{"id":322,"date":"2011-08-17T15:07:10","date_gmt":"2011-08-17T14:07:10","guid":{"rendered":"http:\/\/all-geo.org\/volcan01010\/?p=322"},"modified":"2011-08-17T15:12:02","modified_gmt":"2011-08-17T14:12:02","slug":"grimsvotn-1-crossing-glacier","status":"publish","type":"post","link":"https:\/\/all-geo.org\/volcan01010\/2011\/08\/grimsvotn-1-crossing-glacier\/","title":{"rendered":"Gr\u00edmsv\u00f6tn 1 – Crossing the glacier"},"content":{"rendered":"

Last month, the Institute of Earth Sciences<\/a> of the University of Iceland and the Iceland Glaciological Society<\/a> organised an expedition to Gr\u00edmsv\u00f6tn to study the deposits of the eruption that took place there in May.\u00a0 This post describes the journey to the volcano and the effect of volcanic ash and other debris from the eruption on ice and snow.<\/p>\n

Driving on ice<\/h3>\n

Gr\u00edmsv\u00f6tn lies beneath the Vatnaj\u00f6kull ice cap, which is the largest glacier in Europe.\u00a0 At 120 km by 90 km by 900 m thick, it is huge.\u00a0 If, for some reason, you needed to hide the English Lake District, you could just slip it underneath.\u00a0 There would be room in there for the Yorkshire Dales, too.\u00a0 To get to the volcano it is necessary to drive across this expanse of ice, in our case approaching from the east.<\/p>\n

Fortunately, driving on glaciers seems to be a relatively routine practice in Iceland.\u00a0 Two vehicles, equipped with winches, planks, shovels, compressors and a host of spares and tools can cross snow-covered ice with each providing a backup for the other.\u00a0 The other vital component is a set of massive, waist-high tyres.<\/p>\n

\"\"<\/a>The final stage before driving onto the ice is reducing the air pressure in the tyres, which spreads the weight of the vehicle and greatly improves their grip.\u00a0 It may look like the truck is loaded with everything but the kitchen sink.\u00a0 That isn’t exactly true, but the large white object in the trailer is<\/em> a household chest-freezer.\u00a0 This was brought to store samples containing ash-filled hailstones, which were produced during the eruption.\u00a0 At 08:00hrs, we were ready to get on the ice.<\/p>\n

Follow the black ashy road<\/h3>\n

Ash from the Gr\u00edmsv\u00f6tn eruption is scattered thinly over the eastern part of the glacier.\u00a0 The dark coloured ash absorbs sunlight, heating the snow beneath and causing extra melting.\u00a0 Thus the surface of the snow, normally flat, is currently very uneven with curving ridges and smooth, wide valleys around 50 cm deep.\u00a0 In places they resemble frozen waves on a choppy sea.\u00a0 Crossing them is equally rough, and the maximum speed was around 10 km\/hr.<\/p>\n

\"\"<\/a>The eruption took place in the late spring, so there has been little new snow to bury the ash.\u00a0 Where it was blown into the tracks of vehicles that crossed the glacier back in June, it defines a vague road of long, dark, parallel trenches caused by the extra melting.<\/p>\n

Snowfall accumulation and melting<\/h3>\n

At a seemingly anonymous point, defined only by GPS coordinates, is a snow monitoring station.\u00a0 It uses echo-sounding the measure the distance from the sensor to the snow surface.\u00a0 In an average year, 6 m of snow fall onto the glacier in this area.\u00a0 Of those, 1.5 m melt and evaporate away; the remainder compacts and joins the rest of the ice flowing slowly to the lowlands.\u00a0 We stopped to adjust the height of the sensor and to download the data.<\/p>\n

\"\"<\/a><\/p>\n

Thicker tephra and dirt cones<\/h3>\n

Tephra<\/a> is the technical term for all the ash and pumice and rock fragments that are thrown out by an exploding volcano (strictly speaking, ash only refers to material less than 2 mm in diameter).\u00a0 Closer to Gr\u00edmsv\u00f6tn, the tephra got gradually thicker and coarser.<\/p>\n

