πMount Lewotobi Laki-laki:
β Location: It is located in Indonesiaβs East Nusa Tenggara province on Flores Island.
β It is situated along the famous βRing of Fireβ in the Pacific region.
β It is one of the most frequently active volcanoes in the region.
β It has two peaks arranged on a NW-SE line separated by 2 km and a 1232 m high saddle. This gave the twin volcano its name, Lewotobi, βhusband and wifeβ.
β The two peaks correspond to the Lewotobi Lakilaki (man) and Lewotobi Perempuan (woman)
Lewotobi Lakilaki (1584 m) has a summit crater of 400 m diameter open to the north. Lewotobi Perampuan (1703 m)βs crater is 700 m wide.
β Lewotobi Lakilaki has been frequently active during the 19th and 20th centuries, while the taller and broader Lewotobi Perempuan has erupted only twice in historical time.
β Small lava domes have grown during the 20th century in the summit craters of both volcanoes.
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β Location: It is located in Indonesiaβs East Nusa Tenggara province on Flores Island.
β It is situated along the famous βRing of Fireβ in the Pacific region.
β It is one of the most frequently active volcanoes in the region.
β It has two peaks arranged on a NW-SE line separated by 2 km and a 1232 m high saddle. This gave the twin volcano its name, Lewotobi, βhusband and wifeβ.
β The two peaks correspond to the Lewotobi Lakilaki (man) and Lewotobi Perempuan (woman)
Lewotobi Lakilaki (1584 m) has a summit crater of 400 m diameter open to the north. Lewotobi Perampuan (1703 m)βs crater is 700 m wide.
β Lewotobi Lakilaki has been frequently active during the 19th and 20th centuries, while the taller and broader Lewotobi Perempuan has erupted only twice in historical time.
β Small lava domes have grown during the 20th century in the summit craters of both volcanoes.
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Forwarded from UPSC Mapping Prelims Mains
π Koeppenβs Climatic Classification of India
π Key Concepts
β Developed by Wladimir Koeppen β based on annual mean temperature and precipitation
β Links vegetation distribution with climate types
β Uses letter codes to classify major climate zones based on seasonality
π Major Climatic Types in India
β (Am) Monsoon with short dry season β West coast (e.g., Goa)
β (As) Monsoon with dry summer β Coromandel coast
β (Aw) Tropical Savanna β Most of Peninsular India
β (BShw) Semi-arid Steppe β Interior Deccan, Gujarat, Rajasthan, Punjab, J&K
β (BWhw) Hot Desert β West Rajasthan only
β (Cwg) Monsoon with dry winters β Northern Plains
β (Dfc) Cold-humid winter with short summer β Northeast India
β (E) Polar Climate β Upper Himalayas
β (ET) Tundra Climate β Higher Himalayan ranges, Ladakh
π Utility of the Classification
β Helps in agro-climatic zoning, crop selection, water planning
β Useful for disaster risk reduction, ecological studies, and climate adaptation policies
#Geography
π Key Concepts
β Developed by Wladimir Koeppen β based on annual mean temperature and precipitation
β Links vegetation distribution with climate types
β Uses letter codes to classify major climate zones based on seasonality
π Major Climatic Types in India
β (Am) Monsoon with short dry season β West coast (e.g., Goa)
β (As) Monsoon with dry summer β Coromandel coast
β (Aw) Tropical Savanna β Most of Peninsular India
β (BShw) Semi-arid Steppe β Interior Deccan, Gujarat, Rajasthan, Punjab, J&K
β (BWhw) Hot Desert β West Rajasthan only
β (Cwg) Monsoon with dry winters β Northern Plains
β (Dfc) Cold-humid winter with short summer β Northeast India
β (E) Polar Climate β Upper Himalayas
β (ET) Tundra Climate β Higher Himalayan ranges, Ladakh
π Utility of the Classification
β Helps in agro-climatic zoning, crop selection, water planning
β Useful for disaster risk reduction, ecological studies, and climate adaptation policies
π Prelims Question
Q. Which of the following climate types in India is represented by Koeppenβs classification code βAwβ?
A. Cold-humid winter with short summer
B. Monsoon with short dry season
C. Tropical Savanna
D. Tundra Climate
Answer: β C. Tropical Savanna
π Mains Question (GS1 β Geography)
Q. Discuss the significance of Koeppenβs climatic classification in understanding Indiaβs climatic diversity. How can it assist in agricultural and water resource planning?
