{"id":6746,"date":"2022-08-03T18:36:31","date_gmt":"2022-08-03T18:36:31","guid":{"rendered":"https:\/\/www.iceland.org\/?p=6746"},"modified":"2022-09-29T13:41:06","modified_gmt":"2022-09-29T13:41:06","slug":"tungnaarjokull-glacier-size-ice-caves-cap-and-volcanoes","status":"publish","type":"post","link":"https:\/\/www.iceland.org\/geography\/glacier\/tungnaarjokull\/","title":{"rendered":"Tungna\u00e1rj\u00f6kull Glacier: Size, Ice Caves, Cap and Volcanoes"},"content":{"rendered":"<p><span style=\"font-weight: 400;\">Tungna\u00e1rj\u00f6kull Glacier is one of the 269 glaciers of Iceland. It is located on the western side of Vatnaj\u00f6kull south of Iceland. The size of the Tungna\u00e1rj\u00f6kull Glacier is 17 kilometers wide. The height of the <a class=\"wpil_keyword_link\" href=\"https:\/\/www.iceland.org\/geography\/glacier\/\"   title=\"glacier\" data-wpil-keyword-link=\"linked\">glacier<\/a> has an elevation of 1,095 meters. The glacier is a wide and lobelike glacier of Vatnaj\u00f6kull. Its coordinates are 64.3186\u00b0 N and 18.0222\u00b0 W. Tungna\u00e1rj\u00f6kull Glacier is also called Tungn\u00e1rj\u00f6klar or Tungn\u00e1rj\u00f6kull in <a class=\"wpil_keyword_link\" title=\"Iceland\" href=\"https:\/\/www.iceland.org\" data-wpil-keyword-link=\"linked\">Iceland<\/a>.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Tungna\u00e1rj\u00f6kull Glacier is one of the several outlet glaciers in the country of Iceland. The marginal zone of Tungna\u00e1rj\u00f6kull Glaciers covers the area of its maximum extent during its Little Ice Age up to its current edge.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">The cities around Tungna\u00e1rj\u00f6kull Glaciers are Hverager\u00f0i, Eyrarbakki, <a class=\"wpil_keyword_link\" href=\"https:\/\/www.iceland.org\/selfoss\/\"   title=\"Selfoss\" data-wpil-keyword-link=\"linked\">Selfoss<\/a>, Stokkseyri, Hella, Hvolsv\u00f6llur, Vestmannaeyjar, V\u1f30k, Kirkjub\u0153jarklaustur. In Southern Iceland, Tungna\u00e1rj\u00f6kull is surrounded by mountains and volcanic ridges. One of the ridges surrounding Tungna\u00e1rj\u00f6kull is the J\u00f6kulgrindur volcanic ridges. Most of the volcanic ridges are visible both in the relief of the forefield and in the morphology of the surface of the glacier. Tungna\u00e1rj\u00f6kull Glacier is located in the south of Iceland as an outlet glacier of Vatnaj\u00f6kull. The distance from Reykjav\u00edk to Tungna\u00e1rj\u00f6kull is 190 km via airplane.\u00a0<\/span><\/p>\n<h2><span style=\"font-weight: 400;\">What is the Size of the Tungna\u00e1rj\u00f6kull Glacier?<\/span><\/h2>\n<p><span style=\"font-weight: 400;\">The size of Tungna\u00e1rj\u00f6kull Glacier is 17 km wide and it is 1,095 high. It is an outlet glacier that stretches from the western part of Vatnaj\u00f6kull. Tungna\u00e1rj\u00f6kull Glacier is south of Skaft\u00e1rj\u00f6kull and north of Sylgjuj\u00f6kull. Its marginal zone is 25 km long that extends up to 1.2 km in the northern part of its forefield and 2.5 km from the center to the southern part of its forefield. The size of Tungna\u00e1rj\u00f6kull Glacier is due to the meltwater of the biggest glacier mass and ice cap in Iceland which is known as the Vatnaj\u00f6kull.\u00a0<\/span><\/p>\n<h2><span style=\"font-weight: 400;\">What are the Volcanoes in Tungna\u00e1rj\u00f6kull Glacier?<\/span><\/h2>\n<p><span style=\"font-weight: 400;\">The <a class=\"wpil_keyword_link\" href=\"https:\/\/www.iceland.org\/geography\/volcano\/\"   title=\"volcano\" data-wpil-keyword-link=\"linked\">volcano<\/a> in Tungna\u00e1rj\u00f6kull Glacier is Gr\u1f30msv\u00f6tn. There are 130 volcanoes surrounding the country of Iceland. Iceland has 32 active volcanoes. One of the active volcanoes in Iceland is Gr\u1f30msv\u00f6tn. It is the most active volcanic system in Iceland that is near the Tungna\u00e1rj\u00f6kull Glacier. During the early era of Iceland, the tephra record in Tungna\u00e1rj\u00f6kull Glacier doubled from the number of eruptions known to originate in Gr\u1f30msv\u00f6tn. In the 17th century, an increase in volcanic eruptions contributed to the tephra record for Tungna\u00e1rj\u00f6kull Glacier. Eventually, its frequency of volcanic eruptions slowed down by the mid 15th century.