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EARTH
MATERIALS AND
RESOURCES
“We are part of the
earth, and it is part of us
… What befalls the earth
befalls all the sons of the
earth.” – Chief Seattle,
1852
N
E
S
W
OBJECTIVES:
 Compare and contrast minerals from rocks
 Identify common rock-forming minerals based on their physical and chemical
properties
 Discuss the processes that bring about the rock cycle
 Classify rocks into igneous, sedimentary and metamorphic types
MINERALS AND ROCKS
MINERALS
• Naturally occurring
• Inorganic substance
• Stable crystalline structure and
characteristics
• Definite composition and physical
properties
• A mineral has a
definite chemical
composition.
• Amethyst has a
chemical formula of
SiO2.
• A mineral is solid.
Essential
Characteristics
of minerals
1. Luster
2. Cleavage
3. Color
4. Magnetism
5. Hardness
6. Fracture
7. Crystal Habit
8. Streak
LUSTER
Refers to the general
appearance of a mineral
surface in reflected light
CLEAVAGE
Refers to the property of
minerals to break along
definite plane surfaces
COLOR
Refers to the color of a
freshly broken surface
of a mineral
MAGNETISM
Refers to the property
of being attracted to or
repelled by a magnet
HARDNESS
Refers to resistance to
abrasion or scratching
based on the Moh’s scale
FRACTURE
Refers to the property of
minerals to break irregularly
when they do not yield to
cleavage or parting surfaces.
CRYSTAL HABIT
Refers to the visible
shape exhibited by the
minerals
STREAK
Refers to the color of the finely
formed powder produced by
rubbing the mineral against a
steak plate or unglazed
porcelain tile
Crystal Systems
1. Cubic
2. Tetragonal
3. Hexagonal
4. Trigonal
5. Orthorhombic
6. Monoclinic
7. Triclinic
Cubic
Three equal axes at
right angles
Tetragonal
Three axes at right
angles, one unequal
hexagonal
Three equal axes at 120
degrees, a fourth at right
angels with sixfold
symmetry
Trigonal
As hexagonal, but with
threefold symmetry
Orthorhombic
Three unequal axes at
right angles
Monoclinic
Two axes at right
angles, a third not.
Triclinic
Three axes: none at
right angles
Classes of
Minerals
1. Native Elements Class
2. Carbonate Class
3. Halides Class
4. Oxides Class
5. Phosphate Class
6. Silicates Class
7. Sulfates Class
8. Sulfides Class
Native Class
Minerals composed of
metals, their alloys, and
non metals
Carbonate
Class
Minerals composed of
carbonates, nitrates,
and borates
Halides
Class
Minerals composed of
anions of halogens (Cl,
F, Br, I)
Oxides Class
Minerals containing
oxides and hydroxides
Phosphate
Class
Minerals containing
phosphates, arsenates,
vanadates, antimonates
Silicates
Class
Minerals composed of
silicate tetrahedron
Sulfates
Class
Minerals composed of sulfates,
sulfides, chromates,
molybdates, selenates,
selenites, tellurites, and
tungstates
Sulfides
Class
Minerals composed of
sulfides, selenides,
tellurides, arsenides,
antimonides, bismuthides,
and sulfosalts
ROCKS
• Dry solid part of the earth’s surface
• Any large piece that sticks up out
of the ground or the sea
• Mineral matter of variable
composition, consolidated or
unconsolidated, assembled in
masses of considerable quantities
in nature, as by the action of heat
or water
Types of Rocks
1. Igneous Rocks
2. Sedimentary Rocks
3. Metamorphic Rocks
Igneous
Rocks
Rocks of magmatic
origin with either coarse
grains or fine grains
Granite, basalt,
obsidian, andesite,
porphyry, diorite
Types of
Igneous Rocks
Intrusive Igneous Rocks
- Form below the surface by
slow cooling from large
crystals
Extrusive Igneous Rocks
– Form at or near the
surface by rapid cooling
from fine crystals
Sedimentary
Rocks
Rocks formed from the
sedimentation and
compaction of particles from
other rocks; usually layered
Sandstone,
conglomerate, shale
Metamorphic
Rocks
Rocks formed from other types
of rocks that have been
subjected to intense
temperature and pressure
through million of years
Granite gneiss, biotite
schist
ROCK CYCLE
• The rock cycle is a basic concept in
geology that describes transitions
through geologic time among the
three main rock types: sedimentary,
metamorphic, and igneous.
Each rock type is altered when it is
forced out of its equilibrium
conditions
ROCK CYCLE
Rocks go
through a
process of
transformatio
n from one
type to
another
depending
upon the
physicochemi
cal forces to
which they
are
subjected.
Rock-forming
Minerals
1. Quartz
2. Feldspar
3. Mica
4. Pyroxene
5. Amphibole
6. Olivine
Quartz
Most abundant mineral on
earth’s crust; composed
of silicon dioxide
Feldspar
Most common rock-
forming mineral
Mica
Common rock-forming
mineral
Found in granitic
pegmatite
Pyroxene
Common rock-forming
mineral with varying
composition
Amphibole
Form crystals that are
typically long and
prismatic
Olivine
Commonly contains
magnesium and iron
silicate minerals

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Minerals and Rocks

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  28. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  29. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  30. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  31. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  32. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  33. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  34. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  35. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  36. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  37. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  38. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.
  39. You can use this type of slide for text, images, shapes and tables to help add information in a different way. Duplicate this slide to add additional images of important location in your visit.