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Some Natural Phenomena

Some Natural Phenomena relates to CBSE/Class 8/Science

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1
S. Hemaa Class 8 Tuition trainer in Bangalore Featured
AECS Layout, Marathahalli, Bangalore
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375per hour
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Very successful and satisfying.Regardless of how hard we try some students won't pay attention and some students will score less marks. It's is how...

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Avishake Chatterjee Class 8 Tuition trainer in Kolkata Featured
Behala, Kolkata
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As a passionate mathematics teacher, I have always enjoyed imparting knowledge to others. I am a B.Tech graduate in Electronics and Communication....

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Deepak Joshi Class 8 Tuition trainer in Bangalore Featured
Ashok Nagar D' Souza Layout, Bangalore
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Ph.D candidate with over 10 years of teaching exp. (7 years at BYJU's and 3 years at DPS Gurgaon). Specialized in IGCSE, ICSE & CBSE curricula.

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Megha A. Class 8 Tuition trainer in Lucknow Featured
LDA Colony, Lucknow
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The experience of teaching Maths in grade 8 is wonderful.This is the time when students develop a phobia of Maths.Removing that phobia with my techniques...

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Jayesh Chaudhari Class 8 Tuition trainer in Mumbai Featured
Kharghar Sector 27, Mumbai
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**Teaching Methodology:** My approach to teaching Mathematics and Science is personalized and interactive. I focus on understanding each student's...

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Pooja Patel . Class 8 Tuition trainer in Indore Featured
Scheme No 114, Indore
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4 yrs of Exp
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I bring over five years of hands-on experience in mathematics and science, making complex topics easy to understand. My deep knowledge in areas like...

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Whitefield, Bangalore
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20 yrs of Exp
400per hour
Classes: Class 8 Tuition, Hindi Language and more.

20 years

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Debabrato Chatterjee Class 8 Tuition trainer in Thane Featured
Thane West, Thane
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This is Debabrato Chatterjee online Maths and Science tutor having 13+years of experience. I have already and presently teaching students of IB,...

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Ottapalam, Ottapalam
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Classes: Class 8 Tuition, Class 6 Tuition and more.

I am a resident of Kerala working in a CBSE school.I got the opportunity of working with Kendreya Vidyalaya (Ottapalam) , Cambridge Public School...

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Ajay A S Class 8 Tuition trainer in Kota Featured
Talwandi Sector-B, Kota
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10 yrs of Exp
849per hour
Classes: Class 8 Tuition, Class 12 Tuition and more.

My teaching exp.11 year in most reputed coaching in india. Mentor of jee top rank air-12 yatis agrawal, 19, 28 many more in top 100 in jee adavnced....

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Answered on 21/02/2024 Learn CBSE/Class 8/Science/Some Natural Phenomena

Sadika

When a glass rod is rubbed with a silk cloth, the glass rod acquires a positive charge, and the silk cloth acquires a negative charge. This charging occurs due to the triboelectric effect, where electrons are transferred between the two materials during rubbing. Here's a breakdown of what happens: Contact... read more

When a glass rod is rubbed with a silk cloth, the glass rod acquires a positive charge, and the silk cloth acquires a negative charge. This charging occurs due to the triboelectric effect, where electrons are transferred between the two materials during rubbing.

Here's a breakdown of what happens:

  1. Contact and Rubbing: When the glass rod and silk cloth are rubbed together, the surfaces of the two materials come into contact. During this contact, some electrons from the atoms of the silk cloth are transferred to the atoms of the glass rod.

  2. Electron Transfer: The glass rod has a higher affinity for electrons compared to the silk cloth. As a result, electrons from the silk cloth are transferred to the glass rod. This leaves the silk cloth with a net positive charge, as it has lost electrons, and the glass rod with a net negative charge, as it has gained electrons.

  3. Separation: After rubbing, the glass rod and silk cloth are separated. The charges acquired during rubbing remain localized on the surfaces of the materials.

  4. Final Charge: The glass rod is left with a positive charge, and the silk cloth is left with a negative charge. This means that the glass rod and silk cloth attract each other due to their opposite charges.

In summary, when a glass rod is rubbed with a silk cloth, the glass rod becomes positively charged, and the silk cloth becomes negatively charged. This phenomenon is a result of the transfer of electrons between the two materials during rubbing.

 
 
 
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Answered on 21/02/2024 Learn CBSE/Class 8/Science/Some Natural Phenomena

Sadika

Lightning strikes can have severe and potentially fatal consequences for lightning victims due to the high voltage and current associated with the discharge. Some harmful effects of lightning on a lightning victim include: Electric Shock: Lightning carries a massive amount of electrical energy,... read more

Lightning strikes can have severe and potentially fatal consequences for lightning victims due to the high voltage and current associated with the discharge. Some harmful effects of lightning on a lightning victim include:

  1. Electric Shock: Lightning carries a massive amount of electrical energy, typically ranging from 100 million to 1 billion volts, and can generate currents of tens of thousands of amps. When a person is struck by lightning, this electrical energy can pass through their body, causing electric shock. The electric current can disrupt normal nerve and muscle function, leading to paralysis, respiratory failure, and cardiac arrest.

  2. Burns: Lightning can cause burns of varying severity due to the intense heat generated during the discharge. These burns may be superficial (first-degree burns) or extend deeper into the skin (second-degree or third-degree burns). In some cases, lightning can cause thermal injuries such as flash burns or contact burns if the victim comes into direct contact with objects that are heated by the lightning strike.

  3. Cardiac and Neurological Injuries: Lightning strikes can affect the cardiovascular and nervous systems, leading to irregular heart rhythms (arrhythmias), cardiac arrest, and neurological damage. The electric current can disrupt the normal functioning of the heart, causing fibrillation or cardiac arrest. Additionally, lightning-induced injuries to the brain and nervous system can result in cognitive impairment, memory loss, and other neurological deficits.

