{"id":344,"date":"2011-08-17T14:58:23","date_gmt":"2011-08-17T13:58:23","guid":{"rendered":"http:\/\/all-geo.org\/volcan01010\/?p=344"},"modified":"2011-08-17T15:17:40","modified_gmt":"2011-08-17T14:17:40","slug":"grimsvotn-2-plume-deposits","status":"publish","type":"post","link":"https:\/\/all-geo.org\/volcan01010\/2011\/08\/grimsvotn-2-plume-deposits\/","title":{"rendered":"Gr\u00edmsv\u00f6tn 2 – What was in the plume?"},"content":{"rendered":"

The May 2011 Gr\u00edmsv\u00f6tn eruption blasted ash and pumice and rock fragments (collectively known as tephra<\/a>) through the Vatnaj\u00f6kull glacier, forming a massive plume up to 20 km tall.\u00a0 It was the biggest eruption in Iceland since Hekla 1947.\u00a0 Locally, ash rained down across southern Iceland turning day into night, while the finest grains were swept across the Atlantic to be deposited at least as far afield as in the UK<\/a>.\u00a0 There are nice images of the plume and its consequences at The Boston Globe<\/a> website.<\/p>\n

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.\u00a0 Following an adventurous journey across the glacier to the volcano (see Gr\u00edmsv\u00f6tn 1 – Crossing the glacier<\/a> and Gr\u00edmsv\u00f6tn 3 – Bonus truck pictures<\/a>), it was possible to see the deposits of the eruption, and thus what was in the plume, at first hand.\u00a0 This post shows what was erupted and explains some of what the deposits can tell us.<\/p>\n

All this should be snow<\/h3>\n

The dispersal of volcanic ash is controlled by the wind.\u00a0 During the May 2011 Gr\u00edmsv\u00f6tn eruption, southerly winds blew the top of the plume<\/a> northwards, while northerly winds blew the lower part to the south.\u00a0 It was the lower part that contained most of the tephra that was deposited near the volcano.\u00a0 Tephra is the technical term for all the ash and pumice and rock fragments that are thrown out in an explosive eruption (strictly speaking, ash only refers to material less than 2 mm in diameter).<\/p>\n

This view, looking south from across Vatnaj\u00f6kull, should be dazzling white snow and ice all the way to the coast.\u00a0 Instead, it is black: a vast dark plain of pumice and ash extending tens of kilometres from the crater.<\/p>\n

\"\"<\/a>Calculating the erupted volume<\/h3>\n

Digging through the black surface reveals the bright snow beneath.\u00a0 This makes it easy to measure the thickness of the tephra layer in different locations.\u00a0 A simple, but very important, question can be answered from the resulting map of tephra thickness: how much material was erupted?<\/p>\n

\"\"<\/a>
\nAt this location, if you keep digging, you will pass nothing but snow, ice and ancient tephra layers for over 700 metres before you finally reach the bedrock.<\/p>\n

\"\"<\/a>
\nCloser to the crater, the tephra gets thicker and contains coarser, gravel-sized, pumice grains.\u00a0 At this site 8 km downwind of the crater, the deposit is nearly 2 m thick, and the hole took eight people over an hour to dig.\u00a0 It is clear why lone murderers favour shallow graves.\u00a0 A layer of ashy-hailstones that fell during the eruption has refrozen into an icy layer near the base.\u00a0 These were collected and transported back to Reykjav\u00edk in a freezer.<\/p>\n

Other things that tephra can tell us<\/h3>\n

The deposits mainly contain ash and pumice: broken-up, bubbly rocks.\u00a0 The ash is fragmented pumice and looks like black sand or grit.\u00a0 All of this rock was hot enough to be liquid magma just moments before it erupted from the ground.\u00a0 A detailed look at some of the grains can tell us more about the eruption.<\/p>\n

The first photo shows tephra from a layer that was full of smooth brown spheres called accretionary lapilli<\/a>.\u00a0 If you cut one open, you find concentric rings (like in a gobstopper or an onion) of very fine ash grains.\u00a0 These form as the ash is swirled around in the turbulent plume.\u00a0 Helped by moisture, fine grains stick to the outside of the growing lapillus, building it up layer by layer.<\/p>\n

It is important to understand accretionary lapilli because if these fine ash grains are sticking together and falling out onto the glacier then they aren’t drifting off downwind to bother European airports.<\/p>\n

