Featured
-
-
Comment |
Manage fire regimes, not fires
Globally, land- and fire-management policies have counterproductively caused cascading ecosystem changes that exacerbate, rather than mitigate, wildfires. Given rapidly changing climate and land-use conditions that amplify wildfire risk, a policy shift to adaptive management of fire regimes is urgently needed.
- Mark A. Cochrane
- & David M. J. S. Bowman
-
Article |
Submarine landslides triggered by iceberg collision with the seafloor
Iceberg gouging of continental slopes can initiate submarine landslides, potentially far from the iceberg source region, according to observations and geotechnical analysis of an event in a Baffin Island fjord.
- Alexandre Normandeau
- , Kevin MacKillop
- & John Hughes Clarke
-
Article |
Simple shear origin of the cross-faults ruptured in the 2019 Ridgecrest earthquake sequence
Asymmetric rotation of faults in the Eastern California Shear Zone may result from simple shear, according to an analysis of deformation in the area of the 2019 Ridgecrest earthquake sequence in combination with regional geological data.
- Yuri Fialko
- & Zeyu Jin
-
News & Views |
Calving prediction from ice mélange motion
High-frequency radar tracking of icebergs floating in front of a glacier in Greenland show that movements of the ice mélange consistently increase before calving events, indicating that mélange has the potential to modulate calving.
- Irena Vaňková
-
Article |
Coseismic fault lubrication by viscous deformation
Viscous deformation is a potentially prevalent mechanism of fault lubrication during earthquakes, according to laboratory experiments that simulate seismic faulting of various rock-forming minerals.
- Giacomo Pozzi
- , Nicola De Paola
- & Sylvie Demouchy
-
Editorial |
Megathrusts exhumed
Plate boundary faults in subduction zones can generate large earthquakes and tsunamis. Recent studies have revealed that these faults slip in various ways and may be influenced by many factors. Better understanding them should improve hazard assessments.
-
Article |
Correlation of porosity variations and rheological transitions on the southern Cascadia megathrust
The transition between the locked and slowly slipping regions of the southern Cascadia megathrust has a lower porosity than these regions, according to seismic imaging. This suggests that the transition area is ductile, which may limit rupture propogation.
- Hao Guo
- , Jeffrey J. McGuire
- & Haijiang Zhang
-
Article |
Abrupt Southern Great Plains thunderstorm shifts linked to glacial climate variability
Thunderstorm activity in the Southern Great Plains was closely coupled to abrupt climate shifts during the last glacial period, according to an analysis of oxygen isotopes in modern rainfall and ancient speleothems from Texas.
- Christopher R. Maupin
- , E. Brendan Roark
- & Judson W. Partin
-
Article |
Physical conditions and frictional properties in the source region of a slow-slip event
A shallow slow-slip source region has laterally variable elastic properties and pore pressure, and near-velocity-neutral frictional properties, according to seismic imaging of part of the Hikurangi subduction margin and data-constrained modelling.
- Adrien F. Arnulf
- , James Biemiller
- & Andreia Plaza Faverola
-
News & Views |
Unrushed megathrusts
Corals reveal that part of the plate-boundary fault near Sumatra slipped slowly and quietly for three decades before a large earthquake in 1861. The exceptional duration of this slip event has implications for interpreting deformation to assess seismic hazard.
- Daniel Melnick
-
Article |
Slip rate deficit and earthquake potential on shallow megathrusts
Shallow parts of megathrusts up-dip of locked patches generally have a high slip rate deficit, which could mean tsunami hazard has been underestimated, according to a stress-constrained inversion of geodetic data.
- Eric O. Lindsey
- , Rishav Mallick
- & Emma M. Hill
-
Article |
Long-lived shallow slow-slip events on the Sunda megathrust
A 32-year-long slow-slip event occurred on a shallow part of the Sunda megathrust, perhaps because of stress accumulation after fluid expulsion, according to an analysis of the deformation history of the area and physics-based simulations.