#Geography
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π Global Ocean Heat Content (OHC) β Climate Indicator
π Definition: Total heat absorbed & stored in oceans, measured at various depths.
β Key Facts
β’ Oceans absorb 90% of excess global heat.
β’ Atlantic, Pacific, and Southern Oceans warm faster than global average.
β’ Since 1980s, OHC has doubled/tripled (2023 study).
β Significance
β’ Drives sea level rise, alters weather, disrupts ecosystems, and strengthens cyclones.
β’ A stable climate change indicator beyond surface temperatures.
#Geography
π Definition: Total heat absorbed & stored in oceans, measured at various depths.
β Key Facts
β’ Oceans absorb 90% of excess global heat.
β’ Atlantic, Pacific, and Southern Oceans warm faster than global average.
β’ Since 1980s, OHC has doubled/tripled (2023 study).
β Significance
β’ Drives sea level rise, alters weather, disrupts ecosystems, and strengthens cyclones.
β’ A stable climate change indicator beyond surface temperatures.
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π External Migration: A Double-Edged Sword
πMigration brings economic benefits but also social challenges.
β Positive Impacts
β’ Remittances boost economy: India received over $100 billion recently.
β’ Employment generation abroad: Eases pressure on local job markets.
β’ Skill transfer: Returnees bring global expertise (e.g., IT professionals).
β’ Improved living standards: Better access to health and education.
β’ Cultural exposure: Enhances language, awareness, global ties.
β’ Diplomatic leverage: Diaspora strengthens Indiaβs global influence.
β Negative Impacts
β’ Brain drain: Skilled youth, especially STEM grads, migrate.
β’ Family disruption: Long separation causes emotional stress.
β’ Regional imbalance: Punjab, Kerala over-dependent on remittances.
β’ Worker exploitation: Many face wage theft, legal issues abroad.
β’ Remittance dependency: Economic shocks like COVID-19 hit hard.
β’ Cultural erosion: Identity conflicts among migrant youth.
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πMigration brings economic benefits but also social challenges.
β Positive Impacts
β’ Remittances boost economy: India received over $100 billion recently.
β’ Employment generation abroad: Eases pressure on local job markets.
β’ Skill transfer: Returnees bring global expertise (e.g., IT professionals).
β’ Improved living standards: Better access to health and education.
β’ Cultural exposure: Enhances language, awareness, global ties.
β’ Diplomatic leverage: Diaspora strengthens Indiaβs global influence.
β Negative Impacts
β’ Brain drain: Skilled youth, especially STEM grads, migrate.
β’ Family disruption: Long separation causes emotional stress.
β’ Regional imbalance: Punjab, Kerala over-dependent on remittances.
β’ Worker exploitation: Many face wage theft, legal issues abroad.
β’ Remittance dependency: Economic shocks like COVID-19 hit hard.
β’ Cultural erosion: Identity conflicts among migrant youth.
