


{"id":59590,"date":"2025-12-08T11:14:18","date_gmt":"2025-12-08T05:44:18","guid":{"rendered":"https:\/\/vajiramandravi.com\/current-affairs\/?p=59590"},"modified":"2025-12-08T16:59:28","modified_gmt":"2025-12-08T11:29:28","slug":"indo-gangetic-plains","status":"publish","type":"post","link":"https:\/\/vajiramandravi.com\/current-affairs\/indo-gangetic-plains\/","title":{"rendered":"Indo-Gangetic Plains, Feature, Location, Formation, Significance"},"content":{"rendered":"<p><span style=\"font-weight: 400;\">The Indo-Gangetic Plain, spanning India, Bangladesh, and Nepal, faces recurrent floods due to heavy monsoon rains, glacial melt, deforestation, and urbanization. These floods damage lives, agriculture, and infrastructure. Effective management demands an integrated approach combining sustainable land use, afforestation, advanced forecasting technologies, and active community participation. Building resilience through coordinated planning and environmental conservation is essential to reduce flood impacts and safeguard livelihoods in this densely populated region.<\/span><\/p>\n<h2><b>Indo-Gangetic Plains<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The Indo-Gangetic Plains, or Indo-Gangetic-Brahmaputra Plains, are vast aggradational plains formed by alluvial deposits from the Indus, Ganga, Brahmaputra, and their tributaries. The Northern Plains of India are one of the five physiographic divisions of India and represent its youngest landform. Spanning a massive area, they hold the title of the world\u2019s largest alluvial plain, supporting dense populations, fertile agriculture, and a rich cultural history shaped by these mighty river systems.<\/span><\/p>\n<h2><b>Indo-Gangetic Plains Features<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The Indo-Gangetic Plains has some unique geographical, climatic, and socio-economic characteristics. The table below includes the Indo-Gangetic Plains Features for better understanding:<\/span><\/p>\n<table style=\"width: 95.7912%;\">\n<tbody>\n<tr>\n<td class=\"tb-color\" style=\"text-align: center; width: 95.078%;\" colspan=\"2\"><b>Indo-Gangetic Plains Features<\/b><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">North-South Extension<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">They extend from the south of the Himalayas upto the edge of the Peninsular Plateau.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">East-West Extension<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">They extend from the mouth of the Indus in the west to the mouth of the Ganga in the east.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">Boundaries<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">They are bounded by the Shiwalik range to the north, the Desert to the west, the <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/peninsular-plateau\/\" target=\"_blank\"><strong>Peninsular Plateau<\/strong><\/a> to the south, and the Puruvachal Hills to the east.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">Length<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">The total length of this tract is 3200 km, of which around 2400 km lies in India and the rest lies in Bangladesh.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">Width<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">The average width of the Great Northern Plains is 150-300 km. They are widest in the west where their width goes up to 500 km, and narrow down towards the east where their width shrinks down to 60-100 km.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">Area<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">They occupy an area of around 7.8 lakh sq. km, making it the largest alluvial plain in the world.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">States Covered<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">The Great Northern Plains of India spread over the states \u2013 Punjab, Haryana, Delhi, Uttar Pradesh, Bihar, parts of Jharkhand and West Bengal, and Assam.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">Extreme Horizontality<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">Extreme horizontality is an important feature of this plain. With an average elevation of around 200 m and the highest elevation of about 291 m above the mean sea level, its average gradient range is just 15-20 cm.<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 13.2061%;\">\n<p><span style=\"font-weight: 400;\">Soil Cover<\/span><\/p>\n<\/td>\n<td style=\"width: 81.8719%;\">\n<p><span style=\"font-weight: 400;\">The rivers coming from the northern mountain carry a huge load of sediments which get deposited over these plains. Thus, these plains have a rich and fertile soil cover.