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

Ko'proq ko'rsatish

Tarmoq:UPSC GEOGRAPHY Hindiston4 949 Taʼlim2 433...

📈 Telegram kanali UPSC GEOGRAPHY analitikasi

UPSC GEOGRAPHY (@upsc_geography_notes_optional) Ingliz til segmentidagi kanali faol ishtirokchi. Hozirda hamjamiyat 67 135 obunachidan iborat bo'lib, Taʼlim toifasida 2 433-o'rinni va Hindiston mintaqasida 4 949-o'rinni egallagan.

📊 Auditoriya ko‘rsatkichlari va dinamika

невідомо sanasidan buyon loyiha tez o‘sib, 67 135 obunachiga ega bo‘ldi.

24 Iyun, 2026 dagi oxirgi ma’lumotlarga ko‘ra kanal barqaror faollikka ega. Oxirgi 30 kunda obunachilar soni -1 073 ga, so‘nggi 24 soatda esa -53 ga o‘zgardi va umumiy qamrov yuqori darajada qolmoqda.

Tasdiqlash holati: Tasdiqlanmagan
Jalb etish (ER): Auditoriya o‘rtacha 3.14% darajada jalb etiladi. Nashrdan keyingi dastlabki 24 soatda kontent odatda umumiy obunachilar sonining 3.24% ini tashkil etuvchi reaksiyalarni to‘playdi.
Post qamrovi: Har bir post o‘rtacha 2 109 marta ko‘riladi; birinchi sutkada odatda 2 175 ta ko‘rish yig‘iladi.
Reaksiyalar va o‘zaro ta’sir: Auditoriya faol: har bir postga o‘rtacha 0 ta reaksiya keladi.
Tematik yo‘nalishlar: Kontent prelim, hindu, sanctuary, upsc, polity kabi asosiy mavzularga jamlangan.

📝 Tavsif va kontent siyosati

Muallif resursni shaxsiy fikrni ifoda etish maydoni sifatida ta’riflaydi:
“This channel provides notes from different major books like D.R. khullar, G.C leong etc No copyright material allowed. Queries - @Upscgeographybot”

Yuqori yangilanish chastotasi (oxirgi ma’lumot 25 Iyun, 2026 da olingan) sababli kanal doimo dolzarb va katta qamrovli bo‘lib qoladi. Analitika auditoriya kontent bilan faol hamkorlik qilishini, uni Taʼlim toifasidagi muhim ta’sir nuqtasiga aylantirishini ko‘rsatadi.

67 135

Obunachilar

-5324 soatlar

-1867 kunlar

-1 07330 kunlar

2 109

Post ko'rishlar

~ 2 17524 soatlar

~ 2 18148 soatlar

3.14%

Muloqot nisbati

~ 1

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■ 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

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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

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■ 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

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WHY DO P-WAVES TRAVEL FASTER THAN S-WAVES ? #interiorofearth ◇ P-waves are about 1.7 times faster than the S-waves. ◇ P-waves are compression waves that apply a force in the direction of propagation and hence transmit their energy quite easily through the medium and thus travel quickly. ◇ On the other hand, S-waves are transverse waves or shear waves (motion of the medium is perpendicular to the direction of propagation of the wave) and are hence less easily transmitted through the medium. ▪︎@upsc_geography_notes

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■ BODY WAVES #interiorofearth Body waves are generated due to the release of energy at the focus and move in all directions travelling through the interior of the earth. Hence, the name body waves. There are two types of body waves:- ◇ Primary - waves. ◇ Secondary - waves. ▪︎@upsc_geography_notes.