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Igneous Rocks : Characteristics, Types, Example & Significance

Rocks, the solid components of Earth’s crust, consist of various minerals. Though most rocks contain multiple minerals, their compositions can vary by region. Contrary to common belief, not all rocks are hard, as their texture can differ. They serve as a source of minerals and are categorized into three types based on their formation processes: Igneous, formed from cooled lava; Sedimentary, created by the accumulation of particles; and Metamorphic, produced under intense heat and pressure. This classification helps in understanding their distinct characteristics and origins.

Igneous Rocks

Igneous rocks, originating from the Latin word ‘ignis’ meaning “fire,” are primary rocks formed by the cooling and solidification of molten material known as magma.

Key features:



In essence, igneous rocks are a testament to Earth’s fiery internal processes, visible in their diverse textures and compositions.

Characteristics of Igneous Rocks

Igneous rocks, formed deep inside the Earth, are unique for several reasons:

Types of Igneous Rocks

Igneous rocks are fascinating natural formations, broadly categorized into two types based on the process of their formation. These two major types are:

Intrusive Igneous Rocks

Extrusive Igneous Rocks

In summary, igneous rocks vary based on where and how they cool. Each type offers a unique glimpse into Earth’s dynamic processes, from deep below the surface to dramatic volcanic eruptions. Intrusive rocks tell a story of slow, hidden changes, while extrusive rocks capture the swift drama of volcanic activity.

Types of igneous rocks- Mode of occurrence

Three types of igneous are identified based on their mode of occurrence :

Plutonic Rocks

Volcanic Rocks

Hypabyssal Rocks

From the depths of the underworld to the surface we walk on, igneous rocks are natural witnesses to Earth’s dynamic history.

Examples of Igneous Rocks

Rock Name

Colour

Texture

Characteristic Features

1. Rhyolite

Light coloured

  • Fine-grained
  • Often has trapped gas bubbles.
  • Forms from rapidly cooling magma or lava.
  • Rich in silica, like quartz.

2. Granite

Smoky grey or white

Coarse-grained to very coarse-grained

  • Forms deep in the earth.
  • Made from magma, cooling slowly.
  • Contains lots of silica, like quartz.
  • Slow cooling leads to large crystals.

3. Diorite

Medium to dark grey

Coarse-grained

  • Diorite and granite form from magma deep in the earth.
  • Unlike light-coloured granite, diorite lacks quartz and light minerals.
  • It’s composed mainly of dark minerals.

4. Basalt

Dark grey to black

Fine-grained

  • Basalt is a volcanic rock.
  • Formed from iron and magnesium-rich, silica-poor magma.
  • Erupts as lava from volcanoes or fissures.
  • Cools quickly, leading to a fine-grained texture.
  • Sometimes, basalt contains gas bubbles, then it is known as vesicular basalt.

5. Diabase

Dark green to black

Medium grain size

  • Formed from iron and magnesium-rich magma.
  • Poor in silica.
  • Emerges in cracks or layers near the Earth’s surface.
  • Similar to basalt but cools slower.
  • Has slightly larger crystals.
  • Develops larger crystals due to slow cooling.

6. Gabbro

Dark green to black

Large grain size

  • Forms deep underground.
  • Comes from iron and magnesium-rich, silica-poor magma.
  • Slow cooling creates large crystals.
  • Related to basalt and diabase, but with slower formation.

7. Pumice

Light to medium grey

  • Full of gas bubbles, giving a sponge-like appearance.
  • Very lightweight, it often floats in water.
  • May have flow lines or bands.
  • Pumice is formed from explosive volcanic eruptions.
  • It’s made of highly silicic magma, which is thick and sticky.
  • Trapped gases cause the bubbly texture.
  • Similar in composition to granite.
  • Used for exfoliating skin and in abrasive cleaners.

8. Scoria

9. Dark coloured

  • Vesicular Texture
  • Characterized by holes in the rock.
  • Forms at the top of lava flows.
  • Originates from sticky lava.
  • Cools quickly, limiting crystal formation.

10. Obsidian

Black

Glassy

  • Obsidian is a volcanic rock.
  • Forms from quickly cooled, silica-rich lava.
  • Rapid cooling prevents crystal formation.

Significance of Igneous Rocks

Conclusion

Igneous rocks, also called primary rocks which are formed when magma cools and solidifies. About 95% part of the earth’s crust is made up of igneous rocks. Magma (molten rock) cools and crystallises at volcanoes on the Earth’s surface or when the melted rock is still inside the crust, igneous rocks are formed. In essence, igneous rocks are a testament to Earth’s fiery internal processes, visible in their diverse textures and compositions. Igneous rocks vary based on where and how they cool. Each type offers a unique glimpse into Earth’s dynamic processes, from deep below the surface to dramatic volcanic eruptions. Intrusive rocks tell a story of slow, hidden changes, while extrusive rocks capture the swift drama of volcanic activity. From the depths of the underworld to the surface we walk on, igneous rocks are natural witnesses to Earth’s dynamic history.

FAQs- Igneous Rocks

1. Define Igneous Rocks.

Igneous rocks, originating from the Latin word ‘ignis’ meaning “fire,” are primary rocks formed by the cooling and solidification of molten material known as magma.

2. What are the two types of igneous rocks, based on their formation?

Igneous rocks are fascinating natural formations, broadly categorized into two types based on the process of their formation. These two major types are:

  • Intrusive Igneous Rocks
  • Extrusive Igneous Rocks

3. What are the characteristics of igneous rocks?

Igneous rocks, formed deep inside the Earth, are unique for several reasons:

  • Lack of Fossils: Unlike other rock types, igneous rocks don’t contain fossils. The intense heat destroys any potential fossils during the rock’s formation.
  • Mineral Rich: These rocks are often composed of multiple minerals, making them diverse in composition.
  • Texture Variety: Their appearance can vary greatly; some are glassy, while others are coarser.
  • Acid Resistance: Igneous rocks typically don’t react to acids.
  • Mineral Patches: The minerals in these rocks often appear in patches of varying sizes, adding to their distinct look.

4. Name some igneous rocks.

Some igneous rocks are: Scoria, Pumice, Basalt, Diorite, Granite etc.

5. What are the features of igneous rocks.

The key features of igneous rocks are:

  • Formation: They originate from magma, a hot liquid inside the Earth, or lava, which emerges at the surface during volcanic activity.
  • Cooling and Crystallisation:
    • Below Earth’s Surface (Magma): Slow cooling leads to coarse-grained rocks.
    • Above Earth’s Surface (Lava): Rapid cooling results in fine-grained rocks, often with air cavities indicating escaped gas.
  • Texture & Composition: Their texture varies based on crystal shape, size, cooling duration, and mineral composition within the rock. They’re identifiable by their density, colour, and proportion of minerals.
  • Role in Rock Cycle: As the first to form from magma, they begin the rock cycle, earning the title of primary rocks.

In essence, igneous rocks are a testament to Earth’s fiery internal processes, visible in their diverse textures and compositions.


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