Intrusive Igneous Rocks: Formation and Features — Reading Comprehension

Intrusive igneous rocks form when magma cools slowly beneath the Earth's surface. This slow cooling allows large mineral crystals to grow, giving these rocks their characteristic coarse-grained texture. Unlike extrusive rocks that cool quickly, intrusive rocks remain hidden underground until erosion exposes them over millions of years.

Examples of Intrusive Igneous Rocks

Common intrusive igneous rocks include:

●       Granite – A light-colored rock with visible quartz, feldspar, and mica crystals, often used in countertops and buildings.

●       Diorite – A grayish rock with a mix of light and dark minerals, similar to granite but darker.

●       Gabbro – A dark, heavy rock rich in iron and magnesium, forming much of the oceanic crust.

●       Pegmatite – An extremely coarse-grained rock with exceptionally large crystals, sometimes containing rare minerals.

Characteristics of Intrusive Igneous Rocks

1. Coarse-Grained Texture – Slow cooling creates large, interlocking crystals visible to the naked eye.
2. High Density – Most intrusive rocks are dense and hard due to their mineral composition.
3. Varied Colors – Colors range from light (granite) to dark (gabbro), depending on mineral content.
4. Massive Formations – They often occur in large bodies like batholiths (mountain-sized formations) or dikes (sheet-like intrusions).

Intrusive igneous rocks make up much of Earth's continental crust. Their study helps geologists understand deep Earth processes and ancient mountain-building events. Because of their durability and beauty, many intrusive rocks are valued in construction and decoration.

How do intrusive igneous rocks form?

Which is NOT an intrusive igneous rock?

What texture do intrusive rocks typically have?

Why does granite have visible crystals?

What makes pegmatite unique?

Where are intrusive rocks typically found?

How does gabbro differ from granite?

Why are intrusive rocks important to geologists?