


{"id":101555,"date":"2026-05-02T17:34:38","date_gmt":"2026-05-02T12:04:38","guid":{"rendered":"https:\/\/vajiramandravi.com\/current-affairs\/?p=101555"},"modified":"2026-05-02T17:34:38","modified_gmt":"2026-05-02T12:04:38","slug":"deccan-trap","status":"publish","type":"post","link":"https:\/\/vajiramandravi.com\/current-affairs\/deccan-trap\/","title":{"rendered":"Deccan Trap, Distribution, Formation, Characteristics, Black Soil"},"content":{"rendered":"<p><span style=\"font-weight: 400;\">The <\/span><b>Deccan Traps<\/b><span style=\"font-weight: 400;\"> form one of the most extensive volcanic landscapes in the world, dominating the <\/span><b>west-central Indian Peninsula<\/b><span style=\"font-weight: 400;\">. These are classic examples of <\/span><b>flood basalt formations<\/b><span style=\"font-weight: 400;\">, where highly fluid lava spread over vast areas, creating a layered, step-like terrain.\u00a0<\/span><\/p>\n<h2><b>What are Deccan Traps?<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The <\/span><b>Deccan Traps<\/b><span style=\"font-weight: 400;\"> are a massive accumulation of <\/span><b>basaltic lava flows<\/b><span style=\"font-weight: 400;\"> formed during intense volcanic activity in the <\/span><b>Late Cretaceous period (~66 million years ago)<\/b><span style=\"font-weight: 400;\">. These lava flows now cover about <\/span><b>500,000 sq. km<\/b><span style=\"font-weight: 400;\"> of India.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">The term <\/span><b>\u201cTrap\u201d<\/b><span style=\"font-weight: 400;\"> comes from the Swedish word <\/span><i><span style=\"font-weight: 400;\">Trappa<\/span><\/i><span style=\"font-weight: 400;\">, meaning <\/span><b>stairs<\/b><span style=\"font-weight: 400;\">, referring to the <\/span><b>terraced topography<\/b><span style=\"font-weight: 400;\"> formed due to successive lava layers.<\/span><\/p>\n<h2><b>How are Deccan Traps Formed?<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The Deccan Traps were formed due to massive fissure volcanic eruptions during the Late <\/span><b>Cretaceous period <\/b><span style=\"font-weight: 400;\">(<\/span><b>~66 million years ago<\/b><span style=\"font-weight: 400;\">), when large volumes of highly fluid basaltic lava flowed out onto the Earth\u2019s surface and spread over vast areas of peninsular India.<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The formation began when the <\/span><b>Indian Plate <\/b><span style=\"font-weight: 400;\">passed over the <\/span><b>Reunion hotspot<\/b><span style=\"font-weight: 400;\">, causing intense volcanic activity.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Instead of erupting from a single volcanic cone, lava emerged through <\/span><b>long linear cracks (fissures)<\/b><span style=\"font-weight: 400;\"> in the Earth\u2019s crust.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">These eruptions were <\/span><b>non-explosive (quiet eruptions)<\/b><span style=\"font-weight: 400;\">, allowing lava to flow smoothly over long distances.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The lava was <\/span><b>highly fluid (low viscosity)<\/b><span style=\"font-weight: 400;\">, which enabled it to spread across hundreds of kilometers, forming a vast <\/span><b>lava plateau<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Multiple eruptions occurred over time, creating <\/span><b>layer upon layer of basalt flows<\/b><span style=\"font-weight: 400;\">, leading to great thickness (up to 3000+ meters).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The eruptions took place in a <\/span><b>sub-aerial environment<\/b><span style=\"font-weight: 400;\">, meaning lava spread over land rather than underwater.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Vertical intrusions called <\/span><b>dykes<\/b><span style=\"font-weight: 400;\"> acted as feeder channels through which magma reached the surface.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The volcanic activity was <\/span><b>not continuous<\/b><span style=\"font-weight: 400;\">, there were intervals of inactivity during which:<\/span>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Rivers and lakes developed<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Sediments were deposited<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Plant and animal life existed<\/span><\/li>\n<\/ul>\n<\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">These breaks resulted in the formation of <\/span><b>inter-trappean beds<\/b><span style=\"font-weight: 400;\">, which contain fossil evidence.