{"id":949,"date":"2025-06-18T11:58:57","date_gmt":"2025-06-18T06:28:57","guid":{"rendered":"http:\/\/knowledgekart.in\/blog\/?page_id=949"},"modified":"2025-06-18T11:59:31","modified_gmt":"2025-06-18T06:29:31","slug":"peninsular-plateau-indian-geography-2-for-upsc-ias","status":"publish","type":"page","link":"https:\/\/knowledgekart.in\/blog\/peninsular-plateau-indian-geography-2-for-upsc-ias\/","title":{"rendered":"Peninsular Plateau-2"},"content":{"rendered":"\n<h3 class=\"wp-block-heading\" id=\"h-physiographic-divisions\">Physiographic Divisions:<\/h3>\n\n\n\n<p>Peninsular Plateau Indian Geography UPSC On the basis of prominent relief features, the peninsular plateau can be divided into three broad groups:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The Central Highlands<\/li>\n\n\n\n<li>The Deccan Plateau<\/li>\n\n\n\n<li>The Northeastern Plateau.<\/li>\n<\/ul>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"576\" src=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/subdivisions-Copy-1024x576.jpg\" alt=\"Physiographic Divisions and Important Mountain Ranges of the Peninsular Plateau\" class=\"wp-image-950\" title=\"\" srcset=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions-Copy-1024x576.jpg 1024w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions-Copy-416x234.jpg 416w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions-Copy-300x169.jpg 300w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions-Copy-768x432.jpg 768w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions-Copy.jpg 1366w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n<\/div>\n\n\n<p>Let\u2019s take up these divisions one by one:<\/p>\n\n\n\n<p><strong>1. The Central Highlands<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The northern segment of the peninsular plateau is known as the Central Highlands.<\/li>\n\n\n\n<li><strong>Location<\/strong>:\n<ol class=\"wp-block-list\">\n<li>North of Narmada river.<\/li>\n\n\n\n<li>They are bounded to the west by the Aravallis.<\/li>\n\n\n\n<li>Satpura ranges (formed by a series of scarped plateaus) lie in the South.<\/li>\n<\/ol>\n<\/li>\n\n\n\n<li><strong>General Elevation<\/strong>: 700-1,000 m above the mean sea level and it slopes towards the north and northeastern directions.<\/li>\n\n\n\n<li>These highlands consist of the:\n<ol class=\"wp-block-list\">\n<li><strong>Marwar upland<\/strong> \u2013 to the east of Aravallis in Rajasthan\n<ul class=\"wp-block-list\">\n<li>A rolling plain carved by Banas river. [Rolling Plain: \u2018Rolling <br>plains\u2019 are not completely flat; there are slight rises and fall in the <br>land form. Ex: Prairies of USA]<\/li>\n\n\n\n<li>Average elevation is 250-500 m above sea level.<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li><strong>Madhya Bharat Pathar<\/strong> \u2013 to the east of Marwar upland.<\/li>\n\n\n\n<li><strong>Malwa plateau<\/strong> \u2013 It lies in Madhya Pradesh between <br>Aravali and Vindhyas. It is composed of extensive lava flow and is <br>covered with black soils.<\/li>\n\n\n\n<li><strong>Bundelkhand plateau<\/strong> \u2013 It lies along the borders of <br>UP and MP. Because of intensive erosion, semi-arid climate and <br>undulating area, it is unfit for cultivation.<\/li>\n\n\n\n<li><strong>Baghelkhand plateau<\/strong> \u2013 It lies to the east of the Maikal range.<\/li>\n\n\n\n<li><strong>Chhotanagpur plateau<\/strong> \u2013 the north\u2013east part of Peninsular plateau.\n<ul class=\"wp-block-list\">\n<li>It Includes Jharkhand, parts of Chhattisgarh and West Bengal.<\/li>\n\n\n\n<li>This plateau consists of series of step like sub-plateaus (locally <br>called patlands \u2013 high-level plateau). It is thus famous as the <strong>Patland plateau<\/strong> and known as <strong>Ruhr of India<\/strong>.<\/li>\n\n\n\n<li>Rajmahal Hills are the northeastern projection of Chhota Nagpur Plateau.<\/li>\n\n\n\n<li>It is a mineral rich plateau.