Extrusive igneous rocks, also known as volcanic rocks, form from the rapid cooling and solidification of molten rock (magma) that erupts onto the Earth's surface. Here’s a step-by-step overview of the process:
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Magma Generation: Magma forms in the Earth's mantle due to the melting of pre-existing rocks. This can occur due to various factors, including increased temperature, decreased pressure, and the addition of volatiles like water.
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Eruption: When the pressure from the magma builds up, it can erupt through volcanic vents. This eruption can occur explosively or effusively, depending on the viscosity of the magma and the amount of gas it contains.
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Lava Flow: Once the magma reaches the surface, it is referred to as lava. The lava can flow out of the volcano and spread across the landscape. The flow can take various forms, including sheets, plateaus, or more viscous formations.
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Cooling and Solidification: As the lava comes into contact with the relatively cooler air or water at the surface, it begins to cool rapidly. The quick cooling prevents the formation of large crystals, resulting in a fine-grained or glassy texture typical of extrusive rocks.
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Formation of Rock Types: The composition of the lava (which can vary in terms of silica content) will influence the kind of extrusive igneous rock that forms. Common types include:
- Basalt: Low in silica, dark-colored, and typically forms from fluid lava flows.
- Rhyolite: High in silica, light-colored, and tends to form from more viscous lava eruptions.
- Pumice: Volcanic glass that forms when lava cools quickly with trapped gas bubbles, resulting in a light, porous texture.
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Post-Eruption Processes: After the lava cools and solidifies, it can undergo further weathering and erosion or may be subject to additional volcanic activity.
In summary, extrusive igneous rocks form when lava erupts from volcanoes, cools quickly at the Earth's surface, and crystallizes into solid rock.