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Over millions of years, <\/span><b>cooling, <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/weathering\/\" target=\"_blank\">weathering<\/a>, and <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/soil-erosion\/\" target=\"_blank\">erosion<\/a><\/b><span style=\"font-weight: 400;\"> shaped the lava flows into a <\/span><b>step-like (trap) topography<\/b><span style=\"font-weight: 400;\"> seen today.<\/span><\/li>\n<\/ul>\n<h2><b>Deccan Trap Distribution<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The Deccan Trap spread reflects the vast outpouring of basaltic lava that once covered a much larger area, later reduced due to erosion.<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The largest coverage of Deccan Traps is found in <\/span><b>Maharashtra<\/b><span style=\"font-weight: 400;\">, forming the core of the Deccan Plateau.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Significant extensions occur in <\/span><b>Madhya Pradesh, Gujarat (Kutch and Kathiawar), Karnataka, Telangana, and Andhra Pradesh<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">In <\/span><b>Gujarat<\/b><span style=\"font-weight: 400;\">, the traps are well-developed in the <\/span><b>Saurashtra peninsula and Kutch region<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The lava flows extend eastward into the <\/span><b><a href=\"https:\/\/vajiramandravi.com\/upsc-exam\/godavari-river-system\/\" target=\"_blank\">Godavari<\/a> and Krishna river valleys<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Thickness varies from <\/span><b>over 3,000 m in the Western Ghats<\/b><span style=\"font-weight: 400;\"> to thinner layers toward the eastern margins.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Deccan Traps originally covered a much larger area, possibly extending into <\/span><b>parts of central India and beyond<\/b><span style=\"font-weight: 400;\">, but have been reduced due to <\/span><b>erosion and <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/denudation\/\" target=\"_blank\">denudation<\/a><\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Isolated remnants of basalt flows are also found in <\/span><b>Jharkhand, Bihar, and northern Andhra<\/b><span style=\"font-weight: 400;\">, indicating their former wider spread.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The traps form a <\/span><b>step-like topography<\/b><span style=\"font-weight: 400;\">, especially visible in the <\/span><b><a href=\"https:\/\/vajiramandravi.com\/current-affairs\/western-ghats\/\" target=\"_blank\">Western Ghats<\/a> region<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">After the <\/span><b>Archaean rock system<\/b><span style=\"font-weight: 400;\">, the Deccan Traps are the <\/span><b>second most widespread geological formation in India<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<\/ul>\n<h2><b>Deccan Trap Characteristics<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The <\/span><b>Deccan Traps<\/b><span style=\"font-weight: 400;\"> exhibit distinctive geological, structural, and soil-related features that reflect their origin from extensive <\/span><b>flood basalt eruptions<\/b><span style=\"font-weight: 400;\">.<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Deccan Traps consist of <\/span><b>thick, horizontal layers of basaltic lava flows<\/b><span style=\"font-weight: 400;\">, giving rise to a <\/span><b>step-like or terraced topography<\/b><span style=\"font-weight: 400;\"> (trap structure).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The lava flows are remarkably <\/span><b>uniform in composition<\/b><span style=\"font-weight: 400;\">, indicating repeated eruptions of similar magma over a long period.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The <\/span><b>average dip of layers is low (about 5\u00b0\u201310\u00b0)<\/b><span style=\"font-weight: 400;\">, showing that lava spread widely over flat surfaces.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Individual lava flows vary in thickness from <\/span><b>3 to 30 meters<\/b><span style=\"font-weight: 400;\">, while the total thickness may exceed <\/span><b>3,000 meters<\/b><span style=\"font-weight: 400;\"> in some regions.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">These flows extend over <\/span><b>very large areas (sometimes up to 100 km or more)<\/b><span style=\"font-weight: 400;\">, highlighting the fluid nature of basaltic lava.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The rocks are primarily <\/span><b>basalt (igneous)<\/b><span style=\"font-weight: 400;\">, often showing <\/span><b>vesicular texture<\/b><span style=\"font-weight: 400;\"> (gas bubbles) and <\/span><b>amygdaloidal structure<\/b><span style=\"font-weight: 400;\"> (mineral-filled cavities).