Reply to “Comment on ‘If Not Brittle: Ductile, Plastic, or Viscous?’ by Kelin Wang” by Marco A. Lopez‐Sanchez, Sylvie Demouchy, and Catherine Thoraval

Lateral variation in slab window viscosity inferred from global navigation satellite system (GNSS)–observed uplift due to recent mass loss at Patagonia ice fields

If Not Brittle: Ductile, Plastic, or Viscous?

Seismic Characteristics of the Nootka Fault Zone: Results from the Seafloor Earthquake Array Japan–Canada Cascadia Experiment (SeaJade)

Spatiotemporal Variation of Crustal Anisotropy in the Source Area of the 2004 Niigata, Japan Earthquake

Diagenetic, metamorphic, and hydrogeologic consequences of hydrothermal circulation in subducting crust

Revising Estimates of Spatially Variable Subsidence during the A.D. 1700 Cascadia Earthquake Using a Bayesian Foraminiferal Transfer Function

Learning from crustal deformation associated with the M9 2011 Tohoku-oki earthquake

Fracture Alignments in Marine Sediments Off Vancouver Island from Ps Splitting Analysis

Beating Fear with Hope: On Sustaining Earthquake Preparedness

Do subducting seamounts generate or stop large earthquakes?

Intertidal Biological Indicators of Coseismic Subsidence during the M w 7.8 Haida Gwaii, Canada, Earthquake

GPS Observations of Crustal Deformation Associated with the 2012 M w 7.8 Haida Gwaii Earthquake

Thermal Condition of the 27 October 2012 M w 7.8 Haida Gwaii Subduction Earthquake at the Obliquely Convergent Queen Charlotte Margin

Earthquake Activity in Northern Cascadia Subduction Zone Off Vancouver Island Revealed by Ocean‐Bottom Seismograph Observations

Earthquake Preparedness Should Not Fluctuate on a Daily or Weekly Basis

Simulated tsunami inundation for a range of Cascadia megathrust earthquake scenarios at Bandon, Oregon, USA

Do subducting seamounts generate or stop large earthquakes?

The 2008 Wenchuan Earthquake and Earthquake Prediction in China

Intraslab Stresses in the Cascadia Subduction Zone from Inversion of Earthquake Focal Mechanisms