{"id":15654,"date":"2018-10-23T15:27:41","date_gmt":"2018-10-23T13:27:41","guid":{"rendered":"https:\/\/npolar.no\/?page_id=15654"},"modified":"2023-01-23T23:57:09","modified_gmt":"2023-01-23T22:57:09","slug":"geology-of-antarctica","status":"publish","type":"page","link":"https:\/\/npolar.no\/en\/themes\/geology-of-antarctica\/","title":{"rendered":"Geology of Antarctica"},"content":{"rendered":"\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4o0uzq-6c818ce4b48cac84aa493264daa48212\">\n.flex_column.av-4o0uzq-6c818ce4b48cac84aa493264daa48212{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div  class='flex_column av-4o0uzq-6c818ce4b48cac84aa493264daa48212 av_two_third  avia-builder-el-0  el_before_av_one_third  avia-builder-el-first  first flex_column_div av-zero-column-padding  '     ><section  class='av_textblock_section av-5o3ccgi-7c7f0989b331597600cba6e70b7b1f9b '   itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><p>Most of Antarctica is covered by ice, but where mountains breach the ice, exposures are completely free of vegetation. This gives geologists a unique opportunity to study how the rocks were formed in relation to the various geological processes that have taken place in the Earth\u2019s crust. Geophysical techniques have recently begun to be employed to acquire information about the bedrock beneath the ice.<\/p>\n<\/div><\/section><\/div>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2u46bq-b8a6ad5623015222b28bba9072157b83\">\n.flex_column.av-2u46bq-b8a6ad5623015222b28bba9072157b83{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div  class='flex_column av-2u46bq-b8a6ad5623015222b28bba9072157b83 av_one_third  avia-builder-el-2  el_after_av_two_third  el_before_av_masonry_gallery  avia-builder-el-last  flex_column_div av-zero-column-padding  '     ><section class=\"av_textblock_section\"  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div role='complementary' class='avia_textblock NP-factsheet-enfold no '  style=' '  itemprop=\"text\" ><p class='title'>Related pages<\/p><div class='hsep-relevantlinks' ><\/div><div class='NP-factsheet-content'><p><a href=\"https:\/\/npolar.no\/en\/themes\/jan-mayen\/#geology\">The geology of Jan&nbsp; Mayen<\/a><\/p>\n<p><a href=\"https:\/\/npolar.no\/en\/themes\/bouvetoya\/#geology\">The geology of Bouvet\u00f8ya<\/a><\/p>\n<p><a href=\"https:\/\/npolar.no\/en\/themes\/the-geology-of-svalbard\/\">The geology&nbsp; of Svalbard<\/a><\/p>\n<\/div><\/div><div tabindex='0' role='button' class=' NP-factToggle' style='text-align:center;'><i class='fas fa-angle-down fa-2x'><\/i><\/div><\/section><\/div>\n<div id='av-masonry-1' class='av-masonry av-jmklisgb-f98e995f2741dcf01b796f4a43a76dcd noHover av-fixed-size av-no-gap av-hover-overlay- av-masonry-animation-active av-masonry-col-5 av-caption-on-hover av-caption-style- av-masonry-gallery ' data-post_id=\"15654\"><div class=\"av-masonry-container isotope av-js-disabled\"><div class='av-masonry-entry isotope-item av-masonry-item-no-image '><\/div><a href=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP009358-hoggstabben.jpg\" data-srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP009358-hoggstabben.jpg 600w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP009358-hoggstabben-450x290.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP009358-hoggstabben-300x193.jpg 300w\" data-sizes=\"(max-width: 600px) 100vw, 600px\"  aria-label=\"image Antarktis\"  id='av-masonry-1-item-14772' data-av-masonry-item='14772' class='av-masonry-entry isotope-item post-14772 attachment type-attachment status-inherit hentry  av-masonry-item-with-image av-grid-img' title=\"Antarktis\" alt=\"Fjell i sne\"    itemprop=\"thumbnailUrl\" ><div class='av-inner-masonry-sizer'><\/div><figure class='av-inner-masonry main_color'><div class=\"av-masonry-outerimage-container\"><div class='av-masonry-image-container' style=\"background-image: url(https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP009358-hoggstabben.jpg);\"  title=\"Antarktis\" ><\/div><\/div><figcaption class='av-inner-masonry-content site-background'><div class='av-inner-masonry-content-pos'><div class='av-inner-masonry-content-pos-content'><div class='avia-arrow'><\/div><h3 class='av-masonry-entry-title entry-title '  itemprop=\"headline\" >Antarktis<\/h3><\/div><\/div><\/figcaption><\/figure><\/a><!