{"id":2881,"date":"2023-07-31T09:15:37","date_gmt":"2023-07-31T09:15:37","guid":{"rendered":"https:\/\/www.borthakursiasacademy.com\/blog\/?p=2881"},"modified":"2025-05-02T15:54:31","modified_gmt":"2025-05-02T15:54:31","slug":"a-comprehensive-guide-to-earths-diverse-geomorphic-features","status":"publish","type":"post","link":"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/","title":{"rendered":"Earth\u2019s Diverse Geomorphic Features\u2014A Comprehensive Guide for UPSC"},"content":{"rendered":"\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Introduction\"><\/span><strong>Introduction<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>The Earth&#8217;s surface is a dynamic and ever-changing canvas shaped by a variety of natural processes. These processes give rise to a wide array of <strong>geomorphic features<\/strong>\u2014landforms that range from towering mountains to vast plains, deep valleys, and rugged coastlines. If you are preparing for the UPSC\/APSC, understanding the origin and evolution of these features is important, as it forms the foundation of physical geography in both the Preliminary and Mains stages of the Civil Services Examination.<\/p><div id=\"ez-toc-container\" class=\"ez-toc-v2_0_77 counter-hierarchy ez-toc-counter ez-toc-grey ez-toc-container-direction\">\n<div class=\"ez-toc-title-container\">\n<p class=\"ez-toc-title\" style=\"cursor:inherit\">Table of Contents<\/p>\n<span class=\"ez-toc-title-toggle\"><a href=\"#\" class=\"ez-toc-pull-right ez-toc-btn ez-toc-btn-xs ez-toc-btn-default ez-toc-toggle\" aria-label=\"Toggle Table of Content\"><span class=\"ez-toc-js-icon-con\"><span class=\"\"><span class=\"eztoc-hide\" style=\"display:none;\">Toggle<\/span><span class=\"ez-toc-icon-toggle-span\"><svg style=\"fill: #999;color:#999\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" class=\"list-377408\" width=\"20px\" height=\"20px\" viewBox=\"0 0 24 24\" fill=\"none\"><path d=\"M6 6H4v2h2V6zm14 0H8v2h12V6zM4 11h2v2H4v-2zm16 0H8v2h12v-2zM4 16h2v2H4v-2zm16 0H8v2h12v-2z\" fill=\"currentColor\"><\/path><\/svg><svg style=\"fill: #999;color:#999\" class=\"arrow-unsorted-368013\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"10px\" height=\"10px\" viewBox=\"0 0 24 24\" version=\"1.2\" baseProfile=\"tiny\"><path d=\"M18.2 9.3l-6.2-6.3-6.2 6.3c-.2.2-.3.4-.3.7s.1.5.3.7c.2.2.4.3.7.3h11c.3 0 .5-.1.7-.3.2-.2.3-.5.3-.7s-.1-.5-.3-.7zM5.8 14.7l6.2 6.3 6.2-6.3c.2-.2.3-.5.3-.7s-.1-.5-.3-.7c-.2-.2-.4-.3-.7-.3h-11c-.3 0-.5.1-.7.3-.2.2-.3.5-.3.7s.1.5.3.7z\"\/><\/svg><\/span><\/span><\/span><\/a><\/span><\/div>\n<nav><ul class='ez-toc-list ez-toc-list-level-1 ' ><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-1\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Introduction\" >Introduction<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-2\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Geomorphic_Processes\" >Geomorphic Processes<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-3\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Classification_of_Geomorphic_Processes\" >Classification of Geomorphic Processes<\/a><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-4\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#1_Endogenic_Processes_Internal_Forces\" >1. Endogenic Processes (Internal Forces)<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-5\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Most_volcanic_mountains_are_found_around_the_Pacific_Ocean_in_an_area_called_the_Pacific_Ring_of_Fire\" >Most volcanic mountains are found around the Pacific Ocean in an area called the Pacific Ring of Fire.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-6\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#B_Plateaus\" >B. Plateaus<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-7\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#C_Earthquakes_and_Fault_Valleys\" >C.&nbsp; Earthquakes and Fault Valleys<\/a><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-8\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#2_Exogenic_Processes_External_Forces\" >2. Exogenic Processes (External Forces)<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-9\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#A_Fluvial_Landforms_Formed_by_rivers\" >A. Fluvial Landforms (Formed by rivers)<\/a><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-10\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Erosional_Features\" >Erosional Features:<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-11\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#bAeolian_Landforms_Formed_by_Wind\" >b.Aeolian Landforms (Formed by Wind)<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-12\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Erosional_Features-2\" >Erosional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-13\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Depositional_Features\" >Depositional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-14\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Examples_Thar_Desert_in_India_Sahara_Desert_in_Africa\" >Examples: Thar Desert in India, Sahara Desert in Africa<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-15\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#C_Glacial_Landforms_Formed_by_Glaciers\" >C. Glacial Landforms (Formed by Glaciers)<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-16\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#In_very_cold_places_glaciers_large_moving_bodies_of_ice_shape_the_land_by_eroding_wearing_away_rocks_and_depositing_the_material_they_carry\" >In very cold places, glaciers (large moving bodies of ice) shape the land by eroding (wearing away) rocks and depositing the material they carry.