<\/span><\/p>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h2><b>Indo-Gangetic Plains Formation<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The Indo-Gangetic Plains were formed by the deposition of sediments from the <a href=\"https:\/\/vajiramandravi.com\/upsc-exam\/indian-river-systems\/\" target=\"_blank\"><strong>Indus<\/strong><\/a>, <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/ganga-river-system\/\" target=\"_blank\"><strong>Ganga<\/strong><\/a>, and <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/brahmaputra-river-system\/\" target=\"_blank\"><strong>Brahmaputra<\/strong><\/a> river systems, which filled a vast depression between the Peninsular Plateau and the Himalayas. During the Tertiary Period, the collision of the Indo-Australian and Eurasian plates created the Himalayas and a large syncline to the south. Over time, rivers from the Himalayas deposited immense alluvial material into this depression, giving rise to the Northern Plains of India.<\/span><\/p>\n<h2><b>Indo-Gangetic Plains Regional Division<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Regionally, the Indo-Gangetic Plains are divided into four major sections:<\/span><\/p>\n<ol>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Rajasthan Plain &#8211; Occupies the arid western part, largely desert with some fertile tracts along river channels.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Punjab-Haryana Plain &#8211; Known for extensive alluvial deposits and intensive agriculture, supported by canal irrigation.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Ganga Plain &#8211; The largest and most fertile stretch, spanning several states from Uttarakhand to West Bengal.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Brahmaputra Plain &#8211; A flood-prone yet highly fertile region in Assam, shaped by the Brahmaputra River and its tributaries.<\/span><\/li>\n<\/ol>\n<h2><b>Rajasthan Plain<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Forming the western edge of the Indo-Gangetic Plains, this region includes the Thar or Great Indian Desert, extending across western Rajasthan and into Pakistan. It has two main parts:<\/span><\/p>\n<h3><b>Marusthali\u00a0<\/b><\/h3>\n<p><span style=\"font-weight: 400;\">The true desert area in the east covers much of the Marwar plain. While it appears as an aggradational plain, geologically it belongs to the Peninsular Plateau, evident from scattered outcrops of gneiss, schist, and granite. Its eastern side is rocky; the west is dominated by shifting sand dunes called Dhrian.<\/span><\/p>\n<h3><b>Rajasthan Bagar<\/b><\/h3>\n<p><span style=\"font-weight: 400;\">A semi-arid tract between the Thar desert and the Aravalli Range. Seasonal streams from the Aravallis create fertile patches called Rohi. The Luni River, flowing southwest into the Rann of Kutch, is the main watercourse. North of the Luni lies the sandy plain called Thali. The region also has saline lakes such as Sambhar, Didwana, and Khatu.<\/span><\/p>\n<h2><b>Punjab-Haryana Plain<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Located east and northeast of the Rajasthan Plain, this region stretches about 640 km from northwest to southeast, with an average width of 300 km. It slopes gently southwest, so rivers follow the same direction. The soil is mainly silty and porous.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Key subdivisions and features:<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Bet &#8211; Floodplain areas near riverbanks formed by new alluvium.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Bhabar Plain &#8211; Foothill zone with boulders, gravel, sand, and clay that cannot retain water.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Punjab Plain &#8211; Formed by the alluvium of the Satluj, Beas, Ravi, Chenab, and Jhelum; hence called the Land of Five Rivers. Divided into five Doabs:<\/span>\n<ol>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Bist-Jalandhar Doab &#8211; Between Beas and Satluj<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Bari Doab &#8211; Between Beas and Ravi<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Rachna Doab &#8211; Between Ravi and Chenab<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Chaj Doab &#8211; Between Chenab and Jhelum<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Sind Sagar Doab &#8211; Between Jhelum-Chenab and the Indus<\/span><\/li>\n<\/ol>\n<\/li>\n<\/ul>\n<p><span style=\"font-weight: 400;\">Other notable features:<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Bet Lands &#8211; Khadar-rich fertile floodplains replenished annually.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Dhayas &#8211; Broad Khadar floodplains bordered by bluffs.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Chos &#8211; Eroded tracts in the north near the Shiwalik Hills caused by seasonal streams.