--end av-masonry entry--><a href=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget.jpg\" data-srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget.jpg 516w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-450x698.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-194x300.jpg 194w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-455x705.jpg 455w\" data-sizes=\"(max-width: 516px) 100vw, 516px\"  aria-label=\"image Antarktis\"  id='av-masonry-1-item-14774' data-av-masonry-item='14774' class='av-masonry-entry isotope-item post-14774 attachment type-attachment status-inherit hentry  av-masonry-item-with-image av-grid-img' title=\"Antarktis\" alt=\"To persomer foran steinvegg\"    itemprop=\"thumbnailUrl\" ><div class='av-inner-masonry-sizer'><\/div><figure class='av-inner-masonry main_color'><div class=\"av-masonry-outerimage-container\"><div class='av-masonry-image-container' style=\"background-image: url(https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-455x705.jpg);\"  title=\"Antarktis\" ><\/div><\/div><figcaption class='av-inner-masonry-content site-background'><div class='av-inner-masonry-content-pos'><div class='av-inner-masonry-content-pos-content'><div class='avia-arrow'><\/div><h3 class='av-masonry-entry-title entry-title '  itemprop=\"headline\" >Antarktis<\/h3><\/div><\/div><\/figcaption><\/figure><\/a><!--end av-masonry entry--><a href=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056102.jpg\" data-srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056102.jpg 542w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056102-450x664.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056102-203x300.jpg 203w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056102-478x705.jpg 478w\" data-sizes=\"(max-width: 542px) 100vw, 542px\"  aria-label=\"image NP056102\"  id='av-masonry-1-item-14776' data-av-masonry-item='14776' class='av-masonry-entry isotope-item post-14776 attachment type-attachment status-inherit hentry  av-masonry-item-with-image av-grid-img' title=\"NP056102\" alt=\"H\u00f8y steinformasjon\"    itemprop=\"thumbnailUrl\" ><div class='av-inner-masonry-sizer'><\/div><figure class='av-inner-masonry main_color'><div class=\"av-masonry-outerimage-container\"><div class='av-masonry-image-container' style=\"background-image: url(https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056102-478x705.jpg);\"  title=\"NP056102\" ><\/div><\/div><figcaption class='av-inner-masonry-content site-background'><div class='av-inner-masonry-content-pos'><div class='av-inner-masonry-content-pos-content'><div class='avia-arrow'><\/div><h3 class='av-masonry-entry-title entry-title '  itemprop=\"headline\" >NP056102<\/h3><\/div><\/div><\/figcaption><\/figure><\/a><!--end av-masonry entry--><a href=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056103.jpg\" data-srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056103.jpg 600w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056103-450x290.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056103-300x193.jpg 300w\" data-sizes=\"(max-width: 600px) 100vw, 600px\"  aria-label=\"image Antarktis\"  id='av-masonry-1-item-14778' data-av-masonry-item='14778' class='av-masonry-entry isotope-item post-14778 attachment type-attachment status-inherit hentry  av-masonry-item-with-image av-grid-img' title=\"Antarktis\" alt=\"Fjell som stikker opp av sne\"    itemprop=\"thumbnailUrl\" ><div class='av-inner-masonry-sizer'><\/div><figure class='av-inner-masonry main_color'><div class=\"av-masonry-outerimage-container\"><div class='av-masonry-image-container' style=\"background-image: url(https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056103.jpg);\"  title=\"Antarktis\" ><\/div><\/div><figcaption class='av-inner-masonry-content site-background'><div class='av-inner-masonry-content-pos'><div class='av-inner-masonry-content-pos-content'><div class='avia-arrow'><\/div><h3 class='av-masonry-entry-title entry-title '  itemprop=\"headline\" >Antarktis<\/h3><\/div><\/div><\/figcaption><\/figure><\/a><!