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
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📈 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 62 748 suscriptores, ocupando la posición 2 683 en la categoría Educación y el puesto 5 159 en la región India.
📊 Métricas de audiencia y dinámica
Desde su creación el невідомо, el proyecto ha mostrado un crecimiento acelerado, reuniendo a 62 748 suscriptores.
Según los últimos datos del 05 noviembre, 2026, el canal mantiene una actividad estable. En los últimos 30 días la variación de miembros fue de -902, y en las últimas 24 horas de -35, conservando un alto alcance.
- Estado de verificación: No verificado
- Tasa de interacción (ER): El promedio de interacción de la audiencia es 3.51%. Durante las primeras 24 horas tras publicar, el contenido suele obtener 1.85% de reacciones respecto al total de suscriptores.
- Alcance de las publicaciones: Cada publicación recibe en promedio 2 200 visualizaciones. En el primer día suele acumular 1 159 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 06 noviembre, 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.
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Suscriptores
-3524 horas
-2127 días
-90230 días
Archivo de publicaciones
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■ HYDRATION
#Geomorphology
#Geomorphicmovements
#Chemicalweathering
◇ Hydration is the chemical addition of water that involves the rigid attachment of H+ and OH- ions to the atoms and molecules of a mineral.
◇ When rock minerals take up water, the increased volume creates physical stresses within the rock. For example, iron oxides are converted to iron hydroxides which are larger in volume.
◇ Hydration is reversible, and continued repetition of this process causes fatigue in the rocks and may lead to their disintegration.
◇ The volume changes in minerals due to hydration will also help in physical weathering through exfoliation and granular disintegration.
◇ Hydration is reversible, and continued repetition of this process causes fatigue in the rocks and may lead to their disintegration.
◇ The volume changes in minerals due to hydration will also help in physical weathering through exfoliation and granular disintegration.
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■ ANTHROPOGENIC SOLUTION WEATHERING
#Geomorphology
#Geomorphicmovements
#Chemicalweathering
◇ Rainfall is naturally acidic ― pH of ~5.6 (CO2 dissolves in the rainwater producing weak carbonic acid).
◇ Acid rain occurs when gases such as sulphur dioxide and nitrogen oxides are present in the atmosphere.
◇ These oxides react in the rainwater to produce stronger acids and can lower the pH to less than 4.
◇ These acids are capable of attacking certain kinds of rocks in much the way that carbonic acid does.
◇ Sulphur dioxide, SO2, comes from volcanic eruptions or fossil fuels. The conversion of metallic ores to the pure metals often results in the formation of sulphur dioxide.
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■ CARBONATION – NATURAL SOLUTION WEATHERING
#Geomorphology
#Geomorphicmovements
#Chemicalweathering
◇ Carbonation refers to reactions of carbon dioxide to give carbonates, bicarbonates, and carbonic acid.
◇ Carbonation weathering is a process in which atmospheric carbon dioxide leads to solution weathering.
◇ As rain falls, it dissolves small amounts of carbon dioxide from the air, forming a weak acid that can dissolve some minerals like limestone (calcium carbonate) (solution weathering).
◇When carbonic acid reacts with limestone, it produces calcium bicarbonate, which is partially soluble in water (dissolution weathering.
◇ Caves are formed when underground water containing carbonic acid travels through blocks of limestone, dissolves out the limestone, and leaves empty pockets (caves) behind (E.g. Karst topography).
6. Carbonation process speeds up with a decrease in temperature because colder water holds more dissolved carbon dioxide gas.
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