Explain How Have Scientist Helped Save Lives In Earthquake Prone Areas

Despite decades of research and the use of modern technology, scientists are still not able to detect in time an imminent earthquake. Even though seismologists mostly know where the faults are and are able to closely monitor the rate of activity on them ranging from a scale of a year to a decade and even a century, