Survival Emergency Preparedness


 First Aid Kit: Complete Emergency Preparedness for Home, Office, Car, Camping, Outdoors and Office Uses

 

 

 

 


Michael Jackson - Earth Song (Official Video)

Music video by Michael Jackson performing Earth Song. © 1995 MJJ Productions Inc.
https://www.youtube.com/user/michaeljacksonVEVO/videos

 

 

 

https://youtu.be/UN1G4BSyIos


If you saw the Warner Bros. disaster movie, San Andreas, then you know all about the infamous California fault line and its potential for causing chaos. But why does the San Andreas Fault get all the attention in movieland? Contrary to popular belief, this isn’t the only fault system threatening imminent disaster.


 https://youtu.be/yftHosO0eUo


 


https://youtu.be/UN1G4BSyIos


 

What Mexico's earthquake means for California?

Check out these 5 scary seismic zones that are just as nerve-racking as the San Andreas Fault.

1. The Cascadia Subduction Zone

By the time Lewis and Clark arrived on the West Coast in 1805, it had been 105 years since the Cascadia Subduction Zone last ruptured, sending a large portion of the Pacific Ocean roaring toward the coast. The few remaining Native Americans in the area spoke of the earth shaking and ocean rising to consume the land. Many tribes even left the region permanently. However, it wasn’t until the discovery of the Cascadia Fault in the 1960s that modern settlers truly understood the dangers they faced.

Running 680 miles along the Pacific Northwest coastline, the Cascadia Fault directly threatens 3 major metropolitan areas (Portland, Seattle, and Vancouver). With Cascadia capable of producing a magnitude 9.0 or 10.0 earthquake, the Pacific Northwest may soon face shaking (16 times more powerful than San Francisco’s devastating 1906 earthquake) lasting 4 minutes and delivering a mighty tsunami of unimaginable proportions.

2. The New Madrid Seismic Zone

It’s not just the West Coast that needs to watch out for tectonic obliteration. The New Madrid Seismic Zone spans southeastern Missouri, northeastern Arkansas, western Tennessee, western Kentucky, and southern Illinois. It’s the most active earthquake zone east of the Rocky Mountains.

Between 1811 and 1812, this zone experienced some of the largest quakes in history. And although they originated in the Mississippi Valley, they rang church bells in Boston and shook New York City — over 1,000 miles away! Even then-President James Madison and his wife Dolley reportedly felt shaking at the White House.

After one particularly large rupture in the fault, the mighty Mississippi River was forced to run backward for several hours, devastating acres of forest and creating 2 temporary waterfalls. Fortunately the Mississippi Valley was sparsely populated back then. Today millions of people live in densely populated urban areas like St. Louis and Memphis, making this zone one of the biggest concerns for the Federal Emergency Management Agency.

3. The Ramapo Seismic Zone

In 1884, Brooklyn was rattled by an earthquake originating near the Ramapo Fault System. Toppling chimneys in New York City and felt as far away as Maine and Virginia, the magnitude 5.2 earthquake was a sudden wake-up call for settlers in the region.

Running through Pennsylvania, New Jersey, and New York, the Ramapo has remained quiet for about 200 years. While studies have shown that a quake greater than 5.0 to 5.5 in magnitude is unlikely, urbanization in the tristate region leaves the area extremely vulnerable.

A mid-magnitude earthquake in the right (or worst) place could cause devastating damage. One of the faults in the Ramapo system even crosses New York City around 125th Street. A magnitude 5.0 rupture lasting more than a minute or 2 could cause intense structural damage to numerous Manhattan skyscrapers, most of which are not designed to withstand such tectonic activity.

4. The Hayward Fault

This very unstable fault in California has been threatening the San Francisco Bay Area for generations. It’s capable of producing quakes ranging from 7.0 to 8.0 in magnitude. The last major movement along the Hayward Fault occurred on October 21, 1868, virtually destroying downtown Hayward. In fact, it was considered the “great earthquake” until the San Andreas Fault tore San Francisco apart 38 years later.

Running for nearly 74 miles through cities including Fremont, Hayward, Oakland, Berkeley, and Richmond, the Hayward Fault has the potential to wreak more havoc than most California faults. Over 2.4 million people live within close proximity to the fault today, not to mention the key infrastructure developments (including a major public transit system and the Caldecott Tunnel) that run precariously through the fault.

