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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

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کانال UPSC GEOGRAPHY (@upsc_geography_notes_optional) در بخش زبانی انگلیسی بازیگری فعال است. در حال حاضر جامعه شامل 66 638 مشترک است و جایگاه 2 452 را در دسته آموزش و رتبه 4 961 را در منطقه الهند دارد.

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از زمان ایجاد در невідомо، پروژه رشد سریعی داشته و 66 638 مشترک جذب کرده است.

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.

  • وضعیت تأیید: تأیید نشده
  • نرخ تعامل (ER): میانگین تعامل مخاطب 4.43% است و در ۲۴ ساعت نخست پس از انتشار، محتوا معمولاً 3.49% واکنش نسبت به کل مشترکان کسب می‌کند.
  • دسترسی پست‌ها: هر پست به طور میانگین 2 953 بازدید دریافت می‌کند. در اولین روز معمولاً 2 324 بازدید جمع‌آوری می‌شود.
  • واکنش‌ها و تعامل: مخاطبان به‌طور فعال حمایت می‌کنند؛ میانگین واکنش به هر پست 0 است.
  • علایق موضوعی: محتوا بر موضوعات کلیدی مانند prelim, hindu, sanctuary, upsc, polity تمرکز دارد.

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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.

66 638
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-2807 روز
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◇ A feature almost similar to doline in appearance but with shallow depth and larger areal extent is called solution pan. ◇ Sometimes, the floor of dolines is plugged due to deposition of clay, with the result water cannot percolate downward and thus doline is filled with water. Such dolines full of water are called karst lakes. ◇ Rock walled steep depressions caused by the collapse of ground surface are called cockpits. ◇ Karst windows formed due to collapse of upper surface of sink holes or dolines. These windows enable the investigators to observe sub-surface drainage and other features formed below the ground surface. ◇ Extensive depressions are called uvalas which are upto one kilometre across. They are formed in a number of ways e.g. • due to coalescence of several dolines due to continuous solution and enlargement of dolines, • due to collapse of upper roof of large cavities formed underground, • due to coalescence of various sink holes etc. Elongated uvalas are formed either due to (i) the elongated pattern of joints or (ii) due to coalescence of numerous sink holes aligned in a line. Smaller uvalas are called jamas. ▪︎Join - @upsc_geography_notes

■ SOLUTION HOLES AND ASSOCIATED FEATURES #Physiography #Karstlandforms ◇ Chemically active rainwater (charged with atmospheri
SOLUTION HOLES AND ASSOCIATED FEATURES #Physiography #Karstlandforms ◇ Chemically active rainwater (charged with atmospheric carbon dioxide) dissolves limestones and other carbonate rocks along their joints and thus numerous types of solution holes (e.g. sink holes, dolines etc.) are developed at the ground surface when limestones are directly exposed to the atmospheric processes. ◇ Smaller holes are called sink holes. ◇ Gradual enlargement of sink holes due to continuous Area dissolution of limestones results in the coalescence of closely spaced sink holes into one large hole which is called swallow hole. ◇ Some swallow holes are further enlarged due to continuous solution into larger depressions which are called dolines in the Karst Region and dolinas in Serbia. ◇ The solution holes enlarged due to collapse of some portion of upper surface because of formation of cavities below the ground surface are called collapse sinks.

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