{"id":90419,"date":"2025-06-01T10:28:15","date_gmt":"2025-06-01T10:28:15","guid":{"rendered":"https:\/\/exam.pscnotes.com\/mcq\/?p=90419"},"modified":"2025-06-01T10:28:15","modified_gmt":"2025-06-01T10:28:15","slug":"the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid","status":"publish","type":"post","link":"https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/","title":{"rendered":"The gently sloping accumulation of coarse alluvium deposits by a braid"},"content":{"rendered":"

The gently sloping accumulation of coarse alluvium deposits by a braided stream is known as<\/p>\n

[amp_mcq option1=”sand bar” option2=”alluvial fan” option3=”bajada” option4=”diaras” correct=”option2″]<\/p>\n

\n
\n
This question was previously asked in<\/div>\n
UPSC CAPF – 2019<\/div>\n<\/div>\n
Download PDF<\/a>Attempt Online<\/a><\/div>\n<\/div>\n
\nThe correct answer is B) alluvial fan. A gently sloping accumulation of coarse alluvium deposited by a stream, especially where it exits a confined area (like a mountain valley) onto a flatter plain, is known as an alluvial fan. Braided streams, due to their high sediment load and variable discharge, are commonly associated with the formation of alluvial fans, particularly in arid or semi-arid environments or areas with high sediment supply.
\n<\/section>\n
\n– Alluvial fans are triangular or cone-shaped depositional landforms created by streams.
\n– They form where a stream undergoes a decrease in gradient and\/or velocity, leading to the deposition of its sediment load.
\n– Braided streams are often the type of channel found on the surface of alluvial fans, as they are effective transporters and depositors of coarse sediment.
\n– The deposits typically consist of sand, gravel, and larger clasts (coarse alluvium).
\n<\/section>\n
\nWhile a braided stream can deposit material in other forms (like sandbars within channels or extensive alluvial plains), the description “gently sloping accumulation” points towards a large, widespread landform, and among the given options, ‘alluvial fan’ best fits the description of a significant depositional feature composed of coarse alluvium deposited by a stream, often braided, losing energy.
\n<\/section>\n","protected":false},"excerpt":{"rendered":"

The gently sloping accumulation of coarse alluvium deposits by a braided stream is known as [amp_mcq option1=”sand bar” option2=”alluvial fan” option3=”bajada” option4=”diaras” correct=”option2″] This question was previously asked in UPSC CAPF – 2019 Download PDFAttempt Online The correct answer is B) alluvial fan. A gently sloping accumulation of coarse alluvium deposited by a stream, especially … <\/p>\n

