This event is in the past.It took place on May 14, 2026 at Stanford Court San Francisco.


Dilatant hydro-shearing fracture growth - theory & observations
Nob Hill
Earthquakes, geothermal power, and glacier movement share a surprising connection: how pressurized fluids crack rock. This free Stanford talk breaks down the physics behind fluid-driven ruptures in plain terms.
geoscience research talk
free admission
lunch hour event
academic lecture
Tips
🆓free and open to all
⏰perfect lunch hour length
Free
Dilatant hydro-shearing fracture growth - theory & observations
Nob Hill


Earthquakes, geothermal power, and glacier movement share a surprising connection: how pressurized fluids crack rock. This free Stanford talk breaks down the physics behind fluid-driven ruptures in plain terms.
geoscience research talk
free admission
lunch hour event
academic lecture
Tips
🆓free and open to all
⏰perfect lunch hour length
Free
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