SH
Member Since 2012
Simon Henry Lamb
Associate Professor, Victoria University of Wellington
AGU Research
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Using InSAR and GNSS to characterise present-day vertical deformation at New Zealand coastal strips
GEODESY FOR CLIMATE RESEARCH III POSTER
geodesy | 13 december 2022
Jesse Kearse, Tim A. Stern, Ian J. Hamling, Simon ...
Today, the average rate of global mean sea-level rise is ~3 mm/y and is expected to increase in the future. This represents a hazard to low elevation ...
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Hydrological controls on seismic velocity changes after large earthquakes: The WELLington WELLbore VELocity change project (WELLVEL)
ENVIRONMENTAL SEISMOLOGY: A GEOPHYSICAL TOOL TO STUDY SURFACE AND NEAR-SURFACE PROCESSES II ORAL
seismology | 12 december 2022
Martha K. Savage, Pasan Herath, Hubert J. Zal, Cor...
The 2016 Kaikōura earthquake in New Zealand caused changes in seismic wave speeds, water bore levels and GNSS station locations. The WellVel project i...
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WELLVEL: WELLington (New Zealand) region water WELLbore levels and seismic VELocity changes
TIME-LAPSE SEISMOLOGY II POSTER
seismology | 15 december 2021
Martha K. Savage, Sam Thorpe-Loversuch, Hubert J. ...
Seismic wave speeds, water bore levels and GNSS station locations all changed at the time of the 2016 Kaikōura earthquake. The WELLVEL project is dete...
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Evidence for Lithospheric instability beneath two different mountain ranges: Southern Alps (New Zealand) and the Transantarctic Mountains
LITHOSPHERIC FOUNDERING: DETECTION AND EFFECTS ON DEFORMATION, TOPOGRAPHY, THERMAL/COMPOSITIONAL STRUCTURE, AND MAGMATISM I ORAL
tectonophysics | 13 december 2021
Tim A. Stern, James D. Moore, Simon H. Lamb
Detecting the role of foundering mantle instabilities in the evolution of mountain ranges is challenging. The wavelength and amplitude of disturbances...
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Global Whole Lithosphere Isostasy: Implications for Surface Elevations, Structure, Strength, and Densities of the Continental Lithosphere
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
23 october 2020
Simon H. Lamb, James Moore, Marta Perez-Gussinye, ...
The observed variations in the thickness of the conductive lithosphere, derived from surface wave studies, have a first‐order control on the ...
Ductile deformation explains the physics of rock friction
PHYSICAL PROPERTIES OF EARTH MATERIALS (PPEM): FROM RAPID TO SLOW AND FROM MICROTECTONICS TO PLATE TECTONICS III
mineral and rock physics | 12 december 2019
James D. Moore, Giacomo Pozzi, Stefan Nielsen, Lar...
Rock friction plays a role in a wide range of processes in the solid Earth and material science and is actively investigated in laboratory experiments...
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Whole lithosphere isostasy of the continents, and the elevation and crustal thickness of Antarctica
GEODYNAMICS, TECTONICS, AND DEPOSITIONAL SYSTEMS IN THE CONTINENTS AND CONVERGENT MARGINS II POSTERS
tectonophysics | 09 december 2019
Simon H. Lamb, Tim A. Stern, James D. Moore
Isostasy exerts a fundamental control on the elevation of the continents, determined by the density structure of the lithosphere and asthenosphere. Th...
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Convective Removal of Lithosphere and Uplift of the Transantarctic Mountains
GEODYNAMICS, TECTONICS, AND DEPOSITIONAL SYSTEMS IN THE CONTINENTS AND CONVERGENT MARGINS II POSTERS
tectonophysics | 09 december 2019
Tim A. Stern, Simon H. Lamb, James D. Moore, Weise...
Convective removal of the lower lithosphere is a key process for explaining the bulk composition of the continental crust, distinctive volcanism and u...
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