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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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تُعد قناة UPSC GEOGRAPHY (@upsc_geography_notes_optional) في القطاع اللغوي الإنكليزية لاعباً نشطاً. يضم المجتمع حالياً 66 707 مشتركاً، محتلاً المرتبة 2 457 في فئة التعليم والمرتبة 4 958 في منطقة الهند.

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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

بفضل وتيرة التحديث المرتفعة (أحدث البيانات بتاريخ 05 يوليو, 2026) تحافظ القناة على حداثتها ومستوى وصول مرتفع. وتُظهر التحليلات تفاعلاً نشطاً من الجمهور، ما يجعلها نقطة تأثير مهمة ضمن فئة التعليم.

66 707
المشتركون
-4224 ساعات
-2747 أيام
-1 13130 أيام
أرشيف المشاركات
◇ Gradient of longitudinal profiles of the canyons varies significantly but, on an average, it is 1.7 per cent. ◇ The canyons facing the river mouths are usually long (e.g., Congo Canyon) but have gentle gradient. The canyons located near the island are deep with steepest gradient (13.8 per cent). ◇ The submarine canyons carry various types of ocean deposits but the steep valley sides are devoid of unconsolidated materials. The floors of the canyons have coarser materials than the adjacent continental shelves. The deposits include sands, clays, silt, gravels and pebbles. ▪︎JOIN - @upsc_geography_notes

■ SUBMARINE CANYONS #Oceanography #oceanrelief ◇ Long, narrow and very deep valleys or trenches located on the continental sh
SUBMARINE CANYONS #Oceanography #oceanreliefLong, narrow and very deep valleys or trenches located on the continental shelves and slopes with vertical walls resembling the continental canyons are called submarine canyons because of their location under oceanic water. ◇ On the basis of morphogenetic processes these are classified into (i) glacially eroded canyons and (ii) non-glacial canyons. ◇ submarine canyons are similar to the youthful river valleys on the land but are decidedly deeper and a few of them have dendritic pattern of tributaries of secondary canyons. The longitudinal course of submarine canyons is usually sinuous while that of the subaerial canyons is generally straight.

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