{"id":1285,"date":"2024-08-07T20:19:36","date_gmt":"2024-08-07T20:19:36","guid":{"rendered":"https:\/\/travelshelper.com\/staging\/staging\/?p=1285"},"modified":"2026-02-27T01:01:24","modified_gmt":"2026-02-27T01:01:24","slug":"vatnajokull-the-largest-glacier-in-europe","status":"publish","type":"post","link":"https:\/\/travelshelper.com\/staging\/magazine\/unusual-places\/vatnajokull-the-largest-glacier-in-europe\/","title":{"rendered":"VATNAJOKULL \u2013 The Largest Glacier In Europe"},"content":{"rendered":"\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull reigns as Iceland\u2019s (and, by many counts, Europe\u2019s) largest glacier. This vast ice cap covers roughly 8,100\u202fkm\u00b2 \u2013 about 8% of the country \u2013 and contains around 3,000\u202fkm\u00b3 of ice. Its average thickness is 400\u2013500\u202fm, reaching up to ~1,000\u202fm in places. Locally called <em>Vatna Glacier<\/em> (Icelandic <em>vatn<\/em> \u201cwater\u201d) for the meltwater it stores, Vatnaj\u00f6kull\u2019s name literally means \u201cglacier of waters\u201d. Its scale is astonishing: dozens of mountain peaks and eight subglacial volcanoes lie hidden beneath the ice. Since 2008 the glacier (and surrounding landscape) has formed Vatnaj\u00f6kull National Park, and in 2019 UNESCO inscribed it as part of the &#8220;Vatnaj\u00f6kull \u2013 Dynamic Nature of Fire and Ice&#8221; World Heritage Site.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Quick Facts:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><em>Area:<\/em> ~8,100\u202fkm\u00b2 (\u22488% of Iceland)<\/li>\n\n\n\n<li><em>Volume:<\/em> \u22483,000\u202fkm\u00b3 (four times that of Denmark)<\/li>\n\n\n\n<li><em>Thickness:<\/em> avg. ~450\u202fm (max ~1,000\u202fm)<\/li>\n\n\n\n<li><em>Highest elevation:<\/em> 2,110\u202fm (Hvannadalshnj\u00fakur peak)<\/li>\n\n\n\n<li><em>Volcanoes:<\/em> 8 major subglacial systems (Gr\u00edmsv\u00f6tn, B\u00e1r\u00f0arbunga, \u00d6r\u00e6faj\u00f6kull, etc.)<\/li>\n\n\n\n<li><em>National Park:<\/em> Established 2008 (covers ~14,967\u202fkm\u00b2)<\/li>\n\n\n\n<li><em>UNESCO:<\/em> World Heritage Site (inscribed July 2019)<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">What Is Vatnaj\u00f6kull? Essential Facts and Figures<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull (pronounced \u201cVAT-nah-YEUH-kootl\u201d) is the immense ice cap in southeast Iceland. It spans roughly 8,000\u20138,300\u202fkm\u00b2 \u2013 making it Iceland\u2019s largest glacier and often cited as Europe\u2019s largest outside the polar Arctic. The ice is relatively \u201cyoung\u201d in geological terms (a few thousand years old). Most of the glacier survives summer: about 60% of its surface lies above the equilibrium line (the summer snowline), so only the highest rims melt completely each summer. Underneath Vatnaj\u00f6kull rise hundreds of nunataks (exposed peaks) and eight central volcanoes. The ice cap flows outward from a plateau (600\u2013800\u202fm elevation) toward all sides, feeding dozens of outlet glaciers and glacial rivers.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">A key point of confusion: Vatnaj\u00f6kull is <em>sometimes<\/em> called \u201cEurope\u2019s largest glacier\u201d, but this usually excludes Arctic Russia. (Russia\u2019s Novaya Zemlya has the 20,500\u202fkm\u00b2 Severny Island ice cap, which is technically larger but lies in the high Arctic.) Vatnaj\u00f6kull remains by far the biggest on the European mainland.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>The name Vatnaj\u00f6kull comes from Old Norse: vatna- is the genitive plural of vatn (water or lake), and j\u00f6kull means glacier. The glacier contains countless subglacial lakes and meltwater channels \u2013 hence the fitting \u201cglacier of waters\u201d moniker.<\/p><cite>Historical Note<\/cite><\/blockquote><\/figure>\n\n\n\n<h3 class=\"wp-block-heading\">Size and Dimensions<\/h3>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>Statistic<\/th><th>Value<\/th><\/tr><\/thead><tbody><tr><td><strong>Area<\/strong><\/td><td>~8,100 km\u00b2 (\u22488% of Iceland)<\/td><\/tr><tr><td><strong>Volume<\/strong><\/td><td>~3,000 km\u00b3<\/td><\/tr><tr><td><strong>Average Thickness<\/strong><\/td><td>~450 m<\/td><\/tr><tr><td><strong>Maximum Thickness<\/strong><\/td><td>~950\u20131,000 m<\/td><\/tr><tr><td><strong>Extent<\/strong><\/td><td>~100 km (E\u2013W) \u00d7 100 km (N\u2013S)<\/td><\/tr><tr><td><strong>Peak Elevation<\/strong><\/td><td>2,110 m (Hvannadalshnj\u00fakur)<\/td><\/tr><tr><td><strong>% of Iceland\u2019s Area<\/strong><\/td><td>~8%<\/td><\/tr><tr><td><strong>Outlet Glaciers<\/strong><\/td><td>~30 major glacier tongues<\/td><\/tr><tr><td><strong>National Park<\/strong><\/td><td>Vatnaj\u00f6kull National Park (est. 2008)<\/td><\/tr><tr><td><strong>UNESCO Status<\/strong><\/td><td>World Heritage Site \u2014 <em>Fire &amp; Ice<\/em> (July 2019)<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<h3 class=\"wp-block-heading\">The \u201cLargest Glacier in Europe\u201d<\/h3>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull is indeed Iceland\u2019s largest glacier by area and volume. By many definitions it is also Europe\u2019s largest glacier. UNESCO notes that Vatnaj\u00f6kull \u201cis the largest glacier in Europe\u201d. In area (8,000+\u202fkm\u00b2) it far exceeds any glacier on the European mainland \u2013 for comparison, Switzerland\u2019s Aletsch Glacier covers only ~79\u202fkm\u00b2. Some debate arises only if one includes Arctic Russian ice caps: Novaya Zemlya\u2019s Severny Island ice cap (~20,500\u202fkm\u00b2) is technically bigger, but it lies well north of Iceland. Excluding the Arctic, Vatnaj\u00f6kull holds the title of Europe\u2019s largest ice cap.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Where Is Vatnaj\u00f6kull Located?<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull dominates southeastern Iceland. It spans roughly 64.0\u201365.5\u00b0\u202fN, 16.0\u201318.5\u00b0\u202fW \u2013 an area stretching from the central highlands down to near the coast. To the south it abuts the coastal lowlands and the Ring Road (Route 1); to the east it reaches toward the town of H\u00f6fn and the Ocean; to the west it approaches Skaftafell; and to the north it tapers into the uninhabited highland plateau (the Sprengisandur). The glacier\u2019s meltwater feeds several major rivers (e.g. Skei\u00f0ar\u00e1, J\u00f6kuls\u00e1), forming vast black-sand plains and lagoons (see below). Visitors typically reach Vatnaj\u00f6kull via the Ring Road: from Reykjav\u00edk the drive to the Skaftafell\/Vatnaj\u00f6kull area is ~320\u202fkm (~4\u20135 hours) through scenic south-coast towns and waterfalls. The national park encompasses the entire ice cap and surrounding zones \u2013 on the map it appears as a huge white\/green patch spanning south-central Iceland.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Map &amp; Access:<\/strong> Vatnaj\u00f6kull is effectively bisected by the Ring Road at its southern edge. Key access points are the Skaftafell visitor center (west side), J\u00f6kuls\u00e1rl\u00f3n lagoon \/ Brei\u00f0amerkurj\u00f6kull (east side), and F\u2011roads into the central plateau for 4\u00d74 vehicles (north side). Most paved roads end at the ice margin; interior travel requires specialized tours. There are no towns on the glacier itself \u2013 the nearest villages are H\u00f6fn (east) and Kirkjub\u00e6jarklaustur (west).<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">The Geology and Formation of Vatnaj\u00f6kull<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull grew from active glaciation in the Holocene. Unlike many alpine glaciers, it is <strong>not<\/strong> a relic of the last Ice Age: recent research indicates its thick ice formed only about 2,500 years ago. The ice sits on a highland plateau (600\u2013800\u202fm elevation on average) that tilts gently toward the coast. Around the ice cap\u2019s margins the terrain drops to near sea level, while at the center lies ice fields over subglacial bedrock. Because Iceland lies on the Mid-Atlantic Ridge with high precipitation and geothermal heat, Vatnaj\u00f6kull is very dynamic.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The glacier\u2019s internal structure features layers of compacted snow (firn) turning to ice, with some bubbly glacial ice. Roughly 60% of the surface remains snow-covered year-round (above the summer snowline, or equilibrium line, roughly 1,100\u20131,300\u202fm). The enormous weight of the ice also depresses the crust: geodetic studies show Iceland\u2019s surface rebounds gradually as Vatnaj\u00f6kull thins by melting. Beneath the ice are deep valleys and subglacial canyons carved in past j\u00f6kulhlaups (floods). In sum, Vatnaj\u00f6kull is a \u201ccold\u201d ice cap dominated by accumulation from heavy snowfall (southern Iceland gets up to 5\u201310\u202fm of precipitation at high elevations) and ablation at edges via summer melt.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Volcanoes Beneath the Ice: Vatnaj\u00f6kull\u2019s Fiery Heart<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull conceals a whole volcanic archipelago. Icelandic volcanologists identify <strong>seven major volcanic systems<\/strong> under the ice. The two standout centers are <strong>Gr\u00edmsv\u00f6tn<\/strong> and <strong>B\u00e1r\u00f0arbunga<\/strong>. Gr\u00edmsv\u00f6tn (1,764\u202fm, in the ice\u2019s center) is Iceland\u2019s most active volcano \u2013 it erupts roughly every 5\u201310 years. Its 2011 eruption sent ash plumes ~20\u202fkm high. B\u00e1r\u00f0arbunga (2,010\u202fm) is the ice cap\u2019s largest volcano with a 70\u00d710\u202fkm caldera. In 2014\u201315 it fed the colossal Holuhraun fissure eruption: about 0.85\u202fkm\u00b3 of basalt lava poured out, forming an ~85\u202fkm\u00b2 lava field (one of Iceland\u2019s largest recent eruptions).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Gr\u00edmsv\u00f6tn (Iceland\u2019s Most Active):<\/strong> Subglacial lake Gr\u00edmsv\u00f6tn lies under Vatnaj\u00f6kull\u2019s center. Its 2011 eruption was brief but intense, and it floods frequently: each eruption often melts huge ice volumes. The glacier above Gr\u00edmsv\u00f6tn bulged before eruptions, and j\u00f6kulhlaups (glacial outburst floods) have repeatedly swept from beneath. For instance, a 2004 eruption (Gr\u00edmsv\u00f6tn) led to one of the largest recorded j\u00f6kulhlaups.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>B\u00e1r\u00f0arbunga:<\/strong> This massive volcano, capped by a complex caldera, last \u201cblew\u201d its top in the 2014\u201315 fissure event. The eruption began in August 2014 and continued ~6 months. Over that time, roughly 1.6\u202fkm\u00b3 of lava erupted (\u224884\u202fkm\u00b2 field) \u2013 comparable to the volume of dozens of Vatnaj\u00f6kull\u2019s outlet glaciers combined. The glacier above slowly subsided (by ~65\u202fm in parts). B\u00e1r\u00f0arbunga has shown unrest (swarm earthquakes, deformation), so geologists monitor it closely.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>\u00d6r\u00e6faj\u00f6kull (Highest Volcano):<\/strong> In the glacier\u2019s southeast, \u00d6r\u00e6faj\u00f6kull is a stratovolcano with two ice-covered summits. It is home to Iceland\u2019s highest peak, Hvannadalshnj\u00fakur (2,110\u202fm). \u00d6r\u00e6faj\u00f6kull\u2019s historical eruptions were cataclysmic: in 1362 it produced ~10\u202fkm\u00b3 of rhyolite tephra (VEI ~6), Iceland\u2019s largest known eruption. Another large eruption in 1727\u201328 again caused j\u00f6kulhlaups that dramatically altered the landscape. Today \u00d6r\u00e6faj\u00f6kull is largely quiet, but it contains vast meltwater lakes under the ice.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Other subglacial volcanoes include <strong>Kverkfj\u00f6ll<\/strong> (northeast of B\u00e1r\u00f0arbunga), <strong>Hamarinn<\/strong> (formerly part of B\u00e1r\u00f0arbunga system), and the <strong>Torfaj\u00f6kull<\/strong> system (a large caldera in southwest Vatnaj\u00f6kull). Many smaller fissures and hot springs (e.g. at Kverkfj\u00f6ll) pepper the ice cap\u2019s interior.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Subglacial eruptions and j\u00f6kulhlaups are characteristic here. In the infamous November 1996 event, a Gr\u00edmsv\u00f6tn eruption melted ~3\u202fkm\u00b3 of ice beneath Vatnaj\u00f6kull. On 5\u20136 Nov 1996 the ice dam burst: a torrent of ~50,000\u202fm\u00b3\/s of water surged across the Skei\u00f0ar\u00e1rsandur outwash plain, briefly making it the world\u2019s second-largest river. The flood swept away bridges, roads and towers (estimated $14M damage), and even expanded the plain by new land. This episode remains a textbook example of a glacial outburst flood.<\/p><cite>Historical Note<\/cite><\/blockquote><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Understanding J\u00f6kulhlaups:<\/strong> A <em>j\u00f6kulhlaup<\/em> is a sudden release of subglacial water during\/after an eruption. These floods can carry vast sediment loads, carving braided channels on the outwash plains. Vatnaj\u00f6kull\u2019s volcanic dynamics make it prone to such events whenever an eruption melts the ice cap\u2019s base.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull\u2019s Outlet Glaciers<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Unlike a single sheet, Vatnaj\u00f6kull feeds <strong>~30 major outlet glaciers<\/strong>. These are rivers of ice flowing outward from the main cap, often down into valleys or plains. Major outlets include:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Dyngjuj\u00f6kull<\/strong> (north) \u2013 flows into J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum river system.<\/li>\n\n\n\n<li><strong>Tungna\u00e1rj\u00f6kull<\/strong> (northwest) \u2013 feeds the Tungna\u00e1 river (Rio Thjorsa).<\/li>\n\n\n\n<li><strong>Skaft\u00e1rj\u00f6kull<\/strong> (west-central) \u2013 supplies the Skaft\u00e1 river.<\/li>\n\n\n\n<li><strong>S\u00ed\u00f0uj\u00f6kull<\/strong> (west) \u2013 smaller tongue near Skaftafell.<\/li>\n\n\n\n<li><strong>Skei\u00f0ar\u00e1rj\u00f6kull<\/strong> (south) \u2013 drains Skei\u00f0ar\u00e1 (Skaft\u00e1) and is vast (~15\u202fkm wide).<\/li>\n\n\n\n<li><strong>S\u00ed\u00f0uj\u00f6kull<\/strong> (southwest) \u2013 flows from Hvannadalshnj\u00fakur to Skaftafell area.<\/li>\n\n\n\n<li><strong>Skaftafellsj\u00f6kull<\/strong> and <strong>Sv\u00ednafellsj\u00f6kull<\/strong> (southwest) \u2013 tourist-friendly tongues in Skaftafell.<\/li>\n\n\n\n<li><strong>Brei\u00f0amerkurj\u00f6kull<\/strong> (southeast) \u2013 source of the famous J\u00f6kuls\u00e1rl\u00f3n lagoon and Diamond Beach.<\/li>\n\n\n\n<li><strong>Fjallsj\u00f6kull<\/strong> (southeast) \u2013 a neighbor of Brei\u00f0amerkur.<\/li>\n\n\n\n<li><strong>Hoffellsj\u00f6kull<\/strong> (east) \u2013 smaller toe near H\u00f6fn.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">Each outlet has its own flow rate and dynamics. For example, <strong>Brei\u00f0amerkurj\u00f6kull<\/strong> calves icebergs into J\u00f6kuls\u00e1rl\u00f3n, while <strong>Skei\u00f0ar\u00e1rj\u00f6kull<\/strong> historically has been one of the ice cap\u2019s fastest-moving tongues (until it thinned in recent decades). Many outlets have retreated significantly since the early 1900s, leaving terminal moraines and glacial lakes.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Many of Vatnaj\u00f6kull\u2019s outlets can be seen from parking areas or short walks. Skaftafellsj\u00f6kull and Sv\u00ednafellsj\u00f6kull are accessible via marked trails. The largest (Skei\u00f0ar\u00e1rj\u00f6kull, Tungna\u00e1rj\u00f6kull) are mostly visible only by air or very long hikes. Brei\u00f0amerkurj\u00f6kull is uniquely accessible via boat tours on J\u00f6kuls\u00e1rl\u00f3n (see below).