Home Infographics IAS Exam Preparation via Geography Infographics (8)

IAS Exam Preparation via Geography Infographics (8)

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IAS Exam Preparation of Geography Section via Infographics

You will be tested by UPSC on Questions relating to Geomorphology. Rocks – Types, Characteristics and Related Processes is an important component of Geomorphology.

Geography for IAS Exam Preparation 2016

Topic – Types of Rocks and Related Processes

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Rocks are naturally occurring solid aggregates of minerals or mineraloids.

The Earth’s outer solid layer, the lithosphere, is made of rocks.

The structure and composition of rocks change over time, causing one type of rock to be reclassified as another.

The study of rocks is called petrology.

Types of Rocks

Rocks are broadly classified into 3 categories :

Igneous Rocks

Igneous rocks are rocks which form from the cooling and solidification of magma. Thus they are the results of volcanic processes.
Igneous rocks make up about 90% of the Earth’s crust. However, they are hidden from the surface by a thin layer of sedimentary and metamorphic rocks.
They are crystalline and impervious. They are resistant to erosion and weathering
The geological significance of Igneous rocks is that they come from the mantle. Hence, the minerals and chemistry of igneous rocks give information about the composition of the mantle.
They host important mineral deposits such as uranium, tungsten, tin, chromium, platinum.

Igneous rocks can be of two types

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Intrusive (plutonic) rocks

Intrusive igneous rocks are formed from magma that cools and solidifies within the crust

Extrusive (volcanic) rocks

Extrusive igneous rocks are formed at the surface, from magma released into the surface from volcanic eruptions

Mineral Composition of Igneous Rocks

	Felsic	Mafic	Ultramafic
Intrusive	Granite	Gabbro	Peridotite
Extrusive	Rhyolite	Basalt	Komatite

Did You Know?

The Deccan Traps, one of the largest volcanic features on Earth, is an example of a Large Igneous Province. The Traps consist of multiple layers of basalt, more than 2 km thick and cover an area over 500,000 sq km, and were formed as a result of volcanic eruptions in the Western Ghats about 66 million years ago. It is believed that the enormous volcanic eruptions led to global cooling of around 2C, and were instrumental in the mass extinction of non-avian dinosaurs.

Sedimentary Rocks

Sedimentary rock is the type of rock formed sedimentation of material. This sedimentation can occur on the Earth’s surface or within bodies of water.
Sedimentary rocks form the thin outermost layer of the earth’s crust, making up about 5% of the total volume of the crust.
Sedimentary rocks are deposited in strata called bedding.
Coal is a sedimentary rock.
Examples of sedimentary rocks include shale, sandstone, limestone.
The geological significance of Sedimentary Rocks is that they provide information about subsurface, which is important in civil engineering for construction of roads, bridges.
Sedimentary rocks are also important sources of natural resources like fossil fuels, water, ores etc.

Sedimentary Rocks can be of three types:

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Clastic Sedimentary Rocks

Clastic sedimentary rocks are those that are formed from rocks that have been broken down due to weathering, which are then transported and deposited elsewhere.

Organic Sedimentary Rocks

Organic sedimentary rocks contain materials generated by living organisms. They usually contain carbonate minerals generated by these organisms.

Chemical Sedimentary Rocks

Chemical sedimentary rocks are formed from minerals in solution that become oversaturated. They usually occur as a result of evaporation.

Did you Know?

Sedimentary rocks are the only rocks that contain fossils. Unlike igneous and metamorphic rocks, they form at temperatures and pressures that do not destroy fossils.

Metamorphic Rocks

Metamorphic rocks form as a result of transformation of an existing rock, in a process called metamorphism. The existing rock is called protolith. Metamorphic rocks are formed when the protoliths are subject to extreme temperatures and pressures.
They form from tectonic process, intrusion of magma, or simply by being deep beneath the earth’s surface (being subject to high temperatures and pressures of rock layers above)
Much of the lower continental crust is metamorphic.
Examples of metamorphic rocks include gneiss, slate, marble.

Types of Metamorphic Rocks

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Contact Metamorphic Rocks

Contact metamorphic rocks are those that form when magma is injected into surrounding rock. The cooling magma leads to igneous rocks, and around this is a zone called contact metamorphism aureole where metamorphic rocks are formed.

Regional Metamorphic Rocks

Regional metamorphic rocks are those that form due to metamorphism over a wide area. Regional metamorphism tends to make rocks foliated.