π Important Deserts
π Subtropical Hot Deserts
π Great Victoria Desert
β Largest Australian Desert
β Contains many sand dunes and salt lakes
π Great Sandy Desert
β Passes through the Pilbara region
β An ephemeral river, Rudall, flows through here
π Gibson Desert
π Simpson Desert
π Tanami Desert
π Subtropical Hot Deserts
π Great Victoria Desert
β Largest Australian Desert
β Contains many sand dunes and salt lakes
π Great Sandy Desert
β Passes through the Pilbara region
β An ephemeral river, Rudall, flows through here
π Gibson Desert
π Simpson Desert
π Tanami Desert
π Important Volcanoes
π Mount Yasur
β Location: Tanna Island, Vanuatu
β Details: One of the worldβs most accessible active volcanoes; continuous activity.
π Mount Ruapehu
β Location: North Island, New Zealand
β Details: Active stratovolcano; highest point in the North Island.
π Mount Tavurvur
β Location: East New Britain, Papua New Guinea
β Details: Active volcano; part of the Rabaul caldera.
π Mount Yasur
β Location: Tanna Island, Vanuatu
β Details: One of the worldβs most accessible active volcanoes; continuous activity.
π Mount Ruapehu
β Location: North Island, New Zealand
β Details: Active stratovolcano; highest point in the North Island.
π Mount Tavurvur
β Location: East New Britain, Papua New Guinea
β Details: Active volcano; part of the Rabaul caldera.
π Ellsworth Mountains in Antarctica
β Location:
β’ The Ellsworth Mountains are situated in West Antarctica.
β Key Feature:
β’ These mountains include Mount Vinson, the highest peak in Antarctica, standing at 4,892 meters.
#EllsworthMountains #MountVinson #Antarctica #Geography
β Location:
β’ The Ellsworth Mountains are situated in West Antarctica.
β Key Feature:
β’ These mountains include Mount Vinson, the highest peak in Antarctica, standing at 4,892 meters.
#EllsworthMountains #MountVinson #Antarctica #Geography
Forwarded from UPSC Mapping Prelims Mains
π Indian Ocean Dipole (IOD) & Indian Monsoon π§οΈ
π What is IOD?
The Indian Ocean Dipole (IOD) is a climate phenomenon caused by temperature differences between the eastern (Bay of Bengal) and western (Arabian Sea) regions of the Indian Ocean. It greatly impacts the Indian monsoon and rainfall distribution.
πΉ Positive IOD:
β Warmer West, Cooler East - Warmer sea temperatures in the west and cooler in the east create favorable conditions for rainfall.
β Enhanced Monsoon - Strengthens monsoon circulation, increasing rainfall in central India.
β Increased Rainfall - Observed above-average rainfall in central India during positive IOD years.
π» Negative IOD:
β Cooler West, Warmer East - Temperature reversal leads to a weaker monsoon.
β Weaker Monsoon - Disrupts monsoon circulation, causing a delayed or weak monsoon.
β Drought Risk - Potential drought conditions, particularly in central and eastern India, with below-average rainfall.
#Geography
π What is IOD?
The Indian Ocean Dipole (IOD) is a climate phenomenon caused by temperature differences between the eastern (Bay of Bengal) and western (Arabian Sea) regions of the Indian Ocean. It greatly impacts the Indian monsoon and rainfall distribution.
πΉ Positive IOD:
β Warmer West, Cooler East - Warmer sea temperatures in the west and cooler in the east create favorable conditions for rainfall.
β Enhanced Monsoon - Strengthens monsoon circulation, increasing rainfall in central India.
β Increased Rainfall - Observed above-average rainfall in central India during positive IOD years.
π» Negative IOD:
β Cooler West, Warmer East - Temperature reversal leads to a weaker monsoon.
β Weaker Monsoon - Disrupts monsoon circulation, causing a delayed or weak monsoon.
β Drought Risk - Potential drought conditions, particularly in central and eastern India, with below-average rainfall.
#Geography
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Forwarded from CSE EXAM ( UPSC prelims mains) CAPF
CSP-2025-WR-NameList-Engl-110625.pdf
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Name Wise 2025 Pre
π Rain-Bearing Systems
π Arabian Sea Branch
β Divides into three streams:
β’ Western Coast: Heavy rainfall (250 cm) due to orographic effect.
