This document summarizes the key characteristics and formation processes of the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and solidification of magma. Sedimentary rocks are formed at the Earth's surface from the compaction and cementation of sediments. Metamorphic rocks are formed from the alteration of existing rocks through heat, pressure, and chemical changes in the Earth's crust.
weathering is the process of disintegration (physical breakdown) and decomposition (chemical breakdown) of rocks and minerals. In physical weathering, rocks are reduced in size but the chemical composition remains unaltered. In contrast, chemical weathering alter the chemical composition of rocks by changing the mineral constitutes. In weathering, primary minerals are decomposed to form secondary minerals. Weathering plays a vital role in soil formation.
weathering is the process of disintegration (physical breakdown) and decomposition (chemical breakdown) of rocks and minerals. In physical weathering, rocks are reduced in size but the chemical composition remains unaltered. In contrast, chemical weathering alter the chemical composition of rocks by changing the mineral constitutes. In weathering, primary minerals are decomposed to form secondary minerals. Weathering plays a vital role in soil formation.
Can you solve these questions please with clear explanation Describe.pdfAmansupan
Can you solve these questions please with clear explanation Describe the main difference
between Kaolinite and Montmorillonite clay minerals Differentiate between Sedimentary,
Igneous and metamorphic Rocks. Identify the main Transportation agents for the following
types of soil. Wind Sea (salt water) Lake (fresh water) River\" Ice
Solution
Minerals-Montmorillonite
Minerals-Kaolinite
The main difference between Igneous, Sedimentary and Metamorphic rocks, is the way that they
are formed, and their various textures.
Igneous Rocks
Igneous rocks are formed when magma (or molten rocks) cool down, and become solid. High
temperatures inside the crust of the Earth cause rocks to melt, and this substance is known as
magma. Magma is the molten material that erupts during a volcano. This substance cools down
slowly, and causes mineralization to take place. Gradually, the size of the minerals increase until
they are large enough to be visible to the naked eye. Igneous rocks are mostly formed beneath
the Earth’s surface.
The texture of Igneous rocks can be referred to as Phaneritic, Aphaneritic, Glassy (or vitreous),
Pyroclastic or Pegmatitic. Examples of Igneous Rocks include granite, basalt and diorite.
Sedimentary Rocks
Sedimentary rocks are usually formed by sedimentation of the Earth’s material, and this
normally occurs inside water bodies. The Earth’s material is constantly exposed to erosion and
weathering, and the resulting accumulated loose particles eventually settle, and form
Sedimentary rocks. Therefore, one can say, that these types of rocks are formed slowly from the
sediments, dust and dirt of other rocks. Erosion takes place due to wind and water. After
thousands of years, the eroded pieces of sand and rock settle, and become compacted to form a
rock of their own.
Sedimentary rocks range from small clay-size rocks to huge boulder-size rocks. The textures of
Sedimentary rocks are mainly dependent on the parameters of the clast, or the fragments of the
original rock. These parameters can be of various types, such as surface texture, round, spherical
or in the form of grain. The most common type of Sedimentary rock is the Conglomerate, which
is caused by the accumulation of small pebbles and cobbles. Other types include shale, sandstone
and limestone, which is formed from clastic rocks and the deposition of fossils and minerals.
Metamorphic Rocks
Metamorphic rocks are the result of the transformation of other rocks. Rocks that are subjected to
intense heat and pressure change their original shape and form, and become Metamorphic rocks.
This change in shape is referred to as metamorphism. These rocks are commonly formed by the
partial melting of minerals, and re-crystallization. Gneiss is a commonly found Metamorphic
rock, and it is formed by high pressure, and the partial melting of the minerals contained in the
original rock.
Metamorphic rocks have textures like slaty, schistose, gneissose, granoblastic or hornfelsic.
Examples of these types .
Igneous rocks are formed by the cooling or solidification of magma or lava.
Sedimentary rocks are formed by the compaction and cementation of sediments, a process called lithification.