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-17\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Erosional_Features-3\" >Erosional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-18\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#These_landforms_are_made_when_glaciers_scrape_and_wear_down_the_land\" >These landforms are made when glaciers scrape and wear down the land.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-19\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Depositional_Features-2\" >Depositional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-20\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#These_form_when_glaciers_melt_and_leave_behind_the_rocks_and_soil_they_carried\" >These form when glaciers melt and leave behind the rocks and soil they carried.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-21\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Examples_Himalayas_Alps_Antarctica\" >Examples: Himalayas , Alps, Antarctica<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-22\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#D_Coastal_Landforms_Formed_by_Sea_Waves\" >D. Coastal Landforms (Formed by Sea Waves)<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-23\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#The_sea_shapes_the_coastline_through_waves_tides_and_currents_These_processes_cause_erosion_and_deposition_creating_many_interesting_landforms\" >The sea shapes the coastline through waves, tides, and currents. These processes cause erosion and deposition, creating many interesting landforms.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-24\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Erosional_Features-4\" >Erosional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-25\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Formed_when_strong_sea_waves_wear_away_the_rocks_along_the_coast\" >Formed when strong sea waves wear away the rocks along the coast.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-26\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Depositional_Features-3\" >Depositional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-27\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Formed_when_the_sea_deposits_sand_silt_and_other_materials\" >Formed when the sea deposits sand, silt, and other materials.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-28\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Examples_Kerala_Backwaters_Chilika_Lake_Odisha\" >Examples: Kerala Backwaters, Chilika Lake (Odisha)<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-29\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#E_Karst_Landforms_Chemical_Weathering_of_Limestone\" >E. Karst Landforms (Chemical Weathering of Limestone)<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-30\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Karst_landforms_are_made_in_areas_where_the_ground_is_made_of_limestone_or_dolomite_When_rainwater_mixes_with_carbon_dioxide_it_forms_a_weak_acid_that_dissolves_the_rock_This_is_called_chemical_weathering_especially_solution_and_carbonation\" >Karst landforms are made in areas where the ground is made of limestone or dolomite. When rainwater mixes with carbon dioxide, it forms a weak acid that dissolves the rock. This is called chemical weathering (especially solution and carbonation).<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-31\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Erosional_Features-5\" >Erosional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-32\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Formed_when_acidic_water_dissolves_the_limestone\" >Formed when acidic water dissolves the limestone.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-33\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Depositional_Features-4\" >Depositional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-34\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Depositional_Features-5\" >Depositional Features<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-35\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Formed_when_dissolved_limestone_is_left_behind_as_water_drips_in_caves\" >Formed when dissolved limestone is left behind as water drips in caves.<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-36\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Examples_Karst_region_of_Slovenia_Meghalaya_India\" >Examples: Karst region of Slovenia,&nbsp; Meghalaya (India)<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-37\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Importance_of_Earths_Geomorphic_Features\" >Importance of Earth\u2019s Geomorphic Features<\/a><ul class='ez-toc-list-level-3' ><li class='ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-38\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#1_Agricultural_Significance\" >1. Agricultural Significance<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-39\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#2_Mineral_and_Energy_Resources\" >2. Mineral and Energy Resources<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-40\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#3_Human_Settlement_and_Development\" >3. Human Settlement