<\/p><cite>Practical Information<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull National Park: Europe\u2019s Largest<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Almost the <em>entire<\/em> glacier and its surroundings are protected as Vatnaj\u00f6kull National Park (established 2008). The park spans about 14,967\u202fkm\u00b2 \u2013 roughly 14% of Iceland \u2013 making it one of Europe\u2019s largest national parks. It was created by merging the old Skaftafell and J\u00f6kuls\u00e1rglj\u00fafur parks and adding vast conservation zones. In July 2019 UNESCO inscribed the park on its World Heritage List (as \u201cFire and Ice\u201d), recognizing its outstanding geology (volcanoes, glaciers, rivers, canyons).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The park protects a stunning range of features: glacier ice fields, massive volcanoes and lava fields, glacial rivers and outwash plains, towering waterfalls and deep canyons (e.g. Fjalls\u00e1rglj\u00fafur, parts of Jokuls\u00e1rglj\u00fafur), plus the dynamic coastal lagoons (J\u00f6kuls\u00e1rl\u00f3n, Fjalls\u00e1rl\u00f3n). Conservation goals include preserving pristine wilderness and dynamic processes. Each year park rangers and scientists monitor glacier change, volcanic activity and rare Arctic flora and fauna.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Historical Note:<\/strong> On 7 June 2008 Vatnaj\u00f6kull National Park was officially created. At that time it absorbed two smaller parks (Skaftafell and J\u00f6kuls\u00e1rglj\u00fafur). This combined unit immediately became Iceland\u2019s (and then Europe\u2019s) largest national park. The purpose was to protect the \u201cfire-and-ice\u201d ecosystem as a whole \u2013 an approach that UNESCO lauded in 2019.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Visitor Centers:<\/strong> The park operates information centers at Skaftafell (west) and J\u00f6kuls\u00e1rl\u00f3n (east) that offer maps, exhibits and guidance. The Skaftafell center (closed in winter) provides weather updates, trail info, and advice on glacier tours. At J\u00f6kuls\u00e1rl\u00f3n\/Visitor Center you can book boat tours and hear about wildlife in the lagoon. Both offer basic refreshments and souvenirs. (Note: no entry fees apply, but some parking lots and winter tours may require tickets.)<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Iceland\u2019s Highest Peak: Hvannadalshnj\u00fakur<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull\u2019s southern rim hosts Iceland\u2019s summit: <strong>Hvannadalshnj\u00fakur<\/strong> (2,110\u202fm). This peak sits on the \u00d6r\u00e6faj\u00f6kull volcano. It\u2019s a popular objective among experienced hikers. The climb from Skaftafell is a long glacier trek (12\u201315+ hours round-trip) with ~1,600\u202fm elevation gain. Success requires crampons, ice axes, rope and a glacier guide. Even in summer the upper slopes have deep snow and crevasses. Guides typically rope up groups and break trail through the snow.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The <em>best climbing season<\/em> runs roughly mid-April through June (when snow is firmer and daylight is long). Outside those months the weather is more hazardous and shorter daylight makes summit pushes riskier. Given the glacier crossings and remoteness, climbers must be in excellent shape and carry full winter gear. Despite the challenge, the reward is panoramic views of all of Vatnaj\u00f6kull\u2019s peaks and out into the North Atlantic on a clear day.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>If attempting Hvannadalshnj\u00fakur, go with an experienced guide. Snow\/ice conditions change yearly; professional guides carry avalanche transceivers, probes and radios. Know before you go: even in summer, temperatures at the summit can be below freezing and storms can roll in suddenly. Always pack warm layers, food, and headlamp.<\/p><cite>Practical Information<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">J\u00f6kuls\u00e1rl\u00f3n Glacier Lagoon and Diamond Beach<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">J\u00f6kuls\u00e1rl\u00f3n is a spectacular iceberg lagoon on Vatnaj\u00f6kull\u2019s southeastern edge. It formed as the <strong>Brei\u00f0amerkurj\u00f6kull<\/strong> outlet glacier retreated in the 20th century. Today the lagoon stretches ~18\u202fkm\u00b2 and is very deep (up to ~250\u202fm) \u2013 Iceland\u2019s deepest lake. Icebergs calve constantly from Brei\u00f0amerkurj\u00f6kull and float in the teal water. As they drift into the Atlantic, some wash ashore on the adjacent <em>Diamond Beach<\/em> (above), a black-sand beach where ice chunks glint like gems. These photogenic sights are highlights of any Vatnaj\u00f6kull visit.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Boat tours launched from shore allow tourists to float among the icebergs. Semi-amphibious boats and smaller zodiac tours operate in summer (most around J\u00f6kuls\u00e1rl\u00f3n and nearby Fjalls\u00e1rl\u00f3n). These tours are run year-round (weather permitting) and provide unique views of the lagoon\u2019s ice and resident seals. Harbor seals often lounge on the icebergs or swim alongside boats here. (In winter, parts of the lagoon may freeze over, but some tours still run using open channels.) Marine life also appears: eider ducks and terns can be seen, and occasionally whales or porpoises slip through the icy outflow.