--end av-masonry entry--><a href=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056104-trollslottet.jpg\" data-srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056104-trollslottet.jpg 600w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056104-trollslottet-450x299.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056104-trollslottet-300x200.jpg 300w\" data-sizes=\"(max-width: 600px) 100vw, 600px\"  aria-label=\"image NP056104-trollslottet\"  id='av-masonry-1-item-14780' data-av-masonry-item='14780' class='av-masonry-entry isotope-item post-14780 attachment type-attachment status-inherit hentry  av-masonry-item-with-image av-grid-img' title=\"NP056104-trollslottet\" alt=\"Gr\u00e5e steinmasser\"    itemprop=\"thumbnailUrl\" ><div class='av-inner-masonry-sizer'><\/div><figure class='av-inner-masonry main_color'><div class=\"av-masonry-outerimage-container\"><div class='av-masonry-image-container' style=\"background-image: url(https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP056104-trollslottet.jpg);\"  title=\"NP056104-trollslottet\" ><\/div><\/div><figcaption class='av-inner-masonry-content site-background'><div class='av-inner-masonry-content-pos'><div class='av-inner-masonry-content-pos-content'><div class='avia-arrow'><\/div><h3 class='av-masonry-entry-title entry-title '  itemprop=\"headline\" >NP056104-trollslottet<\/h3><\/div><\/div><\/figcaption><\/figure><\/a><!--end av-masonry entry--><\/div><\/div>\n<section  class='av_textblock_section av-jmkm3cng-276125966bd5468e4b0826c09bd60da3 '   itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><h2 class=\"heading--section-title\">Geology of Dronning Maud Land<\/h2>\n<p>Dronning Maud Land comprises nearly 1\/6 of the Antarctic continent. A mountain chain runs parallel to the coast, about 100-200 km from the ice edge. The geology of Dronning Maud Land has been mapped and described by Norwegian, German, South African, Japanese, Indian and Russian geologists in the last few decades. The mountains in Dronning Maud Land reveal a deeply eroded section through an approximately 500-600 million-year-old mountain range.<\/p>\n<p>At that time, Dronning Maud Land bordered up to Africa, Madagascar, Sri Lanka and India, and was part of the vast&nbsp;<span class='NP-tooltip  '\n    data-tippy='<strong>Gondwana<\/strong> was an&nbsp;ancient supercontinent that incorporated present-day&nbsp;present-day Arabia, Africa, South America, Antarctica, Australia, and India.&nbsp;It was fully assembled by Late&nbsp;Precambrian&nbsp;time, some 600 million years ago.'\n    data-tippy-arrow='true'\n    data-tippy-delay='[null,400]'\n    data-tippy-interactive='true'\n    data-tippy-trigger='mouseenter focus click'\n    >Gondwana<sup class='NP-tooltipmark'>?<\/sup><\/span> supercontinent. This primeval continent comprised Antarctica, Africa, India, Australia and South America. Gondwana began to break up 200 million years ago and some parts, like Africa and India, began drifting northwards towards their present location.<\/p>\n<p>The bedrock of Dronning Maud Land is dominated by <span class='NP-tooltip  '\n    data-tippy='Precambrium is the time span&nbsp;from the formation of Earth about 4.6 billion years ago to the beginning of the Cambrian Period, about 542 million years ago.'\n    data-tippy-arrow='true'\n    data-tippy-delay='[null,400]'\n    data-tippy-interactive='true'\n    data-tippy-trigger='mouseenter focus click'\n    >Precambrium<sup class='NP-tooltipmark'>?<\/sup><\/span> rocks that originated some 1200-1000 million years ago, before the formation of Gondwana. These rocks, which are of <span class='NP-tooltip  '\n    data-tippy='Magma is hot;fluid or semi-fluid material below or within the earth\u2019s crust.'\n    data-tippy-arrow='true'\n    data-tippy-delay='[null,400]'\n    data-tippy-interactive='true'\n    data-tippy-trigger='mouseenter focus click'\n    >magmatic<sup class='NP-tooltipmark'>?<\/sup><\/span> or sedimentary origin, occur as gneiss (ortho- and paragneiss), migmatite, calc-silicate rocks and amphibolite. The bedrock experienced a new episode of deformation, high-temperature transformation (metamorphism) and partial melting during the Pan-African <span class='NP-tooltip  '\n    data-tippy='Pan-African orogeny was a series of major Neoproterozoic orogenic events (mountain building) which related to the formation of the supercontinents Gondwana about 500-600 million years ago.'