Resources: All

Find a resource
  1. Stromboli online

    29 Jun 2011 | Contributor(s): Roberto Carniel

    Stromboli online - Volcanoes of the World http://stromboli.net The primary goal of Stromboli online website is to enrich and stimulate the teaching of Earth Sciences by presenting images, movies, data, virtual field trips and other educational material in relation to volcanoes.Although there is...

  2. Structural architecture and the episodic evolution of the ediacaran Campo Alegre Basin (southern Brazil): Implications for the development of a synorogenic foreland rift and a post-collisional caldera volcano

    09 Apr 2021 | Contributor(s): Lucas Martins Lino, Francy Roxana Quiroz-Valle, Vinicius Abud louro, Miguel Ângelo Stipp Basei, Silvio Roberto Farias Vlach, Mathias Hueck, Patricio Rodrigo Montecinos Munõz, Sérgio Brandolise Citroni

    During the last decades, tectonic models provided new insight into the evolution of the Luis Alves, Curitiba, and Paranaguá terranes, which are all limited by thrust and transpressive shear zones, nowadays outcropping only as deep crustal horizons and presenting poorly known lateral...

  3. STRUCTURAL CONTROLS OF MONOGENETIC VOLCANISM

    04 Sep 2013 | Contributor(s): Adelina Geyer Traver

    The factors controlling the precursory activity in monogenetic volcanic fields are still poorly understood, which means that eruption forecasts in these systems are not very accurate. The fact that in monogenetic volcanism each eruption has a different vent suggests that volcanic susceptibility...

  4. STRUCTURAL CONTROLS ON MONOGENETIC VOLCANISM: THE GARROTXA VOLCANIC FIELD CASE STUDY

    04 Sep 2013 | Contributor(s): Xavier Bolos, Stephanie Barde-Cabusson, Jo Gottsmann, Joan Marti, Dario Pedrazzi, Llorenç Planaguma, Antonio Camacho, Adelina Geyer Traver, Erika Ronchin

    The factors controlling the precursory activity in monogenetic volcanic fields are still poorly understood, which makes that eruption forecasts in these systems is not very accurate. The fact that in monogenetic volcanism each eruption has a different vent suggests that volcanic susceptibility...

  5. Supplementary material for Newhall and Pallister (2014) Using multiple data sets to populate probabilistic volcanic event trees

    27 Sep 2017 | Contributor(s): Chris Newhall, John S Pallister

    For probabilistic forecasting in volcanology, two widely used methods are the Cooke method (Aspinall and others) and BET-EF (Marzocchi and others).   The paper noted in the title, in Papale P (ed), Volcanic Hazards, Risks and Disasters. Academic Press, describes...

  6. Surface Deformation

    22 Feb 2011 | Educational Materials | Contributor(s): Chuck B Connor, Leah Michelle Courtland

    Chuck ConnorPeter LaFeminaC. Connor, P. LaFemina, Spreadsheets across the Curriculum: The Physical Volcanology Collection.

  7. Techniques to measure SO2 volcanic plumes and geometrical consideration

    29 Jun 2011 | Presentations | Contributor(s): Jose Luis Palma

    This presentation is part of the workshop "Volcanic Hazards and Remote Sensing in Pacific Latin America" held in Costa Rica in January 2011.Speaker: Lizzette RodriguezLizzette Rodriguez

  8. Tephra 2014 - Maximizing the potential of tephra for multidisciplinary science

    09 Jan 2014 | Workshops | Contributor(s): Steven Kuehn, Solene Pouget, Marcus I Bursik

    Tephra deposits are used by diverse communities: volcanologists, petrologists, tephrochronologists, paleoclimatologists, paleoecologists and archaeologists. To perhaps be too reductionist, volcanologists are generally interested in tephra to understand eruption behavior, frequency, and hazards;...

  9. Tephra 2014 Field Trip Guide

    08 Dec 2014 | Publications | Contributor(s): Stephen C Kuehn

    Guidebook for the field trip to Mount Saint Helens conducted 4-August-2014 as part of the Tephra 2014 workshop.

