Igneous rocks form when magma, which is molten rock, cools and crystallizes either at volcanoes on the Earth's surface or while it remains inside the crust. All magma originates underground in the lower crust or upper mantle, where intense heat causes the rock to melt.
Igneous rock formation starts deep within the Earth’s mantle, where intense heat generates magma. This molten material can either stay below the surface, slowly cooling and crystallizing into intrusive igneous rocks, which develop larger crystals due to the gradual cooling process. Alternatively, magma can rise to the surface through volcanic activity, erupting as lava. Once exposed to the cooler atmosphere, lava cools rapidly, forming extrusive igneous rocks with smaller crystals or a glassy texture due to the quick solidification.
Formed from magma that cools slowly beneath the Earth's surface. The slow cooling allows large crystals to form. Examples: Granite, Diorite.
Formed from lava that cools quickly on or near the Earth's surface. The rapid cooling results in smaller crystals or glassy textures. Examples: Basalt, Pumice.
Fine-Grained and Course-Grained
Igneous rocks can be both fine-grained or coarse-grained. Fine-grained contains more but smaller components whole coarse-grained contains fewer but larger components. Fine-grained are extrusive rocks, while coarse-grained are intrusive rocks.
Felsic, Intermediate, and Mafic
Igneous rocks can also be felsic, intermediate, or mafic. Felsic are lighter in color and contains more silica and feldspar. Mafic on the other hand is darker in color and contains more magnesium and iron. Most extrusive are felsic while most intrusive are mafic. However, there are also rocks with has both properties of felsic and mafic. These kinds of rock are called Intermediate.
• Diorite - intermediate, coarse-grained
• Harzburgite - mafic, coarse-grained
• Peridotite - mafic, coarse-grained
• Gabbro - mafic, coarse-grained
• Andesite - intermediate, fine-grained
• Basalt - mafic, fine-grained
• Tuff - felsic, fine-grained
• Dacite - felsic, fine-grained
• Pumice - felsic, fine-grained
Intrusive rocks are commonly used for construction and sculptures. In addition, some igneous rocks, such as obsidian, are crafted into sharp tools for cutting. Granite, for instance, is often used for flooring due to its durability. Here are some notable places in the Philippines where igneous rocks have been used in construction.
This iconic monument is made of durable granite, chosen for its strength and resistance to weathering, making it ideal for long-lasting memorials.
A historical landmark in Intramuros, Manila, constructed with granite and basalt, both known for their sturdiness, providing structural support and resistance to the elements.
The floors in this commercial hub are crafted from granite, prized for its polished finish and high durability, offering both aesthetic appeal and functionality for heavy foot traffic.