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By Rodhia Izzati
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Get instant insights and key takeaways from this YouTube video by Rodhia Izzati.
Exogenous Forces Shaping the Earth
๐ Exogenous forces, originating from outside the Earth, are responsible for shaping the surface, contrasting with endogenous forces from within.
โ๏ธ These external processes include weathering (pelapukan), erosion (erosi), sedimentation (andapan), and mass wasting (gerakan tanah).
๐ฅ The primary role of exogenous forces is to destroy or reshape the landforms created by endogenous processes.
Weathering (Pelapukan)
โ๏ธ Weathering is the breakdown of rocks into smaller pieces caused by sunlight, water, glaciers, chemical reactions, and organisms.
๐ ๏ธ Weathering is classified into three types: mechanical/physical (no chemical change), chemical (involves chemical structure change, common in Karst/limestone), and organic (aided by organisms/plants).
โ๏ธ Physical weathering is caused by temperature changes (day/night), freezing water into ice in cracks, and water/glacier movement, altering rock shape and size.
๐งช Chemical weathering relies on agents like oxygen, water, and carbon dioxide (); for example, water rich in dissolves limestone, forming cave features like stalactites and stalagmites.
Erosion (Pengikisan)
๐ Erosion involves the release and transportation of rock material from one place to another by a transporting agent, following three steps: release, transportation, and deposition.
๐ช๏ธ Erosion is categorized into four main types: fluvial/water erosion (ablasi), coastal/sea wave erosion (abrasi), wind erosion (deflasi), and glacial erosion (eksarasi).
๐ง Water erosion progresses through stages: splash erosion (percik), sheet erosion (lembar), rill erosion (alur), and culminating in gully erosion (parit), which severely damages soil fertility.
๐๏ธ Grand Canyon, approximately 1,700 m deep, 29 km wide, and 450 km long, serves as a prime example of fluvial erosion caused by the Colorado River.
Types of Erosion Detailed
๐๏ธ Abrasion (sea wave erosion) creates coastal features like cliffs (dinding curam) and notches (relung); planting mangroves is an effort to prevent land erosion in coastal communities.
๐ต Deflation (wind erosion) typically occurs in dry desert regions experiencing sandstorms, leading to distinctive formations like the mushroom rock (batuan jamur).
๐๏ธ Glacial erosion (eksarasi) leaves characteristic parallel grooves on rocks and forms deep, elongated valleys, observable in areas like Yellowstone National Park.
Key Points & Insights
โก๏ธ Exogenous forces are crucial for reshaping the Earth's surface after internal (endogenous) processes form structures.
โก๏ธ Karst topography, featuring stalactites and stalagmites, is a direct result of chemical weathering dissolving limestone through acidic water containing .
โก๏ธ To combat coastal erosion, communities should implement preventative measures such as planting mangroves or constructing sea walls (tanggul).
โก๏ธ Severe land erosion, such as gully erosion (erosi Parit), results in land that is difficult to restore to its original fertility.
๐ธ Video summarized with SummaryTube.com on Jan 17, 2026, 08:00 UTC
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Full video URL: youtube.com/watch?v=QwMo0yCSuGU
Duration: 10:12
Get instant insights and key takeaways from this YouTube video by Rodhia Izzati.
Exogenous Forces Shaping the Earth
๐ Exogenous forces, originating from outside the Earth, are responsible for shaping the surface, contrasting with endogenous forces from within.
โ๏ธ These external processes include weathering (pelapukan), erosion (erosi), sedimentation (andapan), and mass wasting (gerakan tanah).
๐ฅ The primary role of exogenous forces is to destroy or reshape the landforms created by endogenous processes.
Weathering (Pelapukan)
โ๏ธ Weathering is the breakdown of rocks into smaller pieces caused by sunlight, water, glaciers, chemical reactions, and organisms.
๐ ๏ธ Weathering is classified into three types: mechanical/physical (no chemical change), chemical (involves chemical structure change, common in Karst/limestone), and organic (aided by organisms/plants).
โ๏ธ Physical weathering is caused by temperature changes (day/night), freezing water into ice in cracks, and water/glacier movement, altering rock shape and size.
๐งช Chemical weathering relies on agents like oxygen, water, and carbon dioxide (); for example, water rich in dissolves limestone, forming cave features like stalactites and stalagmites.
Erosion (Pengikisan)
๐ Erosion involves the release and transportation of rock material from one place to another by a transporting agent, following three steps: release, transportation, and deposition.
๐ช๏ธ Erosion is categorized into four main types: fluvial/water erosion (ablasi), coastal/sea wave erosion (abrasi), wind erosion (deflasi), and glacial erosion (eksarasi).
๐ง Water erosion progresses through stages: splash erosion (percik), sheet erosion (lembar), rill erosion (alur), and culminating in gully erosion (parit), which severely damages soil fertility.
๐๏ธ Grand Canyon, approximately 1,700 m deep, 29 km wide, and 450 km long, serves as a prime example of fluvial erosion caused by the Colorado River.
Types of Erosion Detailed
๐๏ธ Abrasion (sea wave erosion) creates coastal features like cliffs (dinding curam) and notches (relung); planting mangroves is an effort to prevent land erosion in coastal communities.
๐ต Deflation (wind erosion) typically occurs in dry desert regions experiencing sandstorms, leading to distinctive formations like the mushroom rock (batuan jamur).
๐๏ธ Glacial erosion (eksarasi) leaves characteristic parallel grooves on rocks and forms deep, elongated valleys, observable in areas like Yellowstone National Park.
Key Points & Insights
โก๏ธ Exogenous forces are crucial for reshaping the Earth's surface after internal (endogenous) processes form structures.
โก๏ธ Karst topography, featuring stalactites and stalagmites, is a direct result of chemical weathering dissolving limestone through acidic water containing .
โก๏ธ To combat coastal erosion, communities should implement preventative measures such as planting mangroves or constructing sea walls (tanggul).
โก๏ธ Severe land erosion, such as gully erosion (erosi Parit), results in land that is difficult to restore to its original fertility.
๐ธ Video summarized with SummaryTube.com on Jan 17, 2026, 08:00 UTC
Find relevant products on Amazon related to this video
As an Amazon Associate, we earn from qualifying purchases

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