
Igneous
Rock Name | Composition | Grain Size | Color | Other Characteristics |
Granite | Quartz, Feldspar, Mica or Amphibole | Coarse | White, Pink, Gray | Color and grain size highly variable |
Rhyolite | Quartz, Feldspar | Very fine to glassy | Light color | Very high silica content, may contain la ... |
Diorite | Plagioclase, Biotite, Hornblende, Pyroxe ... | Coarse | White and dark gray | Fairly rare, often confused with gabbro |
Basalt | Augite, Pyroxene, Plagioclase, low-silic ... | Fine | Dark gray, sometimes light | Often has gas bubbles (vesicles). Can co ... |
How do you identify intrusive igneous rocks?
Method 1 Identifying Igneous Rocks. Intrusive rocks form from the cooling of magma deep beneath the earths surface. Since this occurs below the earth's surface, the magma will cool very slowly. As magma cools, it will form crystals. Intrusive rocks have larger crystals typically formed together to form the rock mass.
What is an example of an igneous rock?
For example, two rocks from identical magma can become either rhyolite or granite, depending on whether they cool quickly or slowly. The two main categories of igneous rocks are extrusive and intrusive. Extrusive rocks are formed on the surface of the Earth from lava, which is magma that has emerged from underground.
How are igneous rocks formed from magma?
1 Answer. Igneous rocks are formed through the solidification or crystallization of molten magma. The type of igneous rocks that form from magma is a function of three factors: the chemical composition of the magma; temperature of solidification; and the rate of cooling which influences the crystallization process.
What is the texture of igneous rocks?
The texture is a description of a rock’s constituent parts in terms of their sizes, shapes and arrangement The size of mineral crystals in an igneous rock may indicate the rate at which the lava or magma cooled to form a rock.

How do you identify an igneous rock?
Igneous rocks can be distinguished from sedimentary rocks by the lack of beds, lack of fossils, and lack of rounded grains in igneous rocks, and the presence of igneous textures.
What is the main characteristic that we use to identify igneous rocks?
Two main characteristics are used to classify igneous rocks: 1) texture (the size of the mineral grains in the rock; and 2) composition (often determined by what the actual minerals are).
What are the 2 ways igneous rocks are identified?
The two main categories of igneous rocks are extrusive and intrusive. Extrusive rocks are formed on the surface of the Earth from lava, which is magma that has emerged from underground. Intrusive rocks are formed from magma that cools and solidifies within the crust of the planet.
What are the 3 ways that we can classify an igneous rock?
Igneous rocks are formed when magma cools and solidifies. They are classified by using grain size, silica content, and/or silica saturation.
How do you identify igneous and metamorphic rocks?
Look for crystals in igneous rocks. Examples of igneous rocks are gabbro, granite, pumice and obsidian. Metamorphic rocks are rocks that have become changed by intense heat or pressure while forming. One way to tell if a rock sample is metamorphic is to see if the crystals within it are arranged in bands.
How do you identify sedimentary and igneous rocks?
1:164:35How to identify the different types of rocks - YouTubeYouTubeStart of suggested clipEnd of suggested clipSo it's always handy sedimentary rocks are made up of broken bits of minerals. Other rocks orMoreSo it's always handy sedimentary rocks are made up of broken bits of minerals. Other rocks or fossils all stuck. Together. You can see that these grains are clearly separate from each other. They may
What are the 2 ways igneous rocks are identified 1 and 2?
Igneous rocks are divided into two groups, intrusive or extrusive, depending upon where the molten rock solidifies.
What 2 characteristics are used to identify rocks?
There are two main characteristics used to identify igneous rocks: texture and composition.
What are two ways to identify a rock?
Grain Size: Coarse grains are visible to the naked eye, and the minerals can usually be identified without using a magnifier. Fine grains are smaller and usually cannot be identified without using a magnifier. Hardness: This is measured with the Mohs scale and refers to the minerals contained within a rock.
What are 2 examples of igneous rocks?
There are two basic types: 1) intrusive igneous rocks such as diorite, gabbro, granite and pegmatite that solidify below the Earth's surface; and 2) extrusive igneous rocks such as andesite, basalt, obsidian, pumice, rhyolite and scoria that solidify on or above the Earth's surface.
What type of rock can be made of magma?
Igneous rocks can have many different compositions, depending on the magma they cool from. They can also look different based on their cooling conditions. For example, two rocks from identical magma can become either rhyolite or granite, depending on whether they cool quickly or slowly.
How are extrusive rocks formed?
Extrusive rocks are formed on the surface of the Earth from lava, which is magma that has emerged from underground. Intrusive rocks are formed from magma that cools and solidifies within the crust of the planet. When lava comes out of a volcano and solidifies into extrusive igneous rock, also called volcanic, the rock cools very quickly.