β’ Narmada-Tapi troughs: Narrow valley system in central India.
β’ Aravalli Range: Minimal rainfall impact.
π Bay of Bengal Branch
β Splits into two streams:
β’ Ganga-Brahmaputra delta: Heavy rainfall, Cherrapunji (1,221 cm) holds record.
β’ Himalayan foothills: Deflected by mountains, widespread rainfall to Ganges Plain.
π Monsoon Break
β Dry spells during monsoon, known as break in monsoon, common after a few days of rain.
π Retreat in Monsoon
β Withdrawal of monsoon winds, known as retreating monsoon, occurs in October-November.
#Geography
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π Arabian Sea Branch
β Divides into three streams:
β’ Western Coast: Heavy rainfall (250 cm) due to orographic effect.
β’ Narmada-Tapi troughs: Narrow valley system in central India.
β’ Aravalli Range: Minimal rainfall impact.
π Bay of Bengal Branch
β Splits into two streams:
β’ Ganga-Brahmaputra delta: Heavy rainfall, Cherrapunji (1,221 cm) holds record.
β’ Himalayan foothills: Deflected by mountains, widespread rainfall to Ganges Plain.
π Monsoon Break
β Dry spells during monsoon, known as break in monsoon, common after a few days of rain.
π Retreat in Monsoon
β Withdrawal of monsoon winds, known as retreating monsoon, occurs in October-November.
#Geography
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π Global Distribution of Earthquakes
π Major Seismic Belts
β The circum-Pacific seismic belt found along the rim of the Pacific Ocean is the worldβs greatest earthquake belt. Around 81% of the worldβs largest earthquakes occur here. Known as the βRing of Fireβ.
β The Alpide earthquake belt spreads from Java to Sumatra, through the Himalayas, the Mediterranean, and into the Atlantic. It causes about 17% of the worldβs earthquakes.
β The third belt is the mid-Atlantic Ridge, a submerged divergent plate boundary where tectonic plates are spreading apart.
π Seismic Mapping of India
π Seismic Zonation Insights
β About 59% of Indiaβs land area is prone to earthquakes.
β The seismic map classifies India into 4 seismic zones based on intensity.
β Zone V is the most active (Very High Risk), while Zone II is the least active.
β€ Approx. 10.79% in Zone V, 17.49% in Zone IV, 30.79% in Zone III, and 40.93% in Zone II.
#Geography
#disaster_management
π Major Seismic Belts
β The circum-Pacific seismic belt found along the rim of the Pacific Ocean is the worldβs greatest earthquake belt. Around 81% of the worldβs largest earthquakes occur here. Known as the βRing of Fireβ.
β The Alpide earthquake belt spreads from Java to Sumatra, through the Himalayas, the Mediterranean, and into the Atlantic. It causes about 17% of the worldβs earthquakes.
β The third belt is the mid-Atlantic Ridge, a submerged divergent plate boundary where tectonic plates are spreading apart.
π Seismic Mapping of India
π Seismic Zonation Insights
β About 59% of Indiaβs land area is prone to earthquakes.
β The seismic map classifies India into 4 seismic zones based on intensity.
β Zone V is the most active (Very High Risk), while Zone II is the least active.
β€ Approx. 10.79% in Zone V, 17.49% in Zone IV, 30.79% in Zone III, and 40.93% in Zone II.
#Geography
#disaster_management
Forwarded from CSE EXAM ( UPSC prelims mains) CAPF
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CAPF FINAL RESULTS24
π Cold Lava (Lahar): A Silent but Deadly Force
π Context: The Mount Kanlaon volcano in the Philippines recently witnessed rivers of cold lava, also known as lahars.
π What is Cold Lava (Lahar)?
β A fast-moving slurry of water, volcanic ash, rock fragments, and pumice.
β Forms when volcanic ash mixes with heavy rain or when glacial ice melts, even without eruptions.
β Moves at high speeds, reaching hundreds of km/h, making it more dangerous than slow-moving lava.
β Hot & destructive**βtraps heat, **burns everything in its path, causes property damage & loss of life.
β Creates floods by damming rivers, harming ecosystems, and increasing flood risks.
β οΈ How to Mitigate Lahars?
β Early warning systems & engineering solutions can reduce damage.
β Community education on lahar-prone zones saves lives.