\n    data-tippy-arrow='true'\n    data-tippy-delay='[null,400]'\n    data-tippy-interactive='true'\n    data-tippy-trigger='mouseenter focus click'\n    >orogeny<sup class='NP-tooltipmark'>?<\/sup><\/span>. Detailed analyses of mineral assemblages and compositions show that the metamorphism took place at temperatures of 700-850\u00b0C and pressures corresponding to a crustal depth of 25-30 km.<\/p>\n<p>Large volumes of magma intruded the gneisses during this period. The magma solidified to form new rocks like granite, charnockite and syenite. These <span class='NP-tooltip  '\n    data-tippy=''\n    data-tippy-arrow='true'\n    data-tippy-delay='[null,400]'\n    data-tippy-interactive='true'\n    data-tippy-trigger='mouseenter focus click'\n    >intrusions<sup class='NP-tooltipmark'>?<\/sup><\/span> are massive and sometimes very coarse grained and the rocks often form spectacular, jagged peaks and alpine ranges that are so characteristic for the landscape in central parts of Dronning Maud Land. Another characteristic feature of the granitoid rocks in Dronning Maud Land is the dark-brown weathering colour, which often makes them recognisable at a long distance.<\/p>\n<p>Towards the end of the pan-African orogeny, the thickened crust became unstable. Extension of the crust in Dronning Maud Land led to rocks from a deeper level in the crust being carried to higher levels. The extension (stretching) continually occurred from deeper crustal levels, where ductile (plastic) deformation of the rock mass takes place, towards higher crustal levels, where the crust deforms in a brittle fashion. Structures formed at the different crustal levels can be observed as folds, shear zones and faults.<\/p>\n<section class=\"av_textblock_section\"  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div role='complementary' class='avia_textblock NP-factsheet-enfold alwaysToggle '   itemprop=\"text\" ><p class='title'>Dronning Maud Land as a natural laboratory<\/p><div class='hsep'><\/div><div class='NP-factsheet-content'><\/p>\n<p>Brown rocks characterise large parts of Dronning Maud Land. You can often see light-coloured zones and stripes on the cliffs. These stripes are caused by fluids which have transformed, bleached, the dark rocks.<\/p>\n<p>Crystalline rocks originating at great crustal depths are basically compact and impermeable. Fluids can, however, invade the rock along fractures which occur as veins in the centre of the light stripes. The marked colour change arose when the fluids flooded along the microfractures in the country rock, transforming the original minerals into new, hydrous minerals. Analyses of fluid inclusions preserved in the minerals show that they consisted of water, carbon dioxide and small amounts of nitrogen. Fluid infiltration in the bedrock of Dronning Maud Land is far-reaching and shows regional distribution. Because fluids can react with minerals in rocks, they alter the properties of the rocks and are thus important for processes in the Earth\u2019s crust. Their significance in geological processes has been an important research topic in recent years.<\/p>\n<p>Owing to the good exposure where the mountains breach the Antarctic ice cap, Dronning Maud Land is a unique laboratory for studying just such processes.<\/p>\n<p><\/div><\/div><div tabindex=\"0\" role=\"button\" class=\"NP-factToggle\" style=\"text-align:center;\"><i class=\"fas fa-angle-down fa-2x\"><\/i><\/div><\/section>\n<h2>The geology of Jutulsessen<\/h2>\n<div id=\"attachment_14773\" style=\"width: 204px\" class=\"wp-caption alignright\"><a href=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-14773\" class=\"size-medium wp-image-14773\" src=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-194x300.jpg\" alt=\"To persomer foran steinvegg\" width=\"194\" height=\"300\" srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-194x300.jpg 194w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-450x698.