- Rishav Mallick
- , Aron J. Meltzner
- & Emma M. Hill
-
News & Views |
Stressed rocks cause big landslides
Near-surface stress patterns, influenced by topography, control the size and location of the largest landslides — but not necessarily smaller ones — according to a study of mountains at the eastern edge of the Tibetan Plateau.
- Peter van der Beek
-
Article |
Topographic stress control on bedrock landslide size
Stress from tectonics and topography may be the primary control on the size of bedrock landslides, according to a comparison of a stress model with landslide inventories for a mountainous area in eastern Tibet.
- Gen K. Li
- & Seulgi Moon
-
Article |
Subslab heterogeneity and giant megathrust earthquakes
Mantle heterogeneity beneath subducting plates may influence giant megathrust earthquakes, according to seismic tomography of the subslab structure beneath six megathrusts that have ruptured in M ≥ 9.0 earthquakes.
- Jianke Fan
- & Dapeng Zhao
-
Article |
Spatiotemporal clustering of great earthquakes on a transform fault controlled by geometry
The rupture mode between major and great earthquakes is controlled by transform fault geometry, according to simulations of a reconstructed record of 20 palaeoearthquakes along the Alpine Fault, New Zealand.
- Jamie D. Howarth
- , Nicolas C. Barth
- & Rupert Sutherland
-
News & Views |
Magma behaving brittly
Low viscosities may not preclude brittle magma fragmentation under certain conditions, according to field observations and experimental evidence that suggest the conditions for brittle fragmentation may be met in many explosive mafic eruptions.
- Emma J. Liu
-
Article |
Fracturing and healing of basaltic magmas during explosive volcanic eruptions
In explosive basaltic eruptions, brittle fragmentation and subsequent healing by viscous melt are documented by textural analysis of products from ten disparate eruptions, suggesting that grain size may not reflect the initial fracture density of magma.
- J. Taddeucci
- , C. Cimarelli
- & F. Di Stefano
-
Article |
Brittle fragmentation by rapid gas separation in a Hawaiian fountain
In a Hawaiian fountain eruption, rapid gas expansion cools the melt below the glass transition temperature and causes brittle magma fragmentation, producing small, vesicular pyroclasts, according to observations of the 2018 eruption of Kīlauea.
- Atsuko Namiki
- , Matthew R. Patrick
- & Bruce F. Houghton
-
Article |
Large-scale thermal unrest of volcanoes for years prior to eruption
Large-scale radiant heat flux increased in the years prior to eruptions at five volcanoes, probably due to enhanced underground hydrothermal activity, according to an analysis of satellite infrared data.
- Társilo Girona
- , Vincent Realmuto
- & Paul Lundgren
-
News & Views |
Fidelity of turbidites as earthquake records
Turbidites record ground motion in the 2016 Kaikōura earthquake. Recent events are now revealing how turbidites record earthquakes, but turbidites are triggered in many ways, and testing if ancient turbidites are earthquake-triggered remains challenging.
- Peter J. Talling
-
Article |
Calibrating the marine turbidite palaeoseismometer using the 2016 Kaikōura earthquake
Marine turbidite deposition is confirmed to relate to earthquake ground motions by an analysis of turbidite deposits and simulations of ground motions from the 2016 Kaikōura earthquake.
- Jamie D. Howarth
- , Alan R. Orpin
- & M. Namik Cağatay
-
Editorial |
Mountains of change
The world’s glaciers are shrinking, with knock-on impacts for local communities. We need a better grasp of the hazards they leave behind.
-
Article |
Increased outburst flood hazard from Lake Palcacocha due to human-induced glacier retreat
Human-induced warming is responsible for the retreat of Palcaraju glacier and the associated increase in glacial lake outburst flood hazard, according to an analysis of observations and numerical models.
- R. F. Stuart-Smith
- , G. H. Roe
- & M. R. Allen
-
Comment |
Paleofloods stage a comeback
Geological and botanical archives can preserve evidence of exceptional floods going back centuries to millennia. Updated risk guidelines offer a new opportunity to apply lessons from paleoflood hydrology to judge the odds of future floods.