<\/li>\n<\/ul>\n<\/li>\n<\/ol>\n<\/li>\n<\/ul>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The extension of the Peninsular plateau can be seen as far as <br>Jaisalmer in the West, where it has been covered by the longitudinal <br>sand ridges and crescent-shaped sand dunes called <strong>barchans<\/strong>.<\/li>\n\n\n\n<li>This region has undergone metamorphic processes in its geological <br>history, which can be corroborated by the presence of metamorphic rocks <br>such as marble, slate, gneiss, etc.<\/li>\n\n\n\n<li>Most of the tributaries of the river Yamuna have their origin in the<br> Vindhyan and Kaimur ranges. Banas is the only significant tributary of <br>the river Chambal that originates from the Aravalli in the west.<\/li>\n<\/ul>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"576\" src=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/subdivisions1_wm2-1024x576.jpg\" alt=\"Physiographic Divisions of the Peninsular Plateau \u2013 the Central Highlands and the Deccan Plateau\" class=\"wp-image-952\" title=\"\" srcset=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions1_wm2-1024x576.jpg 1024w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions1_wm2-416x234.jpg 416w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions1_wm2-300x169.jpg 300w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions1_wm2-768x432.jpg 768w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/subdivisions1_wm2.jpg 1366w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n<\/div>\n\n\n<p><strong>2. The Deccan Plateau<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The Deccan Plateau lies to the south of the Narmada River and is shaped as an inverted triangle.<\/li>\n\n\n\n<li>It is bordered by:\n<ol class=\"wp-block-list\">\n<li>The Western Ghats in the west,<\/li>\n\n\n\n<li>The Eastern Ghats in the east,<\/li>\n\n\n\n<li>The Satpura, Maikal range and Mahadeo hills in the north.<\/li>\n<\/ol>\n<\/li>\n\n\n\n<li>It is volcanic in origin, made up of horizontal layers of solidified<br> lava forming trap structure with step-like appearance. The sedimentary <br>layers are also found in between the layers of solidified lava, making <br>it inter\u2013trapping in structure.<\/li>\n\n\n\n<li>Most of the rivers flow from west to east.<\/li>\n\n\n\n<li>The plateau is suitable for the cultivation of cotton; home to rich <br>mineral resources and a source to generate hydroelectric power.<\/li>\n\n\n\n<li>The Deccan plateau can be subdivided as follows:\n<ol class=\"wp-block-list\">\n<li><strong>The Maharashtra Plateau \u2013 <\/strong>it has typical deccan trap topography underlain by basaltic rock, the regur.<\/li>\n\n\n\n<li><strong>The Karnataka Plateau (<\/strong>also known as<strong> Mysore plateau) \u2013 <\/strong>divided into western hilly country region of \u2018Malnad\u2019 and plain \u2018Maidan\u2019<\/li>\n\n\n\n<li><strong>Telangana Plateau <\/strong><\/li>\n<\/ol>\n<\/li>\n<\/ul>\n\n\n\n<p><strong>3. The Northeastern Plateau:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The Meghalaya (or Shillong) plateau is separated from peninsular rock base by the Garo-Rajmahal gap.<\/li>\n\n\n\n<li>Shillong (1,961 m) is the highest point of the plateau.<\/li>\n\n\n\n<li>The region has the Garo, Khasi, Jaintia and Mikir (Rengma) hills.<\/li>\n\n\n\n<li>An extension of the Meghalaya plateau is also seen in the Karbi Anglong hills of Assam.<\/li>\n\n\n\n<li>The Meghalaya plateau is also rich in mineral resources like coal, iron ore, sillimanite, limestone and uranium.<\/li>\n\n\n\n<li>This area receives maximum rainfall from the south-west monsoon. As a<br> result, the Meghalaya plateau has a highly eroded surface. Cherrapunji <br>displays a bare rocky surface devoid of any permanent vegetation cover.