We can blame plate tectonics for many catastrophes over time – earthquakes, volcanoes, geothermal activity, tsunamis and landslides – while people living on mountain ranges or small islands can ...
When an earthquake occurs, the shockwaves of released energy that shake the Earth and temporarily turn soft deposits, such as clay, into jelly (liquefaction) are called seismic waves, from the ...
Rocks are not all the same. Some are heavy, some are light. Others are dark, while some can be almost pure white. Even igneous rocks that are all formed from magma in the Earth’s mantle can look ...
The Earth rumbles and a hiss of steam issues from the top of Mt Ruapehu. Are these two events related? Is the earthquake caused by the volcano? Or is the steam caused by the earthquake? Tectonic ...
There are many different types of volcanoes around New Zealand. This interactive map shows where the major volcanoes are, the types of volcanoes and various facts such as when they last erupted ...
Base isolation is a technique developed to prevent or minimise damage to buildings during an earthquake. It has been used in New Zealand, as well as in India, Japan, Italy and the USA. A ...
All waves behave in certain characteristic ways. They can undergo refraction, reflection, interference and diffraction. These basic properties define the behaviour of a wave – anything that ...
What is happening inside this 12,700 km diameter ball we call the Earth? Some of the Earth’s internal architecture is an 'educated guess' (mainly from seismology), because the longest drill we ...
The Earth is an enormous place. There is so much that we don’t yet know about what happens on the surface of the Earth, so how could we possibly know about what happens deep down below the Earth’ ...
Everyone knows what a volcano looks like – isn’t it a steep-sided cone with wisps of ash coming from the top, just like Rangitoto, White Island, Mt Ngāuruhoe or Mt Ruapehu? But what about small ...
The city of Auckland is built on a volcanic field. There are 50 volcanoes within an area of 1,000 square kilometres, forming the hills, lakes and basins of the city. Rangitoto Island was formed ...
The Earth’s continents have not always been where they are at present. If you look at a map of the world, you might notice what Alfred Wegener noticed – that the continents look as if they could ...
In the South Island of New Zealand, the boundary between the Australian and Pacific tectonic plates can be seen on land. This is unlike the North Island boundary, where a subduction zone is under ...
Liquefaction is a process that temporarily turns firm ground into a liquid. During the Canterbury earthquakes of September 2010 and February 2011, liquefaction caused silt and fine sand to boil ...
New Zealand has volcanoes stretching from the Bay of Islands down to Otago. Many of our volcanoes are extinct (no longer active), some are dormant (not active but capable of becoming active) and ...
The Auckland Volcanic Field covers around 360 square kilometres under Auckland city. It includes 49 separate volcanoes, each of which is considered extinct. However the field as a whole remains ...
A look at some of the historical aspects of earthquakes, find out how our understanding of what causes earthquakes has changed. 1705 – A discovery by Robert Hooke Robert Hooke realised that ...
Isn’t it funny to think that the Earth is moving! If we stand perfectly still and look into the distance, the Earth appears to be perfectly still, too. But the Earth is actually moving in many ...
We live in a very exciting country. A day’s drive in a car can take us from snowy mountains, past geysers and hot mud pools to white, sandy Pacific beaches. Have you ever wondered why New Zealand ...
Uncovering our explosive past – a look at some of the historical aspects of volcanoes in New Zealand. 10 million BC – Mt Cargill erupts Mt Cargill near Dunedin erupts, forming the Organ Pipes. 6 ...
This animated video shows the movement of the tectonic plates that make up the Earth’s crust. Starting 600 million years ago, watch continents form and break apart as the plates move. Pangaea the ...
Seismic engineering is a branch of engineering that searches for ways to make structures, such as buildings and bridges, resistant to earthquake damage. Seismic engineers aim to develop building ...
The high temperatures (900C) and extremely high pressures that occur in the mantle layer of the Earth are enough to melt rock. The high pressure changes the rock into a viscous semisolid called ...
Choose a mission and then successfully build and launch a satellite that can help gather the data required. Select here for additional information on using this interactive simulation.
