Silicon and oxygen are two of the most common elements on Earth. Together, they make up nearly 75 percent of the Earth's crust, so it is no surprise that they play major roles in forming many of the minerals that we see in rocks. The silicon atom, which has four electrons in its outermost region, likes to form chemical bonds with oxygen atoms, which are attracted to extra electrons. Thus, silicon and oxygen, together with some of the metallic elements, can combine to make hundreds of different minerals. For example, quartz has two oxygen atoms for every silicon atom, and feldspar has two or three silicon atoms grouped with eight oxygen atoms and a few metal atoms. About half of the most common minerals found on Earth belong to the silicate group, as do some beautiful gemstones such as amethyst, opal, and topaz.

One of the most striking, yet least diagnostic, features of many minerals is their color. Well-formed mineral crystals span the entire rainbow of tinctures, from red (cinnabar, garnet) to yellow (sulfur), green (malachite), blue (azurite, lazurite), and violet (the amethyst variety of quartz). Minerals containing iron and magnesium are often dark brown or dark green. Impurities, trace amounts of elements that do not normally belong in the mineral, may change the overall color of a crystal. For instance, depending on the trace amounts of impurities it contains, quartz may look colorless (no impurities), light pink (titanium, iron, or manganese), milky white (tiny bubbles of gas or liquid), purple (iron), yellow (iron), or brown (extra silicon). However, multiple minerals may have almost the same color, so scientists must rely on other physical properties to make definite identifications of mineral specimens.

Certain rare elements such as beryllium, tantalum, lithium, and yttrium occur in small quantities scattered around the world, rather than in rich mineral veins that are easy to mine. The economic importance of these elements, however, has grown substantially over the past few decades, as scientists and engineers have found new ways to use them. For example, tantalum, found primarily in the mineral tantalite, helps miniaturize the electronic components inside computers, gaming consoles, and cell phones. Lithium powers those portable devices by making batteries last longer. Beryllium, found in more than 100 minerals, goes into lightweight structural components of fighter jets, guided missiles, and spacecraft. When added to diesel fuel, cerium lowers the noxious emissions from trucks. Gallium and indium, two elements that are considered electrical semiconductors, go into light-emitting diodes (LEDs). Yttrium is a key ingredient in medical lasers.

For example, the mineral bastnasite (or bastnaesite), which contains cerium, lanthanum, and yttrium, was discovered in Sweden and occurs. The economic importance of these elements, however, has grown substantially over the past few decades, as scientists have put them into many high-tech devices. Cerium added to diesel fuel helps trucks run with fewer noxious emissions; scandium, alloyed with aluminum and other metals, makes lightweight lacrosse sticks and components for fighter jets; yttrium is a key ingredient in medical lasers.