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The presence of numerous <\/span><b>dykes and sills<\/b><span style=\"font-weight: 400;\"> indicates the pathways through which magma rose to the surface.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Inter-trappean beds<\/b><span style=\"font-weight: 400;\"> (sedimentary layers) occur between lava flows, formed during pauses in volcanic activity; these contain <\/span><b>fossils of plants and freshwater organisms<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Deccan Trap region has given rise to <\/span><b>black cotton soil (regur)<\/b><span style=\"font-weight: 400;\"> due to weathering of basalt rocks.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The soils are <\/span><b>clay-rich, moisture-retentive, and fertile<\/b><span style=\"font-weight: 400;\">, but <\/span><b>low in humus and nitrogen<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The terrain often shows <\/span><b>flat-topped hills, plateaus, and steep escarpments<\/b><span style=\"font-weight: 400;\">, especially along the Western Ghats.<\/span><\/li>\n<\/ul>\n<h2><b>Black Cotton Soil (Regur Soil)<\/b><\/h2>\n<p><a href=\"https:\/\/vajiramandravi.com\/current-affairs\/black-soil\/\" target=\"_blank\"><b>Black Cotton Soil<\/b><\/a><span style=\"font-weight: 400;\">, also known as <\/span><b>Regur Soil<\/b><span style=\"font-weight: 400;\">, is a distinctive soil type formed by the <\/span><b>weathering of basaltic rocks of the Deccan Traps<\/b><span style=\"font-weight: 400;\">. It is widely recognized for its <\/span><b>dark color, high clay content, and excellent moisture retention<\/b><span style=\"font-weight: 400;\">, making it especially suitable for <\/span><b>cotton cultivation<\/b><span style=\"font-weight: 400;\">.<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Black soil derives its origin from the <\/span><b>basalt lava flows<\/b><span style=\"font-weight: 400;\"> of the Deccan Trap region, making it a <\/span><b>residual soil<\/b><span style=\"font-weight: 400;\"> formed in situ.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">It is most commonly found in <\/span><b>semi-arid and sub-humid regions<\/b><span style=\"font-weight: 400;\">, where climatic conditions favor its development.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The soil appears <\/span><b>deep black to grey<\/b><span style=\"font-weight: 400;\"> in color due to the presence of <\/span><b>iron, magnesium, and certain mineral salts<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">It has a <\/span><b>fine-grained, clayey texture<\/b><span style=\"font-weight: 400;\">, dominated by <\/span><b>montmorillonite clay minerals<\/b><span style=\"font-weight: 400;\">, which are responsible for its swelling and shrinking nature.<\/span><\/li>\n<\/ul>\n<h3><b>Key Characteristics:<\/b><\/h3>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>High moisture retention capacity<\/b><span style=\"font-weight: 400;\">, allowing crops to survive even during dry periods.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Becomes <\/span><b>sticky and plastic when wet<\/b><span style=\"font-weight: 400;\">, making ploughing difficult.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Develops <\/span><b>wide cracks during dry seasons<\/b><span style=\"font-weight: 400;\">, aiding aeration, this is known as the <\/span><b>self-ploughing property<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Poor in <\/span><b>humus content<\/b><span style=\"font-weight: 400;\">, but rich in certain minerals.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Slow permeability, which helps retain water but can lead to <\/span><b>waterlogging<\/b><span style=\"font-weight: 400;\"> if poorly managed.<\/span><\/li>\n<\/ul>\n<h3><b>Chemical Composition:\u00a0<\/b><\/h3>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Rich in Calcium Carbonate (Lime):<\/b><span style=\"font-weight: 400;\"> Enhances soil structure and supports plant growth.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>High Magnesium Content:<\/b><span style=\"font-weight: 400;\"> Important for chlorophyll formation and crop productivity.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Contains Potash (Potassium):<\/b><span style=\"font-weight: 400;\"> Essential for plant metabolism and disease resistance.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Deficient in <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/nitrogen\/\" target=\"_blank\">Nitrogen<\/a> and Phosphorus:<\/b><span style=\"font-weight: 400;\"> Limits fertility unless supplemented with fertilizers.