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Magma, as you may know, is molten rock found under the Earth's surface. It can sometimes be seen on the Earth's surface as lava after passing through a volcano. At times, magma does not reach the surface and instead remains underground. In both circumstances, the magma eventually solidifies, resulting in igneous rocks and structures. Intrusive or plutonic rocks are those that consolidate beneath the earth, whereas extrusive or volcanic rocks are those that solidify above the surface. Extrusive rocks are occasionally tiny enough to handle in your palm. When lava pours onto the surface, it may construct whole landforms. Intrusive rocks are not always concealed under the surface. They might arise on the surface when the rocks that originally concealed them disintegrate, revealing the intrusive igneous rock. Hot springs and geysers are two further examples of igneous rock surface characteristics.


Volcanoes are the most visible landforms formed by lava. Volcanoes, of course, are where lava rises to the surface. Volcanoes, as previously said, exist in a variety of shapes and sizes, the most frequent of which are cinder cones, stratovolcanoes, and shield volcanoes. Lava, on the other hand, may produce various significant landforms, as mentioned below.

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