The recent over-ice seismic deployments in Antarctica provide datasets that enable exciting opportunities for seismological research. This project involves innovative development in passive seismology methods adapted for challenging icy conditions to unravel ice and solid Earth structure in Antarctica.

The lowermost mantle sits atop the core-mantle boundary – the most dramatic boundary within our planet, with contrasts in physical properties that exceed those that exist at the surface. Despite significant progress, this region is not well understood, and global seismology paves the path towards new understanding.

This project will investigate the submerged fossil coral reefs in the Great Barrier Reef (GBR) and determine the nature and mechanisms responsible for abrupt sea-level rise, climate variability (ie. paleo-ENSO) and geo-biological changes affecting the GBR over the last 20,000 years. We build directly on the already...

The ocean is a sea of internal gravity waves. Similar to the gravity waves that propagate over the ocean surface and break along our coastlines, internal waves propagate great distances through the ocean interior. These waves are generated at the ocean surface and the seafloor by a variety of mechanisms. As the...

Signals transmitted from satellites orbiting the Earth are delayed as they pass through the troposphere of the Earth. This is measurable by GPS and so it is possible to measure how much water vapour is actually in the atmosphere using GPS. This is a new area of research that will involve the student learning about...

The Australian Seismometers in Schools project (AuSIS) is an outreach program to install 50 research quality broadband seismometers in Australian Schools. The goal of the program is to raise awareness of geoscience through observing our dynamic earth in motion. Students are required to look after their own...

The Earth’s inner core is a planet within a planet: a hot sphere with a mass of one hundred quintillion tons of iron and nickel that lies about 5150 kilometres beneath our feet, still waiting to be discovered. Modern global seismology serves as an inverted telescope with which we can probe the Earth's deepest shell.