Numerical simulation of basaltic lava flows in the Auckland Volcanic Field, New Zealand—implication for volcanic hazard assessment Gábor KereszturiAnnalisa CappelloShane J. Cronin Research Article 15 October 2014 Article: 879
Spatial distribution and structural analysis of vents in the Lunar Crater Volcanic Field (Nevada, USA) A. TadiniF. L. BonaliG. A. Valentine Research Article 19 October 2014 Article: 877
Pahoehoe to `a`a transition of Hawaiian lavas: an experimental study A. SehlkeA. WhittingtonE. Médard Research Article 17 October 2014 Article: 876
Craters of elevation revisited: forced-folds, bulging and uplift of volcanoes B. van Wyk de VriesA. MárquezA. Delcamp Research Article 07 October 2014 Article: 875
Determining change points in data completeness for the Holocene eruption record Stuart MeadChristina Magill Research Article 08 October 2014 Article: 874
Magma flow paths and strain patterns in magma chambers growing by floor subsidence: a model based on magnetic fabric study of shallow-level plutons in the Štiavnica volcano–plutonic complex, Western Carpathians Filip TomekJiří ŽákMartin Chadima Research Article 08 October 2014 Article: 873
Replenishment of volatile-rich mafic magma into a degassed chamber drives mixing and eruption of Tungurahua volcano Madison L. MyersDennis J. GeistJosef Dufek Research Article 07 October 2014 Article: 872
Reply to comment from Liotta and Rizzo on “Evolution of CO2, SO2, HCl and HNO3 in the volcanic plumes from Etna” by Voigt et al. [Geophys. Res. Lett.; 41, doi:10.1002/2013GL058974] C. VoigtP. JessbergerG. Salerno Reply Open access 08 October 2014 Article: 865
Comment on “Evolution of CO2, SO2, HCl and HNO3 in the volcanic plumes from Etna” by Voigt et al. [Geophys. Res. Lett.; 41, doi:10.1002/2013GL058974] Marcello LiottaAndrea Luca Rizzo Comment 08 October 2014 Article: 864