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What is a mineral?Mineral- a naturally occurring, inorganic, solid that has a specific crystal structure and chemical composition.1)Naturally occurring- made by the earth
1)Mineral/ quartz, sulfur, diamond, gold, silver2)Not a mineral- coal, brick, glass, steel
2)Inorganic- made of nonliving material3)Specific Chemical Composition- the elements that
make the minerals have a definite chemical formula.4)Crystal Structure- the pattern that the particles form
over and over again creating the shape of the mineral
Characteristics to classify minerals:
1.Color2.Streak- the powder of the minerals3.Luster- the way a mineral shines4.Density-heaviness5.Hardness- scratch glass, scratch steel, can scrape with fingernails...6.Breaks-
Cleavage
Color
Sulfur Amethyst Quartz
Orthoclase Feldspar Rose Quartz
Streak- the powder of the minerals.Streak is determined by scraping the mineral on
a streak plate and observing the color left on the plate.
Luster- the way a mineral shines or reflects light.
Types of lusters to select from:
Metallitic luster-(graphite) Glassy luster-(quartz)
Waxy, pearly, greasy(talc)
Dull luster (kaoloinite)
Density- how heavy the mineral
Galena- extremely heavy mineral
Hardness- if the mineral can scratch things or be scratched.
Test using Mohs Hardness Scale
How the mineral Breaks- a minerals breaks in two ways:
1. Cleavage- when a mineral splits into a pattern because of the arrangement of the atoms.
2. Fracture- the minerals breaks in no specific or irregular way.
Mica- breaks in thin sheets
Calcite-squared edges
Halite is cubic
Rose quartz Hematite Olivine
Other PropertiesSome minerals have other unique
characteristics that determine the name.
Sulfur smells like rotten eggs
Magnetite is magnetic Halite tastes salty
Florescence- glows under UV lightsFranklin County NJ has the most Florescent mineral
mined collection in the world!!!!
Rocks
What is the difference between rocks and
minerals?Rocks are made up of mixtures of minerals and other materials.
-Example: Granite is made up of...
QuartzHornblend
Orthoclase Feldspar
Igneous RocksRocks that are formed from magma (melted rock under the earth’s surface) or lava (melted rock on the earth’s
surface).Two Types of Igneous Rock
Intrusiveformed inside the
earth(magma)
Extrusiveformed on the earth (lava)
Granite
Gabbro
Obsidian
Scoria
Pumice
Texture and Crystals of rocks of Igneous Rocks
A. Texture- the size of the grains that make up the rock
B. Crystals- depends on how fast the rocks cooledVolcanic (from lava)- shot from a volcano,
cool to quickly for crystals to formFrom Magma- magma cools slowly allows
the crystallized minerals to form
Coarse Grain
(large grains)
Fine Grain (small grains, like sand)
Granite Basalt
No Crystals- cooled too quickly for crystals to form
Obsidian
Three Types of Sedimentary Rocks:A. Clastic- formed from pieces/fragments of rocks being
squeezed together.
Examples: Sandstone
Conglomerate
B. Organic- made from remains of plants and/or animals.
Limestone Shale
C. Chemical- formed from minerals dissolving in water and the forms into crystals.
Limestone Geodes
Sedimentary RocksRocks that are formed through a series of
processes: erosion, deposition, compaction and cementation.
Erosion- particles carried away by wind or water.
Deposition- particles placed in an area.
Compaction- particles squeezed under pressure.
Cementation- particles are glued together
Metamorphic RocksRocks that change under the Earth’s surface
from heat and pressure.
Characteristics of metamorphic rocks:
Foliated-layers Nonfoliated- no layers
Gneiss Marble
Rock Cycle- a series of processes on the earth’s surface and under the surface that slowly change rocks from
one type to another.