and Development<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-41\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#4_Natural_Hazards_and_Disaster_Management\" >4. Natural Hazards and Disaster Management<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-42\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#5_Biodiversity_and_Ecosystems\" >5. Biodiversity and Ecosystems<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-43\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Geomorphic_Features_in_the_Indian_Subcontinent\" >Geomorphic Features in the Indian Subcontinent<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-44\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Geomorphic_Cycles_and_Theories\" >Geomorphic Cycles and Theories<\/a><ul class='ez-toc-list-level-3' ><li class='ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-45\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#1_Davis_Geographical_Cycle_of_Erosion\" >1. Davis\u2019 Geographical Cycle of Erosion<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-46\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#2_Pencks_Model\" >2. Penck\u2019s Model<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-47\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#3_Kings_Model\" >3. King\u2019s Model<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-48\" href=\"https:\/\/www.borthakursiasacademy.com\/blog\/a-comprehensive-guide-to-earths-diverse-geomorphic-features\/#Conclusion\" >Conclusion<\/a><\/li><\/ul><\/nav><\/div>\n\n\n\n\n<p>In this article, we will discuss the diverse <strong>geomorphic features of the Earth<\/strong>, exploring their classifications, processes of formation, examples, and significance from both physical and human geography perspectives.&nbsp; Let\u2019s&nbsp; make the journey easier for you and understand each topics.&nbsp;<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img decoding=\"async\" src=\"https:\/\/cdn.shortpixel.ai\/stsp\/to_webp,q_lossy,ret_img\/https:\/\/lh4.googleusercontent.com\/sHJe8G3oQ5WXTTTy6mWuqtfW6E_AzF2CsrhAsQCovqT38gX5YO6Sbk-tv4Auxc8cL_95eied_pMBgHNp7Cc21cFNHfC2J99bBviuRepwO7nu0FHrotaw90dFCJeIdHGwZas5JZEnCZWEHhRIibD44zk\" alt=\"\"\/><\/figure>\n\n\n\n<p><a href=\"https:\/\/edurev.in\/t\/79671\/Chapter-Notes-Chapter-6-Major-Landforms-of-the-Ear\" target=\"_blank\" rel=\"noopener\"><strong>Source<\/strong><\/a><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Geomorphic_Processes\"><\/span><strong>Geomorphic Processes<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p><strong>Geomorphic processes<\/strong> are natural mechanisms responsible for the formation and alteration of landforms on the Earth\u2019s surface. These processes operate through physical forces and chemical reactions, constantly reshaping the landscape.<br><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Classification_of_Geomorphic_Processes\"><\/span><strong>Classification of Geomorphic Processes<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<h4 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"1_Endogenic_Processes_Internal_Forces\"><\/span><strong>1. Endogenic Processes (Internal Forces)<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n\n<p>These originate within the Earth and are driven by internal heat, tectonic activity, magma, radioactivity, and gravitational pressure. They are responsible for building up the Earth\u2019s surface features<\/p>\n\n\n\n<p><strong>Types of Endogenic Processes:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Slow Movements (Diastrophism):<\/strong><strong><br><\/strong> These involve large-scale movements of the Earth\u2019s crust over long periods.<br>\n<ul class=\"wp-block-list\">\n<li><strong><em>Epeirogenic Movements:<\/em><\/strong> It causes uplift or subsidence of landmasses (e.g., the Deccan Plateau).<br><\/li>\n\n\n\n<li><strong><em>Orogenic Movements<\/em><\/strong><em>:<\/em> Lead to the formation of mountains through folding and faulting (e.g., Himalayas, Alps).<br><\/li>\n<\/ul>\n<\/li>\n\n\n\n<li><strong>Sudden Movements:<\/strong><strong><br><\/strong> These occur abruptly and can be highly destructive.<br>\n<ul class=\"wp-block-list\">\n<li><strong><em>Earthquakes<\/em><\/strong><em>:<\/em> Caused by the release of built-up stress along faults.<br><\/li>\n\n\n\n<li><strong><em>Volcanic Eruptions:<\/em><\/strong> Occur due to the rise of magma to the surface.<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n\n\n\n<p><strong>Examples of Endogenic Processes:&nbsp;<\/strong><\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Mountain.&nbsp;<\/strong><\/li>\n\n\n\n<li><strong>Volcanic Mountains : <\/strong>These mountains form when volcanoes erupt. The lava that comes out cools down and becomes hard, slowly building up into a mountain.<strong><br><\/strong><strong> There are two main types:<\/strong><\/li>\n<\/ol>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Shield Volcanoes <\/strong>have gentle slopes because the lava that comes out flows easily. <strong>Example: <\/strong><em>Mauna Loa<\/em> in Hawaii.<\/li>\n\n\n\n<li><strong>Stratovolcanoes, or composite volcanoes, <\/strong>are steeper, and their eruptions are more violent.<strong> Examples:<\/strong> <em>Mount Fuji<\/em> in Japan and <em>Mount Vesuvius<\/em> in Italy.<\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Most_volcanic_mountains_are_found_around_the_Pacific_Ocean_in_an_area_called_the_Pacific_Ring_of_Fire\"><\/span>Most volcanic mountains are found around the Pacific Ocean in an area called the Pacific Ring of Fire.