An earthquake occurs due to the sudden release of energy from the tectonic plates and their sudden movement; earthquakes are sudden and violent movements of the Earth’s crust. Some of the natural calamities with the potency to vary in their magnitude can destroy a lot of life and infrastructure worldwide. Since seismic waves can travel over a long distance, caused by an earthquake, the disaster makes it hard to predict or plan for them. Main points to note on earthquakes:
- The movement of the tectonic plates beneath the Earth’s surface causes earthquakes, resulting in seismic activities.
- They can occur anywhere, but areas near tectonic boundaries are most liable to frequent and severe earthquakes.
- The Richter scale measures the size or magnitude of an earthquake, which determines the intensity and possible damage.
Causes of Earthquakes
Earthquakes are usually triggered by tectonic plate movements, volcanic activity, or human-induced such as mining and reservoir-induced seismicity, which release sudden energy in the crust of the Earth.
Tectonic Causes
Earthquakes primarily result from the movement of tectonic plates. The Earth’s lithosphere is divided into several plates that float on the semi-fluid asthenosphere. Moreover, the boundaries where these plates interact are the most earthquake-prone areas.
- Divergent Boundaries: Where plates move apart, magma rises to fill the gap, creating a new crust, as seen in mid-ocean ridges.
- Convergent Boundaries: Where plates collide, one plate is often forced below the other into the mantle in a process called subduction. This is common along the Pacific Ring of Fire.
- Transform Boundaries: Where plates slide past each other horizontally. The San Andreas Fault in California is a classic example.
Non-Tectonic Causes
- Volcanic Activity: Magma movement can cause earthquakes.
- Human Activities: Activities like mining, reservoir-induced seismicity (due to the filling of large dams), and geothermal energy extraction can induce earthquakes.
Types of Seismic Waves
Seismic waves are energy waves that travel through the Earth’s layers and are recorded by seismographs. They are classified into body waves and surface waves:
Body Waves
- P-Waves (Primary Waves): These are compressional waves, which travel the fastest and represent the first record. They can move through the solid and liquid layers of Earth.
- S-Waves (Secondary Waves): These are shear waves, traveling slower than P-waves and only able to move through solids. Their movement is perpendicular to the direction in which wave propagation occurs.
Surface Waves
- Love Waves: Cause horizontal shifting of the Earth during an earthquake. They are faster than Rayleigh waves but slower than body waves.
- Rayleigh Waves: Cause a rolling motion, combining both vertical and horizontal ground movement. They are usually responsible for the most shaking felt during an earthquake.
Effects of Earthquakes
Earthquakes cause destruction that reaches as high as the damage down to infrastructures and likely entails death. It also triggers other disasters such as landslides and tsunamis, and disrupts essential services, which have long-term impacts socially and economically on an area.
On Human Settlements
- Structural Damage: Buildings, bridges, and roads can collapse, leading to loss of life and property.
- Fires: Ruptured gas lines and damaged electrical infrastructure can ignite fires.
- Landslides: Earthquakes can trigger landslides, especially in hilly and mountainous areas, burying communities and blocking roads.
On Infrastructure
- Utility Failures: Water, electricity, and gas lines can be damaged, leading to extended outages.
- Transportation Disruptions: Damage to roads, railways, and airports can impede emergency response and recovery efforts.
Conclusion
Earthquakes are natural disasters which, although cannot be avoided, have deep socio-economic impacts on society. However, their causes, types of waves produced, and effects can better be understood, and by making total mitigation efforts, it becomes possible to minimize risks and be better prepared for such disasters. So, the installation of early warning systems, strict building codes, and public education are the most crucial steps to reduce damage caused due to earthquakes.
| Earthquakes UPSC Notes |
| 1. Earthquakes are caused by the sudden release of energy due to tectonic movements along faults or volcanic activity. 2. Seismic waves generated by earthquakes are categorized as P-waves, S-waves, and surface waves, affecting the Earth’s crust differently. 3. The Richter scale measures the magnitude of an earthquake, while the Mercalli scale assesses its intensity based on observed effects. 4. Earthquake-prone areas, especially around the Pacific Ring of Fire, experience frequent seismic activities due to active plate boundaries. 5. India’s vulnerability to earthquakes is high, particularly in the Himalayan region, due to the ongoing collision between the Indian and Eurasian plates. 6. Earthquake hazards include ground shaking, surface rupture, landslides, tsunamis, and liquefaction, affecting both natural and human-made environments. 7. Effective earthquake preparedness includes robust building codes, disaster management systems, early warning systems, and community awareness programs. 8. Recent technological advancements, like seismic zoning maps and early detection technologies, are vital in minimizing damage and saving lives during earthquakes. |