#geography #society
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Q.: The average height of the Kosi plain from mean sea level is
Anonymous Quiz
37%
300 m
45%
150 m
16%
30 m
3%
None of the above
Forwarded from UPSC Mapping Prelims Mains
π India Adds 3,582 km to Coastline & 7 New Islands
πA new reassessment using improved tech has increased Indiaβs official coastline length by ~50%
β Previous coastline (1970s): 7,516 km
β New official length: 11,058.6 km
β Reason: Higher-resolution data (1:25000 map scale vs older 1:45000)
β 3,582 km βaddedβ due to better capture of curves, bends & offshore island coastlines
β 7 new offshore islands identified; total island count now 1,389 (1,298 offshore + 91 inshore)
β Coastline measurement now to be done every 10 years
πState-wise highest coastline
β Gujarat (2,340 km), Andaman & Nicobar (3,083 km), Tamil Nadu (1,068 km)
πImplications
β Better disaster management, CRZ rules, coastal zone protection
β Improved planning for shipping, security, and tourism
β Reclassification will not affect boundaries, only accuracy
#GS1 #Geography #Coastline #Mapping
πA new reassessment using improved tech has increased Indiaβs official coastline length by ~50%
β Previous coastline (1970s): 7,516 km
β New official length: 11,058.6 km
β Reason: Higher-resolution data (1:25000 map scale vs older 1:45000)
β 3,582 km βaddedβ due to better capture of curves, bends & offshore island coastlines
β 7 new offshore islands identified; total island count now 1,389 (1,298 offshore + 91 inshore)
β Coastline measurement now to be done every 10 years
πState-wise highest coastline
β Gujarat (2,340 km), Andaman & Nicobar (3,083 km), Tamil Nadu (1,068 km)
πImplications
β Better disaster management, CRZ rules, coastal zone protection
β Improved planning for shipping, security, and tourism
β Reclassification will not affect boundaries, only accuracy
π Prelims Question:
Which state has the longest coastline in India as per the revised measurements?
(a) Maharashtra
(b) Tamil Nadu
(c) Gujarat β
(d) Andhra Pradesh
π Mains Question:
Explain the significance of scientific reassessment of coastline and islands in Indiaβs disaster management and developmental planning.
#GS1 #Geography #Coastline #Mapping
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π Why Large Cities Attract More Migrants than Smaller Towns
π A Developing Country Perspective β UPSC 2024
π Migration is skewed towards big cities due to:
β Diverse & abundant employment in formal/informal sectors
β’ Example: Mumbai & Bengaluru attract rural youth in tech, finance, construction
β Better access to education & healthcare
β’ Example: Delhiβs DU and AIIMS draw families for advancement
β Superior infrastructure & logistics
β’ Example: Metro, airports, 24Γ7 power in Chennai enhance urban appeal
β Urban informal economy absorbs unskilled labor
β’ Example: Bihar & UP migrants work in Mumbaiβs construction/domestic sectors
β Presence of migrant networks & support systems
β’ Example: Malayali migrants in Kochi facilitate Gulf migration links
β Urban aspirations & perceived mobility
β’ Example: Media portrayals of progress create a strong βpull effectβ
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π A Developing Country Perspective β UPSC 2024
π Migration is skewed towards big cities due to:
β Diverse & abundant employment in formal/informal sectors
β’ Example: Mumbai & Bengaluru attract rural youth in tech, finance, construction
β Better access to education & healthcare
β’ Example: Delhiβs DU and AIIMS draw families for advancement
β Superior infrastructure & logistics
β’ Example: Metro, airports, 24Γ7 power in Chennai enhance urban appeal
β Urban informal economy absorbs unskilled labor
β’ Example: Bihar & UP migrants work in Mumbaiβs construction/domestic sectors
β Presence of migrant networks & support systems
β’ Example: Malayali migrants in Kochi facilitate Gulf migration links
β Urban aspirations & perceived mobility
β’ Example: Media portrayals of progress create a strong βpull effectβ
ο»Ώ
π Mains GS1 Question
Explain the economic and socio-cultural factors that make large Indian cities preferred migration destinations compared to smaller towns.
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π Coastal Landforms β UPSC Notes
π Classification & Significance | Erosion, Deposition, and Government Response
β Erosional Landforms
β€ Headlands and Bays: Waves erode softer rock (bays); harder rock forms headlands.
β€ Cliffs and Wave-Cut Platforms: Cliffs formed by relentless wave pounding; erosion creates flat platforms at the base.
β€ Caves, Arches, Stacks, Stumps: Waves carve caves in headlands β grow into arches β collapse into stacks β eroded into stumps.
β Depositional Landforms
β€ Beaches: Formed by accumulation of eroded rock fragments by wave action.
β€ Spits, Bars and Lagoons: Spits = sand extensions into sea; when connected across a bay = bars, forming lagoons behind.
