{"id":34230,"date":"2022-04-13T07:57:06","date_gmt":"2022-04-13T07:57:06","guid":{"rendered":"https:\/\/wordpress.org\/patterns\/pattern\/picolumn-sv_se\/"},"modified":"2026-04-19T17:29:42","modified_gmt":"2026-04-19T17:29:42","slug":"picolumn-sv_se","status":"publish","type":"wporg-pattern","link":"https:\/\/wordpress.org\/patterns\/pattern\/picolumn-sv_se\/","title":{"rendered":"Picolumn"},"content":{"rendered":"\n<div class=\"wp-block-cover is-light has-custom-content-position is-position-bottom-center wp-duotone-000000-ffffff-1\"><span aria-hidden=\"true\" class=\"wp-block-cover__background has-background-dim\"><\/span><img decoding=\"async\" class=\"wp-block-cover__image-background\" alt=\"\" src=\"https:\/\/img.rawpixel.com\/s3fs-private\/rawpixel_images\/website_content\/a010-markusspiske-jan19-msp_0709_8832.jpg?w=1200&amp;h=1200&amp;fit=clip&amp;crop=default&amp;dpr=1&amp;q=75&amp;vib=3&amp;con=3&amp;usm=15&amp;cs=srgb&amp;bg=F4F4F3&amp;ixlib=js-2.2.1&amp;s=81b80c4b527f7afa9ceed195f02d27f3\" data-object-fit=\"cover\" \/><div class=\"wp-block-cover__inner-container is-layout-flow wp-block-cover-is-layout-flow\">\n<p class=\"has-text-align-center has-large-font-size wp-block-paragraph\">Mountain nature scene<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-0e47273b wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:50%\">\n<p class=\"wp-block-paragraph\">A\u00a0<strong>mountain<\/strong>\u00a0is an elevated portion of the\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Earth%27s_crust\">Earth&#8217;s crust<\/a>, generally with steep sides that show significant exposed\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Bedrock\">bedrock<\/a>. A mountain differs from a\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Plateau\">plateau<\/a>\u00a0in having a limited summit area, and is larger than a\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Hill\">hill<\/a>, typically rising at least 300 metres (1000 feet) above the surrounding land. A few mountains are isolated\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Summit_(topography)\">summits<\/a>, but most occur in\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain_range\">mountain ranges<\/a>.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:50%\">\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain_formation\">Mountains are formed<\/a>\u00a0through\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Tectonic_plate\">tectonic forces<\/a>,\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Erosion\">erosion<\/a>, or\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Volcanism\">volcanism<\/a>,\u00a0which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Weathering\">weathering<\/a>, through\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Slump_(geology)\">slumping<\/a>\u00a0and other forms of\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mass_wasting\">mass wasting<\/a>, as well as through\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Erosion\">erosion<\/a>\u00a0by\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/River\">rivers<\/a>\u00a0and\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Glacier\">glaciers<\/a>.<\/p>\n<\/div>\n<\/div>\n","protected":false},"author":490262,"parent":23803,"template":"","meta":{"_crdt_document":"","jetpack_post_was_ever_published":false,"wpop_keywords":"","wpop_description":"Hero-bild med gr\u00e5skalefilter och 2 kolumner.","wpop_viewport_width":800,"wpop_block_types":[""],"wpop_locale":"sv_SE","wpop_wp_version":"","wpop_contains_block_types":"core\/column,core\/columns,core\/cover,core\/paragraph","footnotes":""},"pattern-categories":[3,13,6],"pattern-keywords":[],"wporg-pattern-flag-reason":[],"class_list":["post-34230","wporg-pattern","type-wporg-pattern","status-publish","hentry","wporg-pattern-category-columns","wporg-pattern-category-images","wporg-pattern-category-text"],"category_slugs":["columns","images","text"],"keyword_slugs":[],"pattern_content":"<!-- wp:cover {\"url\":\"https:\/\/img.rawpixel.com\/s3fs-private\/rawpixel_images\/website_content\/a010-markusspiske-jan19-msp_0709_8832.jpg?w=1200&h=1200&fit=clip&crop=default&dpr=1&q=75&vib=3&con=3&usm=15&cs=srgb&bg=F4F4F3&ixlib=js-2.2.1&s=81b80c4b527f7afa9ceed195f02d27f3\",\"id\":null,\"dimRatio\":50,\"contentPosition\":\"bottom center\",\"isDark\":false,\"style\":{\"color\":{\"duotone\":[\"#000000\",\"#ffffff\"]}}} -->\n<div class=\"wp-block-cover is-light has-custom-content-position is-position-bottom-center\"><span aria-hidden=\"true\" class=\"wp-block-cover__background has-background-dim\"><\/span><img class=\"wp-block-cover__image-background\" alt=\"\" src=\"https:\/\/img.rawpixel.com\/s3fs-private\/rawpixel_images\/website_content\/a010-markusspiske-jan19-msp_0709_8832.jpg?w=1200&amp;h=1200&amp;fit=clip&amp;crop=default&amp;dpr=1&amp;q=75&amp;vib=3&amp;con=3&amp;usm=15&amp;cs=srgb&amp;bg=F4F4F3&amp;ixlib=js-2.2.1&amp;s=81b80c4b527f7afa9ceed195f02d27f3\" data-object-fit=\"cover\" \/><div class=\"wp-block-cover__inner-container\"><!-- wp:paragraph {\"align\":\"center\",\"fontSize\":\"large\"} -->\n<p class=\"has-text-align-center has-large-font-size\">Mountain nature scene<\/p>\n<!-- \/wp:paragraph --><\/div><\/div>\n<!-- \/wp:cover -->\n\n<!-- wp:columns -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"50%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:50%\"><!-- wp:paragraph -->\n<p>A\u00a0<strong>mountain<\/strong>\u00a0is an elevated portion of the\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Earth%27s_crust\">Earth's crust<\/a>, generally with steep sides that show significant exposed\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Bedrock\">bedrock<\/a>. A mountain differs from a\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Plateau\">plateau<\/a>\u00a0in having a limited summit area, and is larger than a\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Hill\">hill<\/a>, typically rising at least 300 metres (1000 feet) above the surrounding land. A few mountains are isolated\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Summit_(topography)\">summits<\/a>, but most occur in\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain_range\">mountain ranges<\/a>.<\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"50%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:50%\"><!-- wp:paragraph -->\n<p><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain_formation\">Mountains are formed<\/a>\u00a0through\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Tectonic_plate\">tectonic forces<\/a>,\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Erosion\">erosion<\/a>, or\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Volcanism\">volcanism<\/a>,\u00a0which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Weathering\">weathering<\/a>, through\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Slump_(geology)\">slumping<\/a>\u00a0and other forms of\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mass_wasting\">mass wasting<\/a>, as well as through\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Erosion\">erosion<\/a>\u00a0by\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/River\">rivers<\/a>\u00a0and\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Glacier\">glaciers<\/a>.<\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->","favorite_count":0,"author_meta":{"name":"Hamed Takmil","url":"https:\/\/wordpress.org\/patterns\/author\/silvercover","avatar":"https:\/\/secure.gravatar.com\/avatar\/786c7089f33aadcb93ed5cde643b3b7b7f1bab509acc2ab5dc9d476321041056?s=64&d=mm&r=g"},"unlisted_reason":[],"jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/wporg-pattern\/34230","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/wporg-pattern"}],"about":[{"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/types\/wporg-pattern"}],"version-history":[{"count":1,"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/wporg-pattern\/34230\/revisions"}],"predecessor-version":[{"id":34945,"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/wporg-pattern\/34230\/revisions\/34945"}],"author":[{"embeddable":true,"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wporg\/v1\/users\/silvercover"}],"wp:attachment":[{"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/media?parent=34230"}],"wp:term":[{"taxonomy":"wporg-pattern-category","embeddable":true,"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/pattern-categories?post=34230"},{"taxonomy":"wporg-pattern-keyword","embeddable":true,"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/pattern-keywords?post=34230"},{"taxonomy":"wporg-pattern-flag-reason","embeddable":true,"href":"https:\/\/wordpress.org\/patterns\/wp-json\/wp\/v2\/wporg-pattern-flag-reason?post=34230"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}