- Scott St. George
- , Amanda M. Hefner
- & Judith Avila
-
Article |
Increased typhoon activity in the Pacific deep tropics driven by Little Ice Age circulation changes
Atmospheric circulation shifts during the Little Ice Age led to greater typhoon generation in the tropical North Pacific according to a comparison of sediment proxy records of past storm activity and outputs of general circulation models.
- James F. Bramante
- , Murray R. Ford
- & Jeffrey P. Donnelly
-
Article |
Continuum of earthquake rupture speeds enabled by oblique slip
Long fault ruptures that have both strike-slip and dip-slip components can propagate at a wide range of speeds, including those theoretically predicted to be unstable, according to numerical simulations.
- Huihui Weng
- & Jean-Paul Ampuero
-
News & Views |
Inelastic earthquake damage
Permanent surface deformation caused by the 2019 Ridgecrest earthquakes has been directly measured, constraining the mechanics of surface damage in earthquakes.
- Wanpeng Feng
- & Rafael V. Almeida
-
Article |
Localized fault-zone dilatancy and surface inelasticity of the 2019 Ridgecrest earthquakes
Inelastic failure in the 2019 Ridgecrest earthquakes was localized and influenced by mylonitic deformation of the fault damage zone, according to an analysis of surface displacements derived from satellite images.
- William D. Barnhart
- , Ryan D. Gold
- & James Hollingsworth
-
Editorial |
From our homes to yours
The ongoing COVID-19 global pandemic highlights the very human effort that is peer review. We will continue to do all we can to keep the papers flowing and thank our reviewers and authors for their help and understanding under these difficult circumstances.
-
Article |
Larger tsunamis from megathrust earthquakes where slab dip is reduced
Tsunami generation by megathrust earthquakes is enhanced by extensional faulting in the upper plate when the subducting slab shallows, according to numerical modelling and observations from the Sumatra–Andaman and Tohoku earthquake–tsunami events.
- Bar Oryan
- & W. Roger Buck
-
Article |
Mechanical and hydrological effects of seamount subduction on megathrust stress and slip
Changing stresses and pore fluid pressures during subduction of seamounts, as simulated with a numerical model that couples mechanical and hydrological processes, help explain observed patterns of megathrust slip.
- Tianhaozhe Sun
- , Demian Saffer
- & Susan Ellis
-
Article |
Earthquakes and tsunamis caused by low-angle normal faulting in the Banda Sea, Indonesia
Low-angle normal faults in the Banda Sea have caused large earthquakes that indirectly generated tsunamis due to earthquake-triggered submarine slumping, according to an analysis of historical earthquake and tsunami events and GPS observations.
- Phil R. Cummins
- , Ignatius R. Pranantyo
- & Siyuan Zhao
-
Article |
Carbon release through abrupt permafrost thaw
Analyses of inventory models under two climate change projection scenarios suggest that carbon emissions from abrupt thaw of permafrost through ground collapse, erosion and landslides could contribute significantly to the overall permafrost carbon balance.
- Merritt R. Turetsky
- , Benjamin W. Abbott
- & A. David McGuire
-
Article |
Irrigation-triggered landslides in a Peruvian desert caused by modern intensive farming
Slow-moving landslides in two valleys in Peru were initiated by irrigation programmes in the region, suggest analyses of 40 years of satellite data.
- Pascal Lacroix
- , Amaury Dehecq
- & Edu Taipe
-
Article |
Duplex in the Main Himalayan Thrust illuminated by aftershocks of the 2015 Mw 7.8 Gorkha earthquake
The Main Himalayan Thrust comprises two fault planes connected by imbricated faults, a structure that impedes convergence, according to an analysis of the distribution and orientation of aftershocks of the 2015 Gorkha earthquake in Nepal.
