Lithosphere I Endogenetic Processes
Class 9 | Social Science — Geography | Unit 1
Class 9 Unit 1 Geography
Unit 1 Lithosphere 1 Endogenetic Processes
Learning Objectives
- To know about the spheres of the Earth
- To illustrate the internal structure of the Earth
- To study the rock types and its cycle
- To explain the internal processes of the Earth
- To understand the processes of earthquakes and volcanoes
Introduction
The Earth is a unique planet of the Solar family. The Earth is composed of four spheres namely, the lithosphere, the atmosphere, the hydrosphere and the biosphere. This lesson focuses on the internal processes of the Earth. The sequence of lessons generally follows the spheres of the Earth system in a comprehensive manner.
Have you ever wondered what our Earth is made up of? Or what lies underneath the Earth's surface?
"The Earth can physically be described as a ball of rock (the lithosphere), partly covered by water (the hydrosphere) and wrapped in an envelope of air (the atmosphere). To these three physical zones it is convenient to add a biological zone which includes all the living organisms (the biosphere)." Arthur Holmes
1.1 Spheres of the Earth
Earth's surface is a vast area of 510 million square kilometer, where four spheres of the Earth interact. The abiotic spheres are the lithosphere, atmosphere and hydrosphere. The biotic sphere is the biosphere. Together, these spheres constitute the planet, Earth.
1.2 Structure of the Earth
The outer surface and inner core of the Earth are totally different in their nature and structure. The structure of the Earth's interior is divided into three layers namely the crust, the mantle and the core.
- The lithosphere is the solid outer part of the Earth.
- The atmosphere is a thin layer of gases that surrounds the Earth.
- The hydrosphere is the watery part of the Earth's surface including oceans, rivers, lakes and water vapour
- The biosphere is the layer of Earth where life exists.
Do You Know?
The terms 'lithosphere' and 'crust' are not the same. The lithosphere includes the crust and the uppermost part of the mantle. All terrestrial planets have lithosphere. The lithospheres of Mercury, Venus, and Mars are much thicker and more rigid than that of the Earth.
Crust
Crust is the outer layer of the Earth, where we live. It is the skin of our Earth, which ranges between 5 to 30 km. It is the solid and rigid layer of the Earth. The thickness of the crust is greater below the continents than the ocean floor. The crust is classified as continental crust and oceanic crust. The major elements of crust SIAL are Silica (Si) and Aluminium (Al) and SIMA (Si - Silica and MA – Magnesium) Continental Crust is made up of SIAL and Oceanic Crust is made up of SIMA
Mantle
The interior part beneath the crust is called mantle, which is about 2,900 km thick. In the upper part of the mantle, the rock remains solid, whereas in the lower part of the mantle, rocks are in molten form. This molten rock inside the Earth is called 'magma'.
Core
The core is the innermost and hottest layer of the Earth which lies below the mantle. It is composed mainly of Nickel (Ni) and Iron (Fe). Hence it is called NIFE. The core is divided into Solid inner core and Liquid outer core. The presence of large quantities of iron in the core is responsible for the Earth's gravitational force. As the Earth rotates on its axis, the liquid outer core spins over the solid inner core and generates the Earth's magnetic field. This is responsible for the functioning of the magnetic compass. Due to high pressure, the materials in the inner core are unable to move and hence remain solid.
1.3 Rocks
The crust is a storehouse of rocks. An aggregate of minerals on the Earth's crust is called 'rock'. It may be hard and compact like 'granite' or soft as 'clay' or loose as 'sand'.
Do You Know?
The Deepest Place ever reached by human technology vary from time to time. Till 2011 Kola Super Hole (12,262m) in Murmansk, Russia was the deepest place. But in 2012, Z-44 Chavyo Well (12,376m) broke the record, and is supposed to be 15 times the height of Burj Khalifa in Dubai.The exploration of Earth's interior continues.
Types of Rock
Based on formation, rocks are classified as: Igneous, Sedimentary and Metamorphic.
Fact
The ancient city of Petra in Jordan is an example of an entire city carved out of rocks. There are many specimens of magnificent rock-cut architecture in India, like the Ajanta and Ellora caves in Maharashtra, the Aihole and Badami temples in Karnataka, the Konark temple in Odisha and Mamallapuram in Tamil Nadu.