5. The Denali Fault System

If we’re talking sheer magnitude, the largest recorded earthquake on North American soil hit Alaska on November 3, 2002. Starting on the Susitna Glacier Thrust Fault, the rupture raced along the Denali Fault System and continued 220 kilometers until it reached the Totschunda Fault, rattling 70 more kilometers.

The estimated magnitude of this earthquake ranged from 7.0 to 7.9 with a surface wave magnitude of close to 8.5. This almighty quake caused extensive damage to the transportation systems in central Alaska. Multiple landslides and rock avalanches occurred in the Alaska Range and Black Rapids Glacier. This event was literally felt across the nation, even causing waves in pools and lakes in Texas and Louisiana!

Related: Are you living in a natural disaster zone? Find out what you need to know, and how to be prepared for what nature throws your way.

http://blog.esurance.com/beyond-san-andreas-5-scariest-fault-lines-in-the-u-s/

 

(CNN)As we wake up to footage of the devastation in Mexico in the aftermath of the second earthquake that country has suffered this month, people in California might well be wondering how well-prepared their local communities are.

But earthquakes in California and Mexico differ in ways that are important to understand -- if we are to learn lessons that allow us to better prepare for them in the future.
 
First, the tectonic activity in each area is different: California sits at the boundary between two plates that rub each other horizontally. The plates off the shore of Mexico and the rest of the Pacific "ring of fire," an area of intense seismic activity, rub against each other vertically.
 
 
As a result, Mexico has bigger earthquakes. The biggest Mexican earthquakes happen offshore and create tsunamis, but the earthquakes themselves are far from Mexico City. The biggest Californian earthquakes happen inland on the San Andreas Fault, and as a result generate no tsunami. Though they are smaller than earthquakes like the one we are seeing cause such devastation in Mexico, they occur dangerously close to Los Angeles.
Because of this difference of distance to the major fault, it is more challenging to build an earthquake early warning system for Los Angeles than for Mexico City, which means that the time available to declare a warning is much shorter in California.
The second major difference is the soil upon which both cities are built. Mexico City was built on a former lake, which means that its ground is soft and wet. It behaves like a bowl of jelly when it shakes. It renders ground motion stronger and longer in duration. For this reason, the impact of distant earthquakes is more dramatic in Mexico City than in California.
Finally, houses in California and Mexico are built differently. The typical one-story wooden house in California is light and does not collapse during earthquakes. The biggest danger is caused by objects flying around due to strong shaking, and the general advice in California is to drop, cover and hold on.
The safest reaction to have during an earthquake in Mexico, especially in weak constructions that are likely to collapse, can be completely different.
The biggest dangers in the immediate aftermath of an earthquake are also different in both cities. For example, in California, wooden houses with public gas system have a more severe risk of fire.
We should be careful to understand the different weaknesses of the built environment around us when traveling and migrating. Being aware is the best way to ensure safety during earthquakes in different countries. Wise advice that has worked well in Mexico may fail miserably in California, and vice-versa.
When the damage caused by a large earthquake exceeds the capacity of official emergency responders, citizens become their own first responders.
In the aftermath of the Mexico earthquake, we are seeing inspiring images of people helping each other, going to the rescue of their neighbors and coworkers. The people of Mexico City gave the world a lesson of citizen solidarity and self-organization after the 1985 earthquake, and we've seen similar images from the areas hit by recent hurricanes in the US.
Here is an important lesson: We can be prepared for earthquakes as individuals, and as families, but if we're not prepared as a community, we all sink together. And if California falls, the whole of the US can fall.
 

Preparedness is a community responsibility. We can prepare together by Community Emergency Response Team (CERT) training, by identifying the resources in our neighborhood like knowing who is a medical doctor, who has heavy-duty tools, and by being aware of the most vulnerable people around us.

 
 
 
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Hurricane Harvey ends, Houston's story begins
 
Hurricane Harvey ends, Houston's story begins

Reliable Sources

On the twelfth anniversary of Hurricane Katrina, New Orleans resident and actor Harry Shearer describes how lessons learned from Katrina coverage can be applied to coverage of Harvey's aftermath. He also discusses the "wallpapering" of disaster imagery by TV news.
Source: CNN

 
 
 
US: Tropical Storm Harvey     harvey-houston-texas...


 
 
 

 
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