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Visit Diamond Beach at sunrise or sunset, when the low sun backlights the ice on the black sand for dramatic photos. Late spring and early autumn often have ideal light. Also note that parking at J\u00f6kuls\u00e1rl\u00f3n can be busy; early morning or late evening visits avoid crowds.<\/p><cite>Insider Tip<\/cite><\/blockquote><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Fjalls\u00e1rl\u00f3n, a smaller iceberg lake just west of J\u00f6kuls\u00e1rl\u00f3n, offers a quieter but similar experience (it is fed by the Fjallsj\u00f6kull tongue). Both lagoons were featured in movies (e.g., <em>James Bond<\/em>, <em>Batman Begins<\/em>) for their otherworldly beauty.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Ice Caves of Vatnaj\u00f6kull<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull\u2019s glaciers harbor many <strong>ice caves<\/strong> \u2013 seasonal tunnels carved by meltwater. These caves form anew each winter (often October\u2013March) when surface melting drains through the ice. The caves usually collapse by late summer, so each winter sees a fresh network. The ice walls glow vividly blue, creating surreal chambers. Some notable cave areas are under Kverkfj\u00f6ll in the north and around Svinafellsj\u00f6kull\/Skaftafell in the south. (Many tours also visit summer \u201cice tunnels\u201d at glacier margins.)<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Ice caves are extremely fragile and can be deadly if entered alone. <strong>Always use a guide.<\/strong> Tour operators in H\u00f6fn and Skaftafell run guided ice-caving trips with hardhats and lights. During the peak season (Nov\u2013Mar), one might hike ~2\u20134\u202fkm on the glacier ice, then crawl 50\u2013200\u202fm into a cave. Inside, expect very bright blue walls (due to dense ice) and stalactites of frozen meltwater. Ambient temps are just below 0\u00b0C. Sturdy boots, crampons and layered clothing are essential. Many guides limit cave entry times for safety. The caves also have clear acoustics: a distant drip or crack is unnervingly loud, so listening helps anticipate changes.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Ice cave tours are hugely popular. Book months in advance if visiting winter. Tour prices vary (~$100\u2013200 per person for a small-group hike+ice cave) and typically include all necessary gear. Providers often offer safety briefings and shuttles from nearby towns. Remember: no unattached exploration. Even deep footprints in fresh snow signal a hidden cave \u2013 venturing off marked paths is forbidden.<\/p><cite>Practical Information<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">Activities and Adventures on Vatnaj\u00f6kull<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull is an adventure paradise for experienced travelers. Major activities include:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Glacier Hiking:<\/strong> Guided walks on the ice (usually 2\u20136 hours). Requires crampons and rope. Trips range from easy flat walks (e.g. on Sv\u00ednafellsj\u00f6kull) to strenuous climbs. Suitable for fit beginners on simple hikes.<\/li>\n\n\n\n<li><strong>Ice Climbing:<\/strong> Vertical ice walls on glacier tongues (common in Skaftafell). Climbers use ice axes and harnesses. These half-day or full-day tours demand greater fitness and strength.<\/li>\n\n\n\n<li><strong>Snowmobiling:<\/strong> Summer snowmobiling on the ice cap (from Stafafell base). Riders speed across snowy plateaus and ridges in on-ice tracks \u2013 a thrilling way to experience the wide ice expanse.<\/li>\n\n\n\n<li><strong>Photography Tours:<\/strong> Specialized tours focus on sunrise\/sunset photography (ice caves, lagoons, glacier summit panoramas). Guides know the best light and safe vantage points.<\/li>\n\n\n\n<li><strong>Multi-day Traverses:<\/strong> Expert expeditions that cross the ice cap (7\u201314 days), staying in mountain huts. These require expedition skills and usually include reaching the glacier\u2019s center.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">All glacier activities <em>must<\/em> be guided. Even simple walks use safety ropes and gear. Local operators (e.g. Glacier Guides, Arctic Adventures) emphasize that weather on the ice changes rapidly. Guides carry satellite phones for emergency. Permits aren\u2019t required for Vatnaj\u00f6kull (unlike some western glaciers), but the official advice is always to hire an accredited guide and inform park rangers of your plan.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Equipment rentals (ice boots, crampons, harnesses) are available from most guiding companies. Warm base layers and windproof outerwear are highly recommended; even in summer the wind off Vatnaj\u00f6kull can cut the temperature dramatically. Note that altitudes are low (\u22642,110 m), so altitude sickness is rare \u2013 but cold and exposure are real hazards.