Some Natural Phenomena Class 8

Natural Phenomena

A natural phenomenon refers to any observable event or occurrence that happens in the natural world without direct human intervention. These events are often driven by the laws of nature, including physical, chemical, geological, and biological processes. Natural phenomena can be both large-scale and small-scale, ranging from everyday occurrences to rare and significant events.

A few examples of natural phenomena are:

Earthquakes: The sudden shaking or trembling of the Earth's surface due to the movement of tectonic plates. Earthquakes can cause significant damage and are caused by natural processes within the Earth's crust.

Volcanic Eruptions: The eruption of molten rock, ash, and gases from a volcano. This occurs when pressure builds up within the Earth's crust and is released through a vent.

Thunderstorms: These are intense weather events characterised by lightning, thunder, heavy rain, and strong winds. Thunderstorms result from atmospheric instability and the interaction of warm and cold air masses.

Auroras: Also known as the Northern and Southern Lights, auroras are colourful displays of light in the sky near the polar regions. They are caused by the interaction of charged particles from the sun with Earth's magnetic field.

Tides: The rise and fall of sea levels is caused by the gravitational forces between the Earth, the moon, and the sun. Tides affect ocean currents and coastal ecosystems.

Solar and Lunar Eclipses: Eclipses occur when the Earth, moon, and sun align in a way that causes one to cast a shadow on the other. Solar eclipses happen when the moon blocks the sun's light, and lunar eclipses occur when the Earth's shadow falls on the moon.

Rainbows: A colourful arc of light in the sky caused by the refraction, dispersion, and reflection of sunlight in water droplets in the atmosphere.

Tornadoes: Violently rotating columns of air extending from a thunderstorm to the ground. Tornadoes are capable of causing extreme damage due to their high winds.

These natural phenomena are just a few examples of the countless events that occur in the natural world without direct human influence. They are driven by the fundamental processes and forces that shape our planet and the universe at large.

Static Charge

Static charge is a phenomenon involving the accumulation of electric charges on the surface of objects through the process of rubbing. These charges, referred to as static charges, result from the transfer of electrons between objects.

Key Points

a) Charging by Friction: When two objects are rubbed against each other, such as plastic and hair, or glass and silk cloth, they can become charged. As the objects rub together, charged particles are transferred from one object to the other.

b) Types of Charges: There are two types of electric charges: positive and negative charges. Electrons are negatively charged, and when they move from one object to another, they cause an imbalance of charges.

c) Acquiring Charges: When objects are rubbed together, one object may gain electrons (becoming negatively charged) while the other loses electrons (becoming positively charged). The exchange of electrons creates an electric charge imbalance on the surfaces of the objects.

d) Equal and Opposite Charges: When two objects are charged by rubbing against each other, they acquire equal and opposite charges. For example, if one object gains a positive charge, the other object gains an equal amount of negative charge.

e) Attraction and Repulsion: Objects with opposite charges attract each other. This is why a positively charged object will attract a negatively charged object. On the other hand, objects with the same charge repel each other. Positive charges repel other positive charges, and negative charges repel other negative charges.

f) Testing for Charge: Repulsion is a reliable test to determine whether an object is charged. If two objects repel each other, it indicates that they carry the same type of charge. Conversely, if they attract each other, they carry opposite charges.

Transfer of Charges

The transfer of electric charges is a fundamental aspect of electrostatics and involves various methods by which charges can be moved from one object to another. There are three main methods of transferring charges: conduction, induction, and friction.

a) Conduction: Conduction refers to the transfer of electric charges between objects that are in direct contact. When a charged object comes into contact with a conductor (a material that allows the free movement of electrons), the charges can flow from one object to the other. This occurs because electrons in the conductor can easily move, allowing the charges to redistribute until both objects reach a balanced state.
For example, if a negatively charged object touches a neutral conductor, some of its excess electrons will flow into the conductor, causing it to become negatively charged as well.

