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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 66 614 مشترک است و جایگاه 2 463 را در دسته آموزش و رتبه 4 966 را در منطقه الهند دارد.

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از زمان ایجاد در невідомо، پروژه رشد سریعی داشته و 66 614 مشترک جذب کرده است.

بر اساس آخرین داده‌ها در تاریخ 07 ژوئیه, 2026، کانال فعالیت پایداری دارد. در ۳۰ روز گذشته تغییر اعضا برابر -1 114 و در ۲۴ ساعت گذشته برابر -24 بوده و همچنان دسترسی گسترده‌ای حفظ شده است.

  • وضعیت تأیید: تأیید نشده
  • نرخ تعامل (ER): میانگین تعامل مخاطب 4.58% 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 3 054 بازدید دریافت می‌کند. در اولین روز معمولاً 2 324 بازدید جمع‌آوری می‌شود.
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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 08 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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◇ 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

■ CHARACTERSTICS OF SEDIMENTARY ROCKS #Rocks #Physiography ◇ Formed of sediments derived from the older rocks, plant and anim
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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