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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Tarmoq:UPSC GEOGRAPHY Hindiston4 966 Taʼlim2 463...

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UPSC GEOGRAPHY (@upsc_geography_notes_optional) Ingliz til segmentidagi kanali faol ishtirokchi. Hozirda hamjamiyat 66 608 obunachidan iborat bo'lib, Taʼlim toifasida 2 463-o'rinni va Hindiston mintaqasida 4 966-o'rinni egallagan.

📊 Auditoriya ko‘rsatkichlari va dinamika

невідомо sanasidan buyon loyiha tez o‘sib, 66 608 obunachiga ega bo‘ldi.

07 Iyul, 2026 dagi oxirgi ma’lumotlarga ko‘ra kanal barqaror faollikka ega. Oxirgi 30 kunda obunachilar soni -1 114 ga, so‘nggi 24 soatda esa -24 ga o‘zgardi va umumiy qamrov yuqori darajada qolmoqda.

Tasdiqlash holati: Tasdiqlanmagan
Jalb etish (ER): Auditoriya o‘rtacha 4.58% darajada jalb etiladi. Nashrdan keyingi dastlabki 24 soatda kontent odatda umumiy obunachilar sonining 3.49% ini tashkil etuvchi reaksiyalarni to‘playdi.
Post qamrovi: Har bir post o‘rtacha 3 054 marta ko‘riladi; birinchi sutkada odatda 2 324 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.

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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 08 Iyul, 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.

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Obunachilar

-2424 soatlar

-2857 kunlar

-1 11430 kunlar

3 054

Post ko'rishlar

~ 2 32424 soatlar

~ 2 51948 soatlar

4.58%

Muloqot nisbati

~ 1

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66 608

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◇ Sedimentary rocks may be well consolidated, poorly consolidated and even unconsolidated. The composition of the rocks depends upon the nature of cementing elements and rock forming minerals. ◇ Sedimentary rocks are characterized by different sizes of joints. These are generally perpendicular to the bedding planes. ◇ The connecting plane between two consecutive/beds or layers of sedimentary rocks is called bedding plane. The uniformity of two beds along a bedding plane is called conformity (i.e. when beds are similar in all respect). When two consecutive beds are not uniform or conformal, the structure is called unconformity. ◇ Sedimentation units in the sedimentary rocks having a thickness of greater than one centimetre are called beds . The upper and lower surfaces of a bed are called bedding planes or bounding planes. Sometimes the lower surface of a bed is called sole while the upper surface is known as upper bedding surface. There are further sedimentary units within a bed. ◇ Soft muds and alluvia deposited by the rivers during flood period develop cracks when baked in the sun. These cracks are generally of polygonal shapes. Such cracks are called as mud cracks or sun cracks. ◇ Most of the sedimentary rocks are permeable and porous but a few of them are also nonporous and impermeable. The porosity of the rocks depends upon the ratio between the voids and the volume of a given rocks mass. ▪︎JOIN - @upsc_geography_notes

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■ CHARACTERSTICS OF SEDIMENTARY ROCKS #Rocks #Physiography ◇ Formed of sediments derived from the older rocks, plant and animal remains and thus these rocks contain fossils of plants and animals. ◇ Found over the largest surface area of the globe. It is believed that about 75 per cent of the surface area of the globe is covered by sedimentary rocks whereas igneous and metamorphic rocks cover the remaining 25 per cent area. Inspite of their largest coverage the sedimentary rocks constitute only 5 per cent of the composition of the crust whereas 95 per cent of the crust is composed of igneous and metamorphic rocks. ◇ Sedimentary rocks contain several layers or strata but these are seldom crystalline rocks. ◇ Like igneous rocks sedimentary rocks are not found in massive forms such as batholiths, laccoliths, dykes etc. ◇ Sedimentary layers are generally deformed due to lateral compressive and tensile forces.

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