igneous rocks

14
Igneous Rocks “Liquid Hot Magma!”

Upload: mandek

Post on 24-Feb-2016

22 views

Category:

Documents


0 download

DESCRIPTION

Igneous Rocks. “Liquid Hot Magma!”. Igneous Rocks. Rocks formed from cooling of lava or magma Lava-Melted rock erupted from volcanoes and deposited on the earth’s surface. Cools quickly. Magma-Melted rock that sits inside the earth in a magma chamber. Cools slowly. Magma Chamber. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Igneous Rocks

Igneous Rocks

“Liquid Hot Magma!”

Page 2: Igneous Rocks

Igneous Rocks

• Rocks formed from cooling of lava or magma• Lava-Melted rock erupted from volcanoes and

deposited on the earth’s surface. Cools quickly.• Magma-Melted rock that sits inside the earth in a

magma chamber. Cools slowly.

Magma Chamber

Page 3: Igneous Rocks

Types of Igneous Rocks

• 2 major types: Intrusive and Extrusive• Intrusive igneous rocks cool and harden inside

the earth. • Extrusive igneous rocks cool and harden on

the earth’s surface or outside the earth.

Page 4: Igneous Rocks

Intrusive Igneous Rocks• Form when magma cools

before reaching the surface. – Cool very slowly– Intrusive igneous rocks have

large, interlocking crystals because they cooled slowly inside the earth.

– Examples are Granite, Gabbro, Diorite, and Unakite (Virginia’s State Rock!)

Unakite

Granite

Page 5: Igneous Rocks

Extrusive Igneous Rocks• Form when lava erupts and

hardens on the surface. – Cool very quickly– Extrusive igneous rocks have

fine (small) to no crystal grains at all.

– A rock with no visible grains is called a volcanic glass (examples are pumice and obsidian).

– Examples are Obsidian, Pumice, Scoria, Basalt, Tuff, Porphyry (cools inside then erupts), Rhyolite, Andesite.

Rhyolite

Obsidian

Page 6: Igneous Rocks

Texture of Igneous Rocks

• Grain Size (Glassy, Fine, Medium, Coarse)• Grain Shape (Irregular, Angular)• Sorting:

– Glassy: Looks like glass (Obsidian, Pumice)– Aphanitic: Can’t see crystals (Scoria, Tuff)– Porphyritic: Large crystals in fine matrix (Porphyry)– Phaneritic: Medium to Large interlocking crystals

(Granite, Diorite, Gabbro)

Page 7: Igneous Rocks

TexturesGlassy

Aphanitic

Phaneritic

Porphyritic

Page 8: Igneous Rocks

Vesicles

• Vesicles are holes found ONLY in Igneous rocks.

• Formed from trapped gasses when lava erupts• Examples: Scoria, Pumice, Basalt (sometimes)

Page 9: Igneous Rocks

Tectonic Plate Boundaries

• Places where tectonic plates converge, diverge, or slip past each other.

Page 10: Igneous Rocks

Igneous Rocks form at Convergent Boundaries

• Ocean-Continent Convergent Boundary.

• Forms volcanoes like those in Washington State.

Page 11: Igneous Rocks

Igneous Rocks form at Divergent Boundaries

• Divergent Boundary or Spreading Ridge

• Forms volcanoes like those that make up Iceland and the mid-Atlantic Ridge.

Page 12: Igneous Rocks

Mid-Atlantic Ridge

Page 13: Igneous Rocks

Igneous Rocks Form at Hot Spots

• A hot spot is where magma rises to the surface in the middle of a plate and not a plate boundary.

• Forms volcanoes like those in Hawaii or Yellowstone.

Page 14: Igneous Rocks

Hot Spots

Hawaii Yellowstone