Igneous Rocks
The word 'igneous' is derived from the Latin word Ignis meaning 'Fire'. The interior of the Earth contains very hot molten material called 'Magma'. When the magma reaches the Earth's surface, it is referred to as 'Lava'. The lava on the surface cools down and gets solidified as rocks called igneous rocks. Granite and basalt are examples of such rocks. Igneous rocks are also called Primary or Mother rocks because all other rocks are directly or indirectly formed from them.
Sedimentary Rocks
These sedimentary rocks are named after the latin word 'sediment' meaning ' settle. Rivers, glaciers and winds carry bits of rock and soil and deposit them in layers. After a few million years, these deposits harden into compact rocks and are called Sedimentary rocks. The bodies of plants and animals that fall on the deposits get embedded in the layers and form Fossils. Sandstone, limestone, chalk, gypsum, coal and conglomerate are examples of sedimentary rocks.
Metamorphic Rocks
The term 'metamorphic' is derived from the word 'metamorphosis', which means, 'change of form'. When igneous or sedimentary rocks are subjected to extreme heat and pressure, they undergo a complete change in their form and character that is, in course of time, granite may get transformed to gneiss, basalt to schist, limestone to marble and sandstone to quartzite.
Rock Cycle
The Rock cycle is a continuous process through which igneous, sedimentary and metamorphic rocks are transformed from one form to another.
Activity
Narrate the processes involved in the given rock cycle diagram in your own words.
1.4 Geomorphic Processes
The forces that act from the Earth's interior towards the Earth's surface are called Internal processess or Endogenetic processes. These forces build the landscape and create topographic relief. The forces that act on the surface of the Earth due to natural agents like running water, glacier, wind, waves etc. are called External processes or Exogenetic processes. These external processes tear the landscape down into relatively low elevated plains and shapes the landform created by Endogenetic process.
Internal Processes
The internal processes generate heat and eject materials from deep below the Earth's crust. Internal radioactivity is the principal source of power for this process.
Plate Tectonics
The lithosphere is divided into a number of huge slabs of rocks called 'Tectonic plates.' These tectonic plates are divided into major and minor plates. These plates float independently over the mantle. Collisions of these plates produce mountain ranges and other irregular surface features, both on land and the ocean floor. This phenomenon is called 'plate tectonics'. The movement of tectonic plates is due to thermal energy from the mantle. Now we have a better understanding about the plate movements and its relation to Earthquake and volcanic activities.
Types of Plate Boundaries
- Convergent Boundary - Here the plate moves toward each other and sometimes, a plate sinks under another. The location where the sinking of a plate occurs is called a subduction zone (example) Fold Mountain-Himalayas.
- Divergent Boundary – Here the plates pull away from each other as magma pushes up from the mantle (example) Mid Atlantic Ridge
- Conservative/Transform Boundary – Here the plates slide horizontally past each other. Example San Andres Fault.
Movements of Continental Plates
Due to lateral compressional forces, the plates are forced to move upwards and downwards. This is called 'Folding'. Mountains formed by folding are called fold mountains. The process of folding creates lofty mountain ranges such as the Himalayas and the Alps According to plate tectonics, the plates are in constant motion with an average rate of few centimetres per year. The movement might seem slow, but over millions of years, the plates and the continents riding on them move a long way. For example, about 250 million years ago, the Indian Plate was a part of the Gondwana land, which comprised of modern Africa, Australia, Antarctica, and South America. Approximately 140 million years ago, the Indian plate broke away from the ancient super continent 'Gondwana' and began moving north and collided with Asia. The collision with the Eurasian Plate along the boundary between India and Nepal formed the Orogenic belt that created the Tibetan Plateau and the mighty Himalayan Mountains.
Activity
Here is a list of a few mountains. Ural Mountains, Andes Mountains, Vindhya Range, Alps mountains, Satpura range, Rocky Mountains, Sierra Nevada. Identify and Locate with help of atlas
Earthquake
Earthquakes are generally caused by the sudden vibrations in the Earth's crust, which spreads outward in all directions as waves from the source of disturbance. The point of origin of an Earthquake is called 'Focus' (Hypocenter) which generates a series of elastic waves. 'Epicentre' is a point on the Earth's surface that lies directly above the focus. The impact of the Earthquake is felt the most at the epicentre.