Metamorphic rocks are formed by preexisting rocks that are exposed to extreme heat and pressure in the
Earth’s interior, a process called metamorphism.
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2. Rocks ----SYLLABUS
Difference between minerals and rocks,
Types of rocks:
Igneous,
Sedimentary,
Metamorphic,
Their characteristics
Formation.
3. Introduction
Rocks can be defined as aggregate of minerals .
They are mixture of various minerals in different proportions.
It may hard or soft.
Minerals
Solid inorganic substance occurring naturally.
Having a definite chemical composition and physical
A rock having a large proportion of a single mineral is called
ore of the mineral.
4. Difference between rocks and minerals
Earth is made up of rocks and minerals
Earth’s outer layer made up of solid rock that is why it is called Lithosphere.
ROCKS MINERALS
Aggregate of minerals Solid inorganic substance occurring naturally.
No definite chemical composition Definite chemical composition.
Minerals are organized to form rocks Elements (pure substance )are organized to form
compounds
3 main types- Igneous, Sedimentary, Metamorphic
ISM
4main groups
Silicates Carbonates, Sulphides ,Metallic Minerals----SCSM
Basalt, granite, sand stone, slate et Iron, silicon, magnesium, nickel etc
5. Characteristics of Igneous Rocks
They are hard, massive and compact.
They are formed by solidification of molten magma.
The size of rocks depends upon the rate of cooling of lava or magma.
They are granular and crystalline.
They do not have layers.
These rocks are not easily weathered because there are no pores so
water cannot easily enter.
They are found mostly in volcanic regions.
7. Igneous--- Formation
Comes from the Latin word ignis which means fire.
Igneous rocks form when magma (molten rock) cools and
crystallizes.
Due to high temperature in the interior of the earth the rocks
are in a molten state.
This molten material is called as Magma.
Magma is ejected from the interior of the earth to the surface
through the volcanic activity.
Since they were the first rocks to be formed so igneous rocks
are also called the primary rocks.
8. Characteristics-Sedimentary rocks
Sedimentary rocks are found in layers. So they are known as stratified
rocks.
They have plant and animal remains.so they may contain fossils.
They have pores in which water can easily enter.
They do not have any type of crystals.
These rocks are prone to weathering because they are soft.
These hold all reserves of coal, oil and natural gas.
They constitute above 75% of the surface of the earth.
9. Sedimentary rocks – Formation
Sedimentary rocks are formed through consolidification of accumulated
Sediments deposited on huge depressions like sea or lake.
weathering of pre-existing rocks
Igneous rocks are exposed on the surface of the earth, they are broken down, (sediments) due to
temperature, water, wind etc
Transport of the weathering products
Carried away by the rivers , glaciers and ocean waves.
Deposition of the material
Weathering materials (sediments) deposited in the rivers ,seas, lakes over a long period
Cementation of the sediment to form rock.
and get cemented together and formed as sedimentary rocks
They are called Secondary rocks because they are formed by the solidification of original igneous rocks,
sedimentary or metamorphic parent rocks.
Lithification: the process that turns loose sediments into rocks.
10.
11. Characteristics of metamorphic rocks
Very hard and more compact than their original form.
Eg: marble is harder than from limestone.
Are formed due to change in texture and composition of the pre-existing rocks.
Most of them are impermeable.-they do not allow water to percolate through
them.
They do not have fossils – during formation they destroy fossils.
New minerals are formed during the processes of metamorphism.
12. Metamorphic rocks-- Formation
Formed by the effect of the heat and pressure on existing rocks.
Original rock is transformed in a process is called metamorphism.
The original rock can be either igneous or sedimentary or old metamorphic.
The original rock change in its physical and chemical composition.
The original rocks are metamorphosed to produce new rocks. Limestone into marble,
shale to slate , coal into graphite.
Causes for change 1. High temperature 2. Pressure at great depth.
Metamorphism can be two types:
1.Contact or thermal due to heat or temperature. It involves solidification and
crystallization.
2. Regional or dynamic metamorphism. Is a result of excessive pressure and reluctant
heat caused earth movement.