John Barton from Psychology checks a Geography building office for damage.
Wendy Lawson from Psychology checks a Geography building office for damage.
Wendy Lawson from Psychology checks a Geography building office for damage.
Wendy Lawson from Psychology checks a Geography building office for damage.
John Nicolle from ITCS checks a computer in the the Geography building for damage.
Wendy Lawson and John Barton from Psychology check the Geography building staffroom for damage.
John Nicolle from ITCS checks a computer in the the Geography building for damage.
John Nicolle from ITCS checks a computer in the the Geography building for damage.
Wendy Lawson from Psychology taking a photo of the damage to a Geography building office.
Wendy Lawson from Psychology taking a photo of the damage to a Geography building office.
Among the deformation features produced in Christchurch by the September 4th Darfield Earthquake were numerous and widespread “sand volcanoes”. Most of these structures occurred in urban settings and “erupted” through a hardened surface of concrete or tarseal, or soil. Sand volcanoes were also widespread in the Avon‐ Heathcote Estuary and offered an excellent opportunity to readily examine shallow subsurface profiles and as such the potential appearance of such structures in the rock record.