π Lava vs. Magma:
π Magma β Found inside the Earth (molten rock in the mantle).
π΄ Lava β Magma that has reached the surface through a volcanic vent.
#ColdLava #Lahar #VolcanoHazards #DisasterPreparedness #Geography
π Context: The Mount Kanlaon volcano in the Philippines recently witnessed rivers of cold lava, also known as lahars.
π What is Cold Lava (Lahar)?
β A fast-moving slurry of water, volcanic ash, rock fragments, and pumice.
β Forms when volcanic ash mixes with heavy rain or when glacial ice melts, even without eruptions.
β Moves at high speeds, reaching hundreds of km/h, making it more dangerous than slow-moving lava.
β Hot & destructive**βtraps heat, **burns everything in its path, causes property damage & loss of life.
β Creates floods by damming rivers, harming ecosystems, and increasing flood risks.
β οΈ How to Mitigate Lahars?
β Early warning systems & engineering solutions can reduce damage.
β Community education on lahar-prone zones saves lives.
π Lava vs. Magma:
π Magma β Found inside the Earth (molten rock in the mantle).
π΄ Lava β Magma that has reached the surface through a volcanic vent.
#ColdLava #Lahar #VolcanoHazards #DisasterPreparedness #Geography
π Cold Lava (Lahar): A Silent but Deadly Force
π Context: The Mount Kanlaon volcano in the Philippines recently witnessed rivers of cold lava, also known as lahars.
π What is Cold Lava (Lahar)?
β A fast-moving slurry of water, volcanic ash, rock fragments, and pumice.
β Forms when volcanic ash mixes with heavy rain or when glacial ice melts, even without eruptions.
β Moves at high speeds, reaching hundreds of km/h, making it more dangerous than slow-moving lava.
β Hot & destructive**βtraps heat, **burns everything in its path, causes property damage & loss of life.
β Creates floods by damming rivers, harming ecosystems, and increasing flood risks.
β οΈ How to Mitigate Lahars?
β Early warning systems & engineering solutions can reduce damage.
β Community education on lahar-prone zones saves lives.
π Lava vs. Magma:
π Magma β Found inside the Earth (molten rock in the mantle).
π΄ Lava β Magma that has reached the surface through a volcanic vent.
#ColdLava #Lahar #VolcanoHazards #DisasterPreparedness #Geography
π Context: The Mount Kanlaon volcano in the Philippines recently witnessed rivers of cold lava, also known as lahars.
π What is Cold Lava (Lahar)?
β A fast-moving slurry of water, volcanic ash, rock fragments, and pumice.
β Forms when volcanic ash mixes with heavy rain or when glacial ice melts, even without eruptions.
β Moves at high speeds, reaching hundreds of km/h, making it more dangerous than slow-moving lava.
β Hot & destructive**βtraps heat, **burns everything in its path, causes property damage & loss of life.
β Creates floods by damming rivers, harming ecosystems, and increasing flood risks.
β οΈ How to Mitigate Lahars?
β Early warning systems & engineering solutions can reduce damage.
β Community education on lahar-prone zones saves lives.
π Lava vs. Magma:
π Magma β Found inside the Earth (molten rock in the mantle).
π΄ Lava β Magma that has reached the surface through a volcanic vent.
#ColdLava #Lahar #VolcanoHazards #DisasterPreparedness #Geography
Forwarded from UPSC Mapping Prelims Mains
π Winter Weather in India: Key Drivers & Effects
π 1. Surface Pressure & Winds
β High-pressure zone forms in Central & West Asia.
β Cold continental winds blow into India from the north.
β These collide with trade winds β unstable zone forms.
β Result: Northwest India experiences dry, cold North-Westerlies.
π 2. Jet Stream & Upper Air Circulation
β Westerly jet streams dominate Asia in winter.
β Tibetan Himalayas split jet into two:
βπΉ North branch flows over Tibetan Plateau.
βπΉ South branch crosses south of the Himalayas.
β Subtropical westerly jet brings winter rain to northwest India.
π 3. Western Disturbances & Cyclones
β Western disturbances (from the Mediterranean) hit north & northwest India.
β Bring light winter rain β great for wheat crops.
β Tropical cyclones still possible in OctβNov, driven by easterlies.
β Hit east coast states β TN, AP, Odisha with heavy rain + wind.
#Geography
π 1. Surface Pressure & Winds
β High-pressure zone forms in Central & West Asia.
