Because as an intrusive rock cools underground, it will normally cool more slowly than an extrusive (surface) rock. The slow cooling allows more time for the crystals to grow.
Crystals in intrusive rocks have more time to grow as the magma cools slowly beneath the Earth's surface, allowing for larger crystal sizes to form. In contrast, extrusive rocks cool quickly at the Earth's surface, resulting in smaller crystals due to the rapid cooling process.
Coarse-grained extrusive rocks like dacite typically form under conditions of relatively slow cooling, which allows larger crystals to develop. This often occurs in volcanic environments where magma is expelled from a volcano and cools quickly upon reaching the surface, yet retains some degree of insulation, such as being trapped in a thick lava flow. The presence of gas bubbles and the viscosity of the lava can also influence crystal growth, leading to a textured appearance. However, true coarse-grained textures are more characteristic of intrusive rocks; dacite is generally fine-grained due to rapid cooling, suggesting a need for reconsideration of the classification.
Extrusive, Igneous rocks possibly lavas or ignimbrites.
You would find extrusive igneous rocks. Beyond that it depends on the volcano.
Because as an intrusive rock cools underground, it will normally cool more slowly than an extrusive (surface) rock. The slow cooling allows more time for the crystals to grow.
Crystals in intrusive rocks have more time to grow as the magma cools slowly beneath the Earth's surface, allowing for larger crystal sizes to form. In contrast, extrusive rocks cool quickly at the Earth's surface, resulting in smaller crystals due to the rapid cooling process.
You would expect to find an igneous rock with small crystals near the Earth's surface where the rock cools relatively quickly, such as in volcanic eruptions or magma intrusions that do not have much time to grow large crystals. These rocks are known as volcanic or extrusive igneous rocks.
You would expect a coarse-grained extrusive rock when the magma cools and solidifies slowly underground, allowing larger crystals to form due to extended cooling time. This can happen in magma chambers or in deep-seated volcanic environments where the magma has more time to cool and crystallize before reaching the surface.
Extrusive, Igneous rocks possibly lavas or ignimbrites.
You would find extrusive igneous rocks. Beyond that it depends on the volcano.
Slow cooling in the upper mantle
You would find extrusive igneous rocks. Beyond that it depends on the volcano.
Extrusive rocks produced by an explosive volcano are likely to be dark in color because they cool quickly on the Earth's surface, preventing mineral crystals from forming. This rapid cooling results in a fine-grained texture that appears dark in color due to the presence of minerals like olivine or pyroxene.
Slow cooling in the upper mantle
The largest crystals in a lava flow can typically be found in the center or core of the flow where cooling occurs more slowly, allowing for more extensive crystal growth. These areas are often shielded from rapid cooling by the outer crust of the flow.
extrusive ingeneous rocks