Magma is molten rock that flows beneath the earth’s surface. Igneous rocks are formed by cooling magma. The location of the formation of the rock, as well as how fast the magma cools will determine the type of igneous rock. Intrusive rocks form from the cooling of magma deep beneath the earth’s surface. Since this occurs below the earth’s surface, the magma will cool very slowly. [3] X Trustworthy Source U. S. Geological Survey U. S. government agency responsible for conducting scientific research on the nation’s land, natural resources, and natural disasters Go to source As magma cools, it will form crystals. Intrusive rocks have larger crystals typically formed together to form the rock mass. An example of an intrusive rock is granite. When magma is above the earth’s crust, it is known as lava. Extrusive rocks form through very fast cooling of lava above the Earth’s surface. Extrusive rocks have very small, almost microscopic crystals. These are often described as fine-grained rocks. [4] X Trustworthy Source U. S. Geological Survey U. S. government agency responsible for conducting scientific research on the nation’s land, natural resources, and natural disasters Go to source You usually can’t see these with the naked eye. The most common type of extrusive rock is basalt.
Pegmatitic igneous rocks have very large crystals, more than 1 cm in size. These are the slowest cooling type of igneous rocks. Remember, the slower a rock cools, the larger the crystals will be. Phaneritic igneous rocks are composed of interlocking crystals that are smaller than crystals in pegmatitic but still visible with the naked eye. Porphyritic igneous rocks have crystals of two different sizes, often with large crystals set in areas of smaller crystals. Aphanitic igneous rocks have a fine-grained texture and most of their crystals are too small to see with the naked eye. You will need to use a magnifying glass to observe the crystals in aphanitic rocks. Igneous rocks that form too quickly for crystals to form have what is called a glassy texture. Obsidian is the only glassy igneous rock, and can be identified by its dark color. This looks like dark black glass. Vesicular igneous rocks, such as pumice, look bubbly and form before gases are able to escape as lava forms the rock. This also formed with very rapid cooling. Pyroclastic igneous rock is a texture composed of volcanic fragments ranging from very fine (ash) to very coarse (tuffs and breccias). [6] X Research source
Identifying the composition of your rock can be very difficult if you are not an experienced rock collector or geologist. If you have any questions about how to identify a rock, contact a collector or geologist at a local college or university. Felsic igneous rocks are light in color. Their mineral composition is primarily feldspars and silicates such as quartz. Granite is an example of a felsic rock. Felsic rocks have a low density and contain 0-15% mafic crystals. Mafic minerals are olivine, pyroxene, amphibole, and biotite. Mafic igneous rocks are dark in color and consist mainly of magnesium and iron. They contain 46-85% mafic mineral crystals and are high in density. Basalt is an example of a mafic rock. Ultramafic igneous rocks are also dark in color and contain higher amounts of the minerals found in mafic rocks. These rocks have greater than 85% mafic mineral crystals. Dunite is an example of an ultramafic rock. Intermediate igneous rocks contain 15-45% mafic mineral crystals. They share minerals with both felsic and mafic rocks and are intermediate in color. Diorite is an example of an intermediate rock.
Igneous rocks are made from the rapid or slow cooling of magma/lava. [9] X Research source Metamorphic rocks change form based on the influence of heat, pressure, or chemical activity. [10] X Trustworthy Source U. S. Geological Survey U. S. government agency responsible for conducting scientific research on the nation’s land, natural resources, and natural disasters Go to source Sedimentary rocks are essentially formed by pieces of smaller rocks, fossils, and sediments. [11] X Research source
If a rock is layered, it will have different sections that are different colors and may or may not contain small crystals or fossils. You will need to look for these under a magnifying glass. In cross section, layers in a rock will look like different colors stripes on top of one another. The presence and distribution of layering can help you identify the main type of rock you have. Igneous rocks are not layered. If your rock has layers it will be either a metamorphic or sedimentary rock. Sedimentary rocks will have layers that are softy and crumbly, and are comprised of mud, sand or gravel. Sedimentary rocks can also have crystals. If the layers in your rock are made up of crystals of varying sizes, then your rock is sedimentary. Metamorphic rocks have layers made up crystals that are the same size. The layers of metamorphic rocks are also folded and deformed.
Igneous rocks are very dense and hard. They may have a glassy appearance. Metamorphic rocks may also have a glassy appearance. You can distinguish these from igneous rocks based on the fact that metamorphic rocks tend to be brittle, lightweight, and an opaque black color. Sedimentary rocks with no grains will resemble dry clay or mud. Sedimentary rocks with no grains also tend to be soft, as they can usually be scratched easily with a fingernail. These rocks will also react to hydrochloric acid.
Only metamorphic and sedimentary rocks will contain fossils. Sedimentary rocks may have visible fossils such as whole or partial leaves, shells, footprints etc. Metamorphic rocks will contain only highly fragmented fossils. Sedimentary rocks will have grains made up of sand, silt or gravel. These grains may be rounded in shape (clastic), or be made up of other rocks. If your grains contain crystals, you can use the orientation and size of the crystals to identify the rock. Igneous rocks have crystals that are randomly oriented. They may have large crystals in ground mass with smaller crystals. Sedimentary rocks have crystals that are easily broken or scratched. Metamorphic rocks contain crystals that have a foliated or scaly appearance. These are often long and arranged in a parallel pattern.
Rocks that have a metallic appearance with a scaly or smooth texture are metamorphic. Igneous rocks may have a vesicular texture. This is when the rock appears to be very porous with many holes. Pumice is an example of a rock that has a very porous texture. Igneous rocks will be very hard. Many types of igneous rocks have rocky streamlined flow structures in them.