b) Induction: Induction involves the redistribution of charges in a neutral object when it is brought near a charged object. However, unlike conduction, there is no direct contact between the two objects. The presence of the charged object induces a temporary separation of charges within the neutral object.
For instance, if a negatively charged object is brought close to a neutral conductor, the electrons in the conductor will be repelled by the negatively charged object and move to the farther end of the conductor, leaving a positive charge at the end closest to the charged object.

c) Friction: Friction is the process by which charges are transferred between two objects as a result of rubbing or contact. When two objects are rubbed together, electrons can be transferred from one object to the other due to the triboelectric effect. This effect causes certain materials to gain or lose electrons more easily when they come into contact.
For example, when a plastic comb is rubbed against dry hair, the comb gains a negative charge through the transfer of electrons from the hair.

Gold-leaf Electroscope

A gold-leaf electroscope is a scientific instrument used to detect and measure the presence of electric charge on an object. It can also help determine the nature of the charge (positive or negative).

Components of a Gold-leaf Electroscope

Brass Disc: This is a metal disc at the top of the electroscope where the charged object to be tested is placed.

Insulator Plug: A non-conductive material separates the brass disc from the rest of the electroscope to prevent the charge from leaking away.

Brass Rod: A metal rod extends from the brass disc down into the electroscope.

Glass Bottle: The electroscope's main body is usually a glass bottle that provides a sealed environment to prevent external interference.

Metal Foil: Inside the glass bottle, there are two thin gold or metal foil leaves attached to the brass rod. These leaves are suspended close to each other but not touching.

Earth Connection: A wire connected to the brass rod allows the electroscope to be grounded, helping to discharge the electroscope if needed.

Working of a Gold-leaf Electroscope

a) Detection of Charge: To detect a charge, you touch the object in question with the metal cap of the electroscope. If the leaves move apart, it signifies that the object carries a charge. Conversely, if the leaves remain unchanged, the object lacks any charge.

b) Determining the Charge Nature: To understand the type of charge, we can bring a positively charged object near the metal cap. Then, introduce an unknown object close to the cap. If the leaves diverge even more, it indicates that the unknown object carries a positive charge. Conversely, if the leaves draw closer together, the unknown object holds a negative charge.

c) Neutral Object: If the leaves of the electroscope do not show any movement when brought near both positive and negative charges, it suggests that the electroscope itself is neutral (without a significant charge).

In summary, a gold-leaf electroscope is a valuable tool for detecting and understanding electric charges. It allows scientists and researchers to observe the behaviour of charges and determine whether an object is charged and the nature of that charge.
(add a picture of “Gold-Leaf Electroscope”. Reference image below.)

Earthing

Earthing, also known as grounding, is a process in which the excess electric charge present on a charged object is transferred to the Earth. This is achieved by physically connecting the charged object to the Earth, which acts as a large reservoir of charge that can absorb and neutralise the excess charge on the object. The primary purpose of earthing is to ensure safety by preventing the buildup of potentially harmful electric charges.

Here's how earthing works and its significance:

Transfer of Excess Charge: When an object becomes charged, it can accumulate an excess of either positive or negative electric charges. This excess charge can result from various processes, such as friction, induction, or conduction. If the object is isolated and the excess charge cannot dissipate, it can potentially create a dangerous situation or damage electronic equipment.

Connecting to Earth: To prevent the buildup of excess charge and its associated risks, the charged object is connected to the Earth through a conductive pathway, such as a metal wire or a conductive plate embedded in the ground. The Earth acts as a "sink" for the excess charge, allowing it to flow from the object into the Earth.

Neutralisation: As the excess charges flow through the grounding pathway and into the Earth, they get dispersed and neutralised. The Earth's vast size and ability to readily absorb charge make it an ideal candidate for this purpose.

Safety and Equipment Protection: Earthing is crucial for ensuring safety in various scenarios. For instance, in electrical systems and appliances, earthing helps prevent the buildup of static charge, reduces the risk of electric shock, and protects against damage from voltage surges or lightning strikes. Grounding also plays a vital role in preventing fires caused by electrical faults.

