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Rocks<br />

Rocks<br />

Rock Type Rock Name Characteristics<br />

Reference Handbooks<br />

Igneous Granite Large mineral grains of quartz, feldspar,<br />

(intrusive) hornblende, and mica. Usually light in color.<br />

Diorite Large mineral grains of feldspar, hornblende, and mica.<br />

Less quartz than granite. Intermediate in color.<br />

Gabbro Large mineral grains of feldspar, augite, and olivine.<br />

No quartz. Dark in color.<br />

Igneous Rhyolite Small mineral grains of quartz, feldspar, hornblende,<br />

(extrusive) and mica, or no visible grains. Light in color.<br />

Andesite Small mineral grains of feldspar, hornblende, and mica<br />

or no visible grains. Intermediate in color.<br />

Basalt Small mineral grains of feldspar, augite, and possibly<br />

olivine or no visible grains. No quartz. Dark in color.<br />

Obsidian Glassy texture. No visible grains. Volcanic glass.<br />

Fracture looks like broken glass.<br />

Pumice Frothy texture. Floats in water. Usually light in color.<br />

Sedimentary Conglomerate Coarse grained. Gravel or pebble-size grains.<br />

(detrital) Sandstone Sand-sized grains 1/16 to 2 mm.<br />

Siltstone Grains are smaller than sand but larger than clay.<br />

Shale Smallest grains. Often dark in color. Usually platy.<br />

Sedimentary Limestone Major mineral is calcite. Usually forms in oceans and<br />

(chemical or organic) lakes. Often contains fossils.<br />

Coal Forms in swampy areas. Compacted layers of organic<br />

material, mainly plant remains.<br />

Sedimentary<br />

(chemical)<br />

Rock Salt Commonly forms by the evaporation of seawater.<br />

Metamorphic Gneiss Banding due to alternate layers of different minerals,<br />

(foliated) of different colors. Parent rock often is granite.<br />

Schist Parallel arrangement of sheetlike minerals, mainly<br />

micas. Forms from different parent rocks.<br />

Phyllite Shiny or silky appearance. May look wrinkled.<br />

Common parent rocks are shale and slate.<br />

Slate Harder, denser, and shinier than shale. Common<br />

parent rock is shale.<br />

Metamorphic Marble Calcite or dolomite. Common parent rock is limestone.<br />

(nonfoliated) Soapstone Mainly of talc. Soft with greasy feel.<br />

Quartzite Hard with interlocking quartz crystals. Common<br />

parent rock is sandstone.<br />

REFERENCE HANDBOOKS 791<br />

Matt Meadows<br />

Reference Handbooks

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