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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 66 628 suscriptores, ocupando la posición 2 457 en la categoría Educación y el puesto 4 976 en la región India.
📊 Métricas de audiencia y dinámica
Desde su creación el невідомо, el proyecto ha mostrado un crecimiento acelerado, reuniendo a 66 628 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.
66 628
Suscriptores
-5224 horas
-2807 días
-1 14030 días
Archivo de publicaciones
66 628
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■ SRUCTURAL BENCHES
#Geomorphology #Landforms
◇ The step-like flat surfaces on either side of the present lowest valley floors are called terraces.
◇ The benches or terraces formed due to differential erosion of alternate bands of hard and soft rock beds are called structural benches or terraces because of lithological control in the rate of erosion and consequent development of benches.
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Repost from UPSC GEOGRAPHY
■ EROSIONAL LANDFORMS
#Geomorphology #Landforms
□ Waterfalls
◇ Waterfalls or simply falls are caused because of sudden descents or abrupt breaks in the longitudinal course of the rivers due to a host of factors e.g., variation in the relative resistance of rocks, relative difference in topographic reliefs, fall in the sea level and related rejuvenation, earth movements etc.
◇ Rapids are of much smaller dimension than waterfalls. Generally, they are found upstream from the main falls but they are also found independently.
◇ There is well marked fall line in India. This Indian fall line extends between the Purwa or Tons falls on the Tons river (in the north-west part of the Rewa district of Madhya Pradesh) in the west and Sasaram (Bihar) in the east along the junction of the northern foreland of Peninsular India and the Ganga plains.
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■ EROSIONAL LANDFORMS
#Geomorphology #Landforms
□ Waterfalls
◇ Waterfalls or simply falls are caused because of sudden descents or abrupt breaks in the longitudinal course of the rivers due to a host of factors e.g., variation in the relative resistance of rocks, relative difference in topographic reliefs, fall in the sea level and related rejuvenation, earth movements etc.
◇ Rapids are of much smaller dimension than waterfalls. Generally, they are found upstream from the main falls but they are also found independently.
◇ There is well marked fall line in India. This Indian fall line extends between the Purwa or Tons falls on the Tons river (in the north-west part of the Rewa district of Madhya Pradesh) in the west and Sasaram (Bihar) in the east along the junction of the northern foreland of Peninsular India and the Ganga plains.
▪︎JOIN - @upsc_geography_notes
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◇ They are further transformed into very broad and shallow valleys having concave valley side slope of very gentle gradient during old stage. V-shaped valleys are divided into two types viz (1) gorges and (2) canyons.
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■ EROSIONAL LANDFORM
#Geomorphology #Landforms
□ River Valleys
◇ The shape and dimension of fluvially originated valleys change with the advancement of the stages of fluvial cycle of erosion. The valley formed in the youthful stage of fluvial cycle of erosion and in the initial stage of valley development is V-shaped having steep valley side slope of convex element. The valley is very deep and narrow, both the valley sides meet together at the valley floor and thus water always touches the valley sides. Such type of V-shaped valleys are the result of accelerated rate of downcutting (vertical erosion or valley deepening.
◇ The valleys are gradually widened due to lateral erosion with the advancement of the stage of cycle of erosion and they become quite broad with flat valley floor and uniform or rectilinear valley side slopes during mature stage or valley development and fluvial cycle of erosion.
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