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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
Показати більше📈 Аналітичний огляд Telegram-каналу UPSC GEOGRAPHY
Канал UPSC GEOGRAPHY (@upsc_geography_notes_optional) у мовному сегменті Англійська є активним учасником. На даний момент спільнота об'єднує 67 251 підписників, посідаючи 2 437 місце в категорії Освіта та 4 977 місце у регіоні Індія.
📊 Показники аудиторії та динаміка
З моменту свого створення невідомо, проект продемонстрував стрімке зростання, зібравши аудиторію у 67 251 підписників.
За останніми даними від 21 червня, 2026, канал демонструє стабільну активність. Хоча за останні 30 днів спостерігається зміна кількості учасників на -1 064, а за останні 24 години на -17, загальне охоплення залишається високим.
- Статус верифікації: Не верифікований
- Рівень залученості (ER): Середній показник залученості аудиторії становить 3.45%. Протягом перших 24 годин після публікації контент зазвичай збирає 1.79% реакцій від загальної кількості підписників.
- Охоплення публікацій: В середньому кожен допис отримує 2 324 переглядів. Протягом першої доби публікація в середньому набирає 1 202 переглядів.
- Реакції та взаємодія: Аудиторія активно підтримує контент: середня кількість реакцій на один пост – 0.
- Тематичні інтереси: Контент зосереджений навколо ключових тем, таких як prelim, hindu, sanctuary, upsc, polity.
📝 Опис та контентна політика
Автор описує ресурс як майданчик для висловлення суб'єктивної думки:
“This channel provides notes from different major books like D.R. khullar, G.C leong etc
No copyright material allowed.
Queries - @Upscgeographybot”
Завдяки високій частоті оновлень (останні дані отримано 22 червня, 2026), канал підтримує актуальність та високий рівень охоплення публікацій. Аналітика показує, що аудиторія активно взаємодіє з контентом, що робить його важливою точкою впливу в категорії Освіта.
67 251
Підписники
-1724 години
-1747 днів
-1 06430 день
Архів дописів
67 240
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67 240
■ INTERNAL STRUCTURE OF THE EARTH.
#interiorofearth
◇ The interior of the earth is made up of several concentric layers of which the crust, the mantle, the outer core and the inner core are significant because of their unique physical and chemical properties.
◇ The crust is a silicate solid, the mantle is a viscous molten rock, the outer core is a viscous liquid, and the inner core is a dense solid.
◇ Mechanically, the earth’s layers can be divided into lithosphere, asthenosphere, mesospheric mantle (part of the Earth's mantle below the lithosphere and the asthenosphere), outer core, and inner core.
◇ Chemically, Earth can be divided into the crust, upper mantle, lower mantle, outer core, and inner core.
▪︎ JOIN - @upsc_geography_notes
67 240
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■ SURFACE WAVES ( L-WAVES)
#interiorofearth
◇ The body waves interact with the surface rocks and generate new set of waves called surface waves (long or L-waves). These waves move only along the surface.
◇ Surface Waves are also called long period waves because of their long wavelength.
◇ They are low-frequency transverse waves (shear waves).
◇ They develop in the immediate neighbourhood of the epicentre and affect only the surface of the earth and die out at smaller depth.
◇ They lose energy more slowly with distance than the body waves because they travel only across the surface unlike the body waves which travel in all directions.
◇ Particle motion of surface waves (amplitude) is larger than that of body waves, so surface waves are the most destructive among the earthquake waves.
◇ They are slowest among the earthquake waves and are recorded last on the seismograph.
▪︎@upsc_geography_notes
67 240
Repost from UPSC GEOGRAPHY
■ SECONDARY WAVES (S-WAVES)
#Interiorofearth
◇ They are recorded second on the seismograph or S-waves are also called as transverse waves or shear waves or distortional waves.
◇ They are analogous to water ripples or light waves.
◇ Transverse waves or shear waves mean that the direction of vibrations of the particles in the medium is perpendicular to the direction of propagation of the wave. Hence, they create troughs and crests in the material through which they pass (they distort the medium).
◇ S-waves arrive at the surface after the P-waves.
◇ These waves are of high frequency and possess slightly higher destructive power compared to P-waves.
◇ The trembling on the earth’s surface caused due to these waves is from side to side (horizontal).
◇ S-waves cannot pass through fluids (liquids and gases) as fluids do not support shear stresses.
◇ They travel at varying velocities (proportional to shear strength) through the solid part of the Earth.
▪︎@upsc_geography_notes
67 240
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Repost from UPSC GEOGRAPHY
■ SECONDARY WAVES (S-WAVES)
#Interiorofearth
◇ They are recorded second on the seismograph or S-waves are also called as transverse waves or shear waves or distortional waves.
◇ They are analogous to water ripples or light waves.
◇ Transverse waves or shear waves mean that the direction of vibrations of the particles in the medium is perpendicular to the direction of propagation of the wave. Hence, they create troughs and crests in the material through which they pass (they distort the medium).
◇ S-waves arrive at the surface after the P-waves.
◇ These waves are of high frequency and possess slightly higher destructive power compared to P-waves.
◇ The trembling on the earth’s surface caused due to these waves is from side to side (horizontal).
◇ S-waves cannot pass through fluids (liquids and gases) as fluids do not support shear stresses.
◇ They travel at varying velocities (proportional to shear strength) through the solid part of the Earth.
▪︎@upsc_geography_notes
67 240
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67 240
■ SECONDARY WAVES (S-WAVES)
#Interiorofearth
◇ They are recorded second on the seismograph or S-waves are also called as transverse waves or shear waves or distortional waves.
◇ They are analogous to water ripples or light waves.
◇ Transverse waves or shear waves mean that the direction of vibrations of the particles in the medium is perpendicular to the direction of propagation of the wave. Hence, they create troughs and crests in the material through which they pass (they distort the medium).
◇ S-waves arrive at the surface after the P-waves.
◇ These waves are of high frequency and possess slightly higher destructive power compared to P-waves.
◇ The trembling on the earth’s surface caused due to these waves is from side to side (horizontal).
◇ S-waves cannot pass through fluids (liquids and gases) as fluids do not support shear stresses.
◇ They travel at varying velocities (proportional to shear strength) through the solid part of the Earth.
▪︎@upsc_geography_notes
67 240
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67 240
■ SECONDARY WAVES (S-WAVES)
#Interiorofearth
◇ They are recorded second on the seismograph or S-waves are also called as transverse waves or shear waves or distortional waves.
◇ They are analogous to water ripples or light waves.
◇ Transverse waves or shear waves mean that the direction of vibrations of the particles in the medium is perpendicular to the direction of propagation of the wave. Hence, they create troughs and crests in the material through which they pass (they distort the medium).
◇ S-waves arrive at the surface after the P-waves.
◇ These waves are of high frequency and possess slightly higher destructive power compared to P-waves.
◇ The trembling on the earth’s surface caused due to these waves is from side to side (horizontal).
◇ S-waves cannot pass through fluids (liquids and gases) as fluids do not support shear stresses.
◇ They travel at varying velocities (proportional to shear strength) through the solid part of the Earth.
▪︎@upsc_geography_notes
67 240
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More than 442 students who were using this channel - UPSC CSE TOPPER have cleared prelims cutoff with good margin.
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