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ol start=\"2\" class=\"wp-block-list\">\n<li><strong>Fold Mountains :<\/strong> These are formed when two tectonic plates push against each other. The land between them gets squeezed and rises up in folds, forming mountains.<br><strong>Examples: <\/strong><em>Himalayas<\/em>, <em>Andes<\/em>, <em>Alps<\/em>.<\/li>\n\n\n\n<li><strong>Block Mountains : <\/strong>These mountains form when cracks in the Earth\u2019s surface (called faults) cause blocks of land to rise or fall.&nbsp;<\/li>\n<\/ol>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The higher parts are called horsts.<\/li>\n\n\n\n<li>The lower, sunken parts are called grabens.<\/li>\n\n\n\n<li>Example: <em>Sierra Nevada Range<\/em> in the USA.<\/li>\n<\/ul>\n\n\n\n<ol start=\"4\" class=\"wp-block-list\">\n<li><strong>Residual Mountains : <\/strong>These mountains are what\u2019s left after wind, rain, and other natural forces slowly wear down the surrounding land. That\u2019s why they are also called Mountains of Denudation. Examples: <em>Scottish Highlands<\/em>, <em>Scandinavian Mountains<\/em>, <em>Balkan Peninsula<\/em>.<\/li>\n\n\n\n<li><strong>Dome Mountains :&nbsp; <\/strong>These are formed when hot magma from inside the Earth pushes the crust upward but doesn\u2019t break through. The surface forms a round, dome shape. Over time, the top layers wear away, and the hard rock underneath is exposed. <strong>&nbsp;Examples: <\/strong><strong><em>Black Hills<\/em><\/strong><strong> of South Dakota (USA)&nbsp;<\/strong><\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"B_Plateaus\"><\/span><strong>B. Plateaus<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>Plateaus are large, flat, elevated areas that have been uplifted by <strong>tectonic or volcanic activity<\/strong>. They are often rich in minerals and form important physiographic units.&nbsp;<\/p>\n\n\n\n<p><strong>Types of Plateaus (Based on Location and Rock Structure)<\/strong><\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Intermontane Plateaus : <\/strong>These plateaus are located between or near mountain ranges. Sometimes, they are completely surrounded by mountains.<\/li>\n<\/ol>\n\n\n\n<p><strong>Example:<\/strong> <em>Tibetan Plateau\u2014<\/em>It is surrounded by high mountains like the Himalayas, Karakoram, Kunlun, and Tien Shan.<\/p>\n\n\n\n<ol start=\"2\" class=\"wp-block-list\">\n<li><strong>Piedmont Plateaus : <\/strong>&nbsp;These plateaus are found at the base (foot) of mountains. One side touches the mountains, and the other side opens into plains or the sea.<\/li>\n<\/ol>\n\n\n\n<p>&nbsp;<strong>Examples: <\/strong><em>Malwa Plateau<\/em> in India , <em>Appalachian Plateau<\/em> in the USA (between the Appalachian Mountains and Atlantic Coastal Plain)<\/p>\n\n\n\n<ol start=\"3\" class=\"wp-block-list\">\n<li><strong>Continental Plateaus : <\/strong>These plateaus are formed when large parts of land rise up (uplift) or when lava from volcanoes spreads over the land and hardens, covering the original surface.<\/li>\n<\/ol>\n\n\n\n<p>&nbsp;<strong>Examples: <\/strong><em>Deccan Plateau<\/em> in Maharashtra (lava-covered), <em>Snake River Plateau<\/em> in the northwestern USA<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"C_Earthquakes_and_Fault_Valleys\"><\/span><strong>C.&nbsp; Earthquakes and Fault Valleys<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>Tectonic movements cause <strong>faulting<\/strong> (cracking of Earth\u2019s crust) and <strong>earthquakes<\/strong>, leading to features like <strong>rift valleys<\/strong> and <strong>horsts<\/strong>.<\/p>\n\n\n\n<p><em>Examples<\/em>: East African Rift Valley, Narmada and Tapi Rift Valleys in India<\/p>\n\n\n\n<h4 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"2_Exogenic_Processes_External_Forces\"><\/span><strong>2. Exogenic Processes (External Forces)<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n\n<p>These operate on the Earth\u2019s surface and are driven by external forces such as solar energy and gravity. They lead to the wearing down of elevated areas and the filling of depressions.&nbsp;<\/p>\n\n\n\n<p><strong>Main Exogenic Processes:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Weathering:<\/strong><strong><br><\/strong> The breakdown of rocks in situ due to atmospheric conditions.<br>\n<ul class=\"wp-block-list\">\n<li><strong><em>Physical Weathering<\/em><\/strong><em>:<\/em> Due to temperature changes, frost, etc.<br><\/li>\n\n\n\n<li><strong><em>Chemical Weathering<\/em><\/strong><em>:<\/em> Due to chemical reactions like carbonation.<br><\/li>\n\n\n\n<li><strong><em>Biological Weathering<\/em><\/strong><em>:<\/em> Caused by the actions of plants and animals.<br><\/li>\n<\/ul>\n<\/li>\n\n\n\n<li><strong>Mass Wasting (Mass Movement):<\/strong><strong><br><\/strong> The downslope movement of rock and soil under the influence of gravity.<br>\n<ul class=\"wp-block-list\">\n<li><strong><em>Slow movements:<\/em><\/strong> Creep<br><\/li>\n\n\n\n<li><strong><em>Rapid movements<\/em><\/strong><em>:<\/em> Landslides, mudflows<br><\/li>\n<\/ul>\n<\/li>\n\n\n\n<li><strong>Erosion and Deposition:<\/strong><strong><br><\/strong>\n<ul class=\"wp-block-list\">\n<li><strong><em>Erosion:<\/em><\/strong> The removal and transportation of surface material by agents like rivers, wind, ice, and waves.<br><\/li>\n\n\n\n<li><strong><em>Deposition<\/em><\/strong><em>:<\/em> The laying down of sediments carried by erosional agents when their energy decreases.