<\/span><\/li>\n<\/ul>\n<h3><b>Agricultural Importance<\/b><\/h3>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Black cotton soil (regur)<\/b><span style=\"font-weight: 400;\"> is highly fertile and ideal for farming<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Excellent <\/span><b>moisture retention<\/b><span style=\"font-weight: 400;\"> supports crops even in low rainfall<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Suitable for major crops like <\/span><b>cotton, sugarcane, and millets<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Supports <\/span><b>rain-fed <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/agriculture-in-india\/\" target=\"_blank\">agriculture<\/a><\/b><span style=\"font-weight: 400;\">, reducing dependence on irrigation<\/span><\/li>\n<\/ul>\n<h2><b>Environmental Issues in Deccan Trap Region<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The Deccan Trap region faces multiple environmental challenges due to its basaltic geology, clay-rich black soils, and semi-arid climate, which affect land, water, and agriculture.<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Soil erosion and land degradation:<\/b><span style=\"font-weight: 400;\"> Removal of vegetation and improper farming on slopes leads to <\/span><b>loss of fertile topsoil<\/b><span style=\"font-weight: 400;\"> and reduced productivity.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Water scarcity and groundwater limitations:<\/b><span style=\"font-weight: 400;\"> Hard basalt rocks have <\/span><b>low permeability<\/b><span style=\"font-weight: 400;\">, restricting groundwater recharge and causing <\/span><b>frequent drought-like conditions<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Waterlogging in black soil areas:<\/b><span style=\"font-weight: 400;\"> The <\/span><b>clayey nature of regur soil<\/b><span style=\"font-weight: 400;\"> leads to poor drainage, resulting in temporary waterlogging during heavy rainfall.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Soil salinity and alkalinity:<\/b><span style=\"font-weight: 400;\"> Improper irrigation practices and poor drainage contribute to <\/span><b>salt accumulation<\/b><span style=\"font-weight: 400;\">, reducing soil fertility.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Cracking and structural damage in soil:<\/b><span style=\"font-weight: 400;\"> Deep cracks in dry seasons can damage <\/span><b>plant roots and infrastructure<\/b><span style=\"font-weight: 400;\"> like roads and buildings.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b><a href=\"https:\/\/vajiramandravi.com\/current-affairs\/deforestation\/\" target=\"_blank\">Deforestation<\/a> and biodiversity loss:<\/b><span style=\"font-weight: 400;\"> Expansion of agriculture and urbanization leads to <\/span><b>loss of natural vegetation and wildlife habitats<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Overgrazing pressure:<\/b><span style=\"font-weight: 400;\"> Excessive grazing depletes vegetation cover, accelerating <\/span><b>soil erosion and <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/desertification\/\" target=\"_blank\">desertification<\/a> tendencies<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Climate variability impacts:<\/b><span style=\"font-weight: 400;\"> Erratic rainfall and prolonged dry spells affect <\/span><b>crop yields and water availability<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Mining and quarrying impacts:<\/b><span style=\"font-weight: 400;\"> Extraction of basalt for construction causes <\/span><b>landscape degradation and dust pollution<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Learn about Deccan Traps, a vast flood basalt region of India formed during the Late Cretaceous, covering formation, distribution, characteristics, and black soil.<\/p>\n","protected":false},"author":27,"featured_media":101545,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[786],"tags":[4935,5102],"class_list":{"0":"post-101555","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-general-studies","8":"tag-geography","9":"tag-geography-notes","10":"no-featured-image-padding"},"acf":[],"_links":{"self":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/101555","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/users\/27"}],"replies":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/comments?post=101555"}],"version-history":[{"count":2,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/101555\/revisions"}],"predecessor-version":[{"id":101557,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/101555\/revisions\/101557"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media\/101545"}],"wp:attachment":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media?parent=101555"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/categories?post=101555"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/tags?post=101555"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}