Graham S. Leonard

ORCID: 0000-0002-4859-0180
Publications
Citations
Views
---
Saved
---
About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • Geology and Paleoclimatology Research
  • Disaster Management and Resilience
  • Seismology and Earthquake Studies
  • High-pressure geophysics and materials
  • Landslides and related hazards
  • Evacuation and Crowd Dynamics
  • Flood Risk Assessment and Management
  • Disaster Response and Management
  • Cryospheric studies and observations
  • Public Relations and Crisis Communication
  • Geochemistry and Geologic Mapping
  • Geomagnetism and Paleomagnetism Studies
  • Tropical and Extratropical Cyclones Research
  • Methane Hydrates and Related Phenomena
  • Climate change and permafrost
  • Seismic Waves and Analysis
  • Infrastructure Resilience and Vulnerability Analysis
  • Pacific and Southeast Asian Studies
  • Earthquake and Tsunami Effects
  • Geological and Geophysical Studies
  • Geological formations and processes
  • Risk Perception and Management
  • Pleistocene-Era Hominins and Archaeology

GNS Science
2016-2025

Crown Research Institutes
2015-2023

University of Auckland
2022

University College London
2017

Massey University
2008-2014

University of Canterbury
2001-2003

University of Freiburg
1976

We formally introduce 14 new high-level stratigraphic names to augment existing and hierarchically organise all of New Zealand's onland offshore Cambrian–Holocene rocks unconsolidated deposits. The two highest-level units are Austral Superprovince (new) Zealandia Megasequence (new). These encompass the country's Cambrian–Early Cretaceous basement Late Cretaceous–Holocene cover sediments, respectively. Most constituents in current common usage: Eastern Western Provinces consist 12...

10.1080/00288306.2014.946062 article EN cc-by New Zealand Journal of Geology and Geophysics 2014-10-02

Abstract. The water quality of Lake Rotorua has steadily declined over the past 50 years despite mitigation efforts recent decades. Delayed response groundwater discharges to historic land-use intensification ago was reason suggested by early tritium measurements, which indicated large transit times through system. We use isotopic and chemistry signature for detailed understanding origin, fate, flow pathways, lag future loads contaminants. A unique set high-quality data more than four...

10.5194/hess-19-803-2015 article EN cc-by Hydrology and earth system sciences 2015-02-05

Research Article| January 01, 2007 Double trouble: Paired ignimbrite eruptions and collateral subsidence in the Taupo Volcanic Zone, New Zealand D.M. Gravley; Gravley 1Geology Department, University of Auckland, Private Bag 92019, Auckland 1142, Search for other works by this author on: GSW Google Scholar C.J.N. Wilson; Wilson G.S. Leonard; Leonard 2GNS Science, P.O. Box 30368, Lower Hutt 5040, J.W. Cole 3Department Geological Sciences, Canterbury, 4800, Christchurch, Author Article...

10.1130/b25924.1 article EN Geological Society of America Bulletin 2006-12-27

Taupō volcano (New Zealand) is distinguished as the source of Earth's youngest supereruption (∼25.5 ka), with Lake occupying resulting caldera. has also produced eruptions a wide variety sizes, styles and associated landscape responses over ∼350 kyr period. Early (>54 ka) poorly demarcated, merging Maroa to north, represented by widely scattered, geochemically distinct, effusive domes explosive eruption products from vents all around modern lake. had two independent magmatic systems 54–25.5...

10.1080/00288306.2020.1792515 article EN New Zealand Journal of Geology and Geophysics 2020-07-29

Abstract The evolution of the continental intraarc Taupo Rift in North Island, New Zealand, is rapid, significantly faster than comparative intracontinental rifts such as African Rifts. Based on our faulting data and published geological, geophysical, borehole data, we show that activity ~2 Ma has rapidly asymmetrically narrowed via inward eastward migration (at rates approximately 30 km Myr −1 15 , respectively) propagated southward along its axis ~70 350 kyr. loci voluminous volcanic...

10.1002/2017tc004715 article EN Tectonics 2017-10-01

Abstract. Evacuation of the population from a tsunami hazard zone is vital to reduce life-loss due inundation. Geospatial least-cost distance modelling provides one approach assessing evacuation potential. Previous models have generally used two static exposure scenarios and fixed travel speeds represent movement. Some analyses assumed immediate departure or common time for all exposed population. Here, method proposed incorporate time-variable exposure, distributed speeds, uncertain into an...

10.5194/nhess-14-2975-2014 article EN cc-by Natural hazards and earth system sciences 2014-11-17
Coming Soon ...