<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n\n\n\n<p>Exogenic forces include <strong>weathering, erosion, transportation, and deposition<\/strong>. These shape the Earth\u2019s surface gradually and are responsible for creating <strong>secondary landforms<\/strong> such as valleys, sand dunes, and coastal landforms.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"A_Fluvial_Landforms_Formed_by_rivers\"><\/span><strong>A. Fluvial Landforms (Formed by rivers)<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>Rivers are powerful agents of erosion, transportation, and deposition, especially in humid climates.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Erosional_Features\"><\/span><strong>Erosional Features:<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n\n<p>These are landforms made when rivers wear away the land.<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>V-shaped Valleys\u2014<\/strong>Formed in the upper course of a river, where the river cuts deep into the land, making a valley shaped like a &#8220;V.&#8221;<br><\/li>\n\n\n\n<li><strong>Gorges and Canyons<\/strong> \u2013 Very deep and narrow valleys with steep sides, formed due to the strong cutting action of rivers over a long time.<br><\/li>\n\n\n\n<li><strong>Waterfalls\u2014<\/strong>These occur when the river falls from a great height over a hard rock layer. Example: <em>Jog Falls<\/em>, <em>Niagara Falls<\/em>.<br><\/li>\n<\/ul>\n\n\n\n<p><strong>Depositional Features<\/strong><\/p>\n\n\n\n<p>These are landforms made when rivers drop (deposit) the material they carry.<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Floodplains\u2014<\/strong>Flat areas on both sides of a river formed when the river floods and deposits mud and silt.<br><\/li>\n\n\n\n<li><strong>Alluvial Fans\u2014<\/strong>A fan-shaped area formed where a river slows down and spreads out, usually at the bottom of hills.<strong><br><\/strong><\/li>\n\n\n\n<li><strong>Deltas\u2014<\/strong>Triangle-shaped land at the mouth of a river, formed from rich soil carried by the river.<br>Example: <em>Ganga-Brahmaputra Delta\u2014<\/em>the world\u2019s largest delta.<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"bAeolian_Landforms_Formed_by_Wind\"><\/span><strong>b.Aeolian Landforms (Formed by Wind)<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>These landforms are created by the action of <strong>wind<\/strong>, especially in <strong>desert<\/strong> and <strong>semi-desert<\/strong> areas where the soil is loose and dry.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Erosional_Features-2\"><\/span><strong>Erosional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>These are formed when wind wears away rocks and soil.<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Yardangs\u2014long<\/strong>, narrow ridges of hard rock left behind after wind blows away the softer rock.<br><\/li>\n\n\n\n<li><strong>Mushroom Rocks\u2014<\/strong>Rocks shaped like mushrooms, with a thin base and wider top, formed by strong winds blowing sand at the base.&nbsp;<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Depositional_Features\"><\/span><strong>Depositional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>These form when wind drops the sand and dust it carries.<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Sand Dunes\u2014<\/strong>Hills of sand formed by wind.<br>\n<ul class=\"wp-block-list\">\n<li><strong>Barchans\u2014crescent-<\/strong>shaped dunes.<br><\/li>\n\n\n\n<li><strong>Seif Dunes\u2014<\/strong>Long, narrow dunes that form in the direction of the wind.<br><\/li>\n<\/ul>\n<\/li>\n\n\n\n<li><strong>Loess Plains\u2014<\/strong>Flat plains formed by fine dust (called loess) blown by the wind and deposited over large areas.<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Examples_Thar_Desert_in_India_Sahara_Desert_in_Africa\"><\/span><strong>Examples: <\/strong><em>Thar Desert<\/em> in India, <em>Sahara Desert<\/em> in Africa<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"C_Glacial_Landforms_Formed_by_Glaciers\"><\/span><strong>C. Glacial Landforms (Formed by Glaciers)<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"In_very_cold_places_glaciers_large_moving_bodies_of_ice_shape_the_land_by_eroding_wearing_away_rocks_and_depositing_the_material_they_carry\"><\/span>In very cold places, glaciers (large moving bodies of ice) shape the land by eroding (wearing away) rocks and depositing the material they carry.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Erosional_Features-3\"><\/span><strong>Erosional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"These_landforms_are_made_when_glaciers_scrape_and_wear_down_the_land\"><\/span>These landforms are made when glaciers scrape and wear down the land.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Cirques \u2013 <\/strong>Bowl-shaped hollows found at the start of a glacier, where snow and ice gather.<br><\/li>\n\n\n\n<li><strong>U-shaped Valleys \u2013 <\/strong>Wide, flat valleys with steep sides formed as glaciers move and erode the land. Unlike V-shaped river valleys, they are shaped like the letter &#8220;U.&#8221;<br><\/li>\n\n\n\n<li><strong>Aretes \u2013<\/strong> Sharp ridges between two cirques or glacial valleys.<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Depositional_Features-2\"><\/span><strong>Depositional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"These_form_when_glaciers_melt_and_leave_behind_the_rocks_and_soil_they_carried\"><\/span>These form when glaciers melt and leave behind the rocks and soil they carried.