Title: Igneous Rocks
1Igneous Rocks
2Igneous Rock
- Igneous rocks form when molten rock cools and
solidifies.
3Igneous Rocks
- Molten rock is called magma when it is below the
Earths surface and lava when it is above.
4Igneous Rocks
- Remember
- Rate of cooling affects crystal size
- Fast cooling small crystals
- Slow cooling large crystals
5Crystal size
Magma (below)
when molten rock cools and solidifies
Lava (above)
6Igneous Rock classification
- Igneous rocks are classified two ways
- Where they were formed
- What they are made from (mineral composition)
7Part 1
- Classifying igneous rocks by where they are
formed.
8Igneous Rocks - Classification
- Igneous rocks that form below the Earths surface
are called intrusive igneous rocks (or plutonic).
9Igneous Rocks - classification
- The word plutonic comes from Pluto, the name
for the Roman god of the underworld.
10Igneous Rocks - Classification
- They form when magma enters a pocket or chamber
underground that is relatively cool and
solidifies into crystals as it cools very slowly.
11Intrusive Igneous Rock
- Most intrusive rocks have large, well formed
crystals. The mineral crystals within them are
large enough to see without a microscope.
12Igneous Rocks - Classification
- The more slowly molten rock cools within the
Earth, the larger the igneous rock crystals will
be.
13Crystal size
magma
Intrusive
slowly
Magma (below)
when molten rock cools and solidifies
large
Lava (above)
14Intrusive Igneous Rocks - examples
15Intrusive Igneous Rocks - examples
16Intrusive Igneous Rocks - examples
17Crystal size
magma
Intrusive
slowly
Magma (below)
when molten rock cools and solidifies
large
Lava (above)
Granite, gabbro, diorite
18Extrusive Igneous Rocks
- Extrusive igneous rocks, or volcanic rocks, form
when magma makes its way to Earth's surface. The
molten rock erupts or flows above the surface as
lava, and then cools RAPIDLY forming rock. -
19Extrusive Igneous Rocks
- Most extrusive (volcanic) rocks have small
crystals.
20Extrusive Igneous rocks - examples
21Extrusive Igneous rocks - examples
22Extrusive Igneous rocks - examples
23Lava
Crystal size
Quickly
Small or not visible
Extrusive
Basalt, ryolite, andesite
magma
Intrusive
slowly
Magma (below)
when molten rock cools and solidifies
large
Lava (above)
Granite, gabbro, diorite
24Volcanic Glass
- Pumice, obsidian, and scoria are examples of
volcanic glass.
- These rocks cooled so quickly that few or no
mineral grains formed.
- Most of the atoms in these rocks are not arranged
in orderly patterns, and few crystals are
present.
25Glassy Igneous Rocks
Glassy Igneous Rocks cool so rapidly, that atoms
dont have enough time to get together, bond and
form crystals. To cool this quickly the rocks
MUST be extrusive.
- Pumice (left)
- Scoria (bottom left)
- Obsidian (bottom)
- Note gasses in the lava can cause fine holes
called vesicles as seen in the pumice and scoria.
26Part 2
- Classifying by mineral composition
27Composition Magma types
- A way to further classify these rocks is by the
magma from which they form. An igneous rock can
form from, granitic, andesitic, or basaltic
magma.
28Composition - Properties
- Magma composition determines the physical
chemical properties of an igneous rock
29Lava
Crystal size
Slowly
granitic
Small or not visible
Physical chemical properties
Extrusive
Basalt, ryolite, andesite
andesitic
magma
Intrusive
slowly
Magma (below)
basaltic
when molten rock cools and solidifies
large
Lava (above)
Granite, gabbro, diorite
SiO2 Silicon Fe Iron Mg Magnesium
30Basaltic Igneous Rocks
- They form from magma that is rich in iron (Fe)
and magnesium (Mg) and LOW in silica (SiO2.)
31Basaltic Igneous Rocks
- The presence of iron (Fe) and magnesium (Mg) in
basalt gives basalt its dark color. - Basalt rocks have a high density
32Basaltic Igneous Rocks
- Basaltic lava is fluid and flows freely from
volcanoes in Hawaii, such as Kilauea. - Basalt is the most common rock type in the
Earth's crust (the outer 10 to 50 km). - Makes up the Oceanic Crust
33Lava
Crystal size
Slowly
granitic
Small or not visible
Physical chemical properties
Extrusive
basalt, ryolite, andesite
andesitic
magma
Intrusive
Rich in Fe Mg poor in SiO2
slowly
Magma (below)
basaltic
Dense dark colored
when molten rock cools and solidifies
large
Lava (above)
Ocean floor Hawaii
Granite, gabbro, diorite
34Granitic Rocks
- Granitic igneous rocks are light-colored rocks of
lower density than basaltic rocks.
35Granitic Rocks
- Granitic rocks are coarse-grained
- Granitic magma is thick and stiff, high silica
content, lesser amounts of Fe and Mg.
36Granitic Rocks
- It is the most common rock type on the
continental land masses. - Yosemite Valley in the Sierra Nevada Mtn. range
and Mt. Rushmore are two notable examples of
granitic rocks - Makes up the continental crust
37Lava
High SiO2 Low Fe Mg
Crystal size
Slowly
granitic
Light colored, less dense
Small or not visible
On the continents
Physical chemical properties
Extrusive
basalt, ryolite, andesite
andesitic
magma
Intrusive
Rich in Fe Mg poor in SiO2
slowly
Magma (below)
basaltic
Dense dark colored
when molten rock cools and solidifies
large
Lava (above)
Ocean floor Hawaii
Granite, gabbro, diorite
38Andesitic Rocks
- Andesitic igneous rocks have mineral compositions
between those of basaltic and granitic rocks. - Color tends to be between dark and light.
- Medium density
39Andesitic Rocks
- Many volcanoes around the rim of the Pacific
Ocean formed from andesitic magmas.
40Andesitic Rocks
- Like volcanoes that erupt granitic magma, these
volcanoes also can erupt violently. - Rocks made from andesite tend to be fine-grained.
41Lava
High SiO2 Low Fe Mg
Crystal size
Slowly
granitic
Light colored, less dense
Small or not visible
On the continents
Physical chemical properties
b/t basaltic granitic
Extrusive
basalt, ryolite, andesite
andesitic
Grey, medium
magma
Pacific Rim
Intrusive
Rich in Fe Mg poor in SiO2
slowly
Magma (below)
basaltic
Dense dark colored
when molten rock cools and solidifies
large
Lava (above)
Ocean floor Hawaii
Granite, gabbro, diorite