Types of rocks

3 types of rocks: There are 3 types of rocks found on Earth: Igneous Sedimentary Metamorphic

Igneous Rocks - Formation Igneous Rocks are formed by melting, cooling, and crystallization of other rocks. Igneous rocks form as a result of volcanic activity, hot spots, and melting that occurs in the mantle.

Igneous rocks Igneous rocks are common along plate boundaries or mantle hot spots

Igneous Rocks - Classification Igneous rocks are classified using their texture in the following ways: Glassy Aphanitic (no visible crystals) Phaneritic (visible crystals) Porphyritic (Some visible and some not visible crystals)

Igneous Rocks - Texture Crystal size is used to classify igneous rocks. Crystals form as the rock cools, and the crystal size can tell us a lot about its cooling history: The larger the crystals, the slower it cooled.

Igneous Rocks - Texture Glassy igneous rocks have no crystal structure, and probably formed by very rapid cooling (such as on the surface of a lava, or when a lava enters the water.)

Igneous Rocks - Texture Aphanitic rocks have no visible crystals, and probably formed by fast cooling above ground.

Igneous Rocks - Texture Phaneritic rocks have visible crystals, and probably formed by slow cooling below ground.

Igneous Rocks - Texture Porphyritic rocks have both visible and nonvisible crystals, and probably formed by two different cooling events.

Igneous Rocks - Classification Dark igneous rocks are formed from basaltic or mafic magma. (Mafic because it contains a lot of magnesium and iron). The magma that forms these rocks is usually very hot (around 1000°C) and viscous (about the same viscosity as ketchup.)

Igneous Rocks - Classification Light colored igneous rocks are formed from silicic (high silica content) or felsic magmas. The magmas that form these rocks is usually more cool, (lower than 850°C), and more viscous (about the viscosity of peanut butter.)

Igneous rocks - Formations Structures and formations seen in igneous rocks include: Hexagonal columnar joints Pahoehoe lava flows Dikes, sills, and batholiths (plutons) Pillow basalts Volcanoes

Igneous Rocks - Examples The most common types of igneous rocks include: Rhyolite Andesite Basalt Granite Diorite Gabbro

Igneous rocks charted

Sedimentary Rocks - Formation Sedimentary rocks are formed by weathering, erosion, deposition, compaction, and cementation of other rocks. Sedimentary rocks form in areas where water, wind, or gravity deposit sediments.

Sedimentary rocks - formation Sedimentary rocks are likely to form in areas such as: Deltas Beaches Rivers Glaciers Sand dunes Shallow seas Deep oceans

Sedimentary rocks - Classification Sedimentary rocks are classified into two groups: Clastic rocks Chemically formed rocks

Sedimentary rocks – Classification Sedimentary rocks are Clastic if they are made of pieces of other rocks that have been weathered and eroded. Clastic rocks are grouped based on the size of grain that they are made from.

Sedimentary rocks - Classification Very small particles make up mudrock. Medium sized particles make up sandstone. Large particles make up conglomerates.

Sedimentary rocks - Classification Sedimentary rocks that form from chemical processes are called biochemical rocks (formed from living things) or Chemical precipitates (formed from lakes or shallow seas.)

Sedimentary rocks - formations Structures and formations seen in sedimentary rocks include: Stratification Cross bedding Graded bedding Ripple marks Mud cracks Fossils

Sedimentary rocks - Examples Conglomerate Sandstone Shale Limestone Gypsum Oolites Chert (including black flint and red jasper)

Metamorphic rocks - Formation Metamorphic rocks are formed by heat and pressure changing one type of rock into another type of rock. Metamorphic rocks form near lava intrusions, at plate subduction zones, and in deep mountain roots.

Metamorphic rocks - Formation Lava intrusions can provide heat that causes metamorphic rocks to form. These small areas of metamorphic rock form from contact metamorphosis.

Metamorphic rocks - Formation Rocks that metamorphose because of increasing heat and pressure found at plate subduction zones and in deep mountain roots form large areas of metamorphic rock through regional metamorphosis.

Metamorphic rocks - Classification Metamorphic rocks are classified into 2 major groups: Foliated Nonfoliated

Metamorphic rocks - Classification Foliated rocks form when differential pressure causes minerals to form in layers. These rocks will have stripes or planes that they will break easily along. These “stripes” don’t usually line up with the original bedding planes in sedimentary rocks.

Metamorphic rocks Nonfoliated metamorphic rocks formed in areas where the pressure from all sides was equal, so there is no “linear” quality to the rocks.

Metamorphic rocks - Formations Structures and formations seen in metamorphic rocks include: Folding Plastic deformation Stretching Alternating dark and light layers (gneissic foliation)

Metamorphic rocks - Examples Some common types of metamorphic rock include: Slate Schist Gneiss Amphibolite Marble Quartzite Metaconglomerate

Metamorphic rocks - Charted