Seismic Waves
Earthquakes generate seismic waves. The nature, force and speed of these seismic waves depend on the nature of the medium through which it passes. Accordingly, there are three major types of waves. Primary or P-waves are the fastest of all the Earthquake waves and the first to reach the epicentre. These waves pass through solids, liquids and gases, either through push or pull with an average velocity of 5.3 km per second to 10.6 km per second.
Fact
C.F. Richter devised a scale to measure the magnitude of Earthquakes. This scale relates to the energy released at the epicentre and provides an estimation of the severity of an Earthquake. It is an open ended scale. The highest magnitude ever recorded is 9.5 on Richter scale (Bio-Bio, Chile in 1960).
Secondary or S-waves travel only through solids. These transverse waves shake the ground perpendicular to the direction in which they propagate. The average velocity of these waves is 1Km per second to 8 km per second.
Surface Waves (or) L-waves are similar to P-waves but they travel primarily along the ground surface. These waves travel comparatively slower and are the most destructive waves. The average velocity of these waves are 1 km per second to 5 km per second.
Do You Know?
The instrument which records the Earthquake waves is called 'seismograph' or 'seismometer'. The science that deals with Earthquakes is called 'seismology'.
Tsunami
The word 'Tsunami' is a Japanese term, meaning harbour waves. It is adopted to describe large seismically generated sea waves caused by Earthquakes, submarine explosions and landslides. These waves travel at a great speed (more than 500 km per hour) and the length of the waves exceeds 600 km. These waves reach to a height of more than 15 m near the sea shore and are capable of causing destruction along the coastal area. The 2004 Indian Ocean Earthquake that caused tsunami is the sixth-deadliest natural disaster which travelled at a speed of 600 km per hour with an estimated death toll of 2,80,000. The Earthquake which occurred near Indonesia at 00.58 hours took nearly 7 hours to reach Chennai.
Do You Know?
On 26 December 2004 a tsunami occurred in the Indian Ocean. It was the result of the Indio-Australian Plate subducting below the Eurasian Plate. It was caused by an Earthquake measuring a magnitude of above 9 in the Richter scale. The Earthquake caused the seafloor to uplift, displacing the seawater above.
Volcanoes
A volcano is a vent or an opening on the surface of the Earth crust, through which hot solid, liquid and gaseous materials (Magma) erupt out to the surface from the Earth's interior. Magma rises up and ejects on the surface as Lava. Volcanoes are also formed when plates move apart. Volcanoes generally have the following major components. They are: 1. Magma chamber - a large pool of liquid rock found beneath the surface of the Earth (2). Vents - an opening serving as an outlet for air, smoke, fumes, magma etc (3). Volcanic cone - a landform built by the magma ejected from the vent in the shape of a cone. (4). Crater - a bowl shaped depression found at the top of the volcano through which the magma flows out. Based on the periodicity of eruptions, volcanoes are classified into (1). Active volcano, (2). Dormant volcano, (3). Extinct volcano.
Do You Know?
The term 'volcano' is derived from the Latin term VULCAN, which is the name of Roman "God of Fire".
a. Active Volcano
Active volcanoes are those which constantly eject volcanic lava, gases and fragmented materials. Example Mount St. Helens in the United States.
b. Dormant Volcano (or) Sleeping Volcano
Volcanoes that do not show any sign of volcanic activity for a long period of time are known as dormant volcanoes. Sometimes there may be a sudden explosion which may cause unimaginable loss to life and property. Example Mount Fujiyama, Japan
c. Extinct or Dead Volcano
When a volcano permanently stops its volcanic activity, then it is called as extinct or dead volcano Example Mount Kilimanjaro, Tanzania.
Activity
Take a bottle filled with soda. Shake the bottle twice or thrice. Now twist the cap open. What do you observe?
Volcanoes can also be classified based on their structure and composition as composite volcano, shield volcano and dome volcano
d. Composite Volcano
Composite volcano, also known as strata volcano, is a conical volcano built by many layers of hardened lava, pumice and volcanic ash. These are commonly found in the Pacific Ocean Example Mount Fujiyama, Japan
e. Volcanic Dome
A lava dome or volcanic dome is roughly a circular mound formed due to the slow ejection of viscous lava from a volcano. As the lava is rich in silica with intense viscosity, it is prevented from flowing far from its vent. Example Parícutin, Mexico
Hots
Pacific Ring of Fire — Most seismically and volcanically active. Why?
f. Shield Volcano
Shield volcanoes are formed by intense viscous lava. These are shallow depositions with gently sloping sides. Hence the lava flows out in all directions to create a shield. Example Mauna Loa, Hawaii
Distribution of Earthquakes and Volcanoes
Most Earthquakes and volcanic eruptions do not strike randomly, but occur along the plate boundaries. One such area is the Circum-Pacific Ring of Fire, where the Pacific Plate meets many surrounding plates. The Ring of Fire is the most seismically and volcanically active zone in the world. The other distinctive major belts are Mid- Oceanic Ridges ,Mid-Continental Belts and Alpine - Himalayan belt.
