Chapter 6:

What are igneous rocks? Igneous rocks gets its name from the Latin word for “fire”, because it is formed from hot molten rock (magma) inside the Earth. When the molten rock solidifies, it forms solid igneous rock. The way the magma cools determines the kind of igneous rock that is formed. Magma is molten rock, while lava is magma on the Earth’s surface. Igneous rocks may be either extrusive if they form at the surface (ex. basalt) or intrusive if magma solidifies underground (ex. granite). Watch Video

From Minerals to Rocks…

Igneous Rock Textures Texture refers to a rock’s appearance with respect to the size, shape and arrangement of its grains. Extrusive rocks are typically fine-grained (grains smaller than 1mm). The grains are small because the magma cooled rapidly at the surface, and large crystals did not have time to form. Some intrusive rocks are fine grained, but these would have formed near the surface in “cold rock”. Extrusive rock called obsidian. This is a glass- like rock that forms at the surface

Igneous Rock Textures Intrusive rocks usually form at considerable depth (more than a few km) and are called plutonic rocks (after Pluto, the Roman god of the underworld). Intrusive rocks are typically coarse-grained (bigger than 1mm) because of the slow cooling and solidification of magma

How are igneous rocks classified? Igneous rocks names are based on texture (basically grain-size) and mineral composition. So, each type of igneous rock will have: 1. a specific combination of minerals. 2. coarse or fine grains. Plutonic rocks are easier to identify because of the larger crystals.

Common Igneous Rocks Group 1 GraniteRhyolite Formed inside EarthFormed at surface Coarse-grainedFine-grained Quartz crystals visibleCrystals too small Feldspars

Common Igneous Rocks Group 2 DioriteAndesite Formed inside EarthFormed at surface Coarse-grainedFine-grained No quartzCrystals too small to see Feldspars; 30-50% ferromagnesian minerals Feldspars; 30-50% ferromagnesian minerals

Common Igneous Rocks Group 3 GabbroBasalt Formed inside EarthFormed at surface Coarse-grainedFine-grained Mostly ferromagnesian minerals Some feldspars

Identification of Igneous Rocks

Occurrences of Igneous Rock Occurrence

What happens when magma cools underground? Cooling magma may form intrusive structures, or bodies of magma that crystallize/harden after flooding surrounding rock layers

Examples of Intrusive Structures 1.Volcanic neck (magma is solidified in the neck of a volcano) 2.Dike & Sills (magma solidifies into a wall after being squeezed through two rock layers) Ex. Ship Rock in New Mexico, USA

Volcanic neck Dike Shiprock, New Mexico Shiprock Video Shiprock Video (4:20 mark)

Dikes & Sills

Examples of Intrusive Structures (cont’d) Plutons are blobs of magma that crystallize within the crust. If these plutons make it to the surface, large areas of rock (usually granite) form huge outcrops of rock at the surface. Batholiths are areas of plutons greater than 100km 2. Batholiths are present in the Sierra Nevada Mountains of California and in the Appalachian Mountains

Halifax Pluton, South Mountain Batholith, Nova Scotia

Batholith Formation

Examples of Extrusive Structures The most obvious structures made of extrusive igneous rock (or igneous rock at the surface) are: