Tue, Jun 9, 2009
Environmental Graffiti Will be Changing Dramatically Soon. Get a Sneak Preview By Signing Up Here.
![]()
Image via: U.S. Geological Survey
An earthquake shaking the very foundations you live on would be jeopardy enough for most people to endure, but if upon stepping outside your home you were also to find massive fissures riddling the earth, cathedral-sized alarm bells would start ringing. Fear wouldn’t be the word. Cracks appearing in the ground during major seismic events is picture book stuff, but let’s see how they look for real, while considering the forces that cause them – and the effects they have.
Cracks pass several feet in front of a house, Loma Prieta earthquake, CA, 1989
![]()
Image: G. Plafker, U.S. Geological Survey
Caused chiefly by rupturing geological faults, naturally occurring earthquakes happen almost constantly in seismic danger zones around the globe such as California, Alaska, Japan and Indonesia. Stored energy in the earth’s crust is suddenly released as if an omnipotent entity were playing with an elastic band, and the seismic waves created ripples out from the epicentre, sometimes to devastating effect.
Crack in the ground: Great San Francisco earthquake of 1906
![]()
Image: G.K Gilbert, U.S. Geological Survey
Thankfully earthquakes of larger magnitudes happen less frequently, but when they do take place, they sure cause a scene. It is during these bigger quakes that folks are liable to themsleves start trembling as they witness the severe shaking that is one of the hallmarks of this natural hazard. And it is then that people are more likely to crack mentally as they see the ground beneath their feet begin to rip asunder.
Huge cracks and a sunken hole in the highway: Denali earthquake, Alaska, 2002
![]()
![]()
Images: Steve Fields via Arcticulates
As well as being a near-legendary cataclysmic image, ground ruptures can have decidedly concrete effects, resulting in severe damage to buildings and other rigid structures. These breaks and dislodgements of the earth’s surface along a fault can be several metres in size during major tremors. Ground rupture is a particular risk for large engineering structures like dams, bridges and nuclear power stations, so existing faults need to be scrupulously mapped to pinpoint any that might break the surface during the structure’s lifespan.
The Bay Bridge Collapse: Loma Prieta earthquake, CA, 1989
![]()
Image: U.S. Department of the Interior U.S. Geological Survey
One of the disastrous tremors the famous San Andreas Fault was responsible for was the Loma Prieta earthquake of 1989. It measured 6.9 on the moment magnitude scale and lasted for around 15 seconds, killing 63 people, injuring 3,757, and leaving thousands more homeless. It is remembered as the first major American quake to be broadcast live on TV, as a baseball World Series Championship game was being televised. The upper deck of the San Francisco-Oakland Bay Bridge collapsed onto the deck below it, while closer to the epicenter in the Santa Cruz Mountains, cracks yawned wide.
Crack system that destroyed a driveway, Loma Prieta earthquake, CA, 1989
![]()
Image: J.K Nakata U.S. Geological Survey
An even more massive quake to shake America in recent years was Alaska’s 2002 Denali earthquake. Measuring 7.9 on the moment magnitude scale, it was the largest recorded on the mainland United States for more than 150 years and its shock was the strongest ever recorded in the Alaskan interior. Thanks to the remote location in which it took place, there were no deaths and minimal injuries, though the severe damage on highways that crossed the fault line made driving dangerous or simply impossible.
Road rendered in two: Denali earthquake, Alaska, 2002
![]()
Image: Steve Fields via Arcticulates
Huge cracking and a hole in the highway
![]()
Cracked yet? Ground level changes
![]()
Images: Photographer unknown via Arcticulates
Moving off the American continent, Japan’s Chuetsu earthquake, which took place in 2004, was actually a series of three earthquakes, measuring between 5.9 and 6.9 on the Richter scale, followed by aftershocks that persisted for two weeks. It was the deadliest earthquake to impact on Japan for a decade, with 39 reported fatalities plus thousands injured. Transport networks were particularly hard hit: a train was derailed, bridges and tunnels were affected, and expressways were closed due to damage from ground rupture, landslides and other hazards.
Yamabe Bridge: Chuetsu earthquake, Japan, 2004
![]()
Image: Tubbi
In 2005, what was to become known as the Sumatra or Nias earthquake struck its Indonesian islands of the same names. A truly devastating seismic event, 1,300 people were killed by this tremor, whose literally earth-shattering moment magnitude measured roughly 8.7, making it the most powerful quake the world had seen since 1965. The earthquake lasted for two minutes in total, though there were eight major aftershocks in the twenty four hours that followed. Hundreds of buildings were obliterated.
Cracks in the ground: Nias earthquake, Indonesia, 2005
![]()
Image via: Oxfam America
On this evidence, it’s small wonder cracks in the ground have such apocalyptic associations.
If you want to find out all the latest news on the environment, why not
href=”http://feeds.feedburner.com/environmentalgraffiti”>subscribe to our RSS feed? We’ll even throw in a free album.
“The only true currency in this bankrupt world is what you share with someone else.”
[...] Cuando la tierra se parte www.environmentalgraffiti.com/featured/geological-faults-tea… por thombjork hace pocos segundos [...]
June 10th, 2009 at 10:30 am
The earthquake in Indonesia 2005 was truly horrifying. My roommate went to one of the sites as part of a relief team and brought back photos. The level of damage is something you can’t get out of your head. Makes you realize how helpless we are when an event of that magnitude happens.
http://tinyurl.com/lzm6al
June 10th, 2009 at 3:43 pm
Very interesting article.