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Moraines \u2013 <\/strong>Piles of rocks and soil left along the sides or at the end of a glacier.<br><\/li>\n\n\n\n<li><strong>Drumlins \u2013 <\/strong>Smooth, oval-shaped hills made of glacial deposits.<strong><br><\/strong><\/li>\n\n\n\n<li><strong>Eskers\u2014<\/strong>long, winding ridges of sand and gravel left by streams flowing under a glacier.<br><\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Examples_Himalayas_Alps_Antarctica\"><\/span><strong>Examples: <\/strong><em>Himalayas , Alps, Antarctica<\/em><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"D_Coastal_Landforms_Formed_by_Sea_Waves\"><\/span><strong>D. Coastal Landforms (Formed by Sea Waves)<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"The_sea_shapes_the_coastline_through_waves_tides_and_currents_These_processes_cause_erosion_and_deposition_creating_many_interesting_landforms\"><\/span>The sea shapes the coastline through waves, tides, and currents. These processes cause erosion and deposition, creating many interesting landforms.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Erosional_Features-4\"><\/span><strong>Erosional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Formed_when_strong_sea_waves_wear_away_the_rocks_along_the_coast\"><\/span>Formed when strong sea waves wear away the rocks along the coast.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Cliffs \u2013<\/strong> Steep rock faces along the coastline formed by wave erosion.<strong><br><\/strong><\/li>\n\n\n\n<li><strong>Sea Arches \u2013 <\/strong>Arch-shaped rocks formed when waves cut through a cliff.<br><\/li>\n\n\n\n<li><strong>Stacks\u2014<\/strong>Tall pillars of rock left behind in the sea after a sea arch collapses.<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Depositional_Features-3\"><\/span><strong>Depositional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Formed_when_the_sea_deposits_sand_silt_and_other_materials\"><\/span>Formed when the sea deposits sand, silt, and other materials.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Beaches \u2013 <\/strong>Sandy or pebbly areas along the shore formed by wave deposition.<br><\/li>\n\n\n\n<li><strong>Spits and Bars \u2013 <\/strong>Narrow strips of sand stretching into the sea, formed by waves and currents.<br><\/li>\n\n\n\n<li><strong>Lagoons \u2013 <\/strong>Shallow lakes or water bodies separated from the sea by a sandbar or spit.<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Examples_Kerala_Backwaters_Chilika_Lake_Odisha\"><\/span><strong>Examples: <\/strong><em>Kerala Backwaters, Chilika Lake<\/em> (Odisha)<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"E_Karst_Landforms_Chemical_Weathering_of_Limestone\"><\/span><strong>E. Karst Landforms (Chemical Weathering of Limestone)<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Karst_landforms_are_made_in_areas_where_the_ground_is_made_of_limestone_or_dolomite_When_rainwater_mixes_with_carbon_dioxide_it_forms_a_weak_acid_that_dissolves_the_rock_This_is_called_chemical_weathering_especially_solution_and_carbonation\"><\/span>Karst landforms are made in areas where the ground is made of limestone or dolomite. When rainwater mixes with carbon dioxide, it forms a weak acid that dissolves the rock. This is called chemical weathering (especially <em>solution<\/em> and <em>carbonation<\/em>).<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Erosional_Features-5\"><\/span><strong>Erosional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Formed_when_acidic_water_dissolves_the_limestone\"><\/span>Formed when acidic water dissolves the limestone.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Sinkholes (Dolines)\u2014<\/strong>Round or deep holes formed when the land suddenly collapses as the limestone below dissolves.<br><\/li>\n\n\n\n<li><strong>Lapis \u2013 <\/strong>Grooved and uneven rock surfaces caused by water flowing over limestone.<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Depositional_Features-4\"><\/span><strong>Depositional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Depositional_Features-5\"><\/span><strong>Depositional Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Formed_when_dissolved_limestone_is_left_behind_as_water_drips_in_caves\"><\/span>Formed when dissolved limestone is left behind as water drips in caves.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Stalactites \u2013 <\/strong>Icicle-shaped formations that hang from the roof of caves.<br><\/li>\n\n\n\n<li><strong>Stalagmites \u2013 <\/strong>Cone-shaped formations that grow up from the floor of caves.<strong><br><\/strong><\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Examples_Karst_region_of_Slovenia_Meghalaya_India\"><\/span><strong>Examples: <\/strong><em>Karst region of Slovenia,&nbsp; Meghalaya<\/em> (India)<br><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Importance_of_Earths_Geomorphic_Features\"><\/span><strong>Importance of Earth\u2019s Geomorphic Features<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"1_Agricultural_Significance\"><\/span><strong>1. Agricultural Significance<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Floodplains and deltas<\/strong> are highly fertile due to alluvial deposits.<br><\/li>\n\n\n\n<li>River valleys support intensive agriculture in regions like the Indo-Gangetic plains.