Presentation is loading. Please wait.

Presentation is loading. Please wait.

Chapter 5.2 – Classification of Igneous Rocks

Similar presentations


Presentation on theme: "Chapter 5.2 – Classification of Igneous Rocks"— Presentation transcript:

1 Chapter 5.2 – Classification of Igneous Rocks
Two main types of igneous rock: Intrusive rocks form when magma cools and crystallizes below Earth’s surface. Crystals large enough to see without magnification Extrusive rocks form when magma cools and crystallizes on Earth’s surface (lava flows). Small crystals that need magnification to see

2 Types of Classification
Properties Grain size Texture Mineral composition Basaltic rocks – mafic rocks, dark-colored, low silica contents, and contain mostly plagioclase and pyroxene Granitic rocks – felsic rocks, light-colored, have high silica content, and contain mostly quartz and feldspar

3 Types of Classification
Intermediate rocks – rocks that have mineral compositions in between the two others Ultrabasic – ultramafic, contains rocks with only iron-rich minerals and are always dark Texture refers to size, shape, and distribution of crystals/grains that make up a rock Examples: fine-grained, coarse-grained

4 Other Properties When lava cools on the surface, it cools so quickly that only small crystals form Sometimes crystals don’t form at all This results in volcanic glass called obsidian

5 Other Properties When lava cools slowly under the surface, large crystals form – granite, diorite, gabbro

6 Porphyritic Rocks Porphyritic texture – large, well-formed crystals surrounded by finer-grained crystals of the same mineral or different minerals Complex cooling history (example: slow cooling then rapid cooling) causes different crystal sizes

7 Vesicular Rocks Vesicular texture – Spongy appearance formed when gas is prevented from escaping. The holes left behind are called vesicles Examples are pumice and vesicular basalt

8 Thin Sections A Thin Section is a slice of rock 2 x 4 cm and only 0.03 mm thick Light is able to pass through this sample These samples are viewed through a petrographic microscope and geologists look for certain properties Examples of properties: feldspar grains have banding called “twinning,” quartz grains look wavy as stage is rotated, etc.

9 Igneous Rocks as Resources
Useful in many fields such as Construction Energy production Jewelry making Ores can be extracted from veins of lava flows Gold, silver, lead, copper These elements released at end of magma crystallization process

10 Igneous Rocks as Resources
Pegmatites are igneous rocks made of extremely large-grained materials Found as igneous intrusions or veins Rare elements such as Lithium, Beryllium form in these ores They also produce complex crystals

11 Igneous Rocks as Resources
Kimberlites are ultrabasic rocks that were first found in Kimberly, South Africa Only formed under very high pressure Valuable minerals such as diamonds Most diamonds in the world are found in South African mines. Only one diamond mine in the US in Colorado

12 Igneous Rocks as Resources
Igneous rocks are strong building materials Durable Weather-resistant Countertops, floors, statues, etc.


Download ppt "Chapter 5.2 – Classification of Igneous Rocks"

Similar presentations


Ads by Google