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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بر اساس آخرین داده‌ها در تاریخ 06 ژوئیه, 2026، کانال فعالیت پایداری دارد. در ۳۰ روز گذشته تغییر اعضا برابر -1 140 و در ۲۴ ساعت گذشته برابر -52 بوده و همچنان دسترسی گسترده‌ای حفظ شده است.

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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”

به لطف به‌روزرسانی‌های پرتکرار (آخرین داده در تاریخ 07 ژوئیه, 2026)، کانال همواره به‌روز و دارای دسترسی بالاست. تحلیل‌ها نشان می‌دهد مخاطبان به‌طور فعال با محتوا تعامل دارند و آن را به نقطه اثرگذاری مهم در دسته آموزش تبدیل کرده‌اند.

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■ ORIGIN AND DEVELOPMENT OF PLAINS #Geomorphology #Plains ◇ Most of the plains have been originated due to upliftment or emergence of submerged landmasses under epicontinental seas due to diastrophic movements. Example - The Great Plains Province of the USA. ◇ Plains are formed due to filling of depressions with sediments, which are created in front of the mountains during the process of orogenesis. Example - The northern plains or the Ganga-Yamuna plains of India are typical examples of such plains. ◇ Sometimes, the middle part of the geosynclines remain unfolded after the formation of bordering ranges on both the margins of the geosynclines. Such area unaffected by folding activities, very often known as median mass, becomes plains. It may be pointed out that not all the median masses become plains, rather most of them become plateau like Tibetan plateau.

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■ CLASSIFICATION OF PLATEAU #Plateau #Geomorphology □ On the basis of mode of Origin ◇ Glacial plateaux - When mountains are greatly modified and transformed by glacial erosion, they are lowered in height and their sharp reliefs are rounded to such an extent that they become the example of Glaciers. ◇ Fluvial plateaux - are formed due to continuous deposits of fluvial sediments brought by the rivers. ◇ Aeolian plateau - is formed because of deposition of fine sediments brought by winds. Enormous volumes of sediments are consolidated in due course of time and plateau is formed. ◇ Tectonic Plateau - The plateau formed by horizontal and vertical movements caused by endogenetic forces are called diastrophic plateau. ◇ Intermontane plateaux - These are called intermontane because they are surrounded by hills and mountains almost from all sides. ◇ Piedmont plateau - Plateau formed at the foothill zone of extensive mountains is called piedmont plateau, which is surrounded by mountain range on one side while by plain topography or coastal plain on the other side. ◇ Dome shaped plateau - are formed when the landmass is uplifted in such a manner that the middle portion is upwarped and the sides are rounded. ◇ Volcanic plateaux - are those plateaux which are formed due to accumulation of thick layers of basaltic lavas. ▪︎JOIN - @upsc_polity_notes

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■ CLASSIFICATION OF PLATEAU □ According to mode of origin #Plateau #Geomorphology ◇ Simple Plateau Plateaux formed by exogenetic processes :- • Glacial plateau e.g. Garhwal plateau • Aeolian plateau e.g. Potawar plateau, Loess plateau. ◇ Compound Plateau Plateaux formed by endogenetic processes – • Intermontane plateau e.g. Tibetan plateau • Piedmont plateau e.g. Applachian Piedmont Plateau • Dome plateau e.g. Ozark Massif (USA), Chotanagpur plateau (Jharkhand, India). • Lava plateaux - examples, Columbia plateau (USA), Mahabaleshwar plateau, Panchagni tableland etc. ▪︎JOIN - @upsc_geography_notes

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◇ From the stand point of surficial materials plateaux also register wide range of variations. Some plateaux have thick covers of basaltic lavas e.g. Deccan plateaux in an area of 7,74,000 km² (e.g. Mahabaleshwar plateau and Panchagani plateau in Maharashtra have thick covers of basaltic lavas topped by massive laterite covers. ◇ Some plateaux are so dissected by the network of streams that they are segmented into numerous parts e.g. patlands of Ranchi and Palamau uplands (in Jharkhand) have been segmented by the North Koel river and its tributaries into several flattopped ▪︎JOIN - @upsc_geography_notes

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■ PLATEAU - GENERAL CHARACTERISTICS #Plateau #Geomorphology ◇ On an average, plateaux are extensive upland areas characterized by flat and rough top surface, steep side walls which rise above the neighbouring ground surface at least for 300 m. ◇ From locational point of view plateaux vary from one place to another place. Some plateaux are surrounded by hills and mountains (e.g. Tibetan plateau). ◇ some plateaux are bordered by hills and mountains on one side while they are bordered by plains or coastal areas on the other side e.g. piedmont plateau of the USA. ◇ Some plateaux are very extensive in areal context e.g. Deccan plateau of India, Siberian plateau, Arabian plateau etc. The most characteristic features of plateaux are their flat and rolling top surfaces. Generally, the slopes of the side walls are very steep but the top surfaces, except minor reliefs, are more or less flat.

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4. As the continental plates converge, the ocean basic or a sedimentary basin (geoclinal or geosyncline Sediments found along the continental margins) is squeezed between the two converging plates. 5. Huge slivers of rock, many kilometres wide are thrust on top of one another, forming a towering mountain range. 6. With the building up of resistance, convergence comes to an end. The mountain belt erodes, and this is followed by isostatic adjustment. 7. As two massive continents weld, a single large continental mass joined by a mountain range is produced. 8. Examples: The Himalayas, Alps, Urals, Appalachians and the Atlas Mountains. ▪︎JOIN - @upsc_geography_notes

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■ CONTINENT-CONTINENT CONVERGENCE OR THE HIMALAYAN CONVERGENCE #Earthmovements Understanding Continent-Continent Convergence is important to understand the Formation of the Himalayas, the Alps, the Urals and the Atlas Mountains. ◇ In ocean-ocean convergence and continent-ocean convergence, at least one of the plates is denser and hence the subduction zone is quite deep (few hundred kilometres). ◇ At continent-continent convergent margins, due to lower density, both of the continental crustal plates are too light (buoyant) to be carried downward (subduct) into a trench. ◇ In most cases, neither plate subducts or even if one of the plates subducts, the subduction zone will not go deeper than 40 – 50 km. The two plates converge, buckle up (suture zone), fold, and fault.