Page 2: Research news on subsidence

Subsidence, as a geophysical phenomenon, refers to the downward vertical displacement or gradual sinking of the Earth’s surface relative to a reference datum, driven by processes that reduce support in the underlying materials. Mechanisms include natural compaction of sediments, dissolution of soluble rocks (e.g., karst), tectonic extension, crustal loading and unloading, and anthropogenic drivers such as groundwater, hydrocarbons, or geothermal fluid extraction, as well as mining-induced void creation. Subsidence is quantified using geodetic and remote sensing techniques (e.g., GNSS, InSAR) and significantly influences stress fields, surface drainage, infrastructure stability, and hazard assessment in both natural and urban environments.

When Martian ground falls apart

In its latest postcard from Mars, the European Space Agency's Mars Express returns to Acheron Fossae: a dramatic network of chasms carved into the surface of the red planet.

High-res insights into NZ's sinking coastal sites

Coastal sites subsiding at rates of up to 10 mm/year, making them more vulnerable to sea-level rise, have been pinpointed in new high-resolution maps of five major urban centers.

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