Download presentation
Presentation is loading. Please wait.
Published byBrianne Cummings Modified over 8 years ago
1
Ch 5- Minerals
2
Minerals Ch 5, p. 103 QOD- What is a mineral?
3
Question set- #1-10 today. Show me when you finish 1-10 and then keep in notebook. REMEMBER: LAB TOMORROW! –Missing contracts –Shoes & Lab Safety Rules
4
Sep 14 QOD- What are the seven physical properties used to identify minerals? 1.Review of Identifying Metals Lab 2.Video Clip- Minerals 3.Notes & Questions- ch 5 minerals 4.Keep the questions in your notebook 5.Test 4 – 5 Wednesday
6
Sep23 Earth Systems Test- chapters 4 & 5 is Thursday! Today- –Ch 5 notes Tomorrow- –Last day to turn in mineral projects Wednesday: Crystal Growing-! –Bring 1 pound (2 cups) sugar –Wear close toed shoes Thursday- test ch 4-5
7
Is it a Mineral? Is it inorganic? Does it occur naturally? Is it a crystalline solid? Consistent chemical composition? Must answer yes to all 4 questions for it to be a mineral
8
10 Most common minerals Quartz Calcite Orthoclase Dolomite Plagioclase Halite Muscovite Gypsum Biotite Ferromagnesian minerals These make up 90% of Earth’s mass
9
Mineral Groups Silicates –96% of Earth’s crust –Contains Si (silicon) and O(oxygen) quartz –Can have other elements also –Feldspar – Orthoclase if K (potassium), Plagioclase if Na (sodium) or Ca (calcium) –Ferromagnesian minerals – rich in Fe (iron)
10
Orthoclase - LorenzenitePlagioclase - Albite Ferromagnesian - Olivine
11
Mineral GroupsMineral Groups Nonsilicate Minerals –Do not contain Si and O Can contain one or the other, but not both –Six groups Carbonates Native elements Halides Oxides Sulfates Sulfides
12
Carbonate - Calcite Halide - Halite Native Elements - Gold Oxides - Hematite Sulfates - Gypsum Sulfides - Galena
13
Crystalline Structure Crystal – atoms, ions, or molecules are arranged in a regular, repeating pattern Silicate crystal structure –Silicon – oxygen tetrahedron –1 Si with 4 O’s around it (illustrated in the book) –Basic building block of silicates –Can be connected 6 different ways
14
Silicate Tetrahedron
15
Crystalline Structure Nonsilicate crystals –Diverse chemical composition leads to variety of crystal structures –Cubes, hexagonal prisms… –Crystal structure influences physical properties Native elements are dense due to compact crystal structure
16
Physical Properties of Minerals Mineralogist –Examine, analyze, and classify minerals Result from chemical composition and crystal structure Can be useful in identifying minerals
17
Physical Properties 1)Color Not reliable for ID purposes (subjective)Not reliable for ID purposes (subjective) Small amount of impurities can affect colorSmall amount of impurities can affect color Weathered surfaces may hide colorWeathered surfaces may hide color Only look at fresh surfacesOnly look at fresh surfaces
18
Color
19
Physical Properties 2)Streak Color of mineral in powder formColor of mineral in powder form Streak plate – unglazed ceramic tileStreak plate – unglazed ceramic tile Streak color may differ from mineral colorStreak color may differ from mineral color Metallic minerals – darker streakMetallic minerals – darker streak Nonmetallic minerals – lighter streakNonmetallic minerals – lighter streak
20
Streak
21
Physical Properties 3)Luster Light reflected from mineral’s surface Metallic luster – shiny surface Nonmetallic luster Glassy Waxy Pearly Brilliant Dull / Earthy
22
Metallic Luster
23
Glassy Luster Quartz
24
Waxy Luster Variscite
25
Pearly Luster Talc
26
Brilliant Luster Diamond
27
Dull / Earthy Luster Psilomelane
28
Physical Properties 4)Cleavage / Fracture –Cleavage Splitting along specific lines of weakness Forms smooth, flat surfaces –Fracture Break unevenly into pieces Forms curved, irregular surfaces Conchoidal fractures – curved surface
29
Cleavage - Calcite
30
Fracture Conchoidal
31
Fracture Irregular
32
Physical Properties 5)Hardness Ability to resist scratching Mohs Hardness Scale Scale of 1 to 10 1 = Talc10 = Diamond Glass is about a 5
33
Mohs Hardness Scale
34
Physical Properties 6)Crystal Shape –6 Basic shapes –Certain minerals always form crystals with the same shape 7)Density –Ratio of mass to volume –Can help identify minerals
35
Crystal Shapes
36
Physical Properties Fluorescence and phosphorescence Chatoyancy and asterism Double refraction Magnetism Radioactivity
37
Diamond fluorescence with ultraviolet light Phosphorescence – over time on a watch face
38
ChatoyancyAsterism
39
Double Refraction
40
Crystal Growing Lab- Wedn. Bring 1 pound (2 cups) sugar Wear close toed shoes
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.