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

Network:UPSC GEOGRAPHY India4 961 Education2 452...

📈 Analytical overview of Telegram channel UPSC GEOGRAPHY

Channel UPSC GEOGRAPHY (@upsc_geography_notes_optional) in the English language segment is an active participant. Currently, the community unites 66 638 subscribers, ranking 2 452 in the Education category and 4 961 in the India region.

📊 Audience metrics and dynamics

Since its creation on невідомо, the project has demonstrated rapid growth, gathering an audience of 66 638 subscribers.

According to the latest data from 06 July, 2026, the channel demonstrates stable activity. Although there has been a change in the number of participants by -1 140 over the last 30 days and by -52 over the last 24 hours, overall reach remains high.

Verification status: Not verified
Engagement rate (ER): The average audience engagement rate is 4.43%. Within the first 24 hours after publication, content typically collects 3.49% reactions from the total number of subscribers.
Post reach: On average, each post receives 2 953 views. Within the first day, a publication typically gains 2 324 views.
Reactions and interaction: The audience actively supports content: the average number of reactions per post is 0.
Thematic interests: Content is focused on key topics such as prelim, hindu, sanctuary, upsc, polity.

📝 Description and content policy

The author describes the resource as a platform for expressing subjective opinions:
“This channel provides notes from different major books like D.R. khullar, G.C leong etc No copyright material allowed. Queries - @Upscgeographybot”

Thanks to the high frequency of updates (latest data received on 07 July, 2026), the channel maintains relevance and a high level of publication reach. Analytics show that the audience actively interacts with content, making it an important point of influence in the Education category.

66 638

Subscribers

-5224 hours

-2807 days

-1 14030 days

2 953

Post views

~ 2 32424 hours

~ 2 51948 hours

4.43%

Engagement rate

~ 1

Posts per day

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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

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■ 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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