Results 51 to 60 of about 498 (148)
Abstract The scoria cones called Formica Leo located at the base of the Piton de la Fournaise terminal cone have been chosen for its significant positive Self‐Potential (SP) anomalies associated with hydrothermal uprising fluids to monitor SP signal and study its dynamics in relation with huge and extreme rainfall events.
Emilie Roulleau +12 more
wiley +1 more source
Megabeds in the Marsili Basin, Tyrrhenian Sea
Widepsread and thick megabeds occur in the Marsili Basin of the Tyrrhenian Sea. Megabeds are linked to volcanic eruptions. The Marsili megabeds are recorded by thick turbidites to complex and heterogeneous deposits. ABSTRACT Megabeds, also known as ‘megaturbidites,’ are exceptionally large submarine sediment deposits likely formed by catastrophic ...
Faye Higgins +2 more
wiley +1 more source
Abstract Methane (CH4) and carbon monoxide (CO) are gases with important climate impacts as direct and indirect greenhouse gases, respectively. Methane has a warming potential 28 times that of carbon dioxide on a 100‐year timescale, and carbon monoxide is a precursor to ozone in the troposphere.
Erin McGee +22 more
wiley +1 more source
Abstract Whakaari (White Island) volcano is the most active volcano in New Zealand with a dynamic hydrothermal system. The volcano has had four eruptive periods since 2014. In this study, our aim is to understand the pre‐and post‐eruption deformation processes occurring at Whakaari using interferometric synthetic aperture radar (InSAR).
Shreya Kanakiya +2 more
wiley +1 more source
Abstract We present a novel Deep Learning model based on recurrent neural networks (RNNs) with long short‐term memory (LSTM) cells, designed as a real‐time volcano‐seismic signal recognition system for distributed acoustic sensing (DAS) measurements. The model was trained on an extensive database of volcano‐tectonic events derived from the co‐eruptive ...
J. Fernández‐Carabantes +5 more
wiley +1 more source
Lava Lake Spattering Drives Seismic Tremor During the Geldingadalir 2021 Eruption, Iceland
Abstract Volcanic eruptions generate a continuous ground motion that is commonly referred to as tremor. Although tremor is used worldwide for real‐time monitoring of volcanoes, the mechanisms involved are generally poorly understood. Here, we study the episodic effusion during 2021 Geldingadalir eruption. We use photogrammetric data and videos acquired
Alea Joachim +5 more
wiley +1 more source
Abstract Marine volcanoes exhibit significant topographic relief, as they extend from deep below sea level to thousands of meters above. These volcanoes often have complex, asymmetric topographies due to the submersion of their flanks, yet deformation models often approximate this topographic surface as flat and overlook its effect in modeling ...
Megan Campbell +3 more
wiley +1 more source
Dynamical tools for the analysis of long term evolution of volcanic tremor at Stromboli
Stromboli is characterized by persistent seismic activity, both in terms of tremor and of discrete events associated with moderate explosions defining the so-called "Strombolian activity".
M. Di Cecca, R. Carniel
doaj +1 more source
Abstract A labeled data set of 216,681 infrasound detections was compiled using data from the Central and Eastern European Infrasound Network (CEEIN). Detections associated with quarry blasts, thunderstorms, eruptions of the Etna volcano, industrial activity, and the war in Ukraine were categorized using ground truth information, such as seismic and ...
Marcell Pásztor +7 more
wiley +1 more source
Abstract Magmatism is a known driver of flank instability at volcanoes where flank slip has been observed. Studies of instability at Kı̄lauea, Piton de la Fournaise, and Etna imply that long‐term flank motion likely requires the presence of a layer accommodating the sliding, and a force, such as magma intrusion, that promotes slip.
J. Gonzalez‐Santana +3 more
wiley +1 more source

