Marble: metamorphic; granular limestone or dolomite that has been recrystallized under the influence of heat, pressure, and aqueous solutions.
Quartzite: metamorphic; forms when a quartz-rich sandstone is altered by heat, pressure, and chemical activity.
Soapstone: metamorphic; consists primarily of talc, also varying amounts of other minerals such as micas, chlorite, amphiboles, quartz, magnesite, and carbonates.
Granite: igneous; composed mainly of quartz and feldspar with minor amounts of mica, amphiboles, and other minerals. It forms from the slow crystallization of magma below Earth's surface.
Limestone: sedimentary; composed primarily of calcite, a calcium carbonate mineral; usually forms from the accumulation of shell, coral, algal, fecal, and other organic debris.
Onyx: a plural-banded type of chalcedony, a cryptocrystalline form of silica, composed of very fine intergrowths of quartz and moganite.