\u00a0<\/span><\/p>\n<h2><span style=\"font-weight: 400;\">What is the prominence of Tungna\u00e1rj\u00f6kull Glacier in Icelandic Culture?<\/span><\/h2>\n<p><span style=\"font-weight: 400;\">The prominence of Tungna\u00e1rj\u00f6kull is the identification of landforms around the area of Tungna\u00e1rj\u00f6kull. Landforms like these include preserved shorelines, small wave-cut platforms, fossil deltas, and kame terraces. These discoveries are connected to the ice-dammed lakes of Iceland. The ice-dammed lakes are the result of Tungna\u00e1rj\u00f6kull damming the outflow of melted water between the snout of Tungna\u00e1rj\u00f6kull and the volcanic ridge of J\u00f6kulgrindur.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Part of the Iceland Culture is to protect Tungna\u00e1rj\u00f6kull as it is one of the national parks of Iceland. National parks are protected areas of Iceland since they are unique areas that are part of Iceland&#8217;s cultural heritage. Iceland\u2019s culture is diverse and has close ties to the ancient Vikings. The glaciers in Iceland are part of the country\u2019s identity.\u00a0<\/span><\/p>\n<h2><span style=\"font-weight: 400;\">What are the Similar Glaciers in Iceland to Tungna\u00e1rj\u00f6kull Glaciers?<\/span><\/h2>\n<p><span style=\"font-weight: 400;\">Similar glaciers in Iceland to Tungna\u00e1rj\u00f6kull Glacier are listed below:<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>S\u1f40lheimaj\u00f6kull:<\/b><span style=\"font-weight: 400;\"> It is an outlet glacier In Iceland from the M\u00fdrdalsj\u00f6kull ice cap. This glacier covers a basin that reaches 100 meters below sea level. The S\u1f40lheimaj\u00f6kull glacier\u2019s coverage is a few kilometers inside the present ice margin. This glacier now is retreating at approximately 100 meters\/year that means after a few decades, an ice <a class=\"wpil_keyword_link\" href=\"https:\/\/www.iceland.org\/geography\/lake\/\"   title=\"lake\" data-wpil-keyword-link=\"linked\">lake<\/a> will form in front of S\u1f40lheimaj\u00f6kull.\u00a0<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Brei\u00f0amerkurj\u00f6kull: <\/b><span style=\"font-weight: 400;\">\u00a0Brei\u00f0amerkurj\u00f6kull is an outlet glacier located in the southern part of Vatnaj\u00f6kull. This glacier occupies sub-glacial valleys that may reach below sea level. The glacial retreat of the Brei\u00f0amerkurj\u00f6kull glacier resulted in a glacial lake formation that serves as its border in Iceland.\u00a0<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>M\u00falaj\u00f6kull:<\/b><span style=\"font-weight: 400;\"> It is an outlet glacier from the Hofsj\u00f6kull ice cap located in the central highlands of Iceland.\u00a0<\/span><\/li>\n<\/ul>\n<p><b>G\u1f30gj\u00f6kull or Fallj\u00f6kull:<\/b><span style=\"font-weight: 400;\"> G\u1f30gj\u00f6kull or Fallj\u00f6kull is an outlet glacier from the <a class=\"wpil_keyword_link\" href=\"https:\/\/www.iceland.org\/geography\/volcano\/eyjafjallajokull\/\"   title=\"Eyjafjallaj\u00f6kull\" data-wpil-keyword-link=\"linked\">Eyjafjallaj\u00f6kull<\/a> ice cap. It is an outlet glacier that can be classified as ice fall, which means IceFall Glacier. <\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tungna\u00e1rj\u00f6kull Glacier is one of the 269 glaciers of Iceland. It is located on the western side of Vatnaj\u00f6kull south of Iceland. The size of the Tungna\u00e1rj\u00f6kull Glacier is 17 kilometers wide. The height of the glacier has an elevation of 1,095 meters. The glacier is a wide and lobelike glacier of Vatnaj\u00f6kull. Its coordinates [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":6747,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[312],"tags":[],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/posts\/6746"}],"collection":[{"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/comments?post=6746"}],"version-history":[{"count":0,"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/posts\/6746\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/media\/6747"}],"wp:attachment":[{"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/media?parent=6746"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/categories?post=6746"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.iceland.org\/wp-json\/wp\/v2\/tags?post=6746"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}