About 14,000 earthquakes are recorded in and around Aotearoa New Zealand every year. Canterbury’s 7.1 and Kaikōura's 7.8 magnitude earthquakes and subsequent aftershocks show the constant threat ...
Children’s involvement in science is increased when they have an opportunity to make decisions about science-based issues that have consequences for their lives. It’s bringing science into the ...
Dave Corner of Auckland’s Pakuranga College developed a successful geology unit using resources from several SLH contexts. His students were engaged because they had been to or seen many of the ...
Shaky New Zealand About 14,000 earthquakes are recorded in and around New Zealand every year. Fortunately, most of them are too small for us to feel at the surface. However, many of us have felt ...
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 ...
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 ...
In this activity, students take on the roles of seismologists, vulcanologists and geographers, using maps to look for patterns in the worldwide distribution of earthquakes, volcanoes and ...
In this activity, students use maps to plot a graph of earthquakes under New Zealand to show the shape of the North Island subduction zone and compare this to the distribution of earthquakes in ...
The series of activities described below was designed to help students develop an understanding about earthquakes in New Zealand, including why we get them and how we measure them. The world of ...
Slow slips are silent earthquakes that occur below the Earth’s surface over a large area, unlike traditional earthquakes we feel that occur in a relatively small region. Before discovering slow ...
Chris Gannon and John Meyer from Robinson Seismic explain how the Ro-Glider works. Lead rubber bearings aren’t suitable for light structures, so Robinson Seismic has developed the Ro-Glider to ...
Far underneath the ground we walk on, the Earth is covered with tectonic plates. You can think of tectonic plates as puzzle pieces. Earthquakes and volcanoes often happen where the pieces meet. ...
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 ...
In this interactive follow a core sample as it makes its journey from the Alpine Fault to microscopic examination.
This is the slideshow that supports the Exploring natural hazards PLD webinar. Use the Slideshow menu for further options, including view full screen, and go here for the download option.
