{"id":85268,"date":"2025-06-01T03:10:33","date_gmt":"2025-06-01T03:10:33","guid":{"rendered":"https:\/\/exam.pscnotes.com\/mcq\/?p=85268"},"modified":"2025-06-01T03:10:33","modified_gmt":"2025-06-01T03:10:33","slug":"individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l","status":"publish","type":"post","link":"https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/","title":{"rendered":"Individual lava flows are normally only a few feet thick, but over a l"},"content":{"rendered":"<p>Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano. Such volcanoes are termed as :<\/p>\n<p>[amp_mcq option1=&#8221;Shield volcano&#8221; option2=&#8221;Composite volcano&#8221; option3=&#8221;Strato-volcano&#8221; option4=&#8221;Cinder-cone volcano&#8221; correct=&#8221;option1&#8243;]<\/p>\n<div class=\"psc-box-pyq-exam-year-detail\">\n<div class=\"pyq-exam\">\n<div class=\"psc-heading\">This question was previously asked in<\/div>\n<div class=\"psc-title line-ellipsis\">UPSC CDS-1 &#8211; 2022<\/div>\n<\/div>\n<div class=\"pyq-exam-psc-buttons\"><a href=\"\/pyq\/pyq-upsc-cds-1-2022.pdf\" target=\"_blank\" class=\"psc-pdf-button\" rel=\"noopener\">Download PDF<\/a><a href=\"\/pyq-upsc-cds-1-2022\" target=\"_blank\" class=\"psc-attempt-button\" rel=\"noopener\">Attempt Online<\/a><\/div>\n<\/div>\n<section id=\"pyq-correct-answer\">\nSuch volcanoes are termed as Shield volcano.<br \/>\n<\/section>\n<section id=\"pyq-key-points\">\nThe description &#8220;Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano&#8221; and the implied shape resulting from such flows points to a shield volcano. Shield volcanoes are formed by effusive eruptions of low-viscosity basaltic lava that spreads out thinly and widely, building a broad, gently sloping cone resembling a warrior&#8217;s shield.<br \/>\n<\/section>\n<section id=\"pyq-additional-information\">\nComposite volcanoes (or stratovolcanoes) are built from alternating layers of viscous lava, ash, and volcanic debris, resulting in steeper, conical shapes and often explosive eruptions. Cinder-cone volcanoes are the simplest type, formed by loose pyroclastic material (cinders) ejected from a single vent, resulting in steep slopes but relatively small size.<br \/>\n<\/section>\n","protected":false},"excerpt":{"rendered":"<p>Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano. Such volcanoes are termed as : [amp_mcq option1=&#8221;Shield volcano&#8221; option2=&#8221;Composite volcano&#8221; option3=&#8221;Strato-volcano&#8221; option4=&#8221;Cinder-cone volcano&#8221; correct=&#8221;option1&#8243;] This question was previously asked in UPSC CDS-1 &#8211; 2022 Download PDFAttempt Online Such volcanoes are &#8230; <\/p>\n<p class=\"read-more-container\"><a title=\"Individual lava flows are normally only a few feet thick, but over a l\" class=\"read-more button\" href=\"https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/#more-85268\">Detailed Solution<span class=\"screen-reader-text\">Individual lava flows are normally only a few feet thick, but over a l<\/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":[1087],"tags":[1108,1209,1106],"class_list":["post-85268","post","type-post","status-publish","format-standard","hentry","category-upsc-cds-1","tag-1108","tag-volcano","tag-world-and-physical-geography","no-featured-image-padding"],"yoast_head":"<!-- This site is optimized with the Yoast SEO Premium plugin v22.2 (Yoast SEO v23.3) - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Individual lava flows are normally only a few feet thick, but over a l<\/title>\n<meta name=\"description\" content=\"Such volcanoes are termed as Shield volcano. The description &quot;Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano&quot; and the implied shape resulting from such flows points to a shield volcano. Shield volcanoes are formed by effusive eruptions of low-viscosity basaltic lava that spreads out thinly and widely, building a broad, gently sloping cone resembling a warrior&#039;s shield.\" \/>\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\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Individual lava flows are normally only a few feet thick, but over a l\" \/>\n<meta property=\"og:description\" content=\"Such volcanoes are termed as Shield volcano. The description &quot;Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano&quot; and the implied shape resulting from such flows points to a shield volcano. Shield volcanoes are formed by effusive eruptions of low-viscosity basaltic lava that spreads out thinly and widely, building a broad, gently sloping cone resembling a warrior&#039;s shield.\" \/>\n<meta property=\"og:url\" content=\"https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/\" \/>\n<meta property=\"og:site_name\" content=\"MCQ and Quiz for Exams\" \/>\n<meta property=\"article:published_time\" content=\"2025-06-01T03:10:33+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":"Individual lava flows are normally only a few feet thick, but over a l","description":"Such volcanoes are termed as Shield volcano. The description \"Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano\" and the implied shape resulting from such flows points to a shield volcano. Shield volcanoes are formed by effusive eruptions of low-viscosity basaltic lava that spreads out thinly and widely, building a broad, gently sloping cone resembling a warrior's shield.","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\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/","og_locale":"en_US","og_type":"article","og_title":"Individual lava flows are normally only a few feet thick, but over a l","og_description":"Such volcanoes are termed as Shield volcano. The description \"Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano\" and the implied shape resulting from such flows points to a shield volcano. Shield volcanoes are formed by effusive eruptions of low-viscosity basaltic lava that spreads out thinly and widely, building a broad, gently sloping cone resembling a warrior's shield.","og_url":"https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/","og_site_name":"MCQ and Quiz for Exams","article_published_time":"2025-06-01T03:10:33+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\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/","url":"https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/","name":"Individual lava flows are normally only a few feet thick, but over a l","isPartOf":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/#website"},"datePublished":"2025-06-01T03:10:33+00:00","dateModified":"2025-06-01T03:10:33+00:00","author":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/#\/schema\/person\/5807dafeb27d2ec82344d6cbd6c3d209"},"description":"Such volcanoes are termed as Shield volcano. The description \"Individual lava flows are normally only a few feet thick, but over a long period of time, repeated flows may build up a volcano\" and the implied shape resulting from such flows points to a shield volcano. Shield volcanoes are formed by effusive eruptions of low-viscosity basaltic lava that spreads out thinly and widely, building a broad, gently sloping cone resembling a warrior's shield.","breadcrumb":{"@id":"https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":["https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/exam.pscnotes.com\/mcq\/individual-lava-flows-are-normally-only-a-few-feet-thick-but-over-a-l\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/exam.pscnotes.com\/mcq\/"},{"@type":"ListItem","position":2,"name":"UPSC CDS-1","item":"https:\/\/exam.pscnotes.com\/mcq\/category\/upsc-cds-1\/"},{"@type":"ListItem","position":3,"name":"Individual lava flows are normally only a few feet thick, but over a l"}]},{"@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\/85268","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=85268"}],"version-history":[{"count":0,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/posts\/85268\/revisions"}],"wp:attachment":[{"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/media?parent=85268"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/categories?post=85268"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/exam.pscnotes.com\/mcq\/wp-json\/wp\/v2\/tags?post=85268"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}