minerals. fracture fracture is the tendency of a mineral to break along curved surfaces without a...

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Minerals

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Page 1: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Minerals

Page 2: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Fracture• Fracture is the tendency of a mineral to

break along curved surfaces without a definite shape. These minerals do not have planes of weakness and break irregularly

Page 3: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

• Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding

Cleavage

Page 4: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Luster

• Luster is a description of the way light interacts with the surface of a crystal. This is how you would tell someone how a mineral looks. It has nothing to do with color or shape, but is related to transparency , surface conditions, crystal habit and index of refraction.

Adamantine - very gemmy crystals Dull - just a non-reflective surface of any kind Earthy - the look of dirt or dried mud Fibrous - the look of fibers Greasy - the look of grease Gumdrop - the look a sucked on hard candy Metallic - the look of metals Pearly - the look of a pearl Pitchy - the look of tar Resinous - the look of resins such as dried glue or chewing gum Silky - the look of silk, similar to fibrous but more compact Submetallic - a poor metallic luster, opaque but reflecting little light Vitreous - the most common luster, it simply means the look of glass Waxy - the look of wax

Vitreous Dull Resinous Adamantine Metallic Silky

Page 5: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Streak• The streak of a mineral is the

color it displays in finely powdered form. The streak maybe completely different from the color of the hand specimen. One of the simpliest ways of determining the strak of a mineral is to rub a specimen across a piece of unglazed porcelain known as a streak plate

Magnetite – Black Streak

Amphibole – grey/green streak

Hematite – red/brown streak

Page 6: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Hardness• HardnessMineralTest• 1 Talc Fingernail (2.5)• 2 Gypsum • 3 Calcite Copper coin (3)• 4 Flourite Knife blade (5.5)• 5 Apatite Glass plate (5.5+)• 6 K-feldspar • 7 Quartz Streak plate (7)• 8 Topaz • 9 Corundum • 10 Diamond 

Page 7: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Texture

• Minerals may be rough, like sand, others may be smooth or chalky. Run your fingers on the rock. What does it feel like.

Pegmatitic Texture – big grains

rough & crystalline texture

Glassy textureVesiculartexture

Page 8: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Specific Gravity• Density or specific gravity

is the ratio of the weight of a substance to the weight of an equal volume of water.

• Density = Weight/Volume

Page 9: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Crystal System• Crystal shape can be helpful in

identification. Most minerals have a crystalline structure and can form perfect crystals if allowed to grow in an unrestricted space. Crystal faces resemble cleavage faces because they are flat and reflect light as a single plane, but they are different from cleavage surfaces because crystals have complex geometric shapes. Perfect crystals are rare and are seldom encountered.

Page 10: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Crystal System 2• CRYSTAL SYSTEM - AXES LENGTHS - AXIAL ANGLES• CUBIC All equal All 90• TETRAGONAL a=b not = c all 90• HEXAGONAL two are equal 2 are 90, one 120• ORTHORHOMBIC all unequal all are 90• MONOCLINIC all unequal two are 90• TRICLINIC all unequal none are 90

Tetragonal

Isometric

Hexagonal Orthorhombic

Monoclinic

Triclinic

Page 11: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Color

Quartz Quartz Quartz Quartz Malachite Pyrite Olivine Limonite

Minerals have the same chemical composition but small variations of the quantity and distribution of some elements will give the same mineral different colors.

Page 12: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of
Page 13: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of
Page 14: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of
Page 15: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

• Mineral Silicate• Rock Luster• Crystal Streak• Gem Hardness• Ruby Moh’s Scale• Diamond Cleavage• Sapphire Fracture• Fossil Ore• Crystal System Texture• Specific Gravity Emerald

Page 16: Minerals. Fracture Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of

Mini-Poster

• Mineral Silicate• Luster• Crystal Streak• Gem Hardness• Moh’s Scale• Cleavage• Fracture• Fossil Ore• Crystal System Texture• Specific Gravity