What happens when lava cools?
These fine-grained rocks are known as aphanitic —from a Greek word meaning “invisible.” They are given this name because the crystals that form within them are so small that they can be seen only with a microscope. If lava cools almost instantly, the rocks that form are glassy with no individual crystals, like obsidian . There are many other kinds of extrusive igneous rocks. For example, Pele’s hair is long, extremely thin strands of volcanic glass, while pahoehoe is smooth lava that forms shiny, rounded piles.
What is the name of the rock that is larger than a human hand?
One extreme type of phaneritic rock is called pegmatite, found often in the U.S. state of Maine. Pegmatite can have a huge variety of crystal shapes and sizes, including some larger than a human hand. Devil's Tower National Monument in Wyoming is an example of an igneous rock.
Why are crystals in volcanic rocks small?
Crystals inside solid volcanic rocks are small because they do not have much time to form until the rock cools all the way, which stops the crystal growth. These fine-grained rocks are known as aphanitic —from a Greek word meaning “invisible.”.
What is intrusive rock?
Intrusive rocks, also called plutonic rocks, cool slowly without ever reaching the surface. They have large crystals that are usually visible without a microscope. This surface is known as a phaneritic texture. Perhaps the best-known phaneritic rock is granite.
What is the definition of a rock?
Noun. type of hard, igneous rock. lava. Noun. molten rock, or magma, that erupts from volcanoes or fissures in the Earth's surface. magma. Noun. molten, or partially melted, rock beneath the Earth's surface. mantle.
How are igneous rocks classified?
Identifying igneous rocks is not that simple. They are classified by what minerals they contain, and the size of those mineral pieces, which are called grains.
How many different types of igneous rocks are there?
The different classes of igneous rocks grade into each other, with granite merging smoothly into diorite without a sharp difference. There are over 700 different kinds of igneous rocks, but geologists group them into a few general categories.
What is a fine grained rock that contains large gas bubbles?
Scoria is a fine grained rock that contains large gas bubbles. While it is underground, magma contains dissolved gases. When it reaches the surface as lava, the gases escape, just like the bubbles you get in a glass of carbonated soda. As the lava starts to cool, it gets thicker as tiny grains crystallize.
What type of rock has no mineral grains?
There are a few types of igneous rocks that don't fit into this chart, including volcanic glass and rocks with a large number of gas bubbles. Obsidian is volcanic glass. It has no mineral grains. Obsidian. Obsidian is formed when very hot lava cools so quickly that there is no time for mineral grains to crystallize.
How is obsidian formed?
Obsidian is formed when very hot lava cools so quickly that there is no time for mineral grains to crystallize. Instead, the lava cools into glass with no crystalline structure. Obsidian us usually dark, but can range from black to light brown in color, depending on what chemicals it contains.
How to identify igneous rocks?
Igneous rocks can be easily identified with their texture, density, colour, and mineral composition. Its texture depends on the shape, size, time period to cool down and solidify, and the arrangement of crystals in the rock.
What are Igneous Rocks?
Igneous rocks are defined as types of rocks that are formed when molten rock (rock liquefied by intense heat and pressure) cools to a solid state.
What are intrusive igneous rocks?
Intrusive igneous rocks are rocks that crystallize below the earth’s surface resulting in large crystals as the cooling takes place slowly. Diorite, granite, pegmatite are examples of intrusive igneous rocks.
What does it mean when a rock has a large crystal?
Larger crystals generally indicate intrusive igneous rocks. Smaller crystals generally indicate faster cooling associated with extrusive igneous rocks. Types of Igneous Rock Texture.
What are the characteristics of igneous rocks?
Characteristics of Igneous Rocks 1 The igneous form of rocks does not include any fossil deposits. If there are any chances of fossil deep inside the crust, it erupts out of the Earth’s surface and gets destroyed due to the sheer heat these rocks produce. 2 Most igneous forms include more than one mineral deposit. 3 They can be either glassy or coarse. 4 These usually do not react with acids. 5 The mineral deposits are available in the form of patches with different sizes.
How are sedimentary rocks formed?
Sedimentary rocks are formed by the accumulation or deposition of mineral or organic particles at the Earth’s surface while metamorphic rocks are formed when watery hot fluids are subjected to high heat and pressure, lastly, igneous rocks are formed when lava cools and solidifies.
What is a pyroclastic deposit?
Pyroclastic deposits are accumulations of fragmented material (e.g. ash, bombs, tuffs, and volcanic breccias) ejected during volcanic eruptions. As igneous rocks are formed from magma and begin the rock cycle, they are called primary rocks. Igneous rocks can be easily identified with their texture, density, colour, and mineral composition.
