The Earthquakes of China

2008 Wenchuan Earthquake

Recently, in the last few years, many earthquakes have occurred in China.  Just a few days ago, there were approximately 200 deaths due to an earthquake which happened in the same area as a devastating event about 5 years ago.  The Wenchuan Quake of May 2008 found tens of thousands dead or missing. 

 

The epicenter of the recent event is near the eastern foothills of the Himalayas.  This mountain range is still forming because the Austro-Indian plate is pushing into the Eurasian plate.  Rock underneath the surface has been crushed and rolled right on top of one another, causing an uplift. 

 

The Earthquake that took place April 20, 2013

This phenomenon is similar to when one has a sheet of paper and pushes one side against another.  The paper "rolls."  If one squeezes the paper on a flat table surface, the paper rolls upward.  This experiment shows how it is that mountains are formed.

 

Being near a mountain range during an earthquake could be quite dangerous due to landslides and mass wasting.  Massive boulders on top of the mountains can easily tumble over, destroying anything in it's path.  Add to this faulty building codes, subsidence that compromise foundations along with countless of people trapped in a confined area and one has a recipe for an astronomical environmental  hazard.  This is what happened five years ago and it is what happened less than two weeks ago. 

 

Another cause of the landslides and mass wasting is due to the fact that the Himalayas are getting very high.  These humongous mountains will eventually collapse on itself, simply because of the weight.  This is the mountain range that is home to Earth's highest peak, Mt Everest, which rises 8,848 meters above sea level (29,029 feet).   Amazing thing, this plate tectonics!

 

 

 

 

Though most of us see earthquakes as a "bad" thing (myself included), this phenomenon is actually a good thing.  It is a side effect of a process that keeps life on Earth possible.  Without plate tectonics, volcanoes wouldn't be.  Though volcano can be quite destructive in of itself, fresh basalt deposits renews the surface, adding much minerals that allows vegetation to be sustained.  Plate tectonics also is a sign that our home is indeed alive and is constantly renewing herself.  Our oceans are constantly, though slowly but surely, changing, giving Earth a chance to go through these cycles of constant birth and rebirth.  I do admit, however, that it is unfortunate that these events do happen when they do, wherever they do occur.  

 

It is a constant reminder just how precious human life really is. 

 

From Fayetteville, AR USA

--GeoJack

 

 

 

 

The New Madrid Earthquakes

Reelfoot Rift Zone

The Reelfoot Rift Zone has its biggest concentration in parts of 5 states which are:  Northeast Arkansas, Southwest Illinois, Western Kentucky, Southeast Missouri, Western Tennessee; even extending into Northern Mississippi.

It is here where the famous series of earthquakes during the winter of 1811-1812 rang church bells as far away as Boston and damaged scaffolds at the capitol building in Washington, D.C.  One of these earthquakes even made the mighty Mississippi flow backwards for a few hours, causing the lake “Reelfoot” which got its name from the seismic zone that made it happen!

General Plate Tectonics

Most earthquakes in the United States occur in Alaska and California.  These states are associated with the North American and the Pacific Plate boundaries, along with Oregon and Washington.  At this boundary, the heavier crust of the Pacific Ocean goes underneath the lighter crust of the North American plate.  This causes tension and rocks underneath North America get crushed and melted, causing geologic structures such as mountains and volcanoes, which is exactly what is going on over there.  First, it was the Rocky Mountains.  As North America continued to push and expand westward, the Sierra Nevada Mountains and the Coast Ranges were formed.

On the other side of the North American Plate is the Atlantic Rift, in which the plate is moving away from the Eurasian Plate.  Likewise, the Eurasian Plate is moving further away from North America and going towards the Pacific Ocean to the East.  The rift between North America and the Eurasian plates has caused the crust to split open and magma from underneath to surface upward, creating the Mid-Atlantic Ridge which is an undersea Mountain range going north to south right at the center of the ocean.  It is this rift that fuels the volcanoes in Iceland.  Iceland is a part of that ridge that extends above sea level.  It would be fair to say that the Atlantic Ocean is getting wider as the Pacific is shrinking.

Neither the plate boundary of the West Coast of the US, nor the Atlantic Rift underneath that ocean has anything to do with what is taking place in the central part of the country, where there are no current plate boundaries.  Note the word “current.”  It is believed that at one time (a very long time ago—before the time all the continents were one, the Pangaea), the North American plate was ripping itself up in Southeast Missouri, hence the name “rift.”  This rift never fully completed, (it never ripped open the surface) so geologists today consider this rift zone a “failed” one.  Yet, it is so deep below the surface and the tear is significant enough to cause this area to be a great seismic risk-hazard zone.  All this means is simply, earthquakes do happen in the middle of the country, where there are no plate boundaries and because of that, a greater area may have significant damage than areas that are prone to earthquakes due to crustal boundaries (like the Pacific Coast).  Why is this?

Impacts of Mid-Continent Earthquakes

The map on this page compares the Northridge Earthquake that damaged Northwest Los Angeles in 1994 to an earthquake that occurred at Charleston, MO in 1895.  Even though the LA earthquake was stronger than the Mid-continent one, the area of damage is relatively much smaller.  Again, why is this?  Notice at the West Coast, earthquakes happen much more frequently there because of plate boundaries.  Therefore, the ground below the surface is cracked, always being recycled and comparatively “newer.”   Earthquakes in Missouri, on the other hand, happen with less frequency, the ground is not being continually recycled and is much more brittle, “older.”  This causes surface waves of an earthquake to move with better effectiveness; hence, an earthquake here in the center of the continent will affect a bigger amount of area as the above map shows.

 http://upload.wikimedia.org/wikipedia/en/c/cb/Charleston1895.gif

What does this mean for the future? 

There is at least a 90% chance that an earthquake similar or more potent than the ones during the early nineteenth century could occur here in the rift zone by 2050.  That doesn't really give us much time, really.  These earthquakes could indeed happen in the next 35 or 40 years, but then again, could happen tomorrow.  The 1811-1812 New Madrid Earthquakes didn't cause so much death and destruction, mainly because the immediate area was sparsely populated.  Now, we have quite a few major cities that will no doubt suffer extensive amount of damage, like Memphis or St. Louis.  Other cities that may be profoundly affected would be Nashville, Louisville, Little Rock.  Even Northwest Arkansas could receive an extensive amount of damage even though it is 350 miles away!  Something to think about!  Be prepared, because the government has done a bang up job so far, considering that fiasco called "Katrina!"  Well, maybe we have learned our lesson thus far.  The aftermath of Sandy was much smoother!