{"id":213054,"date":"2025-02-28T18:06:07","date_gmt":"2025-02-28T12:36:07","guid":{"rendered":"https:\/\/www.oliveboard.in\/blog\/?p=213054"},"modified":"2025-02-28T18:06:08","modified_gmt":"2025-02-28T12:36:08","slug":"geomorphic-cycle","status":"publish","type":"post","link":"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/","title":{"rendered":"Geomorphic Cycle &#8211; UGC NET Geography Notes"},"content":{"rendered":"<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 content<\/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 eztoc-toggle-hide-by-default' ><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-1\" href=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/#What_is_the_Geomorphic_Cycle\" >What is the Geomorphic Cycle?<\/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.oliveboard.in\/blog\/geomorphic-cycle\/#Stages_of_the_Geomorphic_Cycle_Cycle_of_Erosion\" >Stages of the Geomorphic Cycle (Cycle of Erosion)<\/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.oliveboard.in\/blog\/geomorphic-cycle\/#Theories_of_Geomorphic_Cycle\" >Theories of Geomorphic Cycle<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-4\" href=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/#Factors_Influencing_the_Geomorphic_Cycle\" >Factors Influencing the Geomorphic Cycle<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-5\" href=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/#Criticism_and_Limitations_of_the_Geomorphic_Cycle\" >Criticism and Limitations of the Geomorphic Cycle<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-6\" href=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/#Importance_of_the_Geomorphic_Cycle_in_UGC_NET_Geography\" >Importance of the Geomorphic Cycle in UGC NET Geography<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-7\" href=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/#Geomorphic_Cycle_Conclusion\" >Geomorphic Cycle Conclusion<\/a><\/li><\/ul><\/nav><\/div>\n\n<p><strong>Geomorphic Cycle: <\/strong>The <strong>geomorphic cycle,<\/strong> also known as the<strong> cycle of erosion<\/strong>, is a fundamental concept in <strong>geomorphology<\/strong> that explains the progressive transformation of landforms due to<strong> exogenic<\/strong> and <strong>endogenic forces<\/strong>. Proposed by <strong>William Morris Davis, <\/strong>this model classifies landscape evolution into three stages: <strong>youth, maturity, <\/strong>and <strong>old age<\/strong>, driven by <strong>fluvial, glacial, aeolian, and marine processes. The concept helps in understanding how denudation, erosion, and deposition shape the <\/strong>Earth&#8217;s surface over geological time.<\/p>\n\n\n\n<p>For<strong> UGC NET Geography <\/strong>aspirants, mastering the geomorphic cycle is essential, as it forms a key part of physical geography. While <strong>Davis&#8217; model <\/strong>remains influential, alternative theories such as <strong>Walther Penck\u2019s slope evolution model <\/strong>and<strong> Julius B\u00fcdel\u2019s polycyclic landscape theory <\/strong>offer different perspectives on landscape development. This article covers the stages, factors, and criticisms of the<strong> geomorphic cycle,<\/strong> providing a comprehensive resource for UGC NET exam preparation.<\/p>\n\n\n\n<div class=\"wp-block-buttons is-content-justification-center is-layout-flex wp-container-core-buttons-is-layout-16018d1d wp-block-buttons-is-layout-flex\">\n<div class=\"wp-block-button\"><a class=\"wp-block-button__link\" href=\"https:\/\/www.oliveboard.in\/ugc-net-mock-test\/?ref=contstuti-ugc-net\" target=\"_blank\" rel=\"noreferrer noopener\">Attempt UGC NET Mock Test 2025<\/a><\/div>\n<\/div>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"What_is_the_Geomorphic_Cycle\"><\/span>What is the Geomorphic Cycle?<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<ul class=\"wp-block-list\"><li>The geomorphic cycle, or cycle of erosion, is a concept by <strong>William Morris Davis <\/strong>that explains the systematic <strong>evolution of landforms<\/strong> through <strong>youth, maturity, <\/strong>and<strong> old age <\/strong>under the influence of erosional and depositional forces. <\/li><li>It highlights how<strong> landscapes<\/strong> undergo continuous<strong> transformation <\/strong>due to <strong>internal (endogenic)<\/strong> and<strong> external (exogenic) <\/strong>processes over geological time.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\"><a href=\"https:\/\/www.oliveboard.in\/blog\/exogenic-and-endogenic-forces\/\" target=\"_blank\" rel=\"noreferrer noopener\">Exogenic vs. Endogenic Processes<\/a><\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li><strong>Exogenic Processes: <\/strong>External forces like erosion, weathering, and deposition, driven by rivers, glaciers, wind, and waves, gradually reshape the land.