β Cold continental winds blow into India from the north.
β These collide with trade winds β unstable zone forms.
β Result: Northwest India experiences dry, cold North-Westerlies.
π 2. Jet Stream & Upper Air Circulation
β Westerly jet streams dominate Asia in winter.
β Tibetan Himalayas split jet into two:
βπΉ North branch flows over Tibetan Plateau.
βπΉ South branch crosses south of the Himalayas.
β Subtropical westerly jet brings winter rain to northwest India.
π 3. Western Disturbances & Cyclones
β Western disturbances (from the Mediterranean) hit north & northwest India.
β Bring light winter rain β great for wheat crops.
β Tropical cyclones still possible in OctβNov, driven by easterlies.
β Hit east coast states β TN, AP, Odisha with heavy rain + wind.
#Geography
Forwarded from UPSC Mapping Prelims Mains
π Effects of Ocean Currents
π Climate Control
β Warm currents raise temperatures; cold ones cool them.
β‘οΈ Example: North Atlantic Drift warms England; Canary cools Spain.
π Rainfall & Deserts
β Warm currents β more rainfall.
β Cold currents β desert formation.
β‘οΈ Example: Cold Humboldt Current causes the Atacama Desert.
π Fishing Zones
β Convergence of warm & cold currents supports plankton β rich fish stocks.
β‘οΈ Example: Grand Banks of Newfoundland.
π Navigation
β Currents aid efficient maritime travel by influencing shipping lanes.
π Temperature Moderation
β Currents redistribute heat and stabilize coastal climates.
β‘οΈ Example: England remains mild due to warm currents.
#Geography
π Climate Control
β Warm currents raise temperatures; cold ones cool them.
β‘οΈ Example: North Atlantic Drift warms England; Canary cools Spain.
π Rainfall & Deserts
β Warm currents β more rainfall.
β Cold currents β desert formation.
β‘οΈ Example: Cold Humboldt Current causes the Atacama Desert.
π Fishing Zones
β Convergence of warm & cold currents supports plankton β rich fish stocks.
β‘οΈ Example: Grand Banks of Newfoundland.
π Navigation
β Currents aid efficient maritime travel by influencing shipping lanes.
π Temperature Moderation
β Currents redistribute heat and stabilize coastal climates.
β‘οΈ Example: England remains mild due to warm currents.
#Geography
Forwarded from UPSC Mapping Prelims Mains
π Why El NiΓ±o Is Hard to Predict
π El NiΓ±o remains a major challenge in climate forecasting due to dynamic ocean-atmosphere interactions
β π ENSO has 3 phases: El NiΓ±o (warm), La NiΓ±a (cool), and neutral.
β π Climate models struggle due to late-emerging ENSO signals (only in early summer).
β π¬οΈ Westerly wind bursts and Indian Ocean anomalies can trigger or dampen ENSO.
β π§ͺ New model: Recharge Oscillator (RO) simulates ENSO as a contest between sea-surface temp & sub-surface heat.
β π Disagreements remain on which ocean basin is most influential in modelling.
#GS1 #Geography #Climate #ENSO #ElNino #Prelims2026 #UPSC #prelims
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π El NiΓ±o remains a major challenge in climate forecasting due to dynamic ocean-atmosphere interactions
β π ENSO has 3 phases: El NiΓ±o (warm), La NiΓ±a (cool), and neutral.
β π Climate models struggle due to late-emerging ENSO signals (only in early summer).
β π¬οΈ Westerly wind bursts and Indian Ocean anomalies can trigger or dampen ENSO.
β π§ͺ New model: Recharge Oscillator (RO) simulates ENSO as a contest between sea-surface temp & sub-surface heat.
β π Disagreements remain on which ocean basin is most influential in modelling.
π Prelims Question:
Which of the following best describes the ENSO phenomenon?
A. Only a Pacific Ocean event
B. Ocean-atmosphere interaction with 3 phases
C. Caused by monsoonal winds
D. Predictable using historical data
Answer: B
π Mains Question (GS1 β Geography):
What makes the prediction of the El NiΓ±o Southern Oscillation (ENSO) phenomenon difficult? Discuss the implications for global weather forecasting and agriculture.
#GS1 #Geography #Climate #ENSO #ElNino #Prelims2026 #UPSC #prelims
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