β Significance of Coastal Landforms
β€ Tourism Hubs: Especially beaches (major attractions).
β€ Mineral Resources: Beaches may contain gold (Subarnarekha River) & thorium (Kerala).
β Threats of Coastal Erosion
β€ Vulnerable Coastlines: 33.6% of Indiaβs coastline under threat; Odisha most affected (28%).
β€ Community Impact: Loss of boats, nets, fishing spaces; habitat destruction and displacement.
β Government Measures to Prevent Erosion
β€ Mangrove planting & shelterbelts
β€ Installing Geo-tubes
β€ Rs. 2500 crore under 15th Finance Commission for resettlement of displaced families and mitigation efforts.
#GS1 #Geography #CoastalErosion #DisasterMitigation
π Classification & Significance | Erosion, Deposition, and Government Response
β Erosional Landforms
β€ Headlands and Bays: Waves erode softer rock (bays); harder rock forms headlands.
β€ Cliffs and Wave-Cut Platforms: Cliffs formed by relentless wave pounding; erosion creates flat platforms at the base.
β€ Caves, Arches, Stacks, Stumps: Waves carve caves in headlands β grow into arches β collapse into stacks β eroded into stumps.
β Depositional Landforms
β€ Beaches: Formed by accumulation of eroded rock fragments by wave action.
β€ Spits, Bars and Lagoons: Spits = sand extensions into sea; when connected across a bay = bars, forming lagoons behind.
β Significance of Coastal Landforms
β€ Tourism Hubs: Especially beaches (major attractions).
β€ Mineral Resources: Beaches may contain gold (Subarnarekha River) & thorium (Kerala).
β Threats of Coastal Erosion
β€ Vulnerable Coastlines: 33.6% of Indiaβs coastline under threat; Odisha most affected (28%).
β€ Community Impact: Loss of boats, nets, fishing spaces; habitat destruction and displacement.
β Government Measures to Prevent Erosion
β€ Mangrove planting & shelterbelts
β€ Installing Geo-tubes
β€ Rs. 2500 crore under 15th Finance Commission for resettlement of displaced families and mitigation efforts.
π Prelims MCQ
Which of the following is a depositional coastal feature?
(a) Stack
(b) Cliff
(c) Lagoon
(d) Cave
β Ans: (c) Lagoon
π Mains Q (GS1 β Geography)
Discuss the formation and significance of coastal landforms. How is coastal erosion impacting Indiaβs coastal communities and what measures are being taken to mitigate it?
#GS1 #Geography #CoastalErosion #DisasterMitigation
πTrinidad and Tobago
β Location: Trinidad and Tobago is situated in the Caribbean Sea, off the northern edge of the South American mainland, just off the coast of Venezuela.
β It is part of the Lesser Antilles in the West Indies, geographically positioned between the Atlantic Ocean and the Caribbean Sea.
β The islands lie close to the continent of South America, separated by the Gulf of Paria.
β Physical Features: Trinidad, the larger of the two islands, is mostly flat with some low mountain ranges and fertile plains.
β Tobago, the smaller island, is more rugged and mountainous.
The region lies close to the Orinoco River Delta and experiences tropical maritime climate.
β Capital: Port of Spain
β Demographic Aspects: Over 35% of the population is of Indian descent, largely tracing their roots to indentured labourers brought from India during British colonial rule.
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β Location: Trinidad and Tobago is situated in the Caribbean Sea, off the northern edge of the South American mainland, just off the coast of Venezuela.
β It is part of the Lesser Antilles in the West Indies, geographically positioned between the Atlantic Ocean and the Caribbean Sea.
β The islands lie close to the continent of South America, separated by the Gulf of Paria.
β Physical Features: Trinidad, the larger of the two islands, is mostly flat with some low mountain ranges and fertile plains.
β Tobago, the smaller island, is more rugged and mountainous.
The region lies close to the Orinoco River Delta and experiences tropical maritime climate.