<\/li><li><strong>Endogenic Processes: <\/strong>Internal forces such as tectonic uplift, volcanic activity, and folding, create landforms that later undergo modification by exogenic agents.<\/li><li><strong>Major Geomorphic Agents<\/strong><ul><li>Rivers erode valleys and form floodplains.<\/li><li>Glaciers carve U-shaped valleys and deposit moraines.<\/li><li>Wind sculpts deserts through deflation and dune formation.<\/li><li>Waves shape coastal features like cliffs and beaches.<\/li><\/ul><\/li><\/ul>\n\n\n\n<p>This cycle plays a key role in<strong> <a href=\"https:\/\/www.oliveboard.in\/blog\/ugc-net-geography-syllabus\/\" target=\"_blank\" rel=\"noreferrer noopener\">UGC NET Geography<\/a><\/strong>, providing insights into landform development and the interaction of geomorphic forces.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Stages_of_the_Geomorphic_Cycle_Cycle_of_Erosion\"><\/span>Stages of the Geomorphic Cycle (Cycle of Erosion)<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>The geomorphic cycle, proposed by William Morris Davis, describes how landforms evolve through three sequential stages under the influence of erosional processes.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\">1. Youth Stage<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Characterized by high relief, steep slopes, and deep valleys.<\/li><li>Rivers actively erode, creating V-shaped valleys, waterfalls, and rapids.<\/li><li>Land is rugged with minimal deposition.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">2. Mature Stage<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Erosion reduces slope steepness, forming wider valleys and floodplains.<\/li><li>Rivers develop meanders, and landscape stability increases.<\/li><li>Landforms begin approaching dynamic equilibrium between erosion and deposition.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">3. Old Age<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Low relief with gentle slopes and extensive floodplains.<\/li><li>Slow erosion leads to the formation of a peneplain (almost levelled landform).<\/li><li>Features like oxbow lakes, deltas, and meandering rivers dominate.<\/li><\/ul>\n\n\n\n<p><strong>Also Check: <a href=\"https:\/\/www.oliveboard.in\/blog\/denudation-and-weathering\/\" target=\"_blank\" rel=\"noreferrer noopener\">Denudation and Weathering<\/a><\/strong><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Theories_of_Geomorphic_Cycle\"><\/span>Theories of Geomorphic Cycle<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>Several theories explain landscape evolution, with notable contributions from William Morris Davis, Walther Penck, and Julius B\u00fcdel. These models differ in their emphasis on erosion, tectonics, and climatic influences.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">William Morris Davis\u2019 Geomorphic Cycle<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Proposed the<strong> Cycle of Erosion<\/strong>, explaining landform evolution through youth, maturity, and old age.<\/li><li>Highlights the role of<strong> tectonic uplift<\/strong>, followed by gradual erosion shaping the landscape.<\/li><li>Assumes a sequential and time-dependent evolution under uniform climatic conditions.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">Walther Penck\u2019s Slope Evolution Model (secondary keyword)<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Criticized <strong>Davis\u2019 model<\/strong> for being too rigid and ignoring continuous uplift.<\/li><li>Emphasized <strong>endogenic forces (tectonics) <\/strong>as a dominant factor in landform development.<\/li><li>Proposed that landforms evolve through <strong>waxing, steady-state, and waning slopes,<\/strong> focusing on simultaneous uplift and erosion.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">Julius B\u00fcdel\u2019s Polycyclic Landscape Theory (secondary keyword)<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Argued that landforms undergo multiple <strong>erosion cycles <\/strong>rather than a single sequential cycle.<\/li><li>Stressed climatic variations as a key factor in landscape evolution.<\/li><li>Explained that <strong>polycyclic landforms <\/strong>result from repeated cycles of uplift and erosion under changing environmental conditions.<\/li><\/ul>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Factors_Influencing_the_Geomorphic_Cycle\"><\/span>Factors Influencing the Geomorphic Cycle<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>The evolution of landforms in the <strong>geomorphic cycle<\/strong> is influenced by several key factors, including <strong>climate, rock structure, and tectonic activity<\/strong>. These factors determine the rate and nature of erosion, deposition, and landform development over time.