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Chapter 4: Minerals

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Section 1: Properties of Minerals Geologist use a variety of terms to describe fracture Examples: quartz has a shell shaped (conchoidal) fracture. – PowerPoint PPT presentation

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Title: Chapter 4: Minerals


1
Chapter 4 Minerals
  • Section 1 Properties of Minerals

2
Key Concepts
  • What is a mineral?
  • How are minerals identified?

3
What is a Mineral?
  • mineral A naturally occurring, inorganic solid
    that has a crystal structure and a definite
    chemical composition.
  • A substance must have all 5 characteristics to be
    classified as a mineral.

4
5 Characteristics of a Mineral
  • A mineral must be/have
  • Naturally Occurring
  • Inorganic
  • Solid
  • Crystal Structure
  • Definite Chemical Composition

5
Naturally occurring means
  • The substance must be formed by processes that
    occur naturally in the world
  • Example quartz
  • Forms naturally when magma cools and hardens deep
    beneath the Earths surface.

6
NOT naturally occurring
  • Materials such as cement, plastic, brick, steel,
    and glass all come from substances found in
    Earths crust but they are manufactured by people.

7
Inorganic
  • Inorganic the mineral cannot arise from
    materials that were once part of a living thing
  • Ex. Coal is NOT a mineral because it is made up
    the remains of plants and animals

8
Solid
  • A mineral is always solid
  • Has a definite volume and shape.
  • Particles that make up a solid are tightly packed
    together, therefore they move very little
    (compared to the particles of a liquid)

9
Crystal Structure
  • Particles of the mineral line up in a pattern
    that repeats.
  • The repeating pattern of the minerals particles
    forms a solid called a crystal
  • Faces are flats sides of the crystal that meet
    at sharp edges and corners

10
QUICK REVIEW What Is the Difference Between an
Element and a Compound?
  • Element a substance composed of a single kind
    of atom.
  • Ex. Hydrogen
  • Compound Two or more elements combined so that
    the elements no longer have distinct properties
  • Ex. Water H20

11
Definite Chemical Composition
  • Minerals always contain certain elements in
    definite proportions most minerals are compounds
  • example Quartz
  • SiO2
  • One element of silicon, 2 elements of oxygen
  • Compounds have their own unique properties that
    differ from the properties of the elements that
    form it.

12
Definite Chemical Composition
  • Some elements that occur in nature, in pure form,
    that are minerals include
  • Gold (Au), Silver (Ag), Copper (Cu)
  • Listed on the periodic table

13
Identifying Minerals
  • Geologists have identified about 3,800 minerals
  • Each mineral has characteristic properties that
    can be used to identify it.
  • Some properties can be determined by looking at
    it, some properties require testing.

14
Identifying Properties
  • Color
  • Streak
  • Luster
  • Density
  • Hardness
  • Crystal Systems
  • Cleavage and fracture
  • Special Properties

15
Identifying Property- Color
  • An easily observed physical property.
  • Color alone is not enough to make an
    identification.
  • Ex. Gold, pyrite and chalcopyrite gold color
  • Only a few minerals can be identified using color
    only.
  • Ex. Malachite- always green, azurite always
    blue.

16
Identifying Property - Streak
  • The streak of a mineral is the color of its
    powder
  • The streak color and the mineral color are often
    different
  • To test rub a mineral against an unglazed tile
    (streak plate)

17
Identifying Property - Luster
  • Luster used to describe how a mineral reflects
    light from its surface.
  • Minerals containing metals are often shiny.
  • Other terms to describe luster - Earthy, waxy,
    and pearly.

18
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19
Identifying Property - Density
  • Each mineral has a characteristic Density.
  • Density the mass in a given space or mass per
    unit volume.
  • Density mass (g)
  • volume (cm3)
  • Displacement the volume of the displaced water
    equals the volume of the sample

20
Calculating Density
- Properties of Minerals
  • To calculate the density of a mineral, divide the
    mass of the mineral sample by its volume.
  • Density Mass/Volume
  • For example, if a sample of olivine has a mass of
    237 g and a volume of 72 cm3, then the density is
  • 237 g/72 cm3 3.3 g/cm3

21
Stop and Think
  • Take a few minutes to work through the following
    problem with a partner.

22
Practice Problem
  • A sample of calcite has a mass of 324 g and a
    volume of 120 cm3. What is its density?

23
Answer
  • 324 g 120 cm3 2.7 g/cm3

24
Stop and Think
  • Take a few minutes to work through the following
    problem with a partner.

25
Mineral Density
- Properties of Minerals
  • Predicting
  • A piece of pyrite has a volume of 40 cm3. What
    is its mass?

