All virtual University Subjects Groups (Click & Join Your Subject Group)
- ACC - Fundamentals of auditing and business
ACC311 ACC501
- ACF - (Accounting And Finance Related)
ACF619 ACFI619
- BNK - (Banking Related)
BNK601BNK603BNK604BNK619BNKI619
- COM - (Commerce Related)
COM619COMI619
CS - (Computer Sciences)
CS001 CS101 CS201 CS301 CS302 CS304 CS401 CS402 CS403 CS408 CS410 CS501 CS502 CS504 CS506 CS507 CS508 CS601 CS602 CS604 CS605 CS606 CS607 CS609 CS610 CS614 CS615 CS619 CS701 CS702 CS703 CS704 CS708 CS709 CS712 CS716 CS718 CS720 CS723
ECO - (Economics Related)
ECO401 ECO402 ECO403 ECO404
ENG - (English Related)
ENG001 ENG101 ENG201 ENG301 ENG401
ETH201 - Ethics (for Non-Muslims)
ETH201
- FIN - (Finance Related)
FIN611 FIN621 FIN622 FIN623 FIN624 FIN625 FIN630 FIN619
FINI619
HRM - (Human Resources Related)
HRM611 HRM619 HRMI619 HRM623 HRM624 HRM625 HRM627 HRM628
HRM619 HRMI619
ISL201 - Islamic Studies
ISL201
- IT - (Info Tech Related)
IT430
- MCM - (Mass Media Related)
MCM101 MCM301 MCM304 MCM310 MCM311 MCM401 MCM404 MCM411 MCM431 MCM501 MCM511 MCM514 MCM515 MCM516 MCM517 MCM520MCM531 MCM532 MCM601 MCM604 MCM610 MCM619 MCMI619
- MGMT - (Management Related)
MGMT510 MGMT611 MGMT623 MGMT625 MGMT627 MGMT628 MGMT629 MGMT630
- MGT - (Finance And Management Related)
MGT101 MGT111 MGT201 MGT211 MGT301 MGT401 MGT402 MGT411 MGT501 MGT502 MGT503 MGT504 MGT510 MGT520 MGT601 MGT602 MGT603 MGT604 MGT610 MGT611 MGT613 MGT619 MGTI619
MIS - (Project And Internship Report)
MIS619 MISI619
MKT - (Marketing Related)
MKT501 MKT610 MKT611 MKT621 MKT624 MKT625 MKT630 MKT619
MKTI619
MTH - (Maths Related)
MTH001 MTH101 MTH202 MTH301 MTH302 MTH401 MTH501 MTH601
MTH603
PAD - (Public Administration Related)
PAD619 PADI619
PAK301 - Pakistan Studies
PAK301
PHY - (Physics Related)
PHY101 PHY301
- PSC201 - International Relations
PSC201
- PSY - (Psychology Related)
PSY101 PSY401 PSY402 PSY403 PSY404 PSY405 PSY406 PSY407 PSY408 PSY409 PSY502 PSY504 PSY505 PSY510 PSY511 PSY512 PSY513 PSY514 PSY515 PSY610 PSY619 PSY631 PSY632 PSYI619
SOC - (Socialogy Related)
SOC101 SOC401
- STA - (Statistics and Research)
STA301 STA630

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.

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.

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.

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.

More cracks from the Denali earthquake, Alaska, 2002.

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.

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.

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.

Road rendered in two: Denali earthquake, Alaska, 2002.

An even more massive quake to shake America in recent years was Alaska's 2002 Denali earthquake.

Huge cracking and a hole in the highway.

Measuring 7.9 on the moment magnitude scale, the Denali earthquake in Alaska 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.

Cracked yet? Ground level changes.

Thanks to the remote location in which the Denali Earthquake in Alaska 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.

Yamabe Bridge: Chuetsu earthquake, Japan, 2004.

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.

Cracks in the ground: Nias earthquake, Indonesia, 2005.

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.

On this evidence, it's small wonder cracks in the ground have such apocalyptic associations.

Tags: AND, EARTH, FAULTS, GEOLOGICAL, TEAR

Views: 3

 

=======================

Virtual University Services

=======================

|*| VU TV
|*| VU SITES

|*| VU EMAIL

|*| VU RADIO

|*| VU ALUMNI

|*| VU LIBRARY

|*| HEC Recognised Universities
Created By
: Ismail Shah

Senior Admin : Saba Gul

Managment : Moderators

Powered bY eZiLine Developers

© 2012   Created by ¤iSmAiL sHaH¤.

Badges  |  Report an Issue  |  Terms of Service