<\/p><cite>Practical Information<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">How to Visit Vatnaj\u00f6kull: Complete Planning Guide<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Getting There:<\/strong> The Ring Road (Route 1) circles Iceland and passes along Vatnaj\u00f6kull\u2019s southern edge. From Reykjav\u00edk drive east on Route 1: Skaftafell\/Skaft\u00e1rdalur (west glacier entry) is ~330\u202fkm (5\u20136\u202fhr) via V\u00edk. J\u00f6kuls\u00e1rl\u00f3n (east lagoon) is ~380\u202fkm (5.5\u20136.5\u202fhr) via H\u00f6fn. The roads (running north of the glacier) are well-maintained in summer. In winter, heavy snows can close sections of Route 1 (check the Icelandic Road Administration site before travel). No roads penetrate the glacier; all tours depart from main centers (Skaftafell, H\u00f6fn, etc.).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Entry Points &amp; Facilities:<\/strong><br>&#8211; <em>Skaftafell (West Side):<\/em> A visitor center, campground and trailheads into the ice (e.g. Sv\u00ednafellsj\u00f6kull) are here. This is a major hub for hikes and ice caves. There are lodges, hostels and a campsite.<br>&#8211; <em>J\u00f6kuls\u00e1rl\u00f3n (East Side):<\/em> A small visitor center by the lagoon offers parking, restrooms and boat tours. Accommodation (hotels\/guesthouses) is found in nearby H\u00f6fn (~80\u202fkm east).<br>&#8211; <em>H\u00f6fn:<\/em> The town east of Vatnaj\u00f6kull, dubbed the \u201clobster capital,\u201d is a base for eastern ice cap tours (near Brei\u00f0amerkurj\u00f6kull). It has several hotels and restaurants.<br>&#8211; <em>Access Roads:<\/em> F-roads (rough gravel routes) run along Vatnaj\u00f6kull\u2019s north (e.g. F88, F905) connecting to the interior highlands (4\u00d74 only). These require river crossings and are only passable in summer with Super Jeeps.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Best Time to Visit (Month-by-Month):<\/strong><\/p>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><td>Month<\/td><td>Conditions and Highlights<\/td><\/tr><\/thead><tbody><tr><td><strong>Jan\u2013Feb<\/strong><\/td><td>Deep winter: lots of snow, short days (4\u20136\u202fhr light). Ice caves in place; many trails snow-covered. Boat tours seasonal (frozen lagoon). Good for Northern Lights with snowy scenery.<\/td><\/tr><tr><td><strong>Mar\u2013Apr<\/strong><\/td><td>Transition to spring. Ice-caves still open; begin long daylight. Snowmobile season active. Roads remain icy until late April. Early hiking (with crampons) possible.<\/td><\/tr><tr><td><strong>May<\/strong><\/td><td>Late spring: rapid daylight increase, snowline retreats. Some tours on glacier start. Roads clearing. Skaftafell has many wildflowers. Crowds still moderate.<\/td><\/tr><tr><td><strong>Jun\u2013Aug<\/strong><\/td><td>Peak season. Full summer: long (24h in June) daylight, minimal snow on low trails. All tours running (hiking, ice climbing, boating). J\u00f6kuls\u00e1rl\u00f3n navigable. Road access reliable. Expect the most tourists and higher prices.<\/td><\/tr><tr><td><strong>Sep<\/strong><\/td><td>Early fall: cooler, fewer crowds. Some ice caves begin to form (especially Oct). Northern Lights visible as nights return. Fjord fishing season (H\u00f6fn).<\/td><\/tr><tr><td><strong>Oct\u2013Nov<\/strong><\/td><td>First snowfalls. Ice caves open in Nov (weather permitting). Many tour operators wrap up by mid-November. Roads may begin to close after storms. Beautiful autumn colors around glacier edges.<\/td><\/tr><tr><td><strong>Dec<\/strong><\/td><td>Dark winter returns. Ice caves definitely open; days very short (4\u20135\u202fhr in December). Ski touring on glacier possible. Snowmobiles on glacier. Roads often challenged by storms \u2013 check updates.<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Planning Note:<\/strong> Summer (June\u2013Aug) is most accessible, but also busiest and most expensive. If visiting in winter, realize many services suspend or reduce operations. Always check <strong>road.is<\/strong> for highway and weather conditions (especially in Nov\u2013Mar).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>What to Pack:<\/strong> Wool\/base layers, insulated jacket, waterproof shell. Sturdy hiking boots (waterproof, ankle support). Warm hat, gloves and sunglasses (glare off snow). For glacier tours, bring a small daypack, camera with extra batteries (cold drains battery). Tour companies usually provide harness, crampons and helmet; you should have warm underlayers. If self-driving, carry emergency blanket and spares (roads can be remote).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Guides and Safety:<\/strong> For any glacier travel or ice activities, hire a certified guide. Licensed companies know safe routes and carry emergency gear. Going solo on Vatnaj\u00f6kull is strongly discouraged. Always tell someone your plans and expected return time. Weather can change rapidly \u2013 it\u2019s common to set out under clear skies and encounter blizzard-like fog in hours.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Costs and Budget:<\/strong> Tour prices vary: simple 1\u20132 hr glacier walks typically \u20ac100\u2013\u20ac200 per person; full-day hikes \u20ac200\u2013\u20ac300. Ice-cave tours (with equipment) are similar. Boat tours on J\u00f6kuls\u00e1rl\u00f3n run around \u20ac30\u2013\u20ac50. Accommodation near Vatnaj\u00f6kull spans budget guesthouses (~\u20ac100\/night) to upscale hotels (\u20ac200+). Factor in car rental (4\u00d74 recommended in winter), fuel, meals (restaurants in H\u00f6fn are pricier), and insurance for changing conditions.