<br><\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"2_Mineral_and_Energy_Resources\"><\/span><strong>2. Mineral and Energy Resources<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Plateaus<\/strong> and <strong>mountains<\/strong> contain valuable minerals, coal, and fossil fuels.<br><\/li>\n\n\n\n<li>Volcanic regions often contain rich mineral deposits.<br><\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"3_Human_Settlement_and_Development\"><\/span><strong>3. Human Settlement and Development<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Plains and river valleys<\/strong> are favorable for the development of settlements.<br><\/li>\n\n\n\n<li>Coastal regions facilitate <strong>trade and tourism<\/strong>.<br><\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"4_Natural_Hazards_and_Disaster_Management\"><\/span><strong>4. Natural Hazards and Disaster Management<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Understanding tectonic features helps in assessing earthquake-prone zones.<br><\/li>\n\n\n\n<li>Knowledge of geomorphology is essential for <strong>land-use planning<\/strong> and <strong>disaster risk reduction<\/strong>.<br><\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"5_Biodiversity_and_Ecosystems\"><\/span><strong>5. Biodiversity and Ecosystems<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Diverse landforms provide habitats for various flora and fauna.<br><\/li>\n\n\n\n<li>Glacial, coastal, and mountainous ecosystems are biodiversity hotspots.<br><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Geomorphic_Features_in_the_Indian_Subcontinent\"><\/span><strong>Geomorphic Features in the Indian Subcontinent<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>India displays a remarkable diversity of landforms due to its complex geological history:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Northern Mountains<\/strong>: Himalayas (young fold mountains), Karakoram, Zanskar<br><\/li>\n\n\n\n<li><strong>Peninsular Plateau<\/strong>: Deccan Plateau, Chotanagpur Plateau<br><\/li>\n\n\n\n<li><strong>Indo-Gangetic Plains<\/strong>: Formed by alluvium from Himalayan rivers<br><\/li>\n\n\n\n<li><strong>Coastal Plains and Islands<\/strong>: Eastern and Western coasts, Andaman-Nicobar, Lakshadweep<br><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Geomorphic_Cycles_and_Theories\"><\/span><strong>Geomorphic Cycles and Theories<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>Several theories explain the evolution of landforms:<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"1_Davis_Geographical_Cycle_of_Erosion\"><\/span><strong>1. Davis\u2019 Geographical Cycle of Erosion<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Youth \u2192 Maturity \u2192 Old Age<br><\/li>\n\n\n\n<li>Emphasizes sequential landform development over time<br><\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"2_Pencks_Model\"><\/span><strong>2. Penck\u2019s Model<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Highlights the role of <strong>tectonic uplift and erosion<\/strong> simultaneously<br><\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"3_Kings_Model\"><\/span><strong>3. King\u2019s Model<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Introduced the concept of <strong>pediplanation<\/strong> in arid regions<br><\/li>\n<\/ul>\n\n\n\n<p>These theories are important for the UPSC Geography optional and Mains GS Paper 1.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Conclusion\"><\/span><strong>Conclusion<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>The Earth&#8217;s diverse geomorphic features not only tell the story of its geological past but also play a vital role in shaping the present and future of human civilization. From the majestic Himalayas to the fertile Ganga plains and the rugged coastal cliffs, each landform holds ecological, economic, and cultural significance. For UPSC aspirants, a thorough understanding of these features is essential for a holistic grasp of physical geography and environmental management.<\/p>\n\n\n\n<p><strong>UPSC Prelims PYQ<\/strong><\/p>\n\n\n\n<p>When you travel in the Himalayas, you will see the following: [2012]<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><\/li>\n<\/ol>\n\n\n\n<p>1. Deep gorges<\/p>\n\n\n\n<p>2. U-turn river courses<\/p>\n\n\n\n<p>3. Parallel mountain ranges<\/p>\n\n\n\n<p>4. Steep gradients causing landslides<\/p>\n\n\n\n<p>Which of the above can be said to be evidence that the Himalayas are young fold mountains?<\/p>\n\n\n\n<p>a) 1 &amp; 2 Only&nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; b) 1, 2 &amp; 4 Only<\/p>\n\n\n\n<p>c) 3 &amp; 4 Only &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; d) 1,2, 3 &amp; 4<\/p>\n\n\n\n<p>Answer :&nbsp; D<\/p>\n\n\n\n<p><strong>Also Read:-<a href=\"https:\/\/www.borthakursiasacademy.com\/blog\/the-dynamic-geomorphology-of-volcanoes-and-earthquakes\/\" target=\"_blank\" rel=\"noreferrer noopener\"> https:\/\/www.borthakursiasacademy.com\/blog\/the-dynamic-geomorphology-of-volcanoes-and-earthquakes\/<\/a><\/strong><\/p>\n\n\n\n<div class=\"wp-block-coblocks-faq\" itemscope itemtype=\"https:\/\/schema.org\/FAQPage\">\n<h3 class=\"wp-block-heading wp-block-coblocks-faq__title\"><\/h3>\n\n\n\n<details class=\"wp-block-coblocks-faq-item\" itemprop=\"mainEntity\" itemscope itemtype=\"https:\/\/schema.org\/Question\"><summary class=\"wp-block-coblocks-faq-item__question\" itemprop=\"name\"><div class=\"wp-block-coblocks-faq-item__question__content\">W<strong>hat are the four main types of geomorphic processes?