  4. Internal Injuries: Lightning strikes can cause internal injuries such as ruptured eardrums, internal bleeding, and damage to internal organs. The shockwave produced by the lightning discharge can rupture blood vessels and damage tissues within the body, leading to internal injuries that may not be immediately apparent.

  5. Secondary Injuries: Lightning strikes can also cause secondary injuries due to falls, blunt force trauma, or other accidents resulting from the force of the strike or the victim's sudden loss of consciousness. Lightning victims may be thrown or knocked down by the force of the electrical discharge, leading to injuries such as fractures, concussions, or lacerations.

  6. Psychological Trauma: Lightning strikes can have long-lasting psychological effects on survivors, including post-traumatic stress disorder (PTSD), anxiety, depression, and phobias related to thunderstorms and lightning. The experience of being struck by lightning or witnessing a lightning strike can be extremely traumatic and may require counseling or therapy to address the emotional impact.

Overall, the harmful effects of lightning on a lightning victim can be severe and life-threatening, requiring prompt medical attention and emergency treatment to address the various injuries and complications associated with a lightning strike.

 
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Answered on 21/02/2024 Learn CBSE/Class 8/Science/Some Natural Phenomena

Sadika

Seismic waves are the vibrations or waves of energy that travel through the Earth's interior and along its surface as a result of an earthquake, explosion, or other seismic event. These waves carry the energy released by the seismic source and are responsible for the shaking and ground motion observed... read more

Seismic waves are the vibrations or waves of energy that travel through the Earth's interior and along its surface as a result of an earthquake, explosion, or other seismic event. These waves carry the energy released by the seismic source and are responsible for the shaking and ground motion observed during earthquakes. Seismic waves can be classified into several types based on their motion, speed, and propagation characteristics. The three main types of seismic waves are:

  1. Primary Waves (P-Waves):

    • Primary waves are the fastest seismic waves and are the first to arrive at seismograph stations following an earthquake.
    • They are compressional waves that travel by alternately compressing and expanding the material through which they pass.
    • P-waves can travel through solids, liquids, and gases and are capable of passing through the Earth's interior (mantle and core).
    • They cause particles of the material to vibrate in the direction of wave propagation, similar to the way sound waves travel through air.
  2. Secondary Waves (S-Waves):

    • Secondary waves arrive at seismograph stations after P-waves and are slower than P-waves.
    • They are shear waves that propagate by causing particles of the material to move perpendicular to the direction of wave propagation.
    • S-waves can only travel through solids and are unable to pass through liquids or gases. This property is used to infer the presence of a liquid outer core beneath the Earth's mantle.
    • S-waves cause the ground to move from side to side or up and down as they pass through the Earth's interior.
  3. Surface Waves:

    • Surface waves travel along the Earth's surface and are responsible for much of the shaking and damage observed during earthquakes.
    • They are slower than both P-waves and S-waves and typically arrive at seismograph stations last.
    • Surface waves have two main types: Love waves and Rayleigh waves.
    • Love waves cause horizontal shearing motion in the ground, while Rayleigh waves cause both vertical and horizontal motion, similar to the motion of ocean waves.
    • Surface waves can produce the most significant ground shaking and are responsible for the majority of the damage caused by earthquakes to buildings and infrastructure.

Seismic waves are detected and recorded by instruments called seismographs or seismometers, which measure the motion of the ground caused by the passing waves. Analysis of seismic waves recorded by seismographs provides valuable information about the location, magnitude, depth, and focal mechanism of earthquakes, as well as the Earth's internal structure and composition.

 
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Answered on 21/02/2024 Learn CBSE/Class 8/Science/Some Natural Phenomena

Sadika

The shock waves produced by an earthquake travel outward in all directions from the focus (hypocenter) of the earthquake. These waves propagate through the Earth's interior and along its surface, causing the ground to shake and vibrate as they pass through. There are three main types of seismic waves... read more

The shock waves produced by an earthquake travel outward in all directions from the focus (hypocenter) of the earthquake. These waves propagate through the Earth's interior and along its surface, causing the ground to shake and vibrate as they pass through.

There are three main types of seismic waves produced by an earthquake: Primary (P) waves, Secondary (S) waves, and Surface waves. Each type of wave travels at different speeds and has different characteristics, but all propagate outward from the earthquake's focus.

  1. Primary (P) Waves: P-waves are compressional waves that travel through the Earth's interior by alternately compressing and expanding the material they pass through. They are the fastest seismic waves and are capable of traveling through solids, liquids, and gases. P-waves are the first to arrive at seismograph stations following an earthquake and can propagate through the Earth's interior directly from the focus to the surface.

  2. Secondary (S) Waves: S-waves are shear waves that travel through the Earth's interior by causing particles of the material to move perpendicular to the direction of wave propagation. Unlike P-waves, S-waves cannot travel through liquids or gases and are only able to propagate through solids. S-waves are slower than P-waves and arrive at seismograph stations after P-waves.

  3. Surface Waves: Surface waves travel along the Earth's surface and are responsible for much of the shaking and damage observed during earthquakes. They are slower than both P-waves and S-waves and typically arrive at seismograph stations last. Surface waves have two main types: Love waves and Rayleigh waves. Love waves cause horizontal shearing motion in the ground, while Rayleigh waves cause both vertical and horizontal motion, similar to the motion of ocean waves.

Overall, the shock waves produced by an earthquake travel outward from the focus in all directions, causing the ground to shake and resulting in the seismic waves detected by seismographs stationed around the world.

 
 
 
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