\"\"<\/a>
\nThe second photo shows a piece of golden-coloured pumice.\u00a0 It is very lightweight and contains millions of tiny bubbles.\u00a0 This is unusual for basaltic tephra, which commonly has only a few, large bubbles.\u00a0 Bubbles in volcanic rocks form when gases dissolved in the magma are released (exsolved), usually in response to decreasing pressure as the magma rises up from depth.\u00a0 Thermodynamically, it is much easier for exsolving gas to join an existing bubble than to form a new one, so pumice with lots of tiny bubbles tells us that the gas was all trying to get out in a hurry.<\/p>\n

\"\"<\/a>The golden pumice therefore means that the magma rose very quickly from deep beneath the volcano.\u00a0 This is consistent with the very intense eruption.\u00a0 Geochemists can measure how much gas is still dissolved in the rock, and how much is dissolved in material trapped inside crystals that formed at depth.\u00a0 From this, they can estimate the depth at which the magma was stored before the eruption, and how much gas (such as SO2<\/sub>) was released.<\/p>\n

The southern crevasse field<\/h3>\n

Great volumes of ice near the crater was melted during the eruption.\u00a0 Since then, the glacier has flowed back toward the crater, producing a network of crevasses on the surface.\u00a0 Unlike crevasses in a more alpine setting, tephra has fallen into and filled these ones, allowing the area to be explored in relative safety.\u00a0 Unlike crevasses in a more alpine setting, these ones have steam coming out of them.\u00a0 Just a few centimetres down, the tephra pile here is still warm.<\/p>\n

\"\"<\/a>
\nThe long, tall walls produced by the crevasses are a volcanologists dream, as they expose all the individual layers produced by different stages of the eruption.\u00a0 These can be traced and measured over a wide area without the need for any digging whatsoever.\u00a0 Here, the deposit is rich in pale-grey, angular, dense rocky chunks, 10s of centimetres in diameter.\u00a0 These were cold pieces of old lava flows or other parts of the volcano that were ripped up and spat out during the eruption.\u00a0 They are heavy, and rained out from the plume close to the vent.<\/p>\n

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

A view of the crater area<\/h3>\n
\"\"<\/a>

Looking across the crater area. Click for bigger version<\/p><\/div>\n

The photo shows the crater area, looking from the west.\u00a0 The crevassed area in the foreground, with all the exposed tephra layers is clear.\u00a0 The ridge on the skyline is Mt Gr\u00edmsfjall, and the huts are located at the far end.\u00a0 The cliff is about 200 m high.\u00a0 The eruption began along a 1.5 km fissure running parallel to the cliff, before focussing on a few craters.<\/p>\n

The lower, flat, area of ice sits mainly on top of the permanent subglacial lake, Gr\u00edmsv\u00f6tn, which is kept from freezing by geothermal heat at the base.\u00a0 The water drains periodically from Gr\u00edmsv\u00f6tn in floods called j\u00f6kulhlaups<\/a>.\u00a0 The lake in the foreground has formed since the May 2011 eruption by surface water flowing in, and has flooded the site of the craters.\u00a0 The black area at the far end of the lake is not a beach, but a raft of floating pumice stones.\u00a0 The vertical ice cliffs are capped with tens of metres of tephra, and sometimes come crashing down into the lake.<\/p>\n

It is a spectacular place.<\/p>\n

The journey to Gr\u00edmsv\u00f6tn is described in the previous post (Gr\u00edmsv\u00f6tn 1 – Crossing the glacier<\/a>) as well as the effect of the tephra on the glacier.\u00a0 The following post (Gr\u00edmsv\u00f6tn 3 – Bonus truck pictures<\/a>) describes the difficulties of working on the tephra-covered glacier.<\/p>\n","protected":false},"excerpt":{"rendered":"

The May 2011 Gr\u00edmsv\u00f6tn eruption blasted ash and pumice and rock fragments (collectively known as tephra) through the Vatnaj\u00f6kull glacier, forming a massive plume up to 20 km tall.\u00a0 It was the biggest eruption in Iceland since Hekla 1947.\u00a0 Locally, … 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-344","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/344","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=344"}],"version-history":[{"count":9,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/344\/revisions"}],"predecessor-version":[{"id":384,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/posts\/344\/revisions\/384"}],"wp:attachment":[{"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/media?parent=344"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/categories?post=344"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/all-geo.org\/volcan01010\/wp-json\/wp\/v2\/tags?post=344"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}