper and gold products
are found in Baguio and Mankayan district
province of Benguet; although the Surigao-
Davao district are also contributing much to
Philippine gold production. Major producers
of nickel are in Palawan and Surigao.
 Science Grade 7 Learners Module
 Integrated Science I Textbook
 Salandanan, Gloria G. Earth Science, Quezon
City: Phoenix Publishing House, 1988.
 http://www.philippinestamps.net/RP2009-
Minerals.htm
 http://www.denr.gov.ph/news-and-
features/latest-news/16-mineral-
resources.html
 http://nap.psa.gov.ph/peenra/results/miner
al/default.asp

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Identifying Minerals by Their Physical Properties

  • 1. MA. RACHEL B. ESPINO Buhatan National High School Purok Marcos, Buhatan, Sorsogon City
  • 2.  A mineral is a natural inorganic substances with a definite chemical composition. It is found in the earth’s crust and does not come from living things. It is a naturally formed solid element or compound in which atoms and molecules are bound in together in a definite orderly arrangement to form crystals. Most of these crystals are too small to be seen even under a microscope. But some crystals are big enough to be identified.
  • 3.  Minerals are found in rocks. They appear like grains set firmly in a bed of rock. Some are dark and others are light in color. A rock may be composed of only one kind of mineral such as pure limestone, which is composed of calcite. Others may have more than one mineral like granite which has 3 very common minerals – quartz, feldspar and mica.
  • 4.
  • 5.  Minerals are most easily identified by their physical properties. These are: 1. Hardness 2. Color 3. Streak 4. Luster 5. Cleavage and Fracture
  • 6.  Hardness is the resistance of a mineral to scratching or abrasion. To test the hardness of a mineral sample, scratch it against another. That which can scratch by the other is softer.
  • 7.  Diamond is the hardest known mineral and is industrially used to cut or bore holes into glass, stone and other hard metals. Talc is the softest mineral used especially in making talcum powder.
  • 8.  Color is one way of telling one mineral from another. It is their usually most noticeable and interesting property. But it is not the most reliable. The outside color of the mineral may have been changed by the atmosphere; hence, it is safe to examine the color of a fresh surface by breaking it apart.
  • 9.  A mineral may be translucent like mica, white or pink like quartz or lead gray like galena. Hematite is dark red while sulfur is yellow, while silver, tin and magnesium have almost the same gray-white color. MICA QUARTZ GALENA HEMATITE SULFUR SILVER
  • 10.  Streak refers to the color of the powder a rock or mineral leaves behind when rubbed on a rough surface. The streak test consist of rubbing the mineral against a hard surface.
  • 11.  However, the color of the streak is not always the same as the color of the mineral. For example, the mineral pyrite which has the same color as gold leaves a greenish- black streak while gold always leaves a gold streak. PYRITE GOLD
  • 12.  The mineral hematite may be reddish brown or brownish black when viewed in solid form but is always cherry red in powder form, that is why hematite is also called bloodstone.
  • 13.  Luster is the appearance of the surface of a mineral in reflected light. A mineral that can reflect much light appears very shiny. Metals have metallic luster like silver and gold. Nonmetals are dull such as quartz, mica or asbestos.
  • 14.  Cleavage and fracture describe the way a mineral breaks. Any irregular break is termed a fracture while the tendency of a certain minerals to break along one or more planes when put under pressure is called cleavage. Minerals split horizontally into thin sheets. Feldspar splits at nearly right angles in different directions.
  • 16.  The richness of the Philippines in terms of mineral resources is being attributed to its location at the western fringes of so called Pacific Ring of Fire – a ground found to be superloaded with mineral deposits. Globally, we are rankes 5th as most mineralized country in the world.
  • 17.
  • 18.  The Philippines is situated along the circum Pacific Ring of Fire where the processes of volcanism and plate convergence caused the deposition of minerals, both metallic and non-metallic. In fact, the large reserves of various kind of minerals beneath our ground has put the country in the world mineral map as 5th mineral country in the world, 3rd in gold reserves, 4th in copper and 5th in nickel.
  • 19.
  • 20.  Around 9 million hectares or 30% of the country’s total land area of 30 million hectares are believed to contain important metallic mineral deposits; while 5 million are also known to be potential site for nonmetallic reserves.
  • 21.  Among our important metallic minerals found in abundance in various parts of the country include gold, copper, iron, chromite, nickel, cobalt and platinum while our non-metallic resources include sand and gravel, limestone, marble, clay and other quarry materials.
  • 22.  The most prolific copper and gold products are found in Baguio and Mankayan district province of Benguet; although the Surigao- Davao district are also contributing much to Philippine gold production. Major producers of nickel are in Palawan and Surigao.
  • 23.
  • 24.
  • 25.
  • 26.
  • 27.  Science Grade 7 Learners Module  Integrated Science I Textbook  Salandanan, Gloria G. Earth Science, Quezon City: Phoenix Publishing House, 1988.  http://www.philippinestamps.net/RP2009- Minerals.htm  http://www.denr.gov.ph/news-and- features/latest-news/16-mineral- resources.html  http://nap.psa.gov.ph/peenra/results/miner al/default.asp

Notas del editor

  1. You can ask for assistance to the Chemistry teacher to further describe the concept of minerals
  2. Answer to Activity 5, LM (Observation: the location of mineral resources in the Philippines is related to the location of volcanoes and active faults and trenches in the Philippines)
  3. Philippine Minerals are presented in the stamp issued by PhilPost last March 25, 2009
  4. Philippine Minerals are presented in the stamp issued by PhilPost last March 25, 2009
  5. Philippine Minerals are presented in the stamp issued by PhilPost last March 25, 2009
  6. Philippine Minerals are presented in the stamp issued by PhilPost last March 25, 2009
  7. Philippine Minerals are presented in the stamp issued by PhilPost last March 25, 2009