Rocks and The Rock Cycle
Rocks are solid materials formed through three main processes: heat, pressure, or layering. They fall into three major categories based on how they form.
Igneous rocks form when molten rock (magma or lava) cools and solidifies. When magma cools beneath the surface, it creates intrusive igneous rocks like granite. When lava cools on the surface, it forms extrusive igneous rocks like basalt, pumice, and obsidian.
Sedimentary rocks form through lithification—the compaction and cementation of sediments. These rocks, including sandstone, limestone, and shale, are where fossils are commonly found since they form in environments where plants and animals can be preserved.
Metamorphic rocks result from the recrystallization of existing rocks under intense heat and pressure, which changes their mineral composition. Examples include marble, slate, and quartzite. Regional metamorphism often creates foliation—thin sheets within the rock that form along parallel planes.
💡 The rock cycle connects all three rock types in a continuous process. Rocks don't stay in one form forever—they transform from one type to another as they experience different environmental conditions over millions of years!