{"id":168,"date":"2025-01-07T14:48:26","date_gmt":"2025-01-07T14:48:26","guid":{"rendered":"https:\/\/recruitmentdbranlu.in\/?p=168"},"modified":"2025-01-07T14:48:26","modified_gmt":"2025-01-07T14:48:26","slug":"comparison-between-himalayan-and-peninsular-rivers","status":"publish","type":"post","link":"https:\/\/www.reilsolar.com\/pdfdrive\/comparison-between-himalayan-and-peninsular-rivers\/","title":{"rendered":"Comparison Between Himalayan and Peninsular Rivers"},"content":{"rendered":"<p><span style=\"color: #000000\">Difference between the rivers rising in the Himalayas and those rising in the Peninsular plateau are primarily a result of the differences between the two areas in terms of relief and climate.<\/span><\/p>\n<p><span style=\"color: #000000\">Following table shows major differences between these two groups.<\/span><\/p>\n<table style=\"border-collapse: collapse;width: 100%;height: 202px\">\n<tbody>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">S.N.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px;text-align: center\"><span style=\"color: #000000\">Aspects<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px;text-align: center\"><span style=\"color: #000000\">Himalayan River<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px;text-align: center\"><span style=\"color: #000000\">Peninsular River<\/span><\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">1.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px\"><span style=\"color: #000000\">Place of Origin<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px\"><span style=\"color: #000000\">Himalayan mountain covered with glaciers<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px\"><span style=\"color: #000000\">Peninsular plateau and central<\/span><br \/>\n<span style=\"color: #000000\">highland<\/span><\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">2.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px\"><span style=\"color: #000000\">Nature of flow<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px\"><span style=\"color: #000000\">Perennial<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px\"><span style=\"color: #000000\">Ephemeral<\/span><\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">3.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px\"><span style=\"color: #000000\">Type of drainage<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px\"><span style=\"color: #000000\">Antecedent and Consequent leading to dendritic pattern<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px\"><span style=\"color: #000000\">Super imposed, rejuvenated resulting in trellis, radial and rectangular<\/span><br \/>\n<span style=\"color: #000000\">Patterns<\/span><\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">4.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px\"><span style=\"color: #000000\">Nature of river<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px\"><span style=\"color: #000000\">Long course, flowing through the rugged mountains experiencing headward erosion and river capturing; In plains meandering and shifting of Course;<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px\"><span style=\"color: #000000\">Smaller, fixed course with welladjusted valleys;<\/span><\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">5.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px\"><span style=\"color: #000000\">Catchment area<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px\"><span style=\"color: #000000\">Very large basins<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px\"><span style=\"color: #000000\">Relatively smaller basin<\/span><\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">6.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px\"><span style=\"color: #000000\">Age of the river<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px\"><span style=\"color: #000000\">Young, active and deepening of valley<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px\"><span style=\"color: #000000\">Old rivers with graded profile and lateral erosion<\/span><\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 13.9697%;height: 24px;text-align: center\"><span style=\"color: #000000\">7.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 24px\"><span style=\"color: #000000\">Irrigation<\/span><\/td>\n<td style=\"width: 30.8181%;height: 24px\"><span style=\"color: #000000\">Flows through plains and canal system<\/span><\/td>\n<td style=\"width: 30.4546%;height: 24px\"><span style=\"color: #000000\">Flows over uneven plateau; canals only in deltaic region<\/span><\/td>\n<\/tr>\n<tr style=\"height: 10px\">\n<td style=\"width: 13.9697%;height: 10px;text-align: center\"><span style=\"color: #000000\">8.<\/span><\/td>\n<td style=\"width: 24.7576%;height: 10px\"><span style=\"color: #000000\">Hydroelectricity<\/span><\/td>\n<td style=\"width: 30.8181%;height: 10px\"><span style=\"color: #000000\">Eastern region has very high potential and large dams are building up<\/span><\/td>\n<td style=\"width: 30.4546%;height: 10px\"><span style=\"color: #000000\">Natural waterfalls for generating electricity.<\/span><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><span style=\"color: #000000\">The Peninsular drainage system is older than the Himalayan one. This is evident from the broad, largely-graded shallow valleys, and the maturity of the rivers. Rivers follow the relief pattern of the plateau. Except for the rivers flowing through fault valleys, the slope of all rivers is very gentle.<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Difference between the rivers rising in the Himalayas and those rising in the Peninsular plateau are primarily a result of the differences between the two areas in terms of relief and climate. Following table shows major differences between these two groups. S.N. Aspects Himalayan River Peninsular River 1. Place of Origin Himalayan mountain covered with [&hellip;]<\/p>\n","protected":false},"author":84,"featured_media":169,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[863],"tags":[],"class_list":["post-168","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geography"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/posts\/168","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/users\/84"}],"replies":[{"embeddable":true,"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/comments?post=168"}],"version-history":[{"count":0,"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/posts\/168\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/media\/169"}],"wp:attachment":[{"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/media?parent=168"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/categories?post=168"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.reilsolar.com\/pdfdrive\/wp-json\/wp\/v2\/tags?post=168"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}