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Accessibility:<\/strong> Most tourist infrastructure (centers, short trails) is at or near parking areas. However, actual glacier terrain is inaccessible to wheeled devices. Some tour companies offer snowmobile experiences that require minimal walking. Wheelchair access: Limited \u2013 terrain is rough. The visitor centers are mostly wheelchair-friendly, but natural sites (e.g. J\u00f6kuls\u00e1rl\u00f3n) have uneven ground.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Climate Change and Vatnaj\u00f6kull\u2019s Future<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull is undergoing measurable shrinkage. Like all Icelandic glaciers, it peaked during the Little Ice Age (c.1600s) and has retreated since. Estimates indicate Iceland\u2019s glaciers lost ~17% of their area since 1890; much of that loss is from Vatnaj\u00f6kull and Langj\u00f6kull. In the 2000s and 2010s, glacier melt accelerated: between 2000\u20132017, Icelandic ice lost ~43\u202fkm\u00b2 per year on average. The Vatnaj\u00f6kull ice cap currently thins by on the order of 1\u202fm\/year on average (with greater thinning at edges). For context, Vatnaj\u00f6kull contains ~3,000\u202fkm\u00b3 of ice (over 90% of Iceland\u2019s total); if fully melted it would raise global sea level by ~1\u202fcm.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Scientists project continued retreat under warming. Models suggest the glacier could lose half its volume in the next century if climate warms by a few degrees. Already, several outlet glaciers have dramatically pulled back, uncovering bedrock and creating new lakes. The loss of ice also impacts local hydrology: summer meltwater flow has increased in recent decades, affecting river sediment loads and hydroelectric resources.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Climate Context:<\/strong> Observatories note Vatnaj\u00f6kull\u2019s retreat is faster than many smaller glaciers, because of Iceland\u2019s high precipitation and maritime warmth. The glacier is a sensitive climate indicator: decreases in snowfall or increases in melt translate quickly to volume loss (much like Greenland\u2019s outlet glaciers on a smaller scale). The situation reinforces global climate concerns.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">However, Vatnaj\u00f6kull\u2019s sheer size means it will not vanish overnight. Some scientists estimate that, even under aggressive warming, it may remain a significant ice mass (albeit highly reduced) into the late 21st century. Ongoing monitoring by the Icelandic Meteorological Office and glaciologists ensures updated data on thickness change (mass balance) each year.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull vs. Other Major Glaciers<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Here is how Vatnaj\u00f6kull compares to other famous ice masses:<\/p>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><td>Glacier \/ Ice Cap<\/td><td>Location<\/td><td>Area (km\u00b2)<\/td><td>Notes<\/td><\/tr><\/thead><tbody><tr><td><strong>Vatnaj\u00f6kull<\/strong><\/td><td>Iceland<\/td><td>~8,100<\/td><td>Iceland\u2019s largest; <em>often cited as Europe\u2019s largest<\/em> outside the Arctic. Volume ~3,000\u202fkm\u00b3.<\/td><\/tr><tr><td><strong>Severny Island Ice Cap<\/strong><\/td><td>Novaya Zemlya, Russia<\/td><td>~20,500<\/td><td>By area, the largest in (European) Russia \u2013 far north Arctic, so often excluded from \u201cEurope\u201d count.<\/td><\/tr><tr><td><strong>Austfonna (Nordaustl.)<\/strong><\/td><td>Svalbard, Norway<\/td><td>~8,100<\/td><td>Roughly equals Vatnaj\u00f6kull in area (largest Svalbard ice cap). Largest by area in Norway.<\/td><\/tr><tr><td><strong>Langj\u00f6kull<\/strong><\/td><td>Iceland<\/td><td>~950<\/td><td>Iceland\u2019s 2nd-largest ice cap (Western Highlands).<\/td><\/tr><tr><td><strong>Hofsj\u00f6kull<\/strong><\/td><td>Iceland<\/td><td>~925<\/td><td>Iceland\u2019s 3rd-largest ice cap (Central Highlands).<\/td><\/tr><tr><td><strong>Jostedalsbreen<\/strong><\/td><td>Norway (Mainland)<\/td><td>~487<\/td><td>Norway\u2019s largest (European mainland) glacier.<\/td><\/tr><tr><td><strong>Aletsch<\/strong><\/td><td>Switzerland (Alps)<\/td><td>~79<\/td><td>Europe\u2019s largest mountain (non-Arctic) glacier by length\/area.<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Vatnaj\u00f6kull is far larger than any mountain glacier in mainland Europe. Even combined, Langj\u00f6kull+Hofsj\u00f6kull (&lt;2,000\u202fkm\u00b2) are only ~25% of Vatnaj\u00f6kull\u2019s size. (By volume the contrast is even greater.) Globally, Vatnaj\u00f6kull is small compared to Greenland (1.7 million km\u00b2) or Antarctic ice sheets, but among Iceland\u2019s and Europe\u2019s giants it towers above most except that Russian outlier.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Frequently Asked Questions about Vatnaj\u00f6kull<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: What is Vatnaj\u00f6kull?<\/strong><br>A: Vatnaj\u00f6kull is the massive ice cap in southeastern Iceland. Covering ~8,100\u202fkm\u00b2, it is Iceland\u2019s largest glacier and (outside the Arctic) often called Europe\u2019s largest. It sits atop several mountains and volcanoes, and feeds dozens of outlet glaciers. The name means \u201cglacier of waters\u201d in Icelandic.