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UPSC GEOGRAPHY

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

📈 Telegram kanali UPSC GEOGRAPHY analitikasi

UPSC GEOGRAPHY (@upsc_geography_notes_optional) Ingliz til segmentidagi kanali faol ishtirokchi. Hozirda hamjamiyat 66 628 obunachidan iborat bo'lib, Taʼlim toifasida 2 457-o'rinni va Hindiston mintaqasida 4 976-o'rinni egallagan.

📊 Auditoriya ko‘rsatkichlari va dinamika

невідомо sanasidan buyon loyiha tez o‘sib, 66 628 obunachiga ega bo‘ldi.

06 Iyul, 2026 dagi oxirgi ma’lumotlarga ko‘ra kanal barqaror faollikka ega. Oxirgi 30 kunda obunachilar soni -1 140 ga, so‘nggi 24 soatda esa -52 ga o‘zgardi va umumiy qamrov yuqori darajada qolmoqda.

  • Tasdiqlash holati: Tasdiqlanmagan
  • Jalb etish (ER): Auditoriya o‘rtacha 4.43% 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 2 953 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.

📝 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 07 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.

66 628
Obunachilar
-5224 soatlar
-2807 kunlar
-1 14030 kunlar
Postlar arxiv
GEOGRAPHY MINDMAPS - CLICK HERE

■ LAKES #Lakes ◇ Lakes are those static bodies of water on the land surface which are surrounded by lands on all sides and ar
LAKES #Lakes ◇ Lakes are those static bodies of water on the land surface which are surrounded by lands on all sides and are always located on the land surface. ◇ Some lakes are as small as ponds while some lakes are as large as the Great Lakes of North America. ◇ Lakes are also called as inland standing water but this is not always true as some lakes are also located along the sea coasts e.g. Chilka lake in Orissa. ◇ Lakes are not permanent features on the earth's surface. Lakes are formed, developed and are ultimately obliterated due to siltation and upliftment of lake beds due to diastrophic movements, for example, several lakes have disappeared in the Kumaun region of Uttaranchal e.g., Sukha Tal. ▪︎JOIN - @upsc_geography_notes

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■ LAVA PLAINS #Plains #Geomorphology ◇ are formed due to deposition of thin sheets of lavas coming out through fissure flows.
LAVA PLAINS #Plains #Geomorphology ◇ are formed due to deposition of thin sheets of lavas coming out through fissure flows. ◇ Several examples of lava plains are found in France, New Zealand, Iceland, USA, Argentina etc. Lava plains are economically very important because black soils are formed due to weathering of lavas. ▪︎JOIN - @upsc_geography_notes

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GEOGRAPHY MINDMAPS - CLICK HERE

■ FLOOD PLAINS #Geomorphology #Plains ◇ are formed due to deposition of fine sediments consisting of sands, silts, muds, clay
FLOOD PLAINS #Geomorphology #Plains ◇ are formed due to deposition of fine sediments consisting of sands, silts, muds, clays etc. in the flood zones of the rivers. Flood plains are also known as alluvial plains because they are formed of the argillaceous sediments or alluvial soils. ◇ In India flood plains are divided into (i) khadar plains and (ii) bhangar plains. ▪︎JOIN - @upsc_geography_notes

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RIVER DEPOSITED PLAINS #Geomorphology #Plains The alluvial plains deposited by rivers are most extensive depositional plains. The North Indian Plains or the Ganga-Yamuna Plains were formed due to deposition of eroded materials into extensive foredeep which was formed due to Himalayan orogenetic movements. Piedmont alluvial plains - are formed at the foothill zones of the mountains. ◇ The gradient of the rivers is remarkably reduced at the foothill zones where the river leaves the mountain and enters the plains topography of level to gentle slope (less than 5 degree of slope), with the result sediments of fairly large size, e.g. cobbles, pebbles, boulders together with silt and gravels are deposited at the foot of the mountains because the rivers are unable to carry them further downstream due to decrease in transportation capacity because of marked decrease in the channel gradient. ◇ If several rivers descend through a mountain range numerous alluvial fans are formed parallel to the mountain range. ◇ These alluvial fans gradually and gradually grow in size and thus coalesce to form one extensive fan which becomes piedmont alluvial fan plain. ◇ The mountainward portion of the piedmont alluvial plains is called Bhabar in India. ▪︎JOIN - @upsc_geography_notes

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GEOGRAPHY MINDMAPS - CLICK HERE

Karst plains ◇ The plateau composed of massive limestones are subjected to chemical weathering and erosion by groundwater and are ultimately transformed into subdued topographic surface of very low relief. Such plains are called karst plains which are formed at the end of karst cycle of erosion. ▪︎JOIN - @upsc_geography_notes

■ EROSIONAL PLAINS #Geomorphology #Plains □ Peneplains ◇ Peneplains are the most characteristic plains formed by river erosio
EROSIONAL PLAINS #Geomorphology #Plains Peneplains ◇ Peneplains are the most characteristic plains formed by river erosion at the end of 'normal cycle of erosion'. ◇ Peneplains are characterized by convexo-concave residual hills, known as monadnocks, which project above the general surface. ◇ The peneplains are formed by lateral erosion by the rivers and weathering processes. The weathered materials are deposited over the peneplains. Rivers are well adjusted to the structure. Glaciated plains ◇ Glaciers transform highland areas through their slow but continued erosive works into lowland with flat surface but with sufficient low reliefs of rounded shape. Wind eroded plains ◇ Rocks become loose due to disintegration caused by mechanical (physical) weathering in the hot desert areas. Strong winds pick up these weathered and communited fine particles and deposit them elsewhere.

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Karst plains ◇ The plateau composed of massive limestones are subjected to chemical weathering and erosion by groundwater and are ultimately transformed into subdued topographic surface of very low relief. Such plains are called karst plains which are formed at the end of karst cycle of erosion. ▪︎JOIN - @upsc_geography_notes

■ EROSIONAL PLAINS #Geomorphology #Plains □ Peneplains ◇ Peneplains are the most characteristic plains formed by river erosio
EROSIONAL PLAINS #Geomorphology #Plains Peneplains ◇ Peneplains are the most characteristic plains formed by river erosion at the end of 'normal cycle of erosion'. ◇ Peneplains are characterized by convexo-concave residual hills, known as monadnocks, which project above the general surface. ◇ The peneplains are formed by lateral erosion by the rivers and weathering processes. The weathered materials are deposited over the peneplains. Rivers are well adjusted to the structure. Glaciated plains ◇ Glaciers transform highland areas through their slow but continued erosive works into lowland with flat surface but with sufficient low reliefs of rounded shape. Wind eroded plains ◇ Rocks become loose due to disintegration caused by mechanical (physical) weathering in the hot desert areas. Strong winds pick up these weathered and communited fine particles and deposit them elsewhere.

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◇ Sometimes, coastal lands are submerged under sea water because of transgressional phase of sea. Such coastal lands submerged under shallow water receive sediments regularly and after long time of continuous sedimentation narrow coastal plains are formed. Ex - The eastern coastal plains of India, mainly North Circar. ◇ Submerged coastal lands emerge as marine coastal plains due to withdrawal of sea water during regressional phase of sea. The Kutch plain of India is the example of such plain. ◇ Extensive plateaux denudation become plains. ◇ Deposition of enormous volume of lavas over extensive area gives birth to lava or volcanic plains. ▪︎JOIN - @upsc_geography_notes

UPSC GEOGRAPHY - Telegram kanali @upsc_geography_notes_optional statistikasi va tahlili