The Basic Cycle
Igneous Rocks
Igneous Textures
Sedimentary Rocks
Igneous and Sedimentary
100

This molten rock is found under Earth's surface.

Magma

100

Cooling of molten rock leads to this rock type.

Igneous rock

100

This texture features large crystals embedded in smaller ones, like in porphyritic rocks.

Porphyritic

100

This process forms sedimentary rock through the weight and pressure of overlaying rock.

Compaction

100

This process slowly breaks down rocks via the atmosphere.

Weathering

200

This is molten rock that erupts onto Earth's surface.

Lava

200

Formed at the surface from lava, these rocks are also called volcanic.

Extrusive

200

Fast cooling creates this texture composed of minute particles

Fine-grained

200

This clastic rock consists of rounded, gravel-sized particles.

Conglomerate

200

Sediment turns into rock via pressure from above and cementing fluids.

Lithification

300

This rock type is composed of layers composite minerals

Sedimentary rock

300

The 1980 explosive eruption of this Washington volcano formed new igneous rocks.

Mount St. Helens

300

This lightweight rock with bubble holes shows vesicular texture.

Pumice

300

This biochemical rock is composed mostly of calcite and marine organisms

Limestone

300

Early-formed, denser crystals sink in magma, creating varied compositions.

Crystal setting

400

Rock particles produced by weathering are called this.

Sediment

400

Felsic and light-colored, this intrusive rock is common in continental crust.

Granite

400

Rapid cooling freezes ions before crystals form, creating this rock with a glassy texture

Obsidian

400

This angular clastic rock indicates short transport distance for its particles.

Breccia

400

Norman Levi Bowen devised this series showing mineral crystallization order in cooling magma.

Bowen's Reaction Series

500

When sedimentary rocks face heat and pressure, they become this type.

Metamorphic rock

500

Mafic in composition, this extrusive rock forms from quiet, slow lava flows.

Basalt

500

Consolidated volcanic ash and fragments create this texture, seen in welded tuff.

Pyroclastic

500

Compacted organic matter like lignite evolves into this rock under heat and pressure.

Coal

500

Water percolates through sediments, depositing minerals like calcite or silica to bind grains

Cementation

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