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Anzac Cliffs –Geotechnical aspects of cliff stabilisation works

Anzac Cliffs –Geotechnical aspects of cliff stabilisation works

Abstract The Anzac Cliffs project involves two main elements: reshaping of the steep cliff, and realignment of the Manawatu River away from the cliff. The realignment of the river below Anzac Cliff was the last major development of the Lower Manawatu Scheme, City Reach Project….

A risk based assessment to rockfall mitigation

A risk based assessment to rockfall mitigation

Abstract The Health and Safety at Work Act (2015) requires companies to provide safe working environments for its staff. In response to this, our client sought to identify effective mitigation solutions for a rockfall hazard above an operational access road. The slope consists of a…

Elastic soil-structure interaction – is it worth the effort?

Elastic soil-structure interaction – is it worth the effort?

Abstract It is widely acknowledged that soil-structure interaction (SSI) has an important effect on foundation performance during earthquake loading. The standard way of handling this is to assume elastic behaviour of the soil beneath and around the foundation. For shallow foundation response there are three…

Use of UAVs and photogrammetry to reduce uncertainty in bulk earthwork calculations

Use of UAVs and photogrammetry to reduce uncertainty in bulk earthwork calculations

ABSTRACT The application of Unmanned Aerial Vehicles (UAVs) and photogrammetry for bulk earthwork calculations is a recent development for ground engineering in New Zealand. The approach developed on the Deans Head Land Remediation Project has proven to be an innovative solution increasing workflow efficiency to…

Volcanic hazard from the Auckland Volcanic Field

Volcanic hazard from the Auckland Volcanic Field

Abstract The Auckland Volcanic Field, which last erupted ~600 years ago, is a late Quaternary monogenetic basaltic volcanic field of approximately 500 km2. A recent study (Leonard et al., 2017) has improved the accuracy of eruption dates for 23 of the eruptive centres. Previously only 12…