Energy can build up when the Earths crustal plates move against one another, compressing and stretching the surface of our planet. Mining and the building of dams also leed to a build up of energy or weakening of rocks that have stored compressed energy.
When the energy is released suddenly a shockwave ripples through the Earth. The release point of the energy is the focus of the Earthquake, and the point on the surface directly above the focus is the epicentre.
Visit the Geoscience Australia Earthquake Website here
When you open the page it will show a map of Australia, with any Earthquakes from the past week appearing as yellow dots.
The size of the dot indicates the magnitude of the Earthquake.
Then select "Recent Earthquakes" tab on upper right.
Change the time period from "7 Days" to "30 Days"
Then zoom in and explore the recent earthquakes near Wollongong.
Earthquakes vary in strength. The magnitude (strength) of the earthquake is measured by the Moment Magnitude scale.
This measurement scale for Earthquakes officially replaced the more well known Richter scale in 2002.
While a 7.0 Earthquake is far stronger, it will cause little damage in a rural area. An earthquake greater than 6.0 will be devastating in a big city. Thus, population density contributes to the impacts of earthquakes.
Earthquakes have primary effects, such as the collapse of buildings, which are a direct and immediate consequence of the shock waves.
Secondary effects are those that occur shortly afterward, such as fires or even Tsunamis.
The tertiary effects are the more long term consequences for the people and places affected by the earthquake. This could be homelessness, famine, or outbreaks of disease.
Earth tremors associated with human constructed dams are well documented.
Imagine the unlikely scenario that the water catchments west of Wollongong lead to an earthquake in the Illawarra.
In the table in your worksheet make predictions of the effects if the earthquake was more than magnitude 7.0