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Extrusive rocks are formed when magma erupts onto the Earth's surface and cools quickly, forming small crystals. This rapid cooling prevents the formation of large crystals, resulting in a fine-grained texture. Examples of extrusive rocks include basalt, andesite, and rhyolite.
Igneous rocks are formed from the cooling and solidification of magma or lava. Igneous rocks can be classified into two main types: intrusive and extrusive. Intrusive rocks are formed from magma that cools and solidifies beneath the Earth's surface, resulting in larger crystals due to slower cooling. Examples of intrusive rocks include granite, diorite, and gabbro.
Overall, the formation of extrusive and igneous rocks involves the cooling and solidification of magma or lava, with extrusive rocks forming on the Earth's surface and igneous rocks forming beneath the surface.
Igneous rocks are formed from the cooling and solidification of magma or lava. Igneous rocks can be classified into two main types: intrusive and extrusive. Intrusive rocks are formed from magma that cools and solidifies beneath the Earth's surface, resulting in larger crystals due to slower cooling. Examples of intrusive rocks include granite, diorite, and gabbro.
Overall, the formation of extrusive and igneous rocks involves the cooling and solidification of magma or lava, with extrusive rocks forming on the Earth's surface and igneous rocks forming beneath the surface.
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Google Gemini AI
1 day ago
Extrusive Rocks
Extrusive rocks are formed from magma that flows out onto the Earth's surface. When magma erupts from a volcano, it cools and solidifies quickly, forming extrusive rocks such as:
- Lava flows: Formed when magma flows out of a volcano as a continuous stream.
- Ash flows: Formed when hot, gas-rich magma explodes and fragments into ash particles that flow down the volcano's slopes.
- Pumice: A light, porous rock formed when gas bubbles in magma expand and freeze during cooling.
- Scoria: A dark, vesicular rock formed when gas bubbles in magma rupture during cooling.
Intrusive Rocks
Intrusive rocks are formed from magma that cools and solidifies slowly beneath the Earth's surface. Over time, these rocks are exposed by erosion. Examples of intrusive rocks include:
- Batholiths: Large, deep-seated igneous intrusions that form from the cooling of large volumes of magma.
- Dikes: Narrow, vertical sheets of intrusive rock that cut across existing rock formations.
- Sills: Horizontal sheets of intrusive rock that form between layers of existing rock formations.
- Plutons: General term for any large intrusive body of igneous rock, including batholiths, stocks, and laccoliths.
Process of Formation
- Magma Generation: Rocks melt to form magma due to high temperatures, pressure, and the presence of water and other volatile elements.
- Crystallization: As magma cools, minerals crystallize and the magma becomes more solid.
- Solidification: When magma solidifies completely, it forms igneous rock.
- Extrusive Formation: If magma erupts onto the surface, it cools quickly and forms extrusive rocks.
- Intrusive Formation: If magma remains beneath the surface, it cools slowly and forms intrusive rocks.
Factors Affecting Rock Type
The type of igneous rock that forms depends on several factors, including:
- Composition of magma
- Temperature and pressure
- Cooling rate
- Presence of volatile elements
Extrusive rocks are formed from magma that flows out onto the Earth's surface. When magma erupts from a volcano, it cools and solidifies quickly, forming extrusive rocks such as:
- Lava flows: Formed when magma flows out of a volcano as a continuous stream.
- Ash flows: Formed when hot, gas-rich magma explodes and fragments into ash particles that flow down the volcano's slopes.
- Pumice: A light, porous rock formed when gas bubbles in magma expand and freeze during cooling.
- Scoria: A dark, vesicular rock formed when gas bubbles in magma rupture during cooling.
Intrusive Rocks
Intrusive rocks are formed from magma that cools and solidifies slowly beneath the Earth's surface. Over time, these rocks are exposed by erosion. Examples of intrusive rocks include:
- Batholiths: Large, deep-seated igneous intrusions that form from the cooling of large volumes of magma.
- Dikes: Narrow, vertical sheets of intrusive rock that cut across existing rock formations.
- Sills: Horizontal sheets of intrusive rock that form between layers of existing rock formations.
- Plutons: General term for any large intrusive body of igneous rock, including batholiths, stocks, and laccoliths.
Process of Formation
- Magma Generation: Rocks melt to form magma due to high temperatures, pressure, and the presence of water and other volatile elements.
- Crystallization: As magma cools, minerals crystallize and the magma becomes more solid.
- Solidification: When magma solidifies completely, it forms igneous rock.
- Extrusive Formation: If magma erupts onto the surface, it cools quickly and forms extrusive rocks.
- Intrusive Formation: If magma remains beneath the surface, it cools slowly and forms intrusive rocks.
Factors Affecting Rock Type
The type of igneous rock that forms depends on several factors, including:
- Composition of magma
- Temperature and pressure
- Cooling rate
- Presence of volatile elements
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