Among the most devastating endogenic processes that form Earth's surface, there are earthquakes and volcanoes. They are instantaneous yet affect human settlements and natural landscapes in the long run. Earthquakes occur as a result of tectonic motions that move seismic waves whereas volcanoes eject magma and gases hidden in the earth. These processes are vital in terms of reading plate tectonics and internal processes on the Earth. In spite of their destructive natures, they play a role in formation of landforms and balance geologically.
Key Highlights for RAS Mains
I. Earthquakes
Signification and Concept
- Earthquake: sudden shaking of the surface of Earth as a result of the liberation of energy of the lithosphere.
- The source of the earthquake is the hypocenter (focus): its projection on the ground is the epicenter.
- Resulting primarily due to plate tectonic plate motion.
Types of Earthquakes
A. Based on Causative Factors
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Type
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Description
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Example
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Tectonic
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Caused by movement of tectonic plates and faults
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Gujarat Earthquake (2001)
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Volcanic
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Result of magma movement during volcanic activity
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Krakatoa (1883)
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Isostatic
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Due to crustal adjustment from added or removed surface loads
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Post-glacial rebound
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Plutonic
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Deep-focus, originating from depths of 240–600 km
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Sea of Okhotsk (2013)
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Man-made
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Induced by mining, dam reservoirs, explosions
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Koyna Dam (1967), Maharashtra
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B. Based on Focus (Depth)
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Type
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Depth
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Characteristics
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Shallow-focus
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0–70 km
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Most common and damaging
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Intermediate-focus
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70–300 km
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Common in subduction zones
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Deep-focus
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300–700 km
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Less surface damage; high magnitude
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Earthquakes causes
- Plate tectonics (divergent boundaries, convergent boundaries, transform boundaries)
- Volcanic activity
- Isostatic adjustments
- Human-induced activities
Effects of Earthquakes
- Land depression/ elevations
- River-course changes and coastline
- Arson and loss of lives and property
- Tsunamis, and landslides
Volcanoes
Significance and Idea
- Volcano: Crack on the surface of the earth through which magma, ash and gases spill out.
- Volcanism can be defined as any process related to magma movement as well as volcanic eruption.
Types of Volcanoes
A. Based on Eruption Frequency
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Type
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Description
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Active
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Frequently erupting (e.g., Stromboli, Kilauea)
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Dormant
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Temporarily inactive but may erupt again (e.g., Mount Fuji)
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Extinct
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No expected future eruptions (e.g., Edinburgh’s Arthur’s Seat)
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B. Based on Shape
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Type
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Features
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Example
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Cinder Cone
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Steep, conical; made of ash and scoria
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Parícutin, Mexico
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Composite
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Layered ash and lava; explosive
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Mount St. Helens, USA
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Shield
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Broad, gentle slopes; basaltic lava
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Mauna Loa, Hawaii
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Lava Dome
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Viscous lava; steep mound
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Lava dome at Mount St. Helens
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Volcanic Landscape (Intrusive Landforms)
- Batholiths: Large masses of batholiths, of batholiths.
- Laccoliths: Disks , flat on the bottom, humps in the middle
- Lopoliths (sauceed sill)
- Phacoliths, Found in folds, Lens shaped.
- Sills : Sheets like bodies of intrusion horizontal
- Dykes : Intrusions perpendicular or sloping across beddings,
Difference Between Earthquakes & Volcanoes
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Feature
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Earthquake
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Volcano
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Cause
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Tectonic plate movement
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Magma movement from mantle
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Origin Point
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Focus (hypocenter)
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Vent or fissure
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Duration
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Few seconds to minutes
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Minutes to hours or days
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Warning
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Difficult to predict
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Some precursors exist
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Impact
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Ground shaking, tsunamis
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Lava flow, ash fall, pyroclastic flow
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Conclusion for RPSC
The earthquakes and volcanoes are natural releases of the inner energy of the Earth, which, however, are quite unexpected and are usually devastating. Their mechanisms can be understood to reduce a disaster, increase safety in buildings and to plan where to build in a city. In addition, their power to sculpt the Earth surface, to fill the soils, also underlines their ambivalent nature, being both destructive and beneficial.
Also Read: The Evolution of Indian Plate
FAQs for RPSC RAS
Earthquakes are caused by sudden movements of tectonic plates along faults in the Earth’s crust.
The focus is the point inside the Earth where the earthquake starts; the epicenter is its point directly above on the surface.
Volcanoes can be active, dormant, or extinct based on eruption frequency.
Earthquakes result from crust movement, while volcanoes involve the eruption of magma and gases.
Volcanoes show warning signs, but earthquakes are difficult to predict accurately.