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Minerals Mineral Facts There are about 3000 known minerals on earth. Minerals Mineral Facts There are about 3000 known minerals on earth.

Minerals Mineral Facts There are about 3000 known minerals on earth. - PowerPoint Presentation

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Uploaded On 2018-09-20

Minerals Mineral Facts There are about 3000 known minerals on earth. - PPT Presentation

All rocks are made up of 2 or more of these minerals Minerals are not rocks Silicon and oxygen are the most abundant elements in the crust and in minerals Oxygen is the most abundant element in minerals ID: 672530

mineral minerals easily cleavage minerals mineral cleavage easily scratched fracture quartz scratches glass scratch hardness test properties color internal

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Slide2

MineralsSlide3

Mineral FactsThere are about 3000 known minerals on earth. All rocks are made up of 2 or more of these minerals. Minerals are not rocks!Silicon and oxygen are the most abundant elements in the crust and in minerals

Oxygen is the most abundant element in mineralsSlide4

GoldSlide5

TurquoiseSlide6

QuartzSlide7

SulfurSlide8

MagnetiteSlide9

AzuriteSlide10

DiamondSlide11

How do you identify minerals?By properties/characteristicsProperties stay the same. That’s why we use them.Slide12

Mineral Properties:Color

InorganicNot made from living things or fossilsNaturalNot man madeSolid

Tightly

packed, fixed molecules

Crystal

Repeating patterns

Chemistry

Atomic

structure/chemical/internal structure determines the properties of a mineral

Luster

Pearly, waxy,

earthy, greasy dull

Streak

Color

of powderSlide13

Identifying more Mineral PropertiesHardness scratch test rub minerals against each other or a glass plate,

finger nail, etc.Color-variesStreak (streak test -rub against unglazed tile, powder )Luster (shine, metallic, glassy, earth, pearly, greasy)Density ( amount of matter in a given volume)

Crystal shape

(cubic, right angles, perfect cube)

Cleavage

( splits easily, smoothly along flat surfaces)

Fracture

(does not split evenly)Slide14

DiamondsDiamonds are the hardest mineralsOnly diamonds can scratch diamonds!!A Diamonds internal arrangement of atoms leads to its hardnessSlide15

GemstonesMinerals are cut and polished to make gemstones(jewelry)Includes Amethyst, ruby, emeraldUsually higher up on the MOHS scale(hard)Would you want talc in a ring?Slide16

Scratch Test ExamplesHardness Test Example1 Can be scratched easily with fingernail. talc2 Can be scratched with fingernail, but less easily. gypsum

3 Can just be scratched with a copper penny. calcite4 Can be scratched easily with a knife but will not scratch glass. fluorite5 Can be scratched with a knife with difficulty. apatite6 Cannot be scratched with a knife; barely scratches glass. feldspar7 Scratches glass easily. quartz8 Scratches quartz easily. topaz

9 Scratches topaz. corundum (ruby, sapphire)

10 Scratches topaz and all other minerals. diamondSlide17

Formation of MineralsCrystallization from cooling magmaEvaporationSlide18

How do minerals break?1. CleavageSmooth breakageSlide19

Rock hammer and goggleTo determine cleavage and fracture, you'll need a rock hammer and a safe place to use it on mineralSlide20

Cleavage continued.Cleavage is the way a mineral breaks. Many minerals break along flat planes, or cleavages—some in only one direction (like mica), others in two directions (like feldspar), and some in three directions (like calcite) or more (like fluorite). Some minerals, like quartz, have no cleavage. Cleavage is an important property that results from a mineral's molecular structure, and cleavage is present even when the mineral doesn't form good crystals. Cleavage can also be described as perfect, good or poor.Slide21
Slide22

Moh’s Scale of HardnessSlide23

FractureFracture is breakage that is not flat. The two main kinds of fracture are shell-shaped, as in quartz and uneven. Metallic minerals may have a hackly (jagged) fracture. A mineral may have good cleavage in one or two directions but fracture in another directionSlide24
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Special PropertiesFlorescence-glows under ultra violet light.MagneticElectrical (quartz when pressure is applied)

.Slide26

Internal Arrangement of atomscauses the differences in hardness of different mineralshas geometric patternsis made ofrepeating patternsSlide27

Interior of a mineralThe molecules are used to identify mineralsScientist can see them with a special xray machineThe molecules determine how the mineral will breakSlide28

A microscopic image shows bacteria covered in electrically conductive grains. Bacteria can use minerals in soil as electrical grids, which helps the microbes generate chemicals they need to survive, a new study says.http://news.nationalgeographic.com/news/2012/06/120608-microbes-bacteria-electricity-minerals-chemicals-swap-scienceSlide29

http://tcm.childrensmuseum.org/geomysteries/cube/b2.htmlGreat Website!!Mohs Scale of Hardness pageSlide30