Seismic shaking and tectonic deformation during strong earthquakes can trigger widespread
environmental effects. The severity and extent of a given effect relates to the characteristics …

Liquefaction, which can be defined as a loss of strength and stiffness in soils, is one of the
major causes of damage to buildings and infrastructure during an earthquake. To overcome …

The 6 February 2023 earthquake doublet (Mw 7.7 and Mw 7.6) that occurred on the East
Anatolian Fault Zone (EAFZ) triggered a significant amount of soil liquefaction phenomena …

Anthropogenic changes to the environment can enhance earthquake-triggered landslides,
yet their role in earthquake disasters is often overlooked. Co-seismic landslides frequently …

The 2010–2011 Canterbury earthquake sequence began with the 4 September 2010, Mw7.
1 Darfield earthquake and includes up to ten events that induced liquefaction. Most notably …

Abstract In the 4 September 2010 (MW= 7.1) and 22 February 2011 (MW= 6.2) earthquakes,
widespread liquefaction and lateral spreading occurred throughout Christchurch and the …

Stratified silty soils deposited in back-swamp settings are shown through regional CPT-
based analyses to have mitigating effects on the manifestation of liquefaction in …

The present study provides an insight into the effect of recycled carpet fibre on the
mechanical response of clean sand as backfill material subjected to monotonic loading and …

Lateral spreading is the most pervasive type of earthquake-induced ground deformation,
which can cause considerable damage to engineered structures and lifelines. There are …

On the 20th and 29th of May 2012, two earthquakes occurred in Emilia-Romagna region
(Northern Italy) triggering extensive liquefaction of the subsoil units. The consequences of …