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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>J.-L. Bourdier</dc:contributor>
  <dc:contributor>B. Voight</dc:contributor>
  <dc:creator>E.K. Abdurachman</dc:creator>
  <dc:date>2000</dc:date>
  <dc:description>&lt;p&gt;Nu&amp;eacute;es ardentes associated with dome collapse on 22 November 1994, at Merapi volcano traveled to the south&amp;ndash;southwest as far as 6.5&amp;nbsp;km, and collectively accumulated roughly 2.5&amp;ndash;3 million cubic meters of deposits. The damaged area comprises 9.5&amp;nbsp;km&lt;sup&gt;2&lt;/sup&gt; and is covered by two nu&amp;eacute;e ardente facies, a conventional &amp;ldquo;Merapi-type&amp;rdquo;, valley-fill block-and-ash flow facies and a pyroclastic surge facies. The proximal deposits reflect the accumulation of dozens of nu&amp;eacute;es ardentes, with many subsidiary flow units. The distal deposits are more simply organized, as only a few individual events reached to distances &amp;gt;3.5&amp;nbsp;km. The stratigraphic relationships north of Turgo hill indicate that the surge deposits are a facies of particularly mobile nu&amp;eacute;es ardentes that also deposited channeled block-and-ash flow facies. They further suggest that the surge facies beyond the channel margins correlate laterally with a finer-grained sublayer locally developed at the base of the block-and-ash flow facies. Eyewitness reports suggest that the emplacement of the block-and-ash flow facies in the distal part of the Boyong river may have followed, by a short time interval, the destruction and deposition of the surge facies at Turgo village. The stratigraphy is in accord with the eyewitness reports. The surge facies was emplaced by a dilute surge current, detached from the same dome-collapse nu&amp;eacute;e ardente that, as a separate flow unit, subsequently emplaced the distal block-and-ash deposit in the Boyong valley. The detachment occurred at higher elevations, likely at or above the slope break at about 2000&amp;nbsp;m elevation. This flow separation enabled the surge current to shortcut over the landscape and to emplace its deposit even as the block-and-ash flow continued its tortuous southward movement in the Boyong channel. Dome-collapse nu&amp;eacute;e ardente activity formed the bulk of the eruption, which was accompanied by virtually no significant vertical summit explosive activity.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/S0377-0273(00)00144-X</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Nuées ardentes of 22 November 1994 at Merapi volcano, Java, Indonesia</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>