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There are three main types of rocks: igneous, sedimentary, and metamorphic.

1. Igneous rocks are formed when molten magma cools and solidifies. This can happen either beneath the Earth's surface (intrusive igneous rocks) or on the surface after a volcanic eruption (extrusive igneous rocks). Examples of igneous rocks include granite, basalt, and obsidian.

2. Sedimentary rocks are formed from the accumulation and consolidation of sediments over time. These sediments can be derived from the weathering and erosion of other rocks, organic materials, or chemical precipitation. Examples of sedimentary rocks include sandstone, limestone, and shale.

3. Metamorphic rocks are formed when existing rocks undergo high temperatures and pressures, causing them to change in mineral composition and texture. This transformation happens without melting the rock completely. Examples of metamorphic rocks include marble, slate, and gneiss.

In general, rocks are solid, naturally occurring substances composed of minerals. They are made up of one or more minerals or mineraloids and can vary greatly in composition, texture, and appearance. Rocks are the building blocks of the Earth's crust and provide valuable insights into the geological history and processes that have shaped our planet.

Salamat is a word from the Filipino language, which means "thank you."
 

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