Discharged Object: Once the excess charge has been transferred to the Earth, the object becomes electrically neutral or discharged. This means it no longer carries an excess of positive or negative charge and is in a balanced state.

Lightning

Lightning is a natural phenomenon that involves a powerful discharge of electricity between different areas within a cloud, between different clouds, or between a cloud and the Earth's surface. It typically occurs during thunderstorms and is often accompanied by a bright flash of light, a loud thunderclap, and sometimes even destructive effects.

Process of Lightning

Charge Separation: During a thunderstorm, strong air currents within the clouds cause the movement of water droplets and ice particles. These particles collide with each other, leading to a separation of electric charges.

Accumulation of Charges: As the separation of charges continues, the negative charges accumulate at the bottom of the cloud, closer to the Earth's surface. Simultaneously, the positive charges accumulate at the top of the cloud.

Induction: The buildup of a negative charge at the bottom of the cloud induces a positive charge on the Earth's surface directly beneath the cloud. This positive charge on the ground is attracted to the negative charge in the cloud above.

Ionisation and Conduction: As the charge separation intensifies and the voltage difference between the cloud and the ground increases, the air between them becomes ionised. Normally, air is a poor conductor of electricity, but ionised air or plasma can conduct electricity. This is why lightning can occur despite the air's typical insulating nature.

Lightning Discharge: Once the voltage difference becomes high enough a highly conductive channel is established extending from air to ground.

Light and Thunder: The rapid flow of charged particles along this conductive channel results in a brilliant flash of light, which we perceive as lightning. The immense heat generated by the electric current also causes the surrounding air to expand rapidly, creating a shockwave that we hear as thunder. The reason we see lightning before hearing thunder is because light travels much faster than sound.

Lightning Safety

Lightning is a powerful force of nature that should be taken seriously. By following these safety guidelines, we can significantly reduce the risk of being injured by a lightning strike during a storm.

Do's:

1. Take Shelter in a Closed Car or Bus: If you're outdoors and caught in a lightning storm, seek shelter inside a fully enclosed vehicle like a car or bus. The metal body of the vehicle helps to conduct the lightning's electrical energy around you and into the ground, keeping you safe.

2. Stay Indoors: The safest place to be during a lightning storm is indoors. Stay away from windows, doors, and electrical appliances. Avoid using corded phones and plumbing fixtures, as lightning can travel through these conduits.

Don'ts:

1. Stay Away from Metal Poles: Metal objects, especially tall ones like flagpoles, light poles, and fences, are attractive targets for lightning strikes. Stay away from them to minimise the risk of being struck indirectly.

2. Avoid Taking Shelter Under a Big Tree: While it might seem like a natural instinct to seek shelter under a tree, it's extremely dangerous during a lightning storm. Trees can conduct the lightning's energy and can be struck directly or indirectly, causing serious harm.

3. Don't Lie on the Ground: Lying flat on the ground increases your chances of being in contact with the ground when lightning strikes. This can lead to a dangerous pathway for the electrical energy to travel through your body. Instead, crouch down with your head tucked in and minimise your contact with the ground.

Lightning Conductor

a) A lightning conductor, also known as a lightning rod or lightning rod system, is a safety device designed to protect buildings and structures from the damaging effects of lightning strikes.
b) It works by providing a safe pathway for lightning's electrical energy to travel from the point of impact to the ground, effectively directing the lightning away from the structure and preventing potential fires, explosions, or structural damage.

Working of a Lightning Conductor:

1. Structure Installation: A lightning conductor is typically installed on the highest point of a building, tower, or structure. It consists of a metallic rod or a network of conductive materials.

2. Pathway for Lightning: When a lightning strike occurs, it is attracted to the lightning conductor due to its elevated position and the conductive material it's made of. This prevents the lightning from seeking a path through the building's materials, which could cause damage.