- M. M. Mendoza
- , A. Ghosh
- & A. Velasco
-
Article |
Infrasound from giant bubbles during explosive submarine eruptions
During the submarine eruption of gas-rich magma into shallow water, a gas-tight seal forms, breaks and reseals, a process that results in violent explosions and the release of large gas bubbles, suggest low-frequency sound data from Bogoslof volcano, Alaska.
- John J. Lyons
- , Matthew M. Haney
- & Christopher F. Waythomas
-
Article |
Australian hot and dry extremes induced by weakenings of the stratospheric polar vortex
Hot and dry climate extremes in Australia are linked to stratospheric polar vortex weakening, with potential implications for their predictability, according to statistical analyses of observational data from the past 40 years.
- Eun-Pa Lim
- , Harry H. Hendon
- & Julie M. Arblaster
-
News & Views |
Irrigation and the Palu landslides
Wet rice cultivation in the Palu Valley, Indonesia, prepared the ground for the devastating liquefaction-induced landslides that were triggered by the Mw 7.5 earthquake in 2018, suggest two studies of the spatial relationship between landslide morphology and irrigation.
- Phil R. Cummins
-
Article |
Impact of communal irrigation on the 2018 Palu earthquake-triggered landslides
Landslides triggered during the Palu 2018 earthquake correlate spatially with the presence of irrigation systems according to satellite analyses, suggesting that liquefaction of alluvial fans played a role.
- Ian M. Watkinson
- & Robert Hall
-
Article |
The susceptibility of Oklahoma’s basement to seismic reactivation
Seismicity induced by wastewater injections is widespread in Oklahoma, probably because its basement is susceptible to the reactivation of basement-rooted faults, according to three-dimensional seismic analyses, rock-mechanics experiments and field surveys.
- F. Kolawole
- , C. S. Johnston
- & B. M. Carpenter
-
Article |
Amplification of mega-heatwaves through heat torrents fuelled by upwind drought
The European mega-heatwaves in 2003 and 2010 were intensified by torrents of hot air that were transported in from desiccated regions upwind, suggests an analysis of observations and reanalysis data together with a Lagrangian heat-tracking framework.
- Dominik L. Schumacher
- , Jessica Keune
- & Diego G. Miralles
-
Comment |
Geoscience analysis on Twitter
Social media is increasingly being used to share near-real-time analysis of emergent and sometimes hazardous geological events. Such open discussion can drive new research directions and collaborations for geoscientists.
- Stephen P. Hicks
-
Editorial |
Experiment to save lives
Geohazards can be too dangerous to study directly but too deadly to ignore. For these types of events, data from physical experiments can plug gaps in both hazard models and understanding.
-
News & Views |
Travel on thin air
Pyroclastic density currents generate a basal air cushion that reduces friction with the ground, reveal laboratory experiments. This explains their ability to travel rapidly over large distances from their volcanic source.
- Alain Burgisser
-
Article |
Generation of air lubrication within pyroclastic density currents
Pyroclastic density currents are able to travel large distances because they generate their own air lubrication, according to large-scale laboratory experiments.
- Gert Lube
- , Eric C. P. Breard
- & Ting Wang
-
Article |
Increased landslide activity on forested hillslopes following two recent volcanic eruptions in Chile
A delayed increase of landslide activity occurred about two to six years after two volcanic eruptions in Chile in 2008 and 2011, according to remote-sensing data. The time lag is consistent with decaying tree roots in areas covered by tephra.
- Oliver Korup
- , Jan Seidemann
- & Christian H. Mohr
-
News & Views |
Supershear tsunami disaster
A magnitude 7.5 strike-slip earthquake that struck Palu, Indonesia, in 2018 unexpectedly generated a devastating tsunami. Seismic data reveal that its rupture propagated fast, at supershear speed. Whether the two are connected remains to be seen.
- P. Martin Mai
-
Article |
Early and persistent supershear rupture of the 2018 magnitude 7.5 Palu earthquake
Supershear rupture speed occurred at the devastating 2018 magnitude 7.5 Palu earthquake, Indonesia, according to back-projection of teleseismic data.
- Han Bao
- , Jean-Paul Ampuero
- & Hui Huang