Effect of Volcanoes
Constructive Effects
- Volcanic materials enrich the soil fertility that promotes agricultural activities.
- The hot volcanic region helps in generating geothermal energy.
- Many dormant and active volcanoes are the most attractive tourist spots of the world.
- Most of the volcanic materials are used as building materials.
Destructive Effects
- Volcanic eruption causes Earthquakes, flash floods, mud slide and rock fall.
- Lava can travel very far and burn, bury, or damage anything in its path.
- The large amount of dust and ash makes breathing hard and irritable.
- Volcanic eruptions can alter the weather conditions and disrupt transport (Iceland volcanic eruption) in and around the volcanic region.
Recap
- The spheres of the Earth are the lithosphere, atmosphere, hydrosphere and biosphere.
- Earth's interior is divided into three layers - Crust, Mantle and Core.
- Based on composition, the crust, mantle and core are referred to as SIAL, SIMA and NIFE respectively.
- The formation and deformation of landforms on the surface of the Earth are due to continuous internal and external processes.
- The lithosphere is composed of major and minor tectonic plates.
- Earthquake is the shaking or trembling of the Earth's crust.
- Earthquake and volcanoes are useful to understand the Earth's interior.
Exercise
Exercise 1. Choose the correct answer
1. _____ is the rigid outer layer of the Earth.
a. core b. mantle c. Crust d. inner core
2. _____ layer is made up of liquid iron
a. Inner core b. Outer core c. Mantle d. Crust
3. Magma is found in the _____
a. crust b. mantle c. core d. None of the above
4. The movement of tectonic plates is induced by _____ energy.
a. hydel b. thermal c. wave d. tidal
5. In the ancient period, Gondwanaland moved towards _____ direction.
a. north b. south c. east d. west
6. Many million years ago, India was a part of the super continent _____
a. Gondwana b. Laurasia c. Panthalasa d. Pangea
7. The movement of plates that creates stress and tension in the rocks causing them to stretch and cracks result in _____
a. fold b. fault c. mountain d. earthquake
8. _____ refers to a bowl-shaped depression found at the top of the volcano.
a. crater b. vent c. chamber d. volcanic cone
9. The point of origin of an Earthquake is called the _____
a. epicentre b. focus c. seismic wave d. magnitude Exercise 2. Match the following
| 1. Endogenetic process | |
| 2. Mantle | |
| 3. Convergent boundaries | |
| 4. Earthquake | |
| 5. Composite volcano | |
Options: Seismograph, Subduction Zone, Volcanic, Pacific Ocean, SIMA
Exercise 3. Consider the given statements
1. Consider the statements:
1. Mount Fujiyama is a dormant volcano.
2. Mount Kilimanjaro is a dormant volcano.
3. Mount Tanzania is a dormant volcano.
Which of the statement(s) is/are true?
a. 1 is true b. 2 is true c. 3 is true d. 1, 2, 3 are true
2. Statement: Magma gushes out when it finds vents.
Reason: Interior of the Earth contains compressed hot magma
Which of the statement is are true
a. Statement & reason are true b. Statement is true, reason is false c. Statement is false reason is true d. Statement & reason are false
3. Statement 1: Mountain ranges are formed by the collision of tectonic plates
Statement 2: The movement of tectonic plates is due to the thermal energy from the mantle
a. Statement 1 is false 2 is true b. Statement 1 and 2 are false c. Statement 1 is true 2 is false d. Statement 1 and 2 are true Exercise 4. Answer in brief