Detailed SolutionThe gently sloping accumulation of coarse alluvium deposits by a braid<\/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":[1085],"tags":[1119,1240,1106],"class_list":["post-90419","post","type-post","status-publish","format-standard","hentry","category-upsc-capf","tag-1119","tag-landforms-by-river","tag-world-and-physical-geography","no-featured-image-padding"],"yoast_head":"\nThe gently sloping accumulation of coarse alluvium deposits by a braid<\/title>\n<meta name=\"description\" content=\"The correct answer is B) alluvial fan. A gently sloping accumulation of coarse alluvium deposited by a stream, especially where it exits a confined area (like a mountain valley) onto a flatter plain, is known as an alluvial fan. Braided streams, due to their high sediment load and variable discharge, are commonly associated with the formation of alluvial fans, particularly in arid or semi-arid environments or areas with high sediment supply. - Alluvial fans are triangular or cone-shaped depositional landforms created by streams. - They form where a stream undergoes a decrease in gradient and\/or velocity, leading to the deposition of its sediment load. - Braided streams are often the type of channel found on the surface of alluvial fans, as they are effective transporters and depositors of coarse sediment. - The deposits typically consist of sand, gravel, and larger clasts (coarse alluvium).\" \/>\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-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"The gently sloping accumulation of coarse alluvium deposits by a braid\" \/>\n<meta property=\"og:description\" content=\"The correct answer is B) alluvial fan. A gently sloping accumulation of coarse alluvium deposited by a stream, especially where it exits a confined area (like a mountain valley) onto a flatter plain, is known as an alluvial fan. Braided streams, due to their high sediment load and variable discharge, are commonly associated with the formation of alluvial fans, particularly in arid or semi-arid environments or areas with high sediment supply. - Alluvial fans are triangular or cone-shaped depositional landforms created by streams. - They form where a stream undergoes a decrease in gradient and\/or velocity, leading to the deposition of its sediment load. - Braided streams are often the type of channel found on the surface of alluvial fans, as they are effective transporters and depositors of coarse sediment. - The deposits typically consist of sand, gravel, and larger clasts (coarse alluvium).\" \/>\n<meta property=\"og:url\" content=\"https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/\" \/>\n<meta property=\"og:site_name\" content=\"MCQ and Quiz for Exams\" \/>\n<meta property=\"article:published_time\" content=\"2025-06-01T10:28:15+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 gently sloping accumulation of coarse alluvium deposits by a braid","description":"The correct answer is B) alluvial fan. A gently sloping accumulation of coarse alluvium deposited by a stream, especially where it exits a confined area (like a mountain valley) onto a flatter plain, is known as an alluvial fan. Braided streams, due to their high sediment load and variable discharge, are commonly associated with the formation of alluvial fans, particularly in arid or semi-arid environments or areas with high sediment supply. - Alluvial fans are triangular or cone-shaped depositional landforms created by streams. - They form where a stream undergoes a decrease in gradient and\/or velocity, leading to the deposition of its sediment load. - Braided streams are often the type of channel found on the surface of alluvial fans, as they are effective transporters and depositors of coarse sediment. - The deposits typically consist of sand, gravel, and larger clasts (coarse alluvium).","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/","og_locale":"en_US","og_type":"article","og_title":"The gently sloping accumulation of coarse alluvium deposits by a braid","og_description":"The correct answer is B) alluvial fan. A gently sloping accumulation of coarse alluvium deposited by a stream, especially where it exits a confined area (like a mountain valley) onto a flatter plain, is known as an alluvial fan. Braided streams, due to their high sediment load and variable discharge, are commonly associated with the formation of alluvial fans, particularly in arid or semi-arid environments or areas with high sediment supply. - Alluvial fans are triangular or cone-shaped depositional landforms created by streams. - They form where a stream undergoes a decrease in gradient and\/or velocity, leading to the deposition of its sediment load. - Braided streams are often the type of channel found on the surface of alluvial fans, as they are effective transporters and depositors of coarse sediment. - The deposits typically consist of sand, gravel, and larger clasts (coarse alluvium).","og_url":"https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/","og_site_name":"MCQ and Quiz for Exams","article_published_time":"2025-06-01T10:28:15+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-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/","url":"https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/","name":"The gently sloping accumulation of coarse alluvium deposits by a braid","isPartOf":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/#website"},"datePublished":"2025-06-01T10:28:15+00:00","dateModified":"2025-06-01T10:28:15+00:00","author":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/#\/schema\/person\/5807dafeb27d2ec82344d6cbd6c3d209"},"description":"The correct answer is B) alluvial fan. A gently sloping accumulation of coarse alluvium deposited by a stream, especially where it exits a confined area (like a mountain valley) onto a flatter plain, is known as an alluvial fan. Braided streams, due to their high sediment load and variable discharge, are commonly associated with the formation of alluvial fans, particularly in arid or semi-arid environments or areas with high sediment supply. - Alluvial fans are triangular or cone-shaped depositional landforms created by streams. - They form where a stream undergoes a decrease in gradient and\/or velocity, leading to the deposition of its sediment load. - Braided streams are often the type of channel found on the surface of alluvial fans, as they are effective transporters and depositors of coarse sediment. - The deposits typically consist of sand, gravel, and larger clasts (coarse alluvium).","breadcrumb":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":["https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/exam.pscnotes.com\/mcq\/the-gently-sloping-accumulation-of-coarse-alluvium-deposits-by-a-braid\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/exam.pscnotes.com\/mcq\/"},{"@type":"ListItem","position":2,"name":"UPSC CAPF","item":"https:\/\/exam.pscnotes.com\/mcq\/category\/upsc-capf\/"},{"@type":"ListItem","position":3,"name":"The gently sloping accumulation of coarse alluvium deposits by a braid"}]},{"@type":"WebSite","@id":"https:\/\/exam.pscnotes.com\/mcq\/#website","url":"https:\/\/exam.pscnotes.com\/mcq\/","name":"MCQ and Quiz for Exams","description":"","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/exam.pscnotes.com\/mcq\/?s={search_term_string}"},"query-input":"required name=search_term_string"}],"inLanguage":"en-US"},{"@type":"Person","@id":"https:\/\/exam.pscnotes.com\/mcq\/#\/schema\/person\/5807dafeb27d2ec82344d6cbd6c3d209","name":"rawan239","image":{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/exam.pscnotes.com\/mcq\/#\/schema\/person\/image\/","url":"https:\/\/secure.gravatar.com\/avatar\/761a7274f9cce048fa5b921221e7934820d74514df93ef195a9d22af0c1c9001?s=96&d=mm&r=g","contentUrl":"https:\/\/secure.gravatar.com\/avatar\/761a7274f9cce048fa5b921221e7934820d74514df93ef195a9d22af0c1c9001?s=96&d=mm&r=g","caption":"rawan239"},"sameAs":["https:\/\/exam.pscnotes.com"],"url":"https:\/\/exam.pscnotes.com\/mcq\/author\/rawan239\/"}]}},"amp_enabled":true,"_links":{"self":[{"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/posts\/90419","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/comments?post=90419"}],"version-history":[{"count":0,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/posts\/90419\/revisions"}],"wp:attachment":[{"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/media?parent=90419"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/categories?post=90419"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/tags?post=90419"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}