3. Grounding and Discharge: When lightning strikes the lightning conductor, the electrical energy follows the conductive path down to the ground. The grounding system ensures that the energy is dispersed harmlessly into the Earth.

4. Protection: By providing a controlled and safe pathway for lightning's electrical discharge, the lightning conductor prevents the electrical energy from causing fires, explosions, or structural damage to the building.

The concept of the lightning conductor was pioneered by Benjamin Franklin in the 18th century, and it remains a crucial element in modern building design to ensure the safety of structures and their occupants during lightning storms.

Structure of the Earth

The Earth's interior structure is composed of several distinct layers that vary in composition, density, and physical properties. These layers are responsible for the planet's geophysical processes and phenomena.

The main layers of the Earth are:

Crust

a) The Earth's outermost layer is called the crust. It is relatively thin compared to the other layers and is composed primarily of solid rock.
b) The crust is divided into two types: the continental crust, which forms the continents and is thicker and less dense, and the oceanic crust, which makes up the ocean floors and is thinner and more dense.

Earth's Lithosphere

a) Earth's lithosphere, which includes the crust and a portion of the upper mantle, is divided into several tectonic plates.
b) These plates are large sections of the Earth's crust that float on the semi-fluid upper mantle beneath them.
c) The movement of these plates, driven by the convection currents in the mantle, leads to the formation of various geological features, including mountains, earthquakes, volcanoes, and ocean basins.

Mantle

a) Beneath the crust lies the mantle, a thick layer of semi-solid rock that extends to a depth of about 2,900 kilometres (1,800 miles).
b) The mantle is divided into several sections based on their physical properties: the upper mantle (a partially molten, ductile layer), and the lower mantle.
c) The mantle is responsible for the movement of tectonic plates that drive geological processes.

Core

a) The core is the innermost layer of the Earth and is divided into two parts: the outer core and the inner core.
b) The outer core is composed of liquid iron and nickel and is responsible for generating the Earth's magnetic field through the process of convection.
c) The inner core is solid and primarily composed of iron and nickel.

Earthquake

An earthquake is a natural geological phenomenon characterised by the sudden shaking or trembling of the Earth's surface. It occurs due to the movement of rocks in the lithosphere, which is the outermost layer of the Earth.

Key Points

a) Cause of Earthquakes: Earthquakes are primarily caused by the movement or collision of tectonic plates. When these plates move, slide past each other, or collide, they generate stress along fault lines, which are fractures in the Earth's crust.

b) Seismic Focus and Epicentre: The point within the Earth where the earthquake originates is called the seismic focus or hypocentre. It is usually located within the crust. The point on the Earth's surface directly above the seismic focus is known as the epicentre. The intensity of the earthquake is greatest at the epicentre.

c) Tectonic Plate Boundaries: Earthquakes are most likely to occur at the boundaries of tectonic plates. These areas are known as seismic zones or fault zones. The stress and pressure that build up along these boundaries are eventually released in the form of an earthquake when the accumulated energy exceeds the strength of the rocks.

d) Seismic Waves: When an earthquake occurs, it generates seismic waves that radiate outward from the seismic focus.

e) Seismograph: A seismograph is an instrument used to detect and record the seismic waves generated by an earthquake. It consists of a sensitive recording device that measures the vibrations of the Earth's surface. The data collected from seismographs helps scientists analyse and understand the characteristics of earthquakes.

f) Richter Scale: The Richter scale is a logarithmic scale used to measure the intensity of an earthquake. It quantifies the amount of energy released by an earthquake. The scale ranges from 0 to 9, with each whole number increase representing a tenfold increase in amplitude and approximately 31.6 times more energy release.
As the magnitude of an earthquake increases on the Richter scale, the amount of energy released and the potential for destruction also increase significantly.

The relationship between destructive energy and the Richter scale is as follows:

1. An earthquake with a magnitude of 5 is 31.6 times stronger than an earthquake with a magnitude of 4.
2. Magnitude 6 earthquake releases approximately 1000 times more energy than a magnitude 4 earthquake (31.6 x 31.6 = 1000).
3. Magnitude 7 earthquake releases approximately 31,600 times more energy than a magnitude 4 earthquake (31.6 x 31.6 x 31.6 = 31,600). And so on.

Magnitude and Intensity: Magnitude refers to the size of an earthquake as measured on the Richter scale. Intensity, on the other hand, measures the effects of an earthquake on people, structures, and the environment.

Earthquake Safety

Earthquake safety practices are essential to minimise the risk of injury during an earthquake.
Here are some do's and don'ts for earthquake safety:

‘Do’s’ during the Earthquake

1. Outside the House

a) Find a Clear Spot: Move to an open area away from buildings, trees, streetlights, and utility wires. Being in an open space reduces the risk of falling debris.
b) Drop to the Ground: Once in a clear area, crouch down to the ground to make yourself a smaller target and protect yourself from being knocked over.

2. If in a Car

Stay Inside the Car: If you're in a vehicle, stop in a safe location away from buildings, overpasses, and power lines. Stay inside the car until the shaking stops.

3. Inside the House

a) Take Shelter Under Sturdy Furniture: During an earthquake, seek shelter under a sturdy piece of furniture such as a table, desk, or bed. This can provide protection from falling debris.
b) Stay Indoors: If you're indoors, stay there. Moving around during the shaking can put you at greater risk of injury.

‘Don'ts’ during the Earthquake

a) Don't Stand Near Windows: Stay away from windows, glass doors, and mirrors. Shattered glass can be extremely dangerous during an earthquake.
b) Avoid Doorways: Contrary to popular belief, doorways are not necessarily the safest place to be during an earthquake. Taking cover under sturdy furniture is generally a better option.
c) Don't Use Elevators: Avoid using elevators during an earthquake, as they can become stuck or malfunction during shaking.
d) Don't Panic: While it's natural to feel scared during an earthquake, try to remain calm. Panicking can lead to poor decision-making.
e) Don't Rush Outside: It's not always safer to run outside during an earthquake, especially if you're in a tall building. Falling debris can pose a significant hazard.

After the Shaking Stops:

a) Check for Injuries: Once the shaking stops, check yourself and those around you for injuries. Provide first aid as necessary.
b) Be Prepared for Aftershocks: Aftershocks are smaller tremors that can follow a larger earthquake. Be prepared for them and take the same safety precautions as during the initial quake.

Remember that earthquake safety practices can vary depending on the specific situation and the severity of the earthquake. It's important to educate yourself and your family on how to respond appropriately to earthquakes based on your local area's earthquake risk and building codes.

Frequently Asked Questions

1. What causes thunderstorms?

Thunderstorms are created by the sudden upward movement of warm, wet air colliding with colder air. The impact causes cloud formations called cumulonimbus to develop, which can generate lightning, thunder, heavy rain and in certain cases hailstorms.

2. How do earthquakes occur?

A: Earthquakes occur when there is a rapid release of energy in the Earth's crust, which causes vibrations. This release of energy can be triggered by tectonic plate movement, volcanic activity or human-made events like mining or reservoir-induced shaking.

3. What is lightning and how is it formed?

Lightning is a sudden electrical discharge that happens during thunderstorms. It occurs when ice particles in a cloud meet, creating static electricity. This static energy accumulates until it releases as a lightning bolt, usually between the cloud and the earth or between two clouds.

4. How are tornadoes formed?

Tornadoes develop from intense thunderstorms known as supercells. Wind shear in severe storms creates horizontal spinning columns of air. If the storm's updrafts tilt the rotation vertically, it can form a tornado, which is a fast-spinning column made up of air that extends from the thunderstorm to the ground.

5. What causes the formation of rainbows?

Rainbows arise when sunlight is refracted, or twisted, when it enters a raindrop, reflects off the drop's interior surface, and eventually escapes. This process allows sunlight to divide into its component colours, which will result in a rainbow-like spectrum.