Download presentation
Presentation is loading. Please wait.
1
Rocks Vs. Minerals Many colors Many crystal shapes Many ingredients
Made of many compounds Mostly one color Repeat same crystal shape All the same stuff- made of one compound
2
Non-mineral rocks? Coal- made of compacted plant material
Limestone- organic calcium carbonate from shells Coquina- made of cemented shells Amber- hardened plant resin
3
Characteristics of Minerals
4
Mineral Characteristics
Naturally occurring Inorganic Solid Crystalline (has a repeating arrangement of atoms) Specific chemical composition
5
Naturally Occurring Minerals are made by processes that occur in or on Earth. Mineral are NOT man made
6
Formed by Evaporation Salt does this
7
Formed by Cooling Magma
You could compare this to poured sugar
8
Formed by Precipitation
Geodes Stalactites and Stalagmites Rock candy
9
Inorganic Not organic Organic substances are made by living creatures and include proteins, carbohydrates, and oils We will talk about exceptions to this later.
10
Crystalline Structure
Crystal - a solid in which the atoms are arranged in a regular repeating pattern.
11
Crystalline Structures
12
Chemical Composition 98.5% of Earth’s crust is made of: oxygen silicon
aluminum iron calcium sodium potassium magnesium
13
Families of Minerals Silicates- biggest group, makes up 90% of all igneous rock minerals. Over 50% of Earths Crust is made of Silicon and Oxygen. Other mineral families Oxides, halides, carbonates, sulfides, sulfates, nature elements
14
Chemical Composition All minerals have a specific chemical composition
silver=only silver atoms diamonds=only carbon atoms halite = salt = NaCl Quartz = SiO2
15
Most Rocks are made of Minerals!!!!!
16
Non-mineral rocks? Coal- made of compacted plant material
Limestone- organic calcium carbonate from shells Coquina- made of cemented shells Amber- hardened plant resin
17
Physical Properties of Minerals
18
Physical Properties of Minerals
Color Streak Luster Density Cleavage Fracture Hardness
19
Color The color a mineral. This can be misleading.
20
Streak The color of the mineral’s powder.
It is sometimes different from the color of the sample, but most forms of the mineral have the same streak color.
21
Luster Shininess or lack of shininess
22
Density mass per volume
usually reported in “specific gravity,” which is density compared with water
23
Cleavage Tendency to break along planes of weakness in a predictable way
24
Fracture Tendency of a mineral to break randomly, without cleavage. A mineral either has cleavage or fracture. Not both.
25
Hardness what minerals it can scratch and what minerals can scratch it.
26
How it works If the mineral gets scratched, it is softer than the substance you used. If the mineral scratches the substance, it is harder than the substance you used. What it tells you is how strong the bonds are between atoms in the mineral.
27
Mohs Hardness Scale
28
Other characteristics
Smell- sulfide minerals like pyrite smell like rotten eggs Taste- halite is salty Magnetism- magnetite is attracted to a magnet Reacts with acid- limestone fizzes
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.