<\/strong><\/div><svg fill=\"none\" viewBox=\"0 0 24 24\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"24\" height=\"24\" class=\"wp-block-coblocks-faq-item__question__icon\" aria-hidden=\"true\"><path fill=\"currentColor\" fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M19.39 14.99l-1.41 1.41L12 10.43 6.02 16.4l-1.41-1.41L12 7.6l7.39 7.39z\"><\/path><\/svg><\/summary><div class=\"wp-block-coblocks-faq-item__answer\" itemprop=\"acceptedAnswer\" itemscope itemtype=\"https:\/\/schema.org\/Answer\"><div itemprop=\"text\">\n<p>Weathering, erosion, transportation, and deposition.<br><\/p>\n<\/div><\/div><\/details>\n\n\n\n<details class=\"wp-block-coblocks-faq-item\" itemprop=\"mainEntity\" itemscope itemtype=\"https:\/\/schema.org\/Question\"><summary class=\"wp-block-coblocks-faq-item__question\" itemprop=\"name\"><div class=\"wp-block-coblocks-faq-item__question__content\"><strong>What is the difference between endogenic and exogenic processes?<\/strong><\/div><svg fill=\"none\" viewBox=\"0 0 24 24\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"24\" height=\"24\" class=\"wp-block-coblocks-faq-item__question__icon\" aria-hidden=\"true\"><path fill=\"currentColor\" fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M19.39 14.99l-1.41 1.41L12 10.43 6.02 16.4l-1.41-1.41L12 7.6l7.39 7.39z\"><\/path><\/svg><\/summary><div class=\"wp-block-coblocks-faq-item__answer\" itemprop=\"acceptedAnswer\" itemscope itemtype=\"https:\/\/schema.org\/Answer\"><div itemprop=\"text\">\n<p>Endogenic processes originate within the Earth (e.g., volcanism, tectonics), while exogenic processes originate on or above the surface (e.g., river action, wind, glaciers).<br><\/p>\n<\/div><\/div><\/details>\n\n\n\n<details class=\"wp-block-coblocks-faq-item\" itemprop=\"mainEntity\" itemscope itemtype=\"https:\/\/schema.org\/Question\"><summary class=\"wp-block-coblocks-faq-item__question\" itemprop=\"name\"><div class=\"wp-block-coblocks-faq-item__question__content\"><strong>Which geomorphic feature is most suitable for agriculture?<\/strong><\/div><svg fill=\"none\" viewBox=\"0 0 24 24\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"24\" height=\"24\" class=\"wp-block-coblocks-faq-item__question__icon\" aria-hidden=\"true\"><path fill=\"currentColor\" fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M19.39 14.99l-1.41 1.41L12 10.43 6.02 16.4l-1.41-1.41L12 7.6l7.39 7.39z\"><\/path><\/svg><\/summary><div class=\"wp-block-coblocks-faq-item__answer\" itemprop=\"acceptedAnswer\" itemscope itemtype=\"https:\/\/schema.org\/Answer\"><div itemprop=\"text\">\n<p>River valleys and floodplains are due to fertile alluvial soil.<br><\/p>\n<\/div><\/div><\/details>\n\n\n\n<details class=\"wp-block-coblocks-faq-item\" itemprop=\"mainEntity\" itemscope itemtype=\"https:\/\/schema.org\/Question\"><summary class=\"wp-block-coblocks-faq-item__question\" itemprop=\"name\"><div class=\"wp-block-coblocks-faq-item__question__content\"><strong>&nbsp;Name a depositional landform formed by wind.<\/strong><\/div><svg fill=\"none\" viewBox=\"0 0 24 24\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"24\" height=\"24\" class=\"wp-block-coblocks-faq-item__question__icon\" aria-hidden=\"true\"><path fill=\"currentColor\" fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M19.39 14.99l-1.41 1.41L12 10.43 6.02 16.4l-1.41-1.41L12 7.6l7.39 7.39z\"><\/path><\/svg><\/summary><div class=\"wp-block-coblocks-faq-item__answer\" itemprop=\"acceptedAnswer\" itemscope itemtype=\"https:\/\/schema.org\/Answer\"><div itemprop=\"text\">\n<p>Sand dunes<\/p>\n<\/div><\/div><\/details>\n\n\n<\/div>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Guide to Earth&#8217;s Diverse Geomorphic Features, Landforms are the remarkable physical features that shape the Earth&#8217;s surface, ranging from towering mountains to sprawling plains and winding rivers. In this article, we embark on an exciting journey through the fascinating world of landforms. We will delve into the various types of landforms found across the globe, exploring their formation processes, characteristics, and significance. Join us as we unravel the secrets behind these captivating features and gain a deeper understanding of the dynamic forces that have shaped our planet&#8217;s diverse landscapes.<\/p>\n","protected":false},"author":4,"featured_media":15904,"comment_status":"open","ping_status":"open","sticky":true,"template":"","format":"standard","meta":{"_coblocks_attr":"","_coblocks_dimensions":"","_coblocks_responsive_height":"","_coblocks_accordion_ie_support":"","_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"footnotes":""},"categories":[],"tags":[],"class_list":["post-2881","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/posts\/2881","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/comments?post=2881"}],"version-history":[{"count":3,"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/posts\/2881\/revisions"}],"predecessor-version":[{"id":15905,"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/posts\/2881\/revisions\/15905"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/media\/15904"}],"wp:attachment":[{"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/media?parent=2881"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/categories?post=2881"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.borthakursiasacademy.com\/blog\/wp-json\/wp\/v2\/tags?post=2881"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}