26
Mineral Density
200 g
27
Stop and Think
  • Take a few minutes to work through the following
    problem with a partner.

28
Analyzing Data
  1. What is the mass of sample B? What is the volume
    of sample B?
  2. What is the density of Sample B?
  3. What is the mass of Sample C? What is the
    volume of Sample C?
  4. What is the density of Sample C?
  5. Compare the density of Sample B to that of Sample
    C?

29
Answers
  • 1) 50g and 10cm3
  • 2) 5g/cm3
  • 3) 100g and 20cm3
  • 4) 5g/cm3
  • 5) the density of samples B and C is the same.

30
Identifying Property - Hardness
  • Friedrich Mohs An Austrian mineral expert.
  • In 1812 invented a test to describe the hardness
    of minerals.
  • Called the Mohs hardness scale
  • This scale ranks minerals from softest to hardest
  • A scratch test is used, a mineral can scratch any
    mineral softer than itself, but can be scratched
    by any mineral that is harder.

31
Identifying Property - Hardness
32
Identifying Property Crystal Systems
  • The crystals of each mineral grow atom by atom to
    form the minerals crystal structure.
  • Geologists classify these structures into 6
    groups based on the number and angle of the
    crystal faces.
  • These groups are called crystal systems.
  • Example- Halite crystals are cubic. Halite
    crystals have 6 square faces that meet at right
    angles forming a perfect cube.

33
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34
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35
- Properties of Minerals
Identifying Property Crystal Systems
36
Crystal systems cleavage and fracture
  • Cleavage a property of a mineral that causes it
    to split easily along flat surfaces.
  • Determined by the arrangement of atoms in its
    crystals.
  • The arrangement of the atoms in the mineral
    causes the crystal to break apart more easily in
    one direction than another.
  • Example- Mica separates easily in only one
    direction, forming flat sheets. Feldspar is
    another mineral that has cleavage.

37
Cleavage
38
Crystal Systems cleavage and fracture
  • Fracture describes how a mineral looks when it
    breaks apart in an irregular way.
  • Most minerals do not split apart evenly.

39
  • Geologist use a variety of terms to describe
    fracture
  • Examples quartz has a shell shaped (conchoidal)
    fracture. When it breaks, it produces curved,
    shell like surfaces that look like chipped glass.
  • Pure metals like copper and iron form jagged
    points - hackly (jagged) fracture.
  • soft minerals that crumble - earthy fracture
  • Minerals that form rough, irregular surfaces -
    uneven fracture

40
Conchoidal Fracture
  • Smooth and curved (called clam shell too)

Quartz (SiO2 , Silicon dioxide )
41
Subconchoidal Fracture
  • Subconchoidal Smooth and but not curved

Andalusite (Al2 SiO5, Aluminum Silicate )
42
Uneven Fracture
  • Common Type

Anhydrite (CaSO4, Calcium Sulfate )
43
Jagged Fracture
  • Sharp points in edges that catch on the finger
    when rubbed across

Copper (Cu, Elemental Copper )
44
Splintery Fracture
  • Fibrous or finely needle shaped minerals and have
    a relatively stronger structure in one direction
    than the other two.

Serpentine (Mg,Fe)3Si2O5(OH)4, Magnesium Iron
Silicate Hydroxide Splintery
Kyanite (Al2 SiO5, Aluminum Silicate Non-fibrous
45
Earthy Fracture
  • Produces a texture similar to broken children's
    clay

Limonite (A mixture of hydrated iron oxides)
46
Identifying Properties Special Properties
  • Some minerals can be identified by special
    physical properties.
  • Examples
  • Magnetism
  • Occurs naturally in a few minerals Magnetite
  • Fluorescence (glows under ultraviolet light)
  • Scheelite
  • Reactivity reacts chemically to acids
  • Aragonite and calcite
  • Optical properties bends light to produce
    double image
  • Calcite
  • Radioactivity the process that occurs when a
    nucleus decays and emits alpha, beta or gamma
    radiation.

47
Special Properties
  • Fluorescence minerals that glow in ultraviolet
    light

Scheelite (CaWO4, Calcium Tungstate )
Under ultraviolet
48
Special Properties
  • Magnetism Acts like a magnet

Magnetite (Fe3O4, Iron Oxide )
49
Special Properties
  • Electrical

Quartz (SiO2 , Silicon dioxide)
50
Special Properties
  • Radioactive

Uraninite (UO2 , Uranium Oxide)
51
Special Properties
  • Reactivity to
  • acids

Calcite (CaCO3, Calcium Carbonate )
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