β Capital: Port of Spain
β Demographic Aspects: Over 35% of the population is of Indian descent, largely tracing their roots to indentured labourers brought from India during British colonial rule.
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πNoctilucent Clouds:
β They are thin, wispy clouds that glow with a blue or silvery hue at night when illuminated by sunlight from below the horizon.
β Horizon refers to the apparent line that separates the Earth from the skyβspecifically, the point below which the Sun appears to set.
β The name βnoctilucentβ is derived from the Latin words "nocto" and "lucent" which translates to "night" and "shining" respectively.
β They are sometimes referred to as polar mesospheric clouds.
β Most of our planet's clouds form in the Earth's troposphere. β Noctilucent clouds are located in the third layer of Earth's atmosphere, the mesosphere, making them Earth's highest clouds.
β They only appear during the summer months, and only at latitudes between about 45 and 80 degrees north or south of the equator.
β In the Northern Hemisphere, they can appear from the end of May to the beginning of August, with sightings more likely during June and July.
β In the Southern Hemisphere, noctilucent cloud sightings are much rarer, but they can be visible from the end of November to the beginning of February, with sightings most likely during December and January.
β In these months and at the right latitudes, the Sun only just sets below the horizon at nighttime.
β That means these very high clouds can still be lit by bright sunlight from below, even though the rest of the surface is in darkness β making the clouds appear to glow.
β The Sun sets increasingly less below the horizon the further north you go, which means northern latitudes will experience noctilucent clouds for longer during the night.
πHow are noctilucent clouds formed?
β They are formed of ice crystals; in the summer the mesosphere becomes cold enough to allow ice to form on suspended dust particles floating in the atmosphere.
β The dust particles may originate from micrometeorites falling to Earth from space, or the dust left over from volcanic eruptions.
β Humans have also accidentally seeded our own noctilucent clouds through the exhausts of rockets propelled into space.
β The ice crystals that form reflect the sunlight when the Sun hits them from below, causing the clouds' characteristic shimmer.
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β They are thin, wispy clouds that glow with a blue or silvery hue at night when illuminated by sunlight from below the horizon.
β Horizon refers to the apparent line that separates the Earth from the skyβspecifically, the point below which the Sun appears to set.
β The name βnoctilucentβ is derived from the Latin words "nocto" and "lucent" which translates to "night" and "shining" respectively.
β They are sometimes referred to as polar mesospheric clouds.
β Most of our planet's clouds form in the Earth's troposphere. β Noctilucent clouds are located in the third layer of Earth's atmosphere, the mesosphere, making them Earth's highest clouds.
β They only appear during the summer months, and only at latitudes between about 45 and 80 degrees north or south of the equator.
β In the Northern Hemisphere, they can appear from the end of May to the beginning of August, with sightings more likely during June and July.
β In the Southern Hemisphere, noctilucent cloud sightings are much rarer, but they can be visible from the end of November to the beginning of February, with sightings most likely during December and January.
β In these months and at the right latitudes, the Sun only just sets below the horizon at nighttime.
β That means these very high clouds can still be lit by bright sunlight from below, even though the rest of the surface is in darkness β making the clouds appear to glow.
β The Sun sets increasingly less below the horizon the further north you go, which means northern latitudes will experience noctilucent clouds for longer during the night.
πHow are noctilucent clouds formed?
β They are formed of ice crystals; in the summer the mesosphere becomes cold enough to allow ice to form on suspended dust particles floating in the atmosphere.
β The dust particles may originate from micrometeorites falling to Earth from space, or the dust left over from volcanic eruptions.
β Humans have also accidentally seeded our own noctilucent clouds through the exhausts of rockets propelled into space.
β The ice crystals that form reflect the sunlight when the Sun hits them from below, causing the clouds' characteristic shimmer.
#GS1 #geography #prelims
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Forwarded from CSE EXAM ( UPSC prelims mains) CAPF
doc2025715586701.pdf
2.6 MB
The Indian Monsoon
Natureβs Pulse and Nationβs Lifeline
#Geography #GS1 #prelims
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Natureβs Pulse and Nationβs Lifeline
#Geography #GS1 #prelims
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@PIB_UPSC
π Why Earth Is Spinning Faster Than Before β For Now
πSome of the shortest days in recent history occurred in July 2024, with Earthβs rotation clocking 1.34 milliseconds less than 24 hours on July 9. But this trend is temporary, not permanent.