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget-455x705.jpg 455w, https:\/\/npolar.no\/wp-content\/uploads\/2018\/09\/NP013795-jutulhogget.jpg 516w\" sizes=\"auto, (max-width: 194px) 100vw, 194px\" \/><\/a><p id=\"caption-attachment-14773\" class=\"wp-caption-text\"><span class=\"credit\"><strong>Jutulhogget<\/strong>, Gjelsvikfjella. Grey gneiss is intruded by three generations of dykes. The white dyke consists of felsic pegmatite, the black dykes of amphibolite and the brown one, the youngest, is syenite.&nbsp; Photo: Synn\u00f8ve Elvevold \/ Norwegian Polar Institute<\/span><\/p><\/div>\n<p>The bedrock at Jutulsessen mainly consists of granitic gneiss and migmatite. Syenite and gabbro also occur in the northeastern parts of Jutulsessen. The area is characterised by a large number of&nbsp;<span class='NP-tooltip  '\n    data-tippy='Felsic rocks are a&nbsp;group&nbsp;of&nbsp;light-coloured&nbsp;minerals&nbsp;including&nbsp;feldspar,&nbsp;feldspathoids, quartz, and&nbsp;muscovite.'\n    data-tippy-arrow='true'\n    data-tippy-delay='[null,400]'\n    data-tippy-interactive='true'\n    data-tippy-trigger='mouseenter focus click'\n    >felsic<sup class='NP-tooltipmark'>?<\/sup><\/span> dykes, which locally make up 20-30 % of the rock volume. This can be seen, for example, in the western cliff of S\u00e6tet. Structurally, the gneisses vary from being massive and homogeneous to displaying distinct layering.<\/p>\n<p>The oldest rocks, granitic gneiss and migmatite, date from about 1100 million years ago. Later, during the pan-African mountain building episode, some 500 million years ago, the gneisses underwent amphibolite and granulite facies metamorphism. Along the east side of Jutulsessen, and elsewhere, structures are seen which show that the rocks have undergone partial melting.<\/p>\n<p>Stabben is an impressive mountain with 300 m high, steep cliffs. It consists of massive, coarse-grained syenite which intruded (forced its way into) the country rocks about 500 million years ago. Since syenite is more resistant to erosion than the gabbro of surrounding mountains, Stabben stands up as a crag. The tall, steep cliffs of Jutulhogget consist of homogeneous, resistant (hard) gneisses. Where the rocks are more layered and richer in micas, the mountains are lower and have more gentle slopes, like the north side of Grjotlia.<\/p>\n<p>Jutulsessen is a nunatak between two ice falls to the east and southwest. Small cirque glaciers at Jutulsessen have eroded and formed S\u00e6tet and Grjotlia, and left behind a great deal of morainic debris which consists of clay and sand particles and rocks derived from the surrounding mountains. These areas with superficial deposits are characterised by permafrost, and patterned ground displaying 5-10 m large, up to 1 m high, circles and polygons with large stones accumulated in their centres, is developed in a number of places. The weathering of the ice-free mountainsides takes place through frost shattering and strong winds which carry sand and ice particles. These processes have, for instance, formed deep holes and depressions along some mountainsides.<\/p>\n<\/div><\/section>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":2,"featured_media":33586,"parent":3607,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"tags":[],"emne":[103],"class_list":["post-15654","page","type-page","status-publish","has-post-thumbnail","hentry","emne-geology"],"acf":[],"_links":{"self":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/pages\/15654","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/comments?post=15654"}],"version-history":[{"count":4,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/pages\/15654\/revisions"}],"predecessor-version":[{"id":37800,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/pages\/15654\/revisions\/37800"}],"up":[{"embeddable":true,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/pages\/3607"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/media\/33586"}],"wp:attachment":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/media?parent=15654"}],"wp:term":[{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/tags?post=15654"},{"taxonomy":"emne","embeddable":true,"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/emne?post=15654"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}