3. Introduction
• Rocks itself is both construction materials or part
of engineering structure (cut slope, foundation,
tunnel)
• Rocks are in 3 types – igneous, sedimentary,
metamorphic
• Rocks: solid mass of mineral that occurs naturally as
part of our planet
4. Minerals
• Almost every manufactured product contains
minerals. They are essential for the development of
a modern society
• Rocks are Earth materials made from minerals
• All geological processes on earth such as volcanic
eruption, earthquake, landslide, and erosion
involve earth materials (and minerals are the
building blocks of earth materials)
• Basic knowledge of earth materials is essential to
the understanding of all geological phenomena
5. The big picture
Elements combine to form
the natural compounds
Atoms make up elements
Natural compounds and elements
combine to form minerals.
Minerals make up rocks.
Rocks make up the Earth.
pure chemical substance made
of one type of atom (eg. O2, H2)
Different elements combined
together in a fixed ratio (eg. H2O)
6. Minerals: Building blocks of rocks
• Geological definition of a mineral:
• Naturally occurring
• Inorganic
• Solid
• Ordered internal molecular structure
• Definite chemical composition
• Rocks – consist of one or more minerals
• Eg. Mineral: calcite; rock: limestone
• > 3500 elements identified, only 8 most common
elements forming mineral
7. Element in Earth’s Crust
Element Symbol % of earth’s crust
Oxygen O 49.52
Silicon Si 25.75
Aluminium Al 7.51
Iron Fe 4.70
Calcium Ca 3.39
Sodium Na 2.64
Potassium K 2.40
Magnesium Mg 1.94
Total % 97.85
% of other elements 2.15
pure chemical
substance made
of one type of
atom (eg. O2, H2)
9. Minerals
• Minerals – naturally occurring inorganic solids,
which possess a definite internal structure and
specific chemical composition
• Gold is mineral?
• Synthetic diamonds are minerals?
• Petroleum is mineral?
• Animal bone is mineral?
• Steel is mineral?
10. Mineral Group
• Basically silicate and non-silicate (carbonate)
mineral groups
• Minerals containing silica = silicates minerals
(Olivine Mg2Fe2SiO4 & Orthoclase KAlSi3O8).
• Silicon + oxygen = silica (Quartz SiO2 is pure silica)
• 2 subgroups of silicate mineral:
• Ferromagnesian silicates: (dark colour, > dense).
• Non-ferromagnesian silicates : (light colour, < dense)
• Carbonate mineral (non-silicate) :
• minerals calcite (CaCO3) : limestone
• mineral dolomite CaMg(CO3)2: dolostone
12. How are Minerals Identified?
• By different properties (physical, mechanical,
chemical)
• Colour
• Cleavage
• Lustre
• Hardness
• Specific gravity
• Others
13. Colour
• Generally an unreliable diagnostic property to use
for mineral identification
• Often highly variable for a given mineral due to
slight changes in mineral chemistry
• Impurities of quartz give variety of colour (pink,
purple, milky white)
Same minerals existed in
different colours
14. Cleavage
• In crystalline structure, some bonds are weaker
than others
• Cleavage is the tendency of minerals to break along
planes of weak bonding
• Normally, produces flat, shiny surfaces
• Fracture (mineralogy): tendency of a mineral to
break without a definite shape (mineral not exhibit
cleavage)
19. Lustre
• Lustre – the appearance of light reflected from the
surface of a mineral
• Metallic lustre – minerals that have appearance in
metals
• Nonmetallic lustre – glassy, dull silky
The freshly broken sample of galena displays a
metallic lustre, whereas the sample on the left
is tarnished and has a submetallic lustre.
20. Hardness
• Measure of the resistance of a mineral to abrasion
or stretching
• Determine by rubbing the mineral to identified
against another mineral of known hardness
• Measured on a qualitative scale called Moh's
Hardness Scale.
• Examples: Fingernail = 2.5, Glass = 5.5, Streak Plate
= 6.5, Talc =1, Quartz = 7, Diamond = 10.
22. Specific gravity
• Ratio of the weight of a mineral to the weight of an
equal volume of water
• Eg. 1cm³ of mineral weights 3 times as much as 1cm³ of
water; SG = 3.0
• Average value is approximately 2.7
• SG of pure 24 karat gold = 20