¡Ya disponible! Investigación de Telegram 2025 — los principales insights del año 
UPSC GEOGRAPHY
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This channel provides notes from different major books like D.R. khullar, G.C leong etc No copyright material allowed. Queries - @Upscgeographybot
Mostrar más📈 Análisis del canal de Telegram UPSC GEOGRAPHY
El canal UPSC GEOGRAPHY (@upsc_geography_notes_optional) en el segmento lingüístico de Inglés es un actor destacado. Actualmente la comunidad reúne a 67 144 suscriptores, ocupando la posición 2 444 en la categoría Educación y el puesto 4 960 en la región India.
📊 Métricas de audiencia y dinámica
Desde su creación el невідомо, el proyecto ha mostrado un crecimiento acelerado, reuniendo a 67 144 suscriptores.
Según los últimos datos del 24 junio, 2026, el canal mantiene una actividad estable. En los últimos 30 días la variación de miembros fue de -1 073, y en las últimas 24 horas de -53, conservando un alto alcance.
- Estado de verificación: No verificado
- Tasa de interacción (ER): El promedio de interacción de la audiencia es 3.14%. Durante las primeras 24 horas tras publicar, el contenido suele obtener 3.24% de reacciones respecto al total de suscriptores.
- Alcance de las publicaciones: Cada publicación recibe en promedio 2 109 visualizaciones. En el primer día suele acumular 2 175 visualizaciones.
- Reacciones e interacción: La audiencia responde de forma activa: el promedio de reacciones por publicación es 0.
- Intereses temáticos: El contenido se centra en temas clave como prelim, hindu, sanctuary, upsc, polity.
📝 Descripción y política de contenido
El autor describe el recurso como un espacio para expresar opiniones subjetivas:
“This channel provides notes from different major books like D.R. khullar, G.C leong etc
No copyright material allowed.
Queries - @Upscgeographybot”
Gracias a la alta frecuencia de actualizaciones (últimos datos recibidos el 25 junio, 2026), el canal mantiene la vigencia y un amplio alcance. La analítica demuestra que la audiencia interactúa activamente con el contenido, lo que lo convierte en un punto de referencia dentro de la categoría Educación.
67 144
Suscriptores
-5324 horas
-1867 días
-1 07330 días
Archivo de publicaciones
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■ ALLUVIAL SOIL
#Soil
◇ Alluvial soils are formed mainly due to silt deposited by Indo-Gangetic-Brahmaputra rivers.
◇ In coastal regions, some alluvial deposits are formed due to wave action.
◇ Rocks of the Himalayas form the parent material.
◇ They are the largest soil group covering about 15 lakh sq km or about 45.6 per cent of the total area.
◇ They support more than 40% of India’s population by providing the most productive agricultural lands.
□ CHARACTERSTICS OF ALLUVIAL SOIL.
◇ They are immature and have weak profiles due to their recent origin.
◇ Most of the soil is loamy. Sandy and clayey soils are not uncommon.
◇ Pebbly and gravelly soils are rare.
◇ Kankar (calcareous concretions) beds are present in some regions along the river terraces.
◇ The soil is porous because of its loamy (equal proportion of sand and clay) nature.
◇ Porosity and texture provide good drainage and other conditions favourable for agriculture.
◇ These soils are replenished by the recurrent floods
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Repost from UPSC GEOGRAPHY
■ BLACK SOIL.
#Soil
◇ The parent material for most of the black soil are the volcanic rocks that were formed in the Deccan Plateau.
◇ In Tamil Nadu, gneisses and schists form the parent material. The former are sufficiently deep while the later are generally shallow.
◇ These are the region of high temperature and low rainfall. It is, therefore, a soil group typical to the dry and hot regions of the Peninsula.
◇ A typical black soil is highly argillaceous (containing clay) with a large clay factor, 62 per cent or more.
• In general, black soils of uplands are of low fertility while those in the valleys are very fertile.
◇ The black soil is highly retentive of moisture.
◇ It swells greatly on accumulating moisture.
◇ In the rainy season, the soil gets very sticky and hence ploughing, and other agricultural activities demand more effort.
◇ In summer, the moisture evaporates the soil shrinks and is seamed with broad and deep cracks.
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■ BLACK SOIL.
#Soil
◇ The parent material for most of the black soil are the volcanic rocks that were formed in the Deccan Plateau.
◇ In Tamil Nadu, gneisses and schists form the parent material. The former are sufficiently deep while the later are generally shallow.
◇ These are the region of high temperature and low rainfall. It is, therefore, a soil group typical to the dry and hot regions of the Peninsula.
◇ A typical black soil is highly argillaceous (containing clay) with a large clay factor, 62 per cent or more.
• In general, black soils of uplands are of low fertility while those in the valleys are very fertile.
◇ The black soil is highly retentive of moisture.
◇ It swells greatly on accumulating moisture.
◇ In the rainy season, the soil gets very sticky and hence ploughing, and other agricultural activities demand more effort.
◇ In summer, the moisture evaporates the soil shrinks and is seamed with broad and deep cracks.
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■ FACTORS AFFECTING SOIL FORMATIONS IN INDIA.
#Soil
4. NATURAL VEGETATION.
◇ Natural vegetation reflects the combined effects of relief and climate.
◇ The formation and development of soil is very much influenced by the growth of vegetation.
◇ The decayed leaf material adds much-needed humus to soil thereby increasing its fertility.
◇ The densely forested areas contain some of the best soils in India.
◇ There is a close relationship between the vegetation types and soil types in India.
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■ FACTORS AFFECT SOIL FORMATION IN INDIA.
#Soil
3. CLIMATE.
◇ Temperature and rainfall are the most important factors in soil formation.
◇ They determine the effectiveness of weathering of the parent material, the quantity of water seeping through the soil and the type of micro-organisms present therein.
◇ Two different parent materials may develop the same soil in the same type of climate.
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✅ Reviews: @csatmantra_reviews
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For any queries, feel free to message us @csatmantra.
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■ FACTORS AFFECTING SOIL FORMATION IN INDIA.
#Soil
2. RELIEF
◇ The relief is the most important factor for soil formation in places with steep slopes like the hilly regions, edges of plateaus etc.
◇ Soil erosion on barren slopes is rampant, and it hinders soil formation. Example: Chambal ravines, higher reaches of the Himalayas where there is minimal or no forest cover (most on the steep southern slopes) etc.
◇ The areas of low relief or gentle slope generally experience deposition and have deep soils. Example: Indo Gangetic plain.
◇ The exceptions in the plateau are river basins where the soil layers are sufficiently deep.
▪︎SOURCE - D.R. Khullar (Chapter - 7).