β Key Takeaways
β’ Shortened Days: Earthβs rotation has slightly sped up in the past decade.
β’ Causes: Changes in Earthβs core, atmosphere, ocean currents, and Moonβs position.
β’ Moonβs Role: The Moonβs gravitational pull creates tides, which slow Earthβs rotation over millennia.
β’ Long-Term Trend: Despite current faster spin, Earthβs days are growing longer over time.
β’ Angular Momentum: Earth-Moon act as a systemβas Moon moves away, Earth slows down.
β’ Climate Link: Melting ice from poles shifts mass toward the equator, making Earth more oblate, thus slowing rotation.
#GS1 #Geography #ScienceTech #Prelims2025 #EarthRotation #science_and_technology
πSome of the shortest days in recent history occurred in July 2024, with Earthβs rotation clocking 1.34 milliseconds less than 24 hours on July 9. But this trend is temporary, not permanent.
β Key Takeaways
β’ Shortened Days: Earthβs rotation has slightly sped up in the past decade.
β’ Causes: Changes in Earthβs core, atmosphere, ocean currents, and Moonβs position.
β’ Moonβs Role: The Moonβs gravitational pull creates tides, which slow Earthβs rotation over millennia.
β’ Long-Term Trend: Despite current faster spin, Earthβs days are growing longer over time.
β’ Angular Momentum: Earth-Moon act as a systemβas Moon moves away, Earth slows down.
β’ Climate Link: Melting ice from poles shifts mass toward the equator, making Earth more oblate, thus slowing rotation.
π Prelims MCQο»Ώ
Which of the following factors contributes to the Earthβs changing rotation speed?
A) Atmospheric circulation
B) Movement of the Moon
C) Ice melt and sea level rise
D) All of the above
Answer: D) All of the above
π Mains GS1 Q
Explain the scientific causes of short-term and long-term variations in Earthβs rotation speed. What are their potential implications on timekeeping and Earth-Moon dynamics?
#GS1 #Geography #ScienceTech #Prelims2025 #EarthRotation #science_and_technology
π Aeolian Landforms: Shaped by Wind π¬οΈ
π Overview
β In hot deserts with scarce vegetation and low rainfall, wind acts as a major geomorphic agent.
β It creates two major types of landforms: Erosional and Depositional.
π πͺ¨ Erosional Landforms
β Ventifacts: Rocks polished by wind-blown sand; often pitted and grooved.
β Yardangs: Streamlined ridges aligned with prevailing winds, carved out of compacted sand.
β Deflation Hollows (Blowouts): Depressions formed as wind removes loose surface material.
β Mushroom Rocks: Rocks with narrow bases and wider topsβwind erodes the lower parts more.
β Zeugen: Flat-topped features with hard caprock and soft base, eroded into mesa-like forms.
β Inselbergs: Isolated hills left after wind erodes softer surrounding material.
π ποΈ Depositional Landforms
β Sand Dunes β Formed when wind deposits sand in mounds or ridges:
β Crescentic Dunes: Shaped like the letter βCβ β most common.
β Linear Dunes: Long, straight or slightly wavy ridges.
β Star Dunes: Multi-armed dunes with ridges radiating from a central point.
β Parabolic Dunes: U-shaped, with tips pointing against the wind.
β Dome Dunes: Rare, circular dunes without slipfaces.
β Loess
β Fine wind-blown silt deposited far beyond desert areas.
β Found in fertile regions like the Mississippi River valley.
β Uniform, porous, and valuable for agriculture.
π Remember
β Aeolian processes are most active in arid and semi-arid regions.
β Both erosion and deposition depend on wind velocity, surface material, and vegetation cover.
#GS1 #geography #prelims
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π Overview
β In hot deserts with scarce vegetation and low rainfall, wind acts as a major geomorphic agent.