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\">1. Climatic Conditions<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Temperature fluctuations affect weathering (e.g., frost action in cold regions).<\/li><li>Precipitation controls the intensity of fluvial erosion and sediment transport.<\/li><li>Wind plays a major role in aeolian processes, shaping deserts and coastal landscapes.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">2. Lithology and Rock Structure<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li><strong>Harder rocks <\/strong>like <strong>granite resist erosion, forming highlands, <\/strong>while <strong>softer rocks<\/strong> like <strong>limestone erode faster, creating valleys <\/strong>and<strong> karst landscapes<\/strong>.<\/li><li><strong>Rock fractures, joints, <\/strong>and<strong> bedding planes <\/strong>influence the formation of ridges, cliffs, and plateaus.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">3. Tectonic Activity and Base Level Changes<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li><strong>Tectonic uplift<\/strong> rejuvenates<strong> landscapes, increasing erosion rates <\/strong>and <strong>creating youthful landforms.<\/strong><\/li><li>Subsidence leads to sediment deposition and the formation of coastal plains.<\/li><li>Changes in <strong>base level (sea level rise or fall) <\/strong>influence river incision, terrace formation, and delta development.<\/li><\/ul>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Criticism_and_Limitations_of_the_Geomorphic_Cycle\"><\/span>Criticism and Limitations of the Geomorphic Cycle<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>While <strong>Davis\u2019 Geomorphic Cycle<\/strong> was a pioneering theory in landform evolution, it has faced several criticisms from <strong>modern geomorphologists<\/strong> due to its static approach and oversimplifications.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\">1. Static Nature of Davis\u2019 Model<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Assumes a linear, sequential evolution of landscapes, ignoring ongoing <strong>tectonic activity.<\/strong><\/li><li>Does not account for continuous uplift or erosion occurring simultaneously, as suggested by <strong>Penck\u2019s model.<\/strong><\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">2. Lack of Consideration for Climate Variability<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Treats climate as a <strong>constant factor<\/strong>, failing to incorporate climatic changes over geological time.<\/li><li><strong>B\u00fcdel\u2019s polycyclic theory<\/strong> highlighted how landforms undergo multiple cycles due to climate shifts.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">3. Alternative Perspectives in Modern Geomorphology<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Dynamic equilibrium concept suggests that landforms evolve in response to balancing forces of uplift and erosion rather than fixed stages.<\/li><li>Tectonic geomorphology and process-based models focus on real-time landscape changes rather than long-term hypothetical cycles.<\/li><\/ul>\n\n\n\n<p>Despite its limitations, the <strong>geomorphic cycle<\/strong> remains a foundational concept in <strong>UGC NET Geography, <\/strong>helping understand the basics of landform evolution.<\/p>\n\n\n\n<p><strong>Also Learn: <a href=\"https:\/\/www.oliveboard.in\/blog\/concept-of-continental-drift-theory\/\" target=\"_blank\" rel=\"noreferrer noopener\">Concept of Continental Drift Theory<\/a><\/strong><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Importance_of_the_Geomorphic_Cycle_in_UGC_NET_Geography\"><\/span>Importance of the Geomorphic Cycle in UGC NET Geography<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>The<strong> geomorphic cycle <\/strong>is a crucial topic in <strong>UGC NET Geography<\/strong>, as it forms the foundation for understanding <strong>landform evolution, erosion, <\/strong>and <strong>geomorphic processes<\/strong>. Questions related to this topic often appear in both conceptual and applied formats in the exam.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\">Expected UGC NET Exam Questions<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li><strong>Conceptual Questions: <\/strong>Definitions, stages of the geomorphic cycle (youth, maturity, old age), and theories by Davis, Penck, and B\u00fcdel.<\/li><li><strong>Applied Questions:<\/strong> Role of climate, tectonics, and rock structure in landform development.<\/li><li><strong>Comparative Questions: <\/strong>Differences between Davis\u2019 model and alternative theories like Penck\u2019s slope evolution model.