20
1. Minerals A. can be liquids B. are organic C. are inorganic D. have no crystal structure 2. is a measure of how easily a mineral is scratched. A. lusterB. cleavage C. hardness D. fracture 3. The color of a minerals powder on an unglazed porcelain tile is . A. lusterB. hardness C. density D. streak 4. When halite breaks it displays . A. fracture B. cleavage C. lusterD. crystal form 5. Halite forms crystals. A. triclinic B. monoclinic C. hexagonal D. cubic

Igneous Rocks

Embed Size (px)

DESCRIPTION

 

Citation preview

Page 1: Igneous Rocks

1. Minerals A. can be liquids B. are organicC. are inorganic D. have no crystal structure

2. is a measure of how easily a mineral is scratched.A. luster B. cleavageC. hardness D. fracture

3. The color of a minerals powder on an unglazed porcelain tile is .A. luster B. hardnessC. density D. streak

4. When halite breaks it displays .A. fracture B. cleavageC. luster D. crystal form

5. Halite forms crystals.A. triclinic B. monoclinicC. hexagonal D. cubic

Page 2: Igneous Rocks

ReviewReviewMinerals Identifying minerals

Page 3: Igneous Rocks

Igneous RocksIgneous RocksRocks formed from melted minerals

Page 4: Igneous Rocks

Igneous RocksIgneous RocksSome have crystalsSlow cooling = “large” crystals –Granite

Page 5: Igneous Rocks

Granite

Page 6: Igneous Rocks

Igneous RocksIgneous RocksFast cooling = “small” crystals - Basalt

Page 7: Igneous Rocks

Basalt

Page 8: Igneous Rocks

Granite Basalt

Page 9: Igneous Rocks

Igneous RocksIgneous RocksExtra fast cooling = no crystals

Page 10: Igneous Rocks

Obsidian: Volcanic, “Glassy”

Page 11: Igneous Rocks

Pumice: Volcanic, “Frothy”Pumice: Volcanic, “Frothy”

Page 12: Igneous Rocks

Krakatoa Island 1883

Page 13: Igneous Rocks
Page 14: Igneous Rocks
Page 15: Igneous Rocks

Pumice: Volcanic, “Frothy”

Page 16: Igneous Rocks
Page 17: Igneous Rocks
Page 18: Igneous Rocks
Page 19: Igneous Rocks

Mt. St. Helens 1980

Page 20: Igneous Rocks