A fine-grained igneous rock forms from magma cooling quickly at or near the surface of the Earth. This rapid cooling prevents large mineral crystals from forming, resulting in a fine-grained texture with small mineral grains. Examples of fine-grained igneous rocks include basalt and rhyolite.
The texture of Andesite rock is fine-grained and it Extrusive plus it is an igneous rock .
Igneous rocks tend to be formed from the cooling and solidification of molten magma or lava. They can have a fine-grained or coarse-grained texture, and may contain minerals such as quartz, feldspar, and mica. Examples include basalt, granite, and obsidian.
Glassy textured extrusive igneous rock, such as obsidian.
extrusive igneous rocks =/
Basalt and rhyolite are examples of fine-grained igneous rocks.
Uplift and solidification
Basalt and rhyolite are examples of fine-grained igneous rocks.
Fine-grained igneous rocks are formed when magma cools quickly at or near the Earth's surface, resulting in rapid crystal formation. This rapid cooling prevents large mineral crystals from forming, giving the rock its fine-grained texture. Examples of fine-grained igneous rocks include basalt and rhyolite.
A fine-grained igneous rock forms from magma cooling quickly at or near the surface of the Earth. This rapid cooling prevents large mineral crystals from forming, resulting in a fine-grained texture with small mineral grains. Examples of fine-grained igneous rocks include basalt and rhyolite.
The size of crystals in an igneous rock is called texture. Texture can range from fine-grained (small crystals) to coarse-grained (large crystals).
The texture of Andesite rock is fine-grained and it Extrusive plus it is an igneous rock .
Two examples of fine-grained igneous rocks are basalt and rhyolite. Basalt is a dark-colored rock with a composition rich in iron and magnesium, while rhyolite is light-colored and has a high silica content. Both rocks form from the cooling and solidification of molten magma.
Igneous rocks tend to be formed from the cooling and solidification of molten magma or lava. They can have a fine-grained or coarse-grained texture, and may contain minerals such as quartz, feldspar, and mica. Examples include basalt, granite, and obsidian.
The cooling rate of magma is the primary factor that affects the texture of igneous rocks. Rapid cooling results in fine-grained texture, while slow cooling leads to coarse-grained texture. The mineral composition of the magma also influences the texture, with high silica content producing light-colored and fine-grained rocks, and low silica content resulting in dark-colored and coarse-grained rocks.
Fine grained rocks are considered aphanitic.
Igneous rock that cools quickly may have a fine-grained texture, with small mineral crystals that are not easily visible to the naked eye. Examples include basalt and rhyolite.