  10. Tephra 2014-2020 Document Repository

    01 Jul 2015 | Publications | Contributor(s): Marcus I Bursik, Solene Pouget, Stephen C Kuehn, Kristi L Wallace, Andrei V Kurbatov

    Beginning with the consensus document (with three appendices) resulting from the Tephra 2014 Workshop, this is the document repository for the Tephra 2014, 2017 and 2019 Workshops on standardization.The immediate goal of the tephra standardization effort is to translate checklists...

  11. Tephra 2017 Workshop : Best practices in tephra collection, analysis, and reporting leading toward better tephra databases

    15 Jun 2017 | Workshops | Contributor(s): Marcus I Bursik, Stephen C Kuehn, Kristi L Wallace, Andrei V Kurbatov

    Best practices in tephra collection, analysis, and reporting: Leading toward better tephra databasesThis is a page for the Tephra 2017 workshop, held in Portland, OR, 19 August 2017.  The workshop was a follow-on to the Tephra 2014 workshop, held 3-7 August 2014, also in...

  12. Tephra Impact Lab - Taupo Volcano

    06 Dec 2011 | Educational Materials | Contributor(s): Tom Wilson, Leah Michelle Courtland

    This lab requires students to produce a pre-eruption tephra risk assessment for Taupo volcano, using Tephra2. It requires students to consider the eruptive history of Taupo volcano and a volcanic unrest scenario is provided, so that students must decide what magnitude and style of eruption is...

  13. Tephra in Quaternary Science 2011 Edinburgh Workshop Report: The Eyjafjallajökull eruptions of 2010

    18 Aug 2011 | Publications | Contributor(s): Andrew Julian Dugmore, Anthony Newton, Kate Taylor Smith

    Report and Community Statement from the workshop on the Eyjafjallajokull eruptions of 2010 and implications for tephrochronology, volcanology and Quaternary studies, Institute of Geography, University of Edinburgh, 5th‐6th May 2011. The first meeting of Tephra in Quaternary Science (TIQS), the...

  14. Tephra inversion with Tephra2 and the Metropolis-Hastings algorithm

    21 Jun 2020 | Offline Tools | Contributor(s): Qingyuan Yang, E Bruce Pitman, Marcus I Bursik, Susanna Jenkins

    We couple the Metropolis-Hastings algorithm (Hastings, 1970) with the volcanic ash transport model Tephra2 (Bonadonna et al, 2005; 2010), and present the coupled algorithm as a new method to estimate the Eruption Source Parameters (ESPs) of volcanic eruptions based on mass per unit area...

  15. Tephra isopach, extent and volume calculation in R

    04 Mar 2016 | Offline Tools | Contributor(s): Qingyuan Yang, Marcus I Bursik

    The method presented here is used to interpolate the thickness distribution of tephra fall deposits from point measurements. It first reconstructs the general thickness decay pattern, or "trend," and then models the residuals that cannot be explained by the trend with...

  16. Tephra2

    20 Apr 2010 | *Tools | Contributor(s): Costanza Bonadonna, Laura Connor, Chuck B Connor, Leah Michelle Courtland

    Tephra2 uses the advection diffusion equation to forecast tephra dispersion in a given location based on a user-defined set of eruptive conditions.

  17. Tephra2 Probabilistic Runner

    29 Feb 2012 | *Tools | Contributor(s): Costanza Bonadonna, Laura J Connor, Chuck B Connor, Leah Michelle Courtland

    Will vary the wind field for a given eruption in order to determine the most probable mass loading of tephra on the ground.

  18. Tephra2 Source Code

    14 Jul 2010 | Offline Tools | Contributor(s): Chuck B Connor, Leah Michelle Courtland

    Tephra2 uses the advection diffusion equation to forecast tephra dispersion in a given location based on a user-defined set of eruptive conditions.Tephra2 codes are now maintained on GitHub: https://github.com/geoscience-community-codes/tephra2 Available are:1-processor...

  19. Tephra2 Worksheet IUGG

    18 Nov 2012 | Educational Materials | Contributor(s): Leah Michelle Courtland

    Worksheet for participants of Tephra2 workshop.

  20. Tephra2 _Plume ratio

    27 May 2013 | *Data Sets/Collections | Contributor(s): Ana María García

    Se realizaron 3 simulaciones de caída de ceniza para la erupción del volcán Nevado del Ruíz en el año 1985, cambiando el parámetro radio de la pluma por los valores 0-5-9,al comparar los resultados no se observan cambios