![Seismites of Galera and Castilléjar | Geoparque de Granada sismitas castillejar 410x514 - Seismites of Galera and Castilléjar - Geoparque de Granada](https://www.geoparquedegranada.com/wp-content/uploads/2019/07/sismitas-castillejar-410x514.jpg)
Seismites of Galera and Castilléjar
Seismites of Galera and Castilléjar.
Seismic waves transform sediment into a kind of “quicksand”. The water in the pores of the sediment is expelled, separates the grain and converts the material into a viscous fluid (liquefaction). When the upper sediment is denser (thicker) than the lower one (thinner), these folds happen and are known as seismites.
Location info
- Municipio: Galera
- Superficie: 100 ha
- Periodo: Quaternary (Lower Pleistocene; 1,5-0,8 Ma)
![Seismites of Galera and Castilléjar | Geoparque de Granada sismitas cascaborras 1 800x400 - Seismites of Galera and Castilléjar - Geoparque de Granada](https://www.geoparquedegranada.com/wp-content/uploads/2019/07/sismitas-cascaborras-1-800x400.jpg)