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

Red:UPSC GEOGRAPHY India4 961 Educación2 452...

📈 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 66 638 suscriptores, ocupando la posición 2 452 en la categoría Educación y el puesto 4 961 en la región India.

📊 Métricas de audiencia y dinámica

Desde su creación el невідомо, el proyecto ha mostrado un crecimiento acelerado, reuniendo a 66 638 suscriptores.

Según los últimos datos del 06 julio, 2026, el canal mantiene una actividad estable. En los últimos 30 días la variación de miembros fue de -1 140, y en las últimas 24 horas de -52, conservando un alto alcance.

Estado de verificación: No verificado
Tasa de interacción (ER): El promedio de interacción de la audiencia es 4.43%. Durante las primeras 24 horas tras publicar, el contenido suele obtener 3.49% de reacciones respecto al total de suscriptores.
Alcance de las publicaciones: Cada publicación recibe en promedio 2 953 visualizaciones. En el primer día suele acumular 2 324 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 07 julio, 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.

66 638

Suscriptores

-5224 horas

-2807 días

-1 14030 días

2 953

Visitas de la publicación

~ 2 32424 horas

~ 2 51948 horas

4.43%

Tasa de compromiso

~ 1

Mensajes por día

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◇ A feature almost similar to doline in appearance but with shallow depth and larger areal extent is called solution pan. ◇ Sometimes, the floor of dolines is plugged due to deposition of clay, with the result water cannot percolate downward and thus doline is filled with water. Such dolines full of water are called karst lakes. ◇ Rock walled steep depressions caused by the collapse of ground surface are called cockpits. ◇ Karst windows formed due to collapse of upper surface of sink holes or dolines. These windows enable the investigators to observe sub-surface drainage and other features formed below the ground surface. ◇ Extensive depressions are called uvalas which are upto one kilometre across. They are formed in a number of ways e.g. • due to coalescence of several dolines due to continuous solution and enlargement of dolines, • due to collapse of upper roof of large cavities formed underground, • due to coalescence of various sink holes etc. Elongated uvalas are formed either due to (i) the elongated pattern of joints or (ii) due to coalescence of numerous sink holes aligned in a line. Smaller uvalas are called jamas. ▪︎Join - @upsc_geography_notes

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■ SOLUTION HOLES AND ASSOCIATED FEATURES #Physiography #Karstlandforms ◇ Chemically active rainwater (charged with atmospheric carbon dioxide) dissolves limestones and other carbonate rocks along their joints and thus numerous types of solution holes (e.g. sink holes, dolines etc.) are developed at the ground surface when limestones are directly exposed to the atmospheric processes. ◇ Smaller holes are called sink holes. ◇ Gradual enlargement of sink holes due to continuous Area dissolution of limestones results in the coalescence of closely spaced sink holes into one large hole which is called swallow hole. ◇ Some swallow holes are further enlarged due to continuous solution into larger depressions which are called dolines in the Karst Region and dolinas in Serbia. ◇ The solution holes enlarged due to collapse of some portion of upper surface because of formation of cavities below the ground surface are called collapse sinks.

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