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: Is Vatnaj\u00f6kull really the largest glacier in Europe?<\/strong><br>A: In common usage, yes: Vatnaj\u00f6kull is Europe\u2019s largest glacier outside the Arctic. Novaya Zemlya\u2019s Severny Island (Russia) has a bigger ice cap (~20,500\u202fkm\u00b2) but lies in the far Arctic. If one excludes that, Vatnaj\u00f6kull\u2019s ~8,100\u202fkm\u00b2 area makes it the largest on continental Europe.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: What is J\u00f6kuls\u00e1rl\u00f3n, and where is Diamond Beach?<\/strong><br>A: J\u00f6kuls\u00e1rl\u00f3n is a large glacier lagoon at the southern margin of Vatnaj\u00f6kull, formed by the retreat of the Brei\u00f0amerkurj\u00f6kull outlet. It now covers about 18\u202fkm\u00b2. Diamond Beach is the black-sand beach right next to J\u00f6kuls\u00e1rl\u00f3n. Icebergs float from the lagoon into the sea and often wash up on Diamond Beach, where they sparkle on the dark sand. Boat tours operate on J\u00f6kuls\u00e1rl\u00f3n in summer, offering close views of the icebergs.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: Can tourists walk on Vatnaj\u00f6kull?<\/strong><br>A: You <em>can<\/em> walk on the glacier, but <strong>only with a guided tour and proper gear<\/strong>. Independent travel onto the ice is prohibited due to hidden crevasses and sudden weather changes. Guided glacier hikes (with crampons and ropes) depart from Skaftafell, J\u00f6kuls\u00e1rl\u00f3n or H\u00f6fn and can last from a couple of hours to full days. Even short glacier walks require a certified guide for safety.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: Are the ice caves at Vatnaj\u00f6kull natural, and when can I visit them?<\/strong><br>A: The spectacular blue ice caves are naturally formed by meltwater each winter. They exist roughly November through March when cold air and meltwater carve tunnels under the glacier. By late spring\/summer they collapse. Thus, guided ice-cave tours run mainly in winter. Cave locations change yearly; always go with an experienced guide wearing a helmet and headlamp.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: When is the best time to visit Vatnaj\u00f6kull?<\/strong><br>A: It depends on your interests. For hiking and mild weather, late spring to early autumn (May\u2013Sept) is best: roads are open, and most activities run. For ice caves and winter scenery, December\u2013February offer snowy landscapes and Northern Lights (though daylight is short). Boat tours on J\u00f6kuls\u00e1rl\u00f3n run in summer. Shoulder seasons (April or Sept) mean fewer crowds and moderate weather.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: How far is Vatnaj\u00f6kull from Reykjav\u00edk, and can you drive there?<\/strong><br>A: Vatnaj\u00f6kull\u2019s edge is about 330\u202fkm from Reykjav\u00edk via the Ring Road. The drive takes ~4\u20136 hours (stopping). The Ring Road is paved all the way along the southern glacier margin. In summer the roads are well-maintained. In winter, heavy snow may briefly close sections, so always check current road conditions (see <em>road.is<\/em>) before traveling.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Q: Is there wildlife on or near Vatnaj\u00f6kull?<\/strong><br>A: Yes, especially in the coastal and lower-altitude areas. Arctic foxes roam the highlands. At J\u00f6kuls\u00e1rl\u00f3n and Diamond Beach, harbor seals often bask on ice floes, and you may spot eider ducks, terns, arctic skuas and gulls. Birds of prey like gyrfalcons or golden eagles sometimes hunt in nearby valleys. In winter you might see reindeer on the outskirts of the park. However, no large land animals live <em>on<\/em> the ice itself.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>For millennia, adventurers, scientists, and environmentalists have been enthralled by Europe&#8217;s biggest glacier, Vatnajokull, a magnificent natural wonder. Covering 8,101 square kilometers, it is proof of the unvarnished force and beauty of earthly geological events. Large sheets of ice accumulating in the region marked the start of the story of the glacier 2.5 million years ago Its surface, covered in ice formations with sharp edges and seracs reaching heavens, is always changing masterpiece.<\/p>\n","protected":false},"author":1,"featured_media":2935,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_eb_attr":"","footnotes":""},"categories":[19,5],"tags":[],"class_list":["post-1285","post","type-post","status-publish","format-standard","has-post-thumbnail","category-unusual-places","category-magazine"],"lang":"en","translations":{"en":1285},"pll_sync_post":{},"_links":{"self":[{"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/posts\/1285","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/comments?post=1285"}],"version-history":[{"count":0,"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/posts\/1285\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/media\/2935"}],"wp:attachment":[{"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/media?parent=1285"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/categories?post=1285"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/travelshelper.com\/staging\/wp-json\/wp\/v2\/tags?post=1285"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}