earth and life science
Exploring Types of Rocks in Earth & Life Science
Learning Objectives
Identify and differentiate between intrusive and extrusive igneous rocks.
Describe the formation process of the 3 types of rocks.
Identify common examples of each type of rock.
Overview of Rocks
Earth is composed of solid rock extending to a depth of 2,900 kilometers.
Petrology: The scientific study of rocks.
Classification of Rocks
Rocks are classified into three main types based on their formation:
Igneous Rocks
Sedimentary Rocks
Metamorphic Rocks
Igneous Rocks
Formed from the cooling and solidification of magma or lava.
They can be found deep within the Earth or on its surface.
Exhibits a variety of colors, textures, and sizes depending on their cooling rate.
Types of Igneous Rocks
Extrusive (Volcanic) Rocks
Form when lava cools quickly on Earth's surface.
Result in small, fine-grained crystals.
Intrusive (Plutonic) Rocks
Form when magma cools slowly beneath the Earth's surface.
Exhibit large, coarse-grained crystals.
Classification Criteria for Igneous Rocks
Composition
Felsic: Light colored, silica-rich rocks (e.g., Granite).
Mafic: Dark-colored, low-silica rocks (e.g., Basalt).
Intermediate: Rocks with balanced silica content.
Ultramafic: Very dense, very low-silica content (e.g., Obsidian).
Texture
Aphanitic: Fine-grained rocks visible under a microscope.
Phaneritic: Coarse-grained rocks with large crystals.
Porphyritic: Mixed texture with varying crystal sizes.
Glassy: Gas-like texture with no crystals (e.g., Obsidian).
Pyroclastic: Formed from explosive volcanic activity.
Examples of Igneous Rocks
Diorite, Andesite, Granite, Basalt, Pegmatite, Pumice, Tuff, Scoria, Obsidian.
Metamorphic Rocks
Formed from the transformation of existing rocks (igneous or sedimentary) due to heat, pressure, or fluids within the Earth's crust.
They often display distinct textures and patterns.
Metamorphism Process
Metamorphism: The process of physical and chemical changes without melting.
Types of Metamorphism
Contact Metamorphism: Involves heating by nearby magma, affecting a small area.
Regional Metamorphism: Changes occur over a large region of the crust due to pressure and temperature changes.
Examples of Metamorphic Rocks
Common metamorphic rocks include Marble, Slate, Phyllite, and Schist.
Classification of Metamorphic Rocks
Texture: Size, arrangement, and shape of grains.
Foliation: Planar arrangement of mineral grains or structural features.
Types of Foliated and Non-foliated Rocks:
Foliated Rocks: Layered appearance (e.g., Gneiss).
Non-foliated Rocks: Form under uniform pressure (e.g., Marble).
Sedimentary Rocks
Develop from the accumulation and compression of sediment layers (e.g., sand, mud, flora, and fauna).
These layers solidify over time to form sedimentary rocks.
Types of Sedimentary Rocks
Clastic Sedimentary Rocks: Formed from clasts' accumulation (e.g., Breccia).
Chemical Sedimentary Rocks: Precipitated from mineral solutions.
Organic Sedimentary Rocks: Formed from accumulated biological debris (e.g., Limestone, Coal).
Trivia
The oldest known rocks, the Acasta Gneiss in Canada, are approximately 4 billion years old, nearly as old as Earth itself!