<\/span><\/li>\n<\/ul>\n<h2><b>Ganga Plain<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The largest unit of the Indo-Gangetic Plains, covering about 3.75 lakh sq. km, formed by the alluvium of the Ganga and its Himalayan and Peninsular tributaries. It stretches from Delhi to Kolkata across Uttar Pradesh, Bihar, and West Bengal, sloping east and southeast.<\/span><\/p>\n<h3><b>Upper Ganga Plain<\/b><\/h3>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Location: Westernmost part, bounded by the Shiwaliks (north), Peninsular boundary (south), Yamuna River (west). Eastern limit unclear.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Gradient: ~25 cm\/km; sluggish rivers.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Features: River bluffs, meanders, oxbow lakes, levees, abandoned channels, sandy bhurs.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Major Units: Ganga-Yamuna Doab, Rohilkhand Plains, Avadh Plains.<\/span><\/li>\n<\/ul>\n<h3><b>Middle Ganga Plain<\/b><\/h3>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Location: East of the Upper Ganga Plain; covers eastern Uttar Pradesh and Bihar.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Boundaries: Himalayas (north), Peninsular edge (south).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Features: Levees, bluffs, oxbow lakes, marshes, tals, ravines; highly flood-prone due to shifting river courses\u2014Kosi, the \u201cSorrow of Bihar,\u201d is most notorious.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Major Units: Ganga-Ghaghara Doab, Ghaghara-Gandak Doab, Gandak-Kosi Doab (Mithila Plain).<\/span><\/li>\n<\/ul>\n<h3><b>Lower Ganga Plain<\/b><\/h3>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Location: Eastern Bihar, West Bengal, most of Bangladesh.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Boundaries: Darjeeling Himalaya (north), Bay of Bengal (south), Chotanagpur Highlands (west), Bangladesh (east).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Features: Dominated by deltaic landforms. The Ganga-Brahmaputra Delta, the world\u2019s largest is rich in mangroves and home to the Royal Bengal Tiger.<\/span><\/li>\n<\/ul>\n<h2><b>Brahmaputra Plain<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Location &amp; Names: Northeastern India; also called Brahmaputra Valley or Assam Valley.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Boundaries: Eastern Himalayas of Arunachal Pradesh (north), Patkai Bum &amp; Naga Hills (east), Garo-Khasi-Jaintia &amp; Mikir Hills (south), Indo-Bangladesh border and lower Ganga Plain (west).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Formation: An aggradational plain formed by the depositional work of the Brahmaputra and its tributaries.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Riverine Features: Alluvial fans, sandbars, meanders, oxbow lakes formed as northern tributaries enter the valley abruptly.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Notable Facts: Majuli Island, the world\u2019s largest riverine island, lies here. The valley is also famous for its tea plantations.<\/span><\/li>\n<\/ul>\n<h2><b>Indo-Gangetic Plains Geomorphology<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The table of the distinctive geomorphological features of the Indo-Gangetic Plains is shared below:<\/span><\/p>\n<table style=\"width: 97.5942%;\">\n<tbody>\n<tr>\n<td class=\"tb-color\" style=\"text-align: center; width: 96.3928%;\" colspan=\"5\"><b>Indo-Gangetic Plains Geomorphology<\/b><\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center; width: 7.81563%;\"><strong>Feature<\/strong><\/td>\n<td style=\"text-align: center; width: 24.1211%;\"><strong>Location &amp; Extent<\/strong><\/td>\n<td style=\"text-align: center; width: 17.6304%;\"><strong>Composition<\/strong><\/td>\n<td style=\"text-align: center; width: 27.8236%;\"><strong>Key Characteristics<\/strong><\/td>\n<td style=\"text-align: center; width: 19.0021%;\"><strong>Fertility \/ Use<\/strong><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 7.81563%;\">\n<p><span style=\"font-weight: 400;\">Bhabar<\/span><\/p>\n<\/td>\n<td style=\"width: 24.1211%;\">\n<p><span style=\"font-weight: 400;\">8\u201316 km belt along Shiwalik foothills (Indus to Tista)<\/span><\/p>\n<\/td>\n<td style=\"width: 17.6304%;\">\n<p><span style=\"font-weight: 400;\">Unassorted gravel and pebbles<\/span><\/p>\n<\/td>\n<td style=\"width: 27.8236%;\">\n<p><span style=\"font-weight: 400;\">Streams disappear underground due to porous sediments<\/span><\/p>\n<\/td>\n<td style=\"width: 19.0021%;\">\n<p><span style=\"font-weight: 400;\">Poor for cultivation<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 7.81563%;\">\n<p><span style=\"font-weight: 400;\">Tarai<\/span><\/p>\n<\/td>\n<td style=\"width: 24.1211%;\">\n<p><span style=\"font-weight: 400;\">South of