1. Write a brief note on the various spheres of the Earth.
2. Mention the layers of the interior of the Earth.
3. Define Plate tectonics.
4. What is Tsunami?
5. What is a Volcano? Mention its major components.
6. What is an Earthquake and how it occurs?
7. What are seismic waves and mention its types?
8. Write about the Pacific Ring of fire.
Exercise 5. Give Reasons for the following
1. SIAL floats over SIMA
2. Igneous rocks are also called Primary Rocks or Mother rocks.
Exercise 6. Distinguish between
1. Core and crust.
2. Epicentre and Hypocentre
3. Divergent and convergent boundaries.
4. Primary waves and Secondary waves.
5. Shield volcano and volcanic Dome.
Exercise 7. Write answers in a Paragraph
1. Describe the structure of the Earth.
2. Write a note on the internal and external processes of Earth.
3. How are volcanoes classified based on the periodicity of their eruptions?
4. Explain the effects of Volcanoes.
Exercise 8. Map Skill
On the given outline map of the world, mark the following:
a. Pacific Ring of fire
b. Earthquake prone zones (any two)
c. Locate any two active volcanoes of the world.
d. Himalayas and Alps ranges
Exercise 9. Life Skills
Imagine that you feel tremors or shocks in your locality. What will be your role in saving lives from destruction? List out the Do's and Don'ts.
Book-back Exercises — Questions & Answers
Answers generated strictly from the Samacheer Kalvi textbook content. Attempt each question first, then click "Show Answer" to check.
1. Choose the correct answer
1. _____ is the rigid outer layer of the Earth.
a) core b) mantle c) Crust d) inner core
Answer: c) Crust
Explanation: Crust is the outer layer of the Earth, where we live. It is the solid and rigid layer of the Earth.
2. _____ layer is made up of liquid iron
a) Inner core b) Outer core c) Mantle d) Crust
Answer: b) Outer core
Explanation: The core is divided into solid inner core and liquid outer core. As the Earth rotates on its axis, the liquid outer core spins over the solid inner core.
3. Magma is found in the _____
a) crust b) mantle c) core d) None of the above
Answer: b) mantle
Explanation: In the upper part of the mantle, the rock remains solid, whereas in the lower part of the mantle, rocks are in molten form. This molten rock inside the Earth is called 'magma'.
4. The movement of tectonic plates is induced by _____ energy.
a) hydel b) thermal c) wave d) tidal
Answer: b) thermal
Explanation: The movement of tectonic plates is due to thermal energy from the mantle.
5. In the ancient period, Gondwanaland moved towards _____ direction.
a) north b) south c) east d) west
Answer: a) north
Explanation: Approximately 140 million years ago, the Indian plate broke away from the ancient super continent 'Gondwana' and began moving north and collided with Asia.
6. Many million years ago, India was a part of the super continent _____
a) Gondwana b) Laurasia c) Panthalasa d) Pangea
Answer: a) Gondwana
Explanation: About 250 million years ago, the Indian Plate was a part of the Gondwana land, which comprised of modern Africa, Australia, Antarctica, and South America.
7. The movement of plates that creates stress and tension in the rocks causing them to stretch and cracks result in _____.
a) fold b) fault c) mountain d) earthquake
Answer: d) earthquake
Explanation: Earthquakes are generally caused by the sudden vibrations in the Earth's crust due to movement of tectonic plates.
8. _____ refers to a bowl-shaped depression found at the top of the volcano.
a) crater b) vent c) chamber d) volcanic cone
Answer: a) crater
Explanation: Crater is a bowl shaped depression found at the top of the volcano through which the magma flows out.
9. The point of origin of an Earthquake is called the _____
a) epicentre b) focus c) seismic wave d) magnitude
Answer: b) focus
Explanation: The point of origin of an Earthquake is called 'Focus' (Hypocenter) which generates a series of elastic waves.
(2). Match the following
1. Match the Following
| Column A | Column B |
| 1. Endogenetic process | a) Seismograph |
| 2. Mantle | b) Subduction Zone |
| 3. Convergent boundaries | c) Volcanic |
| 4. Earthquake | d) Pacific Ocean |
| 5. Composite volcano | e) SIMA |
Answers: 1-c, 2-e, 3-b, 4-a, 5-d
(3). Consider the given statements
1. 1. Mount Fujiyama is a dormant volcano. 2. Mount Kilimanjaro is a dormant volcano. 3. Mount Tanzania is a dormant volcano. Which of the statement(s) is/are true?
a) 1 is true b) 2 is true c) 3 is true d) 1, 2, 3 are true
Answer: a) 1 is true
Explanation: Mount Fujiyama, Japan is an example of dormant volcano. Mount Kilimanjaro, Tanzania is an extinct volcano.
