Section 2: Mineral Formation and Resources
Minerals usually form through a process called crystallization. Crystallization occurs when particles dissolved in a liquid solidify in an orderly, repeating pattern to form crystals. Geologists study a mineral’s physical and chemical properties to determine the type of environment in which it formed. Sometimes crystals grow inside hollow spaces in rocks. A geode is a rounded, hollow rock often lined with mineral crystals, such as agate, that forms when silica-rich water fills cavities in volcanic rock and slowly crystallizes in layers.
Minerals form in two different ways. The first is through the crystallization of magma or lava. When hot magma cools slowly beneath Earth’s surface, or when lava cools quickly at the surface, minerals form as the liquid turns solid. As the material cools, atoms bond together and form crystals. Slower cooling generally allows larger crystals to form. For example, potassium feldspar and biotite commonly form in igneous rocks such as granite as magma cools slowly underground. Their crystal size can help scientists understand how quickly the magma cooled.

Minerals are extremely important because they are the source of gemstones, metals, and many materials used in everyday products. Gemstones are naturally occurring minerals that are valued for their hardness, color, and glassy luster. After a gemstone is cut and polished, it is called a gem. Minerals are also the source of useful metals such as aluminum, iron, copper, and silver. A rock that contains enough valuable minerals to be mined for profit is called ore.
To obtain these valuable materials, geologists first locate deposits through prospecting. Ore is then removed from the ground through mining, and the valuable metals are extracted through a process called smelting, which uses heat to separate the metal from the surrounding material.
Review:
- Explain crystallization.
- What are the two different ways that minerals can form?
- What are gemstones?