<\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\" id=\"h-hill-ranges-of-the-peninsula\">Hill ranges of the peninsula:<\/h3>\n\n\n\n<p>Most of the hills in the peninsular region are of the <strong>relict type (residual hills). <\/strong>They are the remnants of the hills and horsts formed many million years ago (horst: uplifted block; graben: subsided block).<\/p>\n\n\n\n<p>The plateaus of the Peninsular region are separated from one another by these hill ranges and various river valleys.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"576\" src=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/hill-ranges-Copy-1024x576.jpg\" alt=\"Hill Ranges of the Peninsula\" class=\"wp-image-953\" title=\"\" srcset=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/hill-ranges-Copy-1024x576.jpg 1024w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/hill-ranges-Copy-416x234.jpg 416w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/hill-ranges-Copy-300x169.jpg 300w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/hill-ranges-Copy-768x432.jpg 768w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/hill-ranges-Copy.jpg 1366w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p><strong>The Aravalli Mountain Range<\/strong><strong>:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>It is a relic of one of the oldest fold mountains of the world.<\/li>\n\n\n\n<li>Its general elevation is only 400-600 m, with few hills well above 1,000 m.<\/li>\n\n\n\n<li>At present, it is seen as a discontinuous ridge from Delhi to Ajmer <br>and rising up to 1722m (Gurushikhar peak in Mount Abu) and thence <br>southward.<\/li>\n\n\n\n<li>It is known as \u2018Jarga\u2019 near Udaipur and \u2018Delhi Ridge\u2019 near Delhi.<\/li>\n\n\n\n<li>Dilwara Jain Temple, the famous Jain temple is situated on Mt. Abu.<\/li>\n<\/ul>\n\n\n\n<p><strong>2. Vindhyan Ranges:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>They rise as an escarpment running parallel to the Narmada-Son valley.<\/li>\n\n\n\n<li>General elevation: 300 to 650 m.<\/li>\n\n\n\n<li>Most of them are made up of sedimentary rocks of ancient ages.<\/li>\n\n\n\n<li>They act as a watershed between Gangetic and peninsular river systems.<\/li>\n<\/ul>\n\n\n\n<p><strong>3. Satpura ranges:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Satpura range is a series of seven mountains (\u2018Sat\u2019 = seven and \u2018pura\u2019 = mountains).<\/li>\n\n\n\n<li>The seven mountain ranges or folds of Satpura\u2019s are:\n<ul class=\"wp-block-list\">\n<li>Maikal Hills<\/li>\n\n\n\n<li>Mahadeo Hills near Pachmarhi<\/li>\n\n\n\n<li>Kalibhit<\/li>\n\n\n\n<li>Asirgarh<\/li>\n\n\n\n<li>Bijagarh<\/li>\n\n\n\n<li>Barwani<\/li>\n\n\n\n<li>Arwani which extends to Rajpipla Hills in Eastern Gujarat.<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li>Satpura ranges run parallel between Narmada and Tapi, parallel to Maharashtra-MP border.<\/li>\n\n\n\n<li>Dhupgarh (1,350 m) near Pachmarhi on Mahadev Hills is the highest peak of the Satpura Range.<\/li>\n\n\n\n<li>Amarkantak (1,127 m) is another important peak. Amarkantak is the <br>highest peak of the Maikal Hills from where two prominent rivers \u2013 the <br>Narmada and the Son originate.<\/li>\n\n\n\n<li>Note that three rivers originate from the three sides of Maikal <br>hills (as shown in the following map) but, from Amarkantak, only two <br>rivers (the Narmada and the Son) originate (and not Mahanadi).<\/li>\n<\/ul>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter\"><img loading=\"lazy\" decoding=\"async\" width=\"768\" height=\"452\" src=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/Untitled2-768x452.png\" alt=\"The Satpura Mountain Range\" class=\"wp-image-954\" title=\"\" srcset=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/Untitled2-768x452.png 768w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/Untitled2-768x452-416x245.png 416w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/Untitled2-768x452-300x177.png 300w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/figure>\n<\/div>\n\n\n<p><strong>Western and Eastern Ghats:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The Western Ghats:\n<ul class=\"wp-block-list\">\n<li>These are a faulted part of the Deccan plateau running parallel from<br> the Tapi valley to a little north of Kanyakumari (1600km). Their <br>western slope is like an escarpment while eastern slope merges gently <br>with the plateau.