{"id":88580,"date":"2025-06-01T07:15:14","date_gmt":"2025-06-01T07:15:14","guid":{"rendered":"https:\/\/exam.pscnotes.com\/mcq\/?p=88580"},"modified":"2025-06-01T07:15:14","modified_gmt":"2025-06-01T07:15:14","slug":"the-rivers-of-north-west-europe-are-good-examples-of","status":"publish","type":"post","link":"https:\/\/exam.pscnotes.com\/mcq\/the-rivers-of-north-west-europe-are-good-examples-of\/","title":{"rendered":"The rivers of North-West Europe are good examples of"},"content":{"rendered":"

The rivers of North-West Europe are good examples of<\/p>\n

[amp_mcq option1=”parallel pattern of drainage.” option2=”radial pattern of drainage.” option3=”barbed pattern of drainage.” option4=”trellis pattern of drainage.” correct=”option4″]<\/p>\n

\n
\n
This question was previously asked in<\/div>\n
UPSC NDA-2 – 2019<\/div>\n<\/div>\n
Download PDF<\/a>Attempt Online<\/a><\/div>\n<\/div>\n
\nThe trellis pattern of drainage is characteristic of regions with folded topography and alternating layers of resistant and less resistant rocks. Rivers flow along the strike of the less resistant rocks, and tributaries join at right angles, cutting across the resistant ridges. While North-West Europe has varied terrain, folded structures are present in some areas (e.g., parts of the Paris Basin, the Ardennes, parts of Germany bordering NW Europe), leading to the development of trellis drainage patterns in those regions.
\n<\/section>\n
\nDifferent drainage patterns (dendritic, trellis, radial, parallel, rectangular, barbed, etc.) develop depending on the underlying geological structure, topography, and rock type. Trellis drainage is strongly controlled by geological structure, specifically folded rocks.
\n<\/section>\n
\nDendritic pattern is the most common pattern and develops on uniform rock strata. Radial pattern develops around a central elevated point (like a volcano or dome). Parallel pattern occurs on uniformly sloping surfaces. Rectangular pattern is found in areas with jointed or faulted bedrock. Barbed pattern occurs when a tributary joins a main river in the opposite direction of the main river’s flow, often indicating river capture.
\n<\/section>\n","protected":false},"excerpt":{"rendered":"

The rivers of North-West Europe are good examples of [amp_mcq option1=”parallel pattern of drainage.” option2=”radial pattern of drainage.” option3=”barbed pattern of drainage.” option4=”trellis pattern of drainage.” correct=”option4″] This question was previously asked in UPSC NDA-2 – 2019 Download PDFAttempt Online The trellis pattern of drainage is characteristic of regions with folded topography and alternating layers … <\/p>\n

Detailed SolutionThe rivers of North-West Europe are good examples of<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1094],"tags":[1119,1307,1106],"class_list":["post-88580","post","type-post","status-publish","format-standard","hentry","category-upsc-nda-2","tag-1119","tag-rivers-of-the-world","tag-world-and-physical-geography","no-featured-image-padding"],"yoast_head":"\nThe rivers of North-West Europe are good examples of<\/title>\n<meta name=\"description\" content=\"The trellis pattern of drainage is characteristic of regions with folded topography and alternating layers of resistant and less resistant rocks. Rivers flow along the strike of the less resistant rocks, and tributaries join at right angles, cutting across the resistant ridges. While North-West Europe has varied terrain, folded structures are present in some areas (e.g., parts of the Paris Basin, the Ardennes, parts of Germany bordering NW Europe), leading to the development of trellis drainage patterns in those regions. Different drainage patterns (dendritic, trellis, radial, parallel, rectangular, barbed, etc.) develop depending on the underlying geological structure, topography, and rock type. Trellis drainage is strongly controlled by geological structure, specifically folded rocks.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/exam.pscnotes.com\/mcq\/the-rivers-of-north-west-europe-are-good-examples-of\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"The rivers of North-West Europe are good examples of\" \/>\n<meta property=\"og:description\" content=\"The trellis pattern of drainage is characteristic of regions with folded topography and alternating layers of resistant and less resistant rocks. Rivers flow along the strike of the less resistant rocks, and tributaries join at right angles, cutting across the resistant ridges. While North-West Europe has varied terrain, folded structures are present in some areas (e.g., parts of the Paris Basin, the Ardennes, parts of Germany bordering NW Europe), leading to the development of trellis drainage patterns in those regions. Different drainage patterns (dendritic, trellis, radial, parallel, rectangular, barbed, etc.) develop depending on the underlying geological structure, topography, and rock type. Trellis drainage is strongly controlled by geological structure, specifically folded rocks.\" \/>\n<meta property=\"og:url\" content=\"https:\/\/exam.pscnotes.com\/mcq\/the-rivers-of-north-west-europe-are-good-examples-of\/\" \/>\n<meta property=\"og:site_name\" content=\"MCQ and Quiz for Exams\" \/>\n<meta property=\"article:published_time\" content=\"2025-06-01T07:15:14+00:00\" \/>\n<meta name=\"author\" content=\"rawan239\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"rawan239\" \/>\n\t<meta name=\"twitter:label2\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"1 minute\" \/>\n<!-- \/ Yoast SEO Premium plugin. -->","yoast_head_json":{"title":"The rivers of North-West Europe are good examples of","description":"The trellis pattern of drainage is characteristic of regions with folded topography and alternating layers of resistant and less resistant rocks. 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Trellis drainage is strongly controlled by geological structure, specifically folded rocks.","og_url":"https:\/\/exam.pscnotes.com\/mcq\/the-rivers-of-north-west-europe-are-good-examples-of\/","og_site_name":"MCQ and Quiz for Exams","article_published_time":"2025-06-01T07:15:14+00:00","author":"rawan239","twitter_card":"summary_large_image","twitter_misc":{"Written by":"rawan239","Est. reading time":"1 minute"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/exam.pscnotes.com\/mcq\/the-rivers-of-north-west-europe-are-good-examples-of\/","url":"https:\/\/exam.pscnotes.com\/mcq\/the-rivers-of-north-west-europe-are-good-examples-of\/","name":"The rivers of North-West Europe are good examples of","isPartOf":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/#website"},"datePublished":"2025-06-01T07:15:14+00:00","dateModified":"2025-06-01T07:15:14+00:00","author":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/#\/schema\/person\/5807dafeb27d2ec82344d6cbd6c3d209"},"description":"The trellis pattern of drainage is characteristic of regions with folded topography and alternating layers of resistant and less resistant rocks. 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