What is an earthquake, and how is it measured?
Artificial satellites orbit the Earth by balancing two forces: the satellite's forward momentum and the gravitational pull of the Earth. Here's how this works: Key Principles of Satellite Orbits Gravity: Earth’s gravity pulls the satellite toward its center. Without this force, the satellite would fRead more
Artificial satellites orbit the Earth by balancing two forces: the satellite’s forward momentum and the gravitational pull of the Earth. Here’s how this works:
Key Principles of Satellite Orbits
- Gravity: Earth’s gravity pulls the satellite toward its center. Without this force, the satellite would fly off into space.
- Inertia: According to Newton’s first law of motion, an object in motion will stay in motion unless acted upon by an external force. The satellite’s inertia keeps it moving in a straight line.
- Orbital Motion: When a satellite is launched, it is given a horizontal speed. The satellite moves forward due to its inertia, while gravity pulls it toward the Earth. The balance between these two forces causes the satellite to follow a curved path around the Earth, which is its orbit.
Types of Orbits
- Low Earth Orbit (LEO): These orbits are close to Earth, typically between 160 to 2,000 kilometers above the surface. Satellites in LEO, like the International Space Station (ISS), circle the Earth quickly, completing an orbit in about 90 minutes.
- Medium Earth Orbit (MEO): These orbits range from 2,000 to 35,786 kilometers. GPS satellites often use MEO.
- Geostationary Orbit (GEO): At about 35,786 kilometers above the equator, satellites in GEO orbit the Earth at the same rate that the Earth rotates. This makes them appear stationary relative to a point on the Earth, ideal for communication and weather satellites.
- Polar Orbit: These satellites pass over the Earth’s poles, allowing them to scan the entire surface over time. They are often used for Earth observation and weather monitoring.
Maintaining Orbits
Satellites are carefully launched at specific speeds and angles to ensure they reach and maintain their designated orbits. Occasionally, small onboard thrusters make adjustments to correct the satellite’s path and altitude, a process known as orbital station-keeping.
By maintaining the delicate balance between gravity and inertia, artificial satellites can stay in orbit around the Earth for many years, serving a variety of functions like communication, navigation, weather monitoring, and scientific research.
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An earthquake is the sudden shaking of the Earth's surface caused by the release of energy from the Earth's lithosphere. This energy release occurs due to the movement of tectonic plates, volcanic activity, or man-made activities like mining or reservoir-induced seismicity. Causes of Earthquakes TecRead more
An earthquake is the sudden shaking of the Earth’s surface caused by the release of energy from the Earth’s lithosphere. This energy release occurs due to the movement of tectonic plates, volcanic activity, or man-made activities like mining or reservoir-induced seismicity.
Causes of Earthquakes
Measurement of Earthquakes
Earthquakes are measured using two main scales: the Richter scale and the Moment Magnitude scale (Mw). The intensity and effects of earthquakes can also be described using the Modified Mercalli Intensity scale.
Seismographs are the instruments used to detect and record earthquakes. They measure the seismic waves generated by the earthquake and help determine the epicenter, depth, and magnitude of the quake.
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