ROCKS
   Presented By
   MD NURUDDIN
   SURVI SONL
   B.TECH(BIOTECH)
   SHARDA UNIVERSITY
What are Rocks?
 A rock is a naturally occurring
  solid mixture of one or more
  minerals, or organic matter

 Rocks are classified by how they
  are formed, their composition, and
  texture

 Rocks change over time through
  the rock cycle
Igneous Rocks
 Igneous rock begins as magma.
 Igneous rock is formed through the cooling
  and solidification of magma or lava.
 Magma freezes between
  700 °C and 1,250 °C
 Magma is a mixture of
 many minerals
Extrusive and Intrusive rocks
 At the surface, lava hardens to form extrusive rocks
 with tiny crystals or glassy texture.

 Beneath the surface, magma hardens to form intrusive
 rocks with easily visible crystal texture.
Sedimentary Rocks
Sedimentary rocks form when
   sediments harden into rocks
Three Types:
1. Clastic: formed from
   fragments of other rocks.
2. Chemical: formed from
   mineral grains that come out
   of solution.
3. Organic: formed from the
   remains of plants/animals.
Metamorphic Rock
 Meaning to change shape
Metamorphic rocks
“morph” (change) from
existing rock, due to heat,
pressure and chemicals.
 Usually takes place deep in
  the Earth
Types of metamorphism
 Regional Metamorphism: large areas of rock are
 under intense heat/pressure, which occurs during
 mountain-building.

 Contact Metamorphism: when hot magma forces
 itself into overlying rock (intrusions) and bakes the
 rock
Metamorphic Rock
 Foliated - contain aligned grains of flat minerals


Gneiss is foliated
metamorphic rock
that has a banded
appearance and is
made up of granular
mineral s.
Metamorphic Rock
 Non-Foliated – mineral grains are not arranged in
 plains or bands

Marble is a non-
foliated
metamorphic rock
that is produced
from the
metamorphism of
limestone.
THE ROCK CYCLE
The three types of rocks are very closely related:
 Igneous rocks are attacked by erosion and
  weathering to form sediments
 Crustal movements can cause deep rocks to
  reach high temperatures and to melt back into
  magma
 Igneous and sedimentary rocks exposed to
  intense heat and pressure can become
  metamorphic
Rocks

Rocks

  • 1.
    ROCKS Presented By MD NURUDDIN SURVI SONL B.TECH(BIOTECH) SHARDA UNIVERSITY
  • 2.
    What are Rocks? A rock is a naturally occurring solid mixture of one or more minerals, or organic matter  Rocks are classified by how they are formed, their composition, and texture  Rocks change over time through the rock cycle
  • 3.
    Igneous Rocks  Igneousrock begins as magma.  Igneous rock is formed through the cooling and solidification of magma or lava.  Magma freezes between 700 °C and 1,250 °C  Magma is a mixture of many minerals
  • 4.
    Extrusive and Intrusiverocks  At the surface, lava hardens to form extrusive rocks with tiny crystals or glassy texture.  Beneath the surface, magma hardens to form intrusive rocks with easily visible crystal texture.
  • 5.
    Sedimentary Rocks Sedimentary rocksform when sediments harden into rocks Three Types: 1. Clastic: formed from fragments of other rocks. 2. Chemical: formed from mineral grains that come out of solution. 3. Organic: formed from the remains of plants/animals.
  • 6.
    Metamorphic Rock  Meaningto change shape Metamorphic rocks “morph” (change) from existing rock, due to heat, pressure and chemicals.  Usually takes place deep in the Earth
  • 7.
    Types of metamorphism Regional Metamorphism: large areas of rock are under intense heat/pressure, which occurs during mountain-building.  Contact Metamorphism: when hot magma forces itself into overlying rock (intrusions) and bakes the rock
  • 8.
    Metamorphic Rock  Foliated- contain aligned grains of flat minerals Gneiss is foliated metamorphic rock that has a banded appearance and is made up of granular mineral s.
  • 9.
    Metamorphic Rock  Non-Foliated– mineral grains are not arranged in plains or bands Marble is a non- foliated metamorphic rock that is produced from the metamorphism of limestone.
  • 10.
    THE ROCK CYCLE Thethree types of rocks are very closely related:  Igneous rocks are attacked by erosion and weathering to form sediments  Crustal movements can cause deep rocks to reach high temperatures and to melt back into magma  Igneous and sedimentary rocks exposed to intense heat and pressure can become metamorphic