β It creates two major types of landforms: Erosional and Depositional.
π πͺ¨ Erosional Landforms
β Ventifacts: Rocks polished by wind-blown sand; often pitted and grooved.
β Yardangs: Streamlined ridges aligned with prevailing winds, carved out of compacted sand.
β Deflation Hollows (Blowouts): Depressions formed as wind removes loose surface material.
β Mushroom Rocks: Rocks with narrow bases and wider topsβwind erodes the lower parts more.
β Zeugen: Flat-topped features with hard caprock and soft base, eroded into mesa-like forms.
β Inselbergs: Isolated hills left after wind erodes softer surrounding material.
π ποΈ Depositional Landforms
β Sand Dunes β Formed when wind deposits sand in mounds or ridges:
β Crescentic Dunes: Shaped like the letter βCβ β most common.
β Linear Dunes: Long, straight or slightly wavy ridges.
β Star Dunes: Multi-armed dunes with ridges radiating from a central point.
β Parabolic Dunes: U-shaped, with tips pointing against the wind.
β Dome Dunes: Rare, circular dunes without slipfaces.
β Loess
β Fine wind-blown silt deposited far beyond desert areas.
β Found in fertile regions like the Mississippi River valley.
β Uniform, porous, and valuable for agriculture.
π Remember
β Aeolian processes are most active in arid and semi-arid regions.
β Both erosion and deposition depend on wind velocity, surface material, and vegetation cover.
#GS1 #geography #prelims
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Forwarded from UPSC Mapping Prelims Mains
π India: Uneven Population Distribution & Density
π Why Population is Unevenly Distributed
β Terrain
β Flat plains = better farming, transport, industry β high density (e.g. Ganges Plain)
β Hilly & rugged terrain = poor access β low density (e.g. Arunachal Pradesh)
β Climate
β Extreme heat or cold, or scarce rainfall areas see low population (e.g. Himalayas, Thar Desert)
β Mineral Resources
β Minerals attract jobs/investment β more people (e.g. Chota Nagpur Plateau, Jharkhand)
β Fertile Soil
β Fertile land = better agriculture = more settlements (e.g. Ganges plain)
β Urbanization
β Jobs, economy pull people to cities β higher density (e.g. Delhi, Mumbai)
π Southern vs Northern India: Population Trends
β Development = Better Demographics
β Health & education improve population pyramid
β Southern states show better indicators vs Northern states
β Stage 4 of Demographic Transition
β South: Low birth/death rates, low TFR (<2.1) β lower growth rate
π Population Census in India
β First Census β 1872 (Lord Mayo, British India)
β Second Census β 1881 (Lord Ripon) β Started 10-year tradition
β Post-Independence β First full census in 1951, conducted every decade since
β Shows Indiaβs long-term commitment to using data for planning & development
π Why Population is Unevenly Distributed
β Terrain
β Flat plains = better farming, transport, industry β high density (e.g. Ganges Plain)
β Hilly & rugged terrain = poor access β low density (e.g. Arunachal Pradesh)
β Climate
β Extreme heat or cold, or scarce rainfall areas see low population (e.g. Himalayas, Thar Desert)
β Mineral Resources
β Minerals attract jobs/investment β more people (e.g. Chota Nagpur Plateau, Jharkhand)
β Fertile Soil
β Fertile land = better agriculture = more settlements (e.g. Ganges plain)
β Urbanization
β Jobs, economy pull people to cities β higher density (e.g. Delhi, Mumbai)
π Southern vs Northern India: Population Trends
β Development = Better Demographics
β Health & education improve population pyramid
β Southern states show better indicators vs Northern states
β Stage 4 of Demographic Transition
β South: Low birth/death rates, low TFR (<2.1) β lower growth rate
π Population Census in India
β First Census β 1872 (Lord Mayo, British India)
β Second Census β 1881 (Lord Ripon) β Started 10-year tradition
β Post-Independence β First full census in 1951, conducted every decade since
β Shows Indiaβs long-term commitment to using data for planning & development