<?xml version='1.0' encoding='utf-8'?>
<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>Jorge Alpala</dc:contributor>
  <dc:contributor>Rosa Alpala</dc:contributor>
  <dc:contributor>Mario Angarita</dc:contributor>
  <dc:contributor>Dario Arcos</dc:contributor>
  <dc:contributor>Leonardo Eullides</dc:contributor>
  <dc:contributor>Pablo Euillades</dc:contributor>
  <dc:contributor>Cyrill Mueller</dc:contributor>
  <dc:contributor>Lourdes Narvaez</dc:contributor>
  <dc:creator>Maurizio Battaglia</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>&lt;p id="sp0235"&gt;Whereas research in volcano geodesy seeks to push the boundaries of our knowledge of the physics of volcanoes, monitoring looks at changes in volcano behavior to predict when a volcanic crisis might develop. To be effective, geodetic monitoring must be done before, during, and after eruptions and must be integrated with other&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;a title="Learn more about Monitoring Technique from ScienceDirect's AI-generated Topic Pages" href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/monitoring-technique" data-mce-href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/monitoring-technique"&gt;monitoring techniques&lt;/a&gt;&lt;span&gt;. It requires the type of long-term commitment of time and resources that academic and industry scientists generally cannot make. A few, well-placed geodetic&amp;nbsp;&lt;a title="Learn more about Monitoring Station from ScienceDirect's AI-generated Topic Pages" href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/monitoring-station" data-mce-href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/monitoring-station"&gt;monitoring stations&lt;/a&gt;&amp;nbsp;can make a huge difference to a country's ability to alert its people to an imminent&amp;nbsp;&lt;a title="Learn more about Volcanic Eruption from ScienceDirect's AI-generated Topic Pages" href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/volcanic-eruption" data-mce-href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/volcanic-eruption"&gt;volcanic eruption&lt;/a&gt;.&lt;/span&gt;&lt;/p&gt;&lt;p id="sp0240"&gt;&lt;span&gt;Monitoring strategies vary greatly depending on several factors such as the activity of the individual volcano, access, and available personnel and funding. Rapid advances in technology allow for more precise geodetic monitoring today than was imaginable when many of the existing volcano&amp;nbsp;observatories&amp;nbsp;were established. Today,&amp;nbsp;&lt;/span&gt;deformation&lt;span&gt;&amp;nbsp;measurements at active volcanoes are usually made with continuous&amp;nbsp;Global Positioning System&amp;nbsp;(CGPS) stations, supplemented by Interferometric Synthetic Aperture Radar (InSAR) images. Neither method requires a continuous presence of personnel in the field, except for the installation and maintenance of the&amp;nbsp;GPS&amp;nbsp;stations; however subsequent data analysis can be highly complex.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/B978-0-12-409548-9.10902-9</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Monitoring volcanic deformation</dc:title>
  <dc:type>chapter</dc:type>
</oai_dc:dc>