Volcanology Landslides Tectonic Plates Sinkholes Natural Disasters Volcanoes Seismic Activity Tectonics Volcanic Activity Seismology Glaciers Natural Hazards Soil Stability Rockfalls Rock Formations Land Subsidence Tectonic Activity Soil Erosion Erosion Mining Geological Hazards Planetary Geology Soil Types Fault Lines Sedimentary Rocks Mineralogy Soil Composition Fossil Formation Geological Features Earth's Mantle Radioactive Waste Rockslides Land Movement Seismic Zones Natural Resources Earthquakes Ground Subsidence Grand Canyon Permafrost Lunar Geology Earth's Crust Magma Accumulation Instability Soil Movement Landslide Hazard Management Plate Tectonics Urban Planning Sedimentology Fossilization Soil Conditions Cave Systems Soil Behavior Natural Calamities Geomorphology Flooding Hydrology Geological Conditions Waste Disposal Groundwater Geothermal Resources Ancient Rocks Landslide Risk Coastal Geology Geological Formations Volcanic Islands Sandstone Natural Landmarks Subterranean Features Sinkhole Formation Tsunamis Fossil Beds Landforms Fossilization Processes Paleoenvironment Martian Geology Landslide Risks Geological Processes Construction Impact Rock Composition Environmental Geology Seismic Studies Geochemical Cycles Volcanic Soil Fossils Sedimentary Environments Fossil Preservation Mine Management Lakes Planetary Environments Natural Events Coastal Geography Soil Science Subsurface Environments Fossil Sites Mountain Geology Landslide Management Land Stability Mountainous Regions Topography Cliff Erosion
New stress and strain data clarify the region’s plate‑boundary geometry, pointing to targets for mapping active faults.
