blog-details

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

Type

Description

Example

Tectonic

Caused by movement of tectonic plates and faults

Gujarat Earthquake (2001)

Volcanic

Result of magma movement during volcanic activity

Krakatoa (1883)

Isostatic

Due to crustal adjustment from added or removed surface loads

Post-glacial rebound

Plutonic

Deep-focus, originating from depths of 240–600 km

Sea of Okhotsk (2013)

Man-made

Induced by mining, dam reservoirs, explosions

Koyna Dam (1967), Maharashtra

B. Based on Focus (Depth)

Type

Depth

Characteristics

Shallow-focus

0–70 km

Most common and damaging

Intermediate-focus

70–300 km

Common in subduction zones

Deep-focus

300–700 km

Less surface damage; high magnitude

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

Type

Description

Active

Frequently erupting (e.g., Stromboli, Kilauea)

Dormant

Temporarily inactive but may erupt again (e.g., Mount Fuji)

Extinct

No expected future eruptions (e.g., Edinburgh’s Arthur’s Seat)

B. Based on Shape

Type

Features

Example

Cinder Cone

Steep, conical; made of ash and scoria

Parícutin, Mexico

Composite

Layered ash and lava; explosive

Mount St. Helens, USA

Shield

Broad, gentle slopes; basaltic lava

Mauna Loa, Hawaii

Lava Dome

Viscous lava; steep mound

Lava dome at Mount St. Helens

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

Feature

Earthquake

Volcano

Cause

Tectonic plate movement

Magma movement from mantle

Origin Point

Focus (hypocenter)

Vent or fissure

Duration

Few seconds to minutes

Minutes to hours or days

Warning

Difficult to predict

Some precursors exist

Impact

Ground shaking, tsunamis

Lava flow, ash fall, pyroclastic flow

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.

RASOnly Interview Guidance Program

Mr. Ashok Jain

Ex-Chief Secretary Govt of Rajasthan

  • IAS officer of the 1981 batch, Rajasthan cadre.
  • Passionate about mentoring the next generation of RAS officers with real-world insights.
  • Got retired in Dec 2017 from the post of Chief Secretary of the state of Rajasthan.

Mr. Guru Charan Rai

Ex-ASP / SP in Jaisalmer

  • Guru Charan Rai, IPS (Retd), retired as Inspector General of Police (Security), Rajasthan, Jaipur in 2017.
  • Served as ASP and SP in Jaisalmer, Nagaur, Sri Ganganagar, Sawai Madhopur, Dausa, Sikar, and Karauli.
  • He also held key positions as DIGP and IGP in the Law and Order division.

Mr. Rakesh Verma

Ex-IAS Officer, B.Tech, MBA, and M.A. (Economics)

  • IAS officer of the 1981 batch and retired in Chief Secretary Rank.
  • Civil servant of high repute and vast experience.
  • Has been teaching UPSC CSE subjects for the last six years.
Request Callback