2. Statement: Magma gushes out when it finds vents. Reason: Interior of the Earth contains compressed hot magma Which of the statement is are true
a) Statement & reason are true b) Statement is true, reason is false c) Statement is false reason is true d) Statement & reason are false
Answer: a) Statement & reason are true
Explanation: A volcano is a vent or an opening on the surface of the Earth crust, through which hot magma erupts. The interior of the Earth contains very hot molten material called 'Magma'.
3. Statement 1: Mountain ranges are formed by the collision of tectonic plates Statement 2: The movement of tectonic plates is due to the thermal energy from the mantle
a) Statement 1 is false 2 is true b) Statement 1 and 2 are false c) Statement 1 is true 2 is false d) Statement 1 and 2 are true
Answer: d) Statement 1 and 2 are true
Explanation: Collisions of tectonic plates produce mountain ranges. The movement of tectonic plates is due to thermal energy from the mantle.
(4). Answer in brief:
1. Write a brief note on the various spheres of the Earth.
Answer: The Earth is composed of four spheres namely, the lithosphere, the atmosphere, the hydrosphere and the biosphere. The lithosphere is the solid outer part of the Earth. The atmosphere is a thin layer of gases that surrounds the Earth. The hydrosphere is the watery part of the Earth's surface including oceans, rivers, lakes and water vapour. The biosphere is the layer of Earth where life exists.
2. Mention the layers of the interior of the Earth.
Answer: The structure of the Earth's interior is divided into three layers namely the crust, the mantle and the core. Crust is the outer layer ranging between 5 to 30 km. The mantle is the interior part beneath the crust about 2,900 km thick. The core is the innermost and hottest layer composed mainly of Nickel and Iron.
3. Define Plate tectonics.
Answer: The lithosphere is divided into a number of huge slabs of rocks called 'Tectonic plates.' These plates float independently over the mantle. Collisions of these plates produce mountain ranges and other irregular surface features. This phenomenon is called 'plate tectonics'.
4. What is Tsunami?
Answer: Tsunami is a Japanese term meaning harbour waves. It describes large seismically generated sea waves caused by Earthquakes, submarine explosions and landslides. These waves travel at great speed (more than 500 km per hour) and can reach heights of more than 15 m near the seashore.
5. What is a Volcano? Mention its major components.
Answer: A volcano is a vent or opening on the Earth's surface through which hot magma erupts. Major components are: (1) Magma chamber - a large pool of liquid rock beneath the surface (2) Vents - openings for magma ejection (3) Volcanic cone - landform built by ejected magma (4) Crater - bowl shaped depression at the top.
6. What is an Earthquake and how it occurs?
Answer: Earthquakes are sudden vibrations in the Earth's crust which spread outward in all directions as waves. They occur due to movement of tectonic plates creating stress in rocks. The point of origin is called 'Focus' and the point directly above on Earth's surface is called 'Epicentre'.
7. What are seismic waves and mention its types?
Answer: Earthquakes generate seismic waves whose nature depends on the medium. Three types are: (1) Primary or P-waves - fastest waves passing through solids, liquids and gases (2) Secondary or S-waves - travel only through solids (3) Surface or L-waves - travel along ground surface and are most destructive.
8. Write about the Pacific Ring of fire.
Answer: The Circum-Pacific Ring of Fire is where the Pacific Plate meets many surrounding plates. Most earthquakes and volcanic eruptions occur along plate boundaries. The Ring of Fire is the most seismically and volcanically active zone in the world.
(5). Give Reasons for the following:
1. SIAL floats over SIMA
Answer: Continental Crust is made up of SIAL (Silica and Aluminium) and Oceanic Crust is made up of SIMA (Silica and Magnesium). SIAL is lighter than SIMA, hence SIAL floats over the denser SIMA layer.
2. Igneous rocks are also called Primary Rocks or Mother rocks.
Answer: Igneous rocks are called Primary or Mother rocks because all other rocks are directly or indirectly formed from them. They are formed when hot molten magma cools and solidifies, making them the original rocks from which sedimentary and metamorphic rocks are derived.
(6). Distinguish between
1. Core and crust.
Answer: Crust is the outer layer of Earth where we live, ranging 5-30 km thick, solid and rigid. Core is the innermost hottest layer below the mantle, composed of Nickel and Iron (NIFE), divided into solid inner core and liquid outer core. Core generates Earth's magnetic field.