Bhabar; 15-30 km wide<\/span><\/p>\n<\/td>\n<td style=\"width: 17.6304%;\">\n<p><span style=\"font-weight: 400;\">Finer alluvium<\/span><\/p>\n<\/td>\n<td style=\"width: 27.8236%;\">\n<p><span style=\"font-weight: 400;\">Marshy, waterlogged; streams re-emerge<\/span><\/p>\n<\/td>\n<td style=\"width: 19.0021%;\">\n<p><span style=\"font-weight: 400;\">Fertile; much converted to farmland<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 7.81563%;\">\n<p><span style=\"font-weight: 400;\">Khadar<\/span><\/p>\n<\/td>\n<td style=\"width: 24.1211%;\">\n<p><span style=\"font-weight: 400;\">Along river floodplains<\/span><\/p>\n<\/td>\n<td style=\"width: 17.6304%;\">\n<p><span style=\"font-weight: 400;\">New alluvium<\/span><\/p>\n<\/td>\n<td style=\"width: 27.8236%;\">\n<p><span style=\"font-weight: 400;\">Renewed annually; no calcareous deposits<\/span><\/p>\n<\/td>\n<td style=\"width: 19.0021%;\">\n<p><span style=\"font-weight: 400;\">Very fertile; intensively cultivated<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 7.81563%;\">\n<p><span style=\"font-weight: 400;\">Bhangar<\/span><\/p>\n<\/td>\n<td style=\"width: 24.1211%;\">\n<p><span style=\"font-weight: 400;\">Terraces above floodplains<\/span><\/p>\n<\/td>\n<td style=\"width: 17.6304%;\">\n<p><span style=\"font-weight: 400;\">Older alluvium with kankar<\/span><\/p>\n<\/td>\n<td style=\"width: 27.8236%;\">\n<p><span style=\"font-weight: 400;\">Not renewed frequently; higher than Khadar<\/span><\/p>\n<\/td>\n<td style=\"width: 19.0021%;\">\n<p><span style=\"font-weight: 400;\">Less fertile<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 7.81563%;\">\n<p><span style=\"font-weight: 400;\">Reh \/ Kallar<\/span><\/p>\n<\/td>\n<td style=\"width: 24.1211%;\">\n<p><span style=\"font-weight: 400;\">Dry tracts of UP and Haryana<\/span><\/p>\n<\/td>\n<td style=\"width: 17.6304%;\">\n<p><span style=\"font-weight: 400;\">Saline\/alkaline efflorescence<\/span><\/p>\n<\/td>\n<td style=\"width: 27.8236%;\">\n<p><span style=\"font-weight: 400;\">Generally barren<\/span><\/p>\n<\/td>\n<td style=\"width: 19.0021%;\">\n<p><span style=\"font-weight: 400;\">Unfit for cultivation<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 7.81563%;\">\n<p><span style=\"font-weight: 400;\">Bhur<\/span><\/p>\n<\/td>\n<td style=\"width: 24.1211%;\">\n<p><span style=\"font-weight: 400;\">Elevated sandy ridges along Ganga<\/span><\/p>\n<\/td>\n<td style=\"width: 17.6304%;\">\n<p><span style=\"font-weight: 400;\">Wind-blown sand<\/span><\/p>\n<\/td>\n<td style=\"width: 27.8236%;\">\n<p><span style=\"font-weight: 400;\">Formed in hot, dry months<\/span><\/p>\n<\/td>\n<td style=\"width: 19.0021%;\">\n<p><span style=\"font-weight: 400;\">Limited agricultural use<\/span><\/p>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h2><b>Indo-Gangetic Plains Significance<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Although the Northern Plains of India cover less than one-third of India\u2019s total area, they support over 40% of the country\u2019s population.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Fertile alluvial soils, flat terrain, slow-moving perennial rivers, and a favorable climate enable intensive agriculture, earning the northern plains the title of Granary of India.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The flat relief supports a dense network of roads and railways, promoting rapid urbanization and industrial growth.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The banks of rivers like the Ganga and Yamuna host numerous pilgrimage sites, adding deep cultural and spiritual significance to the region.<\/span><\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Indo-Gangetic Plains, the world\u2019s largest alluvial plain, span India, Nepal &#038; Bangladesh, offering fertile soils, rich culture, and vital agriculture.<\/p>\n","protected":false},"author":11,"featured_media":59542,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[786],"tags":[2204],"class_list":{"0":"post-59590","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-general-studies","8":"tag-indo-gangetic-plains","9":"no-featured-image-padding"},"acf":[],"_links":{"self":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/59590","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\/11"}],"replies":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/comments?post=59590"}],"version-history":[{"count":0,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/59590\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media\/59542"}],"wp:attachment":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media?parent=59590"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/categories?post=59590"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/tags?post=59590"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}