An active fault surface in Greece – one of the most seismically active places on Earth. The striations on the surface can be used to measure the direction of movement on the fault. The exposed surface can be dated at various heights (using dating systems such as Beryllium-10) to infer the rate of slip. (c) Geology for Global Development
Guest Blog: Earthquakes in the Steppes of Central Asia
Tim Middleton is a first year PhD student in the Department of Earth Science at Oxford University – studying active tectonics in central and eastern Asia. He has recently joined the GfGD National Committee as our Advocacy Development Officer. Here, Tim describes his experience of fieldwork in Kazakhstan and the importance of studying the landscape to assess the risk of future disasters. Tim ...[Read More]
Friday Photo (57): Active Geology – Sinking Buildings from Ancient Greece
These foundations were once part of a building in ancient Greece. Over thousands of years, active faults have lowered the land and the foundations have sunk below sea level. Geology can have a big impact on relatively short timescales. (c) Geology for Global Development