2. Epicentre and Hypocentre
Answer: Focus (Hypocenter) is the point of origin of an earthquake which generates seismic waves. Epicentre is the point on Earth's surface that lies directly above the focus. The impact of earthquake is felt most at the epicentre.
3. Divergent and convergent boundaries.
Answer: Convergent Boundary is where plates move toward each other and sometimes a plate sinks under another (subduction zone), forming fold mountains like Himalayas. Divergent Boundary is where plates pull away from each other as magma pushes up from mantle, example Mid Atlantic Ridge.
4. Primary waves and Secondary waves.
Answer: Primary (P-waves) are fastest earthquake waves, first to reach epicentre, pass through solids, liquids and gases with velocity 5.3-10.6 km/sec. Secondary (S-waves) travel only through solids, shake ground perpendicular to propagation direction with velocity 1-8 km/sec.
5. Shield volcano and volcanic Dome.
Answer: Shield volcanoes are formed by intense viscous lava with shallow depositions and gently sloping sides, creating a shield shape (example: Mauna Loa, Hawaii). Volcanic dome is a circular mound formed by slow ejection of viscous silica-rich lava that cannot flow far (example: Parícutin, Mexico).
(7). Write answers in a Paragraph
1. Describe the structure of the Earth.
Answer: Earth's interior is divided into three layers: crust, mantle and core. The crust is the outer solid layer (5-30 km thick) classified as continental (SIAL) and oceanic (SIMA) crust. The mantle lies beneath the crust (2,900 km thick) with solid upper part and molten lower part containing magma. The core is the innermost hottest layer composed of Nickel and Iron (NIFE), divided into solid inner core and liquid outer core. The liquid outer core generates Earth's magnetic field as it spins over the solid inner core.
2. Write a note on the internal and external processes of Earth.
Answer: Internal processes or Endogenetic processes are forces acting from Earth's interior towards the surface, building landscapes and creating topographic relief. These generate heat and eject materials from deep below the crust with internal radioactivity as the principal power source. External processes or Exogenetic processes are forces acting on Earth's surface due to natural agents like running water, glacier, wind, and waves. These external processes tear down landscapes into relatively low elevated plains and shape landforms created by endogenetic processes.
3. How are volcanoes classified based on the periodicity of their eruptions?
Answer: Based on periodicity of eruptions, volcanoes are classified into three types: (1) Active volcanoes constantly eject volcanic lava, gases and fragmented materials (example: Mount St. Helens, United States). (2) Dormant or sleeping volcanoes show no volcanic activity for long periods but may suddenly explode (example: Mount Fujiyama, Japan). (3) Extinct or dead volcanoes permanently stop volcanic activity (example: Mount Kilimanjaro, Tanzania). This classification helps predict volcanic behavior and associated hazards.
4. Explain the effects of Volcanoes.
Answer: Constructive effects include: volcanic materials enrich soil fertility promoting agriculture, hot volcanic regions generate geothermal energy, dormant and active volcanoes attract tourism, and volcanic materials are used as building materials. Destructive effects include: volcanic eruptions cause earthquakes, flash floods, mudslides and rock falls, lava travels far burning and burying everything, large amounts of dust and ash make breathing difficult, and eruptions alter weather conditions disrupting transport in volcanic regions. The Iceland volcanic eruption is an example of transport disruption.
📝 Summary
- Earth consists of four spheres - lithosphere (solid rock), atmosphere (gases), hydrosphere (water), and biosphere (living organisms) that interact across Earth's surface area of 510 million square kilometers.
- The Earth's internal structure has three main layers: the crust (5 to 30 km thick outer layer), the mantle (2,900 km thick middle layer with solid upper part and molten lower part), and the core (innermost layer composed of Nickel and Iron).
- The crust is divided into continental crust made of SIAL (Silica and Aluminium) and oceanic crust made of SIMA (Silica and Magnesium), with continental crust being thicker than oceanic crust.
- The core consists of a solid inner core and liquid outer core made of NIFE (Nickel and Iron), which generates Earth's magnetic field as the liquid outer core spins over the solid inner core during Earth's rotation.
- Rocks are aggregates of minerals found in the Earth's crust, ranging from hard and compact like granite to soft like clay or loose like sand, with the crust serving as a storehouse of these rocks.