<\/li><\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">How to Approach MCQs Related to Geomorphic Processes?<\/h4>\n\n\n\n<ul class=\"wp-block-list\"><li>Focus on <strong>key terminologies<\/strong> like <strong>peneplain, equilibrium, uplift, exogenic, and endogenic processes.<\/strong><\/li><li>Understand <strong>cause-effect relationships, <\/strong>such as how tectonic uplift influences erosion rates.<\/li><li>Analyze<strong> diagram-based questions,<\/strong> which often test knowledge of landform evolution stages.<\/li><li>Practice previous year <strong><a href=\"https:\/\/www.oliveboard.in\/blog\/ugc-net-geography-previous-year-papers\/\" target=\"_blank\" rel=\"noreferrer noopener\">UGC NET Geography papers<\/a><\/strong> to identify frequently asked patterns.<\/li><\/ul>\n\n\n\n<p><strong>Also Check: <a href=\"https:\/\/www.oliveboard.in\/blog\/ugc-net-geography-previous-year-papers\/\" target=\"_blank\" rel=\"noreferrer noopener\">UGC NET Geography Previous Year Questions Papers<\/a><\/strong><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Geomorphic_Cycle_Conclusion\"><\/span>Geomorphic Cycle Conclusion<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>The geomorphic cycle remains a foundational concept in <strong>geomorphology, <\/strong>explaining the <strong>evolution of landforms<\/strong> through <strong>erosion, deposition, and tectonic processes<\/strong>. While <strong>Davis\u2019 model<\/strong> provides a structured framework, modern theories by<strong> Penck<\/strong> and <strong>B\u00fcdel<\/strong> offer alternative perspectives, incorporating tectonic activity and climatic variations.<\/p>\n\n\n\n<p>For <strong>UGC NET Geography<\/strong>, understanding the stages, factors, and criticisms of the <strong>geomorphic cycle<\/strong> is essential. Exam questions often test <strong>conceptual clarity, theoretical comparisons, and application-based scenarios<\/strong>. A strong grasp of geomorphic processes enhances performance in physical geography sections, ensuring better accuracy in tackling MCQs and analytical questions.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Geomorphic Cycle: The geomorphic cycle, also known as the cycle of erosion, is a fundamental concept in geomorphology that explains<\/p>\n","protected":false},"author":50,"featured_media":213084,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[10236,11846,17417],"tags":[17463],"class_list":["post-213054","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-teaching-exams","category-ugc-net-teaching-exams","category-ugc-net-geography-study-material","tag-geomorphic-cycle","generate-columns","tablet-grid-50","mobile-grid-100","grid-parent","grid-50"],"yoast_head":"<!-- This site is optimized with the Yoast SEO Premium plugin v26.6 (Yoast SEO v26.6) - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Geomorphic Cycle - UGC NET Geography Notes<\/title>\n<meta name=\"description\" content=\"Geomorphic Cycle for UGC NET Geography explains landform evolution through erosion, deposition, and tectonics.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Geomorphic Cycle - UGC NET Geography Notes\" \/>\n<meta property=\"og:description\" content=\"Geomorphic Cycle: The geomorphic cycle, also known as the cycle of erosion, is a fundamental concept in geomorphology that explains the progressive\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/\" \/>\n<meta property=\"og:site_name\" content=\"Oliveboard\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/Oliveboard\" \/>\n<meta property=\"article:published_time\" content=\"2025-02-28T12:36:07+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2025-02-28T12:36:08+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.oliveboard.in\/blog\/wp-content\/uploads\/2025\/02\/Geomorphic-Cycle.png\" \/>\n\t<meta property=\"og:image:width\" content=\"730\" \/>\n\t<meta property=\"og:image:height\" content=\"480\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/png\" \/>\n<meta name=\"author\" content=\"Saloni Singhal\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:creator\" content=\"@Oliveboard\" \/>\n<meta name=\"twitter:site\" content=\"@Oliveboard\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"Saloni Singhal\" \/>\n\t<meta name=\"twitter:label2\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"6 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"NewsArticle\",\"@id\":\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/#article\",\"isPartOf\":{\"@id\":\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/\"},\"author\":{\"name\":\"Saloni Singhal\",\"@id\":\"https:\/\/www.oliveboard.in\/blog\/#\/schema\/person\/6aedd7baaab0f33dc2f40834a257f88c\"},\"headline\":\"Geomorphic Cycle &#8211; 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