Wind‐direction data allow us to select time intervals of stable wind direction.

Selected data can be inverted for shallow elastic structure by the moving pressure model.

If wind data were not available, one can still make a good estimate for structure by analyzing the high‐pressure‐end of data.

New triaxial and CT data are presented on Indiana limestone of porosity 16%.

Digital Volume Correlation reveals several complex failure modes involving shear bands through the brittle‐ductile transition.

The onset of inelastic compaction in dual porosity allochemical limestones is in agreement with the normality condition.

In 2017, up to 12 cm of LOS displacement occurred at the Whitewater groundwater entrainment site.

We compare methods for inferring 3D velocities from 1D InSAR measurements.

The Garnet Hill Fault experienced increased right‐lateral sense of shear in some areas.

A new 3‐D Vs model of northern Taiwan is constructed using Rayleigh wave H/V ratios and phase velocities

The addition of H/V ratio measurements allows detailed shallow crustal structure to be resolved with sub‐kilometer depth resolution

The resolved fine crustal structures provide new geometrical constraints on basin formation and orogeny dynamics

Thermal radiation spectra record nongray interaction with bridgmanite in laser‐heated diamond anvil cells

Radiometric temperature of nongray bridgmanite in laser‐heated diamond anvil cells is up to 5‐10 % off the maximum sample temperature

Extant melting curves and experimental phase transition boundaries in the bridgmanite system contain this systematic error in temperature

An improved InSAR troposphere correction method proposed, based on Global Atmospheric Models (GAM), that considers spatial stochastic properties of the troposphere at different altitude levels for better weighting the GAM samples.

Comparisons with three other GAM corrections (PyAPS, d‐LOS, and GACOS) show a significant reduction in average standard deviation of corrected interferograms and better time‐series analysis results.

The results demonstrate the importance of considering horizontal heterogeneities and spatial stochastic models of the troposphere when using GAM‐corrections.

InSAR time‐series and seismicity analyses of deformation at the Afrera Plain linkage zone in Northern Afar, Ethiopia

Time‐series show fault slip accommodated through stick‐slip and creep along en‐echelon NS‐striking faults

Varying fault behavior could be influenced by elevated heat flows and hydrothermal circulation near the magmatic segments

We use convection models with plate motion history to constrain the mantle viscosity, both its relative variations and absolute values.

Strong plate and weak plate margins with non‐uniform viscosity are critical in reproducing the geoid and surface plate motion.

The lower mantle viscosity is ∼1.3‐2.5× 10^22 Pa·s and ∼30 and ∼600‐1000 times higher than that in the transition zone and asthenosphere.

Single‐crystal elastic properties of omphacite were measured for the first time at high P‐T conditions.

Undeformed eclogite is seismically invisible at 210‐300 km 400‐500 km depth range.

Modeled seismic anisotropy of deformed eclogite can be as high as 4‐5% in the uppermost mantle.

Strain localizes into viscous slip zones that delimit coarser‐grained, cataclastic lenses.

Viscous flow is enabled by a microstructural transformation from microcrystalline to nanocrystalline, partly amorphous material in the slip zones.

Both viscous and brittle processes have to operate in parallel to accommodate deformation