Once the tephra thickness gets more than a few centimetres, the effect that it has on the underlying snow changes.\u00a0 While the black tephra still absorbs extra sunlight, if the layer is thick enough then the heat isn’t transmitted through to the snow.\u00a0 Instead of enhancing melting, the underlying snow is protected.\u00a0 The result is a rough landscape of dirt cones.\u00a0 While the cones may be a metre high, the tephra only accounts for a black, sandy skin over their snowy cores.<\/p>\n

\"\"<\/a><\/h3>\n

Approaching the huts – Plan A<\/h3>\n

We were aiming for three wooden huts built on a ridge of rock called Gr\u00edmsfjall, that pokes out above the ice.\u00a0 The normal approach is to drive up the slopes from the south, as the direct route from the east is blocked by a series of large crevasses<\/a>.\u00a0 It appeared, however, that this route was also impassable.\u00a0 Where the tephra was even thicker (10-15 cm), it gave more uniform protection to the snow beneath, resulting the a series of large plateaux about 2 m taller than their melted-out surroundings.<\/p>\n

\"\"<\/a>After driving back and forth along the foot of Gr\u00edmsfjall and scanning the slope with binoculars, we could not see a way through.\u00a0 Potential leads were explored on foot, but they they were dead ends, finishing in steep dirty walls.<\/p>\n

Approaching the huts – Plan B<\/h3>\n

It was decided that the best approach may be to try a bit further east, where the tephra was thinner.\u00a0 Driving up the slopes, things seemed promising as the black piles gave way to more open snow fields.\u00a0 We progressed steadily higher until CRUNCH!\u00a0 The front of the truck fell into a crevasse.\u00a0 These deep cracks form in the glacier where the ice accelerates down the slope and they are covered in snow-bridges that hide them from view.\u00a0 As the truck drove onto it, the bridge collapsed and it dropped down to its axle.<\/p>\n

\"\"<\/a>Removing the truck was suprisingly straightforward.\u00a0 Jump out, clear the snow from the front, set up a jack on the far side of the crack (which was only about a metre wide), jack up the truck, reverse out.\u00a0 It took less than 20 minutes.\u00a0 We looked for an area to the side where the crevasse was narrower then continued upwards.<\/p>\n

CRUNCH!\u00a0 Another crevasse.\u00a0 We were going to need another plan.<\/p>\n

Approaching the huts – Plan C<\/h3>\n

Where two high ash-covered platforms met, there was sometimes a notch in the wall.\u00a0 The notches were too narrow to drive through, but with a bit of shovelling, they could be enlarged sufficiently to allow the trucks and trailer to pass.\u00a0 A route was staked out on foot, then the gateways were dug through the snow.\u00a0 Four breaks were enough to give us access to the huts.<\/p>\n

\"\"<\/a>
\nThe Gr\u00edmsfjall huts<\/h3>\n

Once through the worst of the tephra platforms, it was easy going to the crest of Gr\u00edmsfjall and the huts.\u00a0 We finally arrived there at 20.30 hrs.\u00a0 With good snow conditions, the journey across the glacier can take just two hours.\u00a0 It had taken us over twelve.\u00a0 The difference was due to the tephra on the ice.<\/p>\n

\"\"<\/a>Some observations from the fieldwork are described in the following post (Gr\u00edmsv\u00f6tn 2 – What was in the plume?<\/a>) and there are some more vehicle-themed photos in another (Gr\u00edmsv\u00f6tn 3 – Bonus truck pictures<\/a>).<\/p>\n","protected":false},"excerpt":{"rendered":"

Last month, the Institute of Earth Sciences of the University of Iceland and the Iceland Glaciological Society organised an expedition to Gr\u00edmsv\u00f6tn to study the deposits of the eruption that took place there in May.\u00a0 This post describes the journey … Continue reading →<\/span><\/a><\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-322","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/322","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/comments?post=322"}],"version-history":[{"count":11,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/322\/revisions"}],"predecessor-version":[{"id":374,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/322\/revisions\/374"}],"wp:attachment":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/media?parent=322"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/categories?post=322"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/tags?post=322"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}