<\/li>\n\n\n\n<li>Their average elevation is about 1,500 m with the height increasing from north to south.<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li>The Eastern Ghats are in the form of residual mountains which are not regular but broken at intervals. Peninsular Plateau Indian Geography UPSC<\/li>\n\n\n\n<li>The Eastern and the Western Ghats meet each other at the Nilgiri hills.<\/li>\n\n\n\n<li>A brief comparison between them:<\/li>\n<\/ul>\n\n\n\n<figure class=\"wp-block-image\"><img loading=\"lazy\" decoding=\"async\" width=\"669\" height=\"539\" src=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/Capture5.png\" alt=\"Differences between the Western and Eastern Ghats. Peninsular Plateau Indian Geography\" class=\"wp-image-955\" title=\"\" srcset=\"https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/Capture5.png 669w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/Capture5-416x335.png 416w, https:\/\/knowledgekart.in\/blog\/wp-content\/uploads\/\/Capture5-300x242.png 300w\" sizes=\"auto, (max-width: 669px) 100vw, 669px\" \/><\/figure>\n\n\n\n<p><strong>Note:<\/strong> The Western Ghats are continuous and can be \ncrossed through passes only. There are four main passes which have \ndeveloped in the Western Ghats. These are:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li>Thal Ghat \u2013 It links Nasik to Mumbai.<\/li>\n\n\n\n<li>Bhor Ghat \u2013 It links Mumbai to Pune.<\/li>\n\n\n\n<li>Pal Ghat \u2013 This pass is located between the Nilgiris and the <br>Annamalai mountains. It is in Kerala and connects Kochi and Chennai.<\/li>\n\n\n\n<li>Senkota Pass \u2013 This pass located between the Nagercoil and the Cardamom hills links Thiruvananthapuram and Madurai. Peninsular Plateau Indian Geography UPSC<\/li>\n<\/ol>\n\n\n\n<h3 class=\"wp-block-heading\" id=\"h-significance-of-the-peninsular-region\">Significance of the Peninsular Region:<\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Rich in mineral resources<\/strong>: The peninsular region of<br> India is rich in both metallic and non-metallic minerals. About 98% of <br>the Gondwana coal deposits of India are found in the peninsular region.<\/li>\n\n\n\n<li><strong>Agriculture<\/strong>: Black soil found in a substantial part<br> of the peninsula is conducive for the cultivation of cotton, maize , <br>citrus fruits etc. Some areas are also suitable for the cultivation of <br>tea, coffee, groundnut etc.<\/li>\n\n\n\n<li><strong>Forest Products<\/strong>: Apart from teal, sal wood and <br>other forest products, the forests of Western and Eastern Ghats are rich<br> in medicinal plants and are home to many wild animals.<\/li>\n\n\n\n<li><strong>Hydel Power<\/strong>: many rivers, which have waterfalls. They help in the generation of hydroelectric power.<\/li>\n\n\n\n<li><strong>Tourism<\/strong>: There are numerous hill stations and hill resorts like Ooty, Mahabaleshwar, Khandala, etc. Peninsular Plateau Indian Geography UPSC<\/li>\n<\/ul>\n\n\n\n<p>Now that we are done with this part, let\u2019s try to attempt some questions from the past UPSC examinations:<\/p>\n\n\n\n<p><strong>Prelims:<\/strong><\/p>\n\n\n\n<p><strong>1995<\/strong><\/p>\n\n\n\n<p>Question: Which one of the following mountain ranges is spread over only one state in India?<\/p>\n\n\n\n<p>A) Aravalli<\/p>\n\n\n\n<p>B) Satpura<\/p>\n\n\n\n<p>C) Ajanta<\/p>\n\n\n\n<p>D) Sahyadri<\/p>\n\n\n\n<p>Ans. C<\/p>\n\n\n\n<p><strong>1997<\/strong><\/p>\n\n\n\n<p>Question: Consider the map given below:<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignleft\"><a href=\"https:\/\/www.civilsdaily.com\/wp-content\/uploads\/2016\/12\/CamScanner-New-Document-10-830920d00b40f30g00B50T10-001.jpg\" rel=\"nofollow noopener\" target=\"_blank\"><img decoding=\"async\" src=\"https:\/\/www.civilsdaily.com\/wp-content\/uploads\/2016\/12\/CamScanner-New-Document-10-830920d00b40f30g00B50T10-001-1024x1009.jpg\" alt=\"Peninsular Plateau Indian Geography\" class=\"wp-image-76921\" title=\"\"><\/a><\/figure>\n<\/div>\n\n\n<p>The places marked A,B, C, and D in the map are respectively<\/p>\n\n\n\n<p>A) Rift valley region, Chattisgarh plain, Rain shadow region, and Chotanagpur Plateau<\/p>\n\n\n\n<p>B) Chattisgarh plain , Chotanagpur Plateau, Rift valley region, Rain shadow region<\/p>\n\n\n\n<p>C) Rift valley region, Chattisgarh plain, Chotanagpur Plateau and Rain shadow region<\/p>\n\n\n\n<p>D) Chattisgarh plain , Rain shadow region, Chotanagpur Plateau, Rift valley region,<\/p>\n\n\n\n<p>Ans. C<\/p>\n\n\n\n<p><strong>2005<\/strong><\/p>\n\n\n\n<p>Question: Which one of the following statements is not correct?<\/p>\n\n\n\n<p>A) The Western Ghats are relatively higher in their northern regions.<\/p>\n\n\n\n<p>B) The Anaimudi is the highest peak in the Western Ghats<\/p>\n\n\n\n<p>C) Tapi river lies to the south of Satpura<\/p>\n\n\n\n<p>D) The Narmada and the Tapi river valleys are said to be old rift valleys.<\/p>\n\n\n\n<p>Ans. A<\/p>\n\n\n\n<p>Question: Which one of the following is the correct sequence of the \ngiven hills starting from the north and going towards the south?<\/p>\n\n\n\n<p>A) Nallamalai Hills \u2013 Nilgiri Hills \u2013 Javadi Hills \u2013 Anaimalai Hills<\/p>\n\n\n\n<p>B) Anaimalai Hills \u2013 Javadi Hills \u2013 Nilgiri Hills \u2013 Nallamalai Hills<\/p>\n\n\n\n<p>C) Nallamalai Hills \u2013 Javadi Hills \u2013 Nilgiri Hills \u2013 Anaimalai Hills<\/p>\n\n\n\n<p>D) Anaimalai Hills \u2013 Nilgiri Hills \u2013 Javadi Hills \u2013 Nallamalai Hills<\/p>\n\n\n\n<p>Ans. C<\/p>\n\n\n\n<p>Read More &#8211; Peninsular Plateau Indian Geography UPSC<\/p>\n\n\n\n<p><a href=\"https:\/\/knowledgekart.in\/blog\/the-peninsular-plateau\/\" target=\"_blank\" rel=\"noreferrer noopener\">The Peninsular Plateau<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/knowledgekart.in\/blog\/indian-geography\/\" target=\"_blank\" rel=\"noreferrer noopener\">Indian geography<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/knowledgekart.in\/blog\/the-northern-and-northeastern-mountains-indian-geography-for-upsc\/\" target=\"_blank\" rel=\"noreferrer noopener\">The Northern and Northeastern Mountains<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/knowledgekart.in\/blog\/upsc-ias-gk-indian-rock-system-indian-geography\/\" target=\"_blank\" rel=\"noreferrer noopener\">UPSC IAS GK Indian Rock System Archaean, Purana, Dravidian &amp; Aryan Rock System<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Physiographic Divisions: Peninsular Plateau Indian Geography UPSC On the basis of prominent relief features, the peninsular plateau can be divided into three broad groups: Let\u2019s take up these divisions one&hellip;<\/p>\n","protected":false},"author":6558,"featured_media":955,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-949","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/pages\/949","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/users\/6558"}],"replies":[{"embeddable":true,"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/comments?post=949"}],"version-history":[{"count":1,"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/pages\/949\/revisions"}],"predecessor-version":[{"id":80647,"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/pages\/949\/revisions\/80647"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/media\/955"}],"wp:attachment":[{"href":"https:\/\/knowledgekart.in\/blog\/wp-json\/wp\/v2\/media?parent=949"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}