Geology lab’s seismometer records New Zealand earthquake

A magnitude 7.8 earthquake struck New Zealand’s South Island at 12:02 a.m. Monday. The seismometer housed in GRCC’s geology lab recorded the earthquake approximately 19 minutes later. The first waves seen in the seismograms below are called body waves, they travel through the Earth, and are the fastest seismic waves. The later waves, that look more spread out, are surface waves. They travel along the surface of the Earth and are responsible for most of the damage caused by earthquake shaking. The earthquake was generated by movement along a fault close to the juncture of two tectonic plates. The nature of movement led to activation of the tsunami warning system in coastal communities close to the main shock. Evacuating residents were further rattled by dozens of aftershocks over the next 9 hours, some as large as magnitude 6.5. For more information about this and other earthquakes visit the United States Geologic Survey’s website.

 

Explore posts in the same categories: Uncategorized

Tags:

You can comment below, or link to this permanent URL from your own site.

Leave a Reply

Fill in your details below or click an icon to log in:

WordPress.com Logo

You are commenting using your WordPress.com account. Log Out / Change )

Twitter picture

You are commenting using your Twitter account. Log Out / Change )

Facebook photo

You are commenting using your Facebook account. Log Out / Change )

Google+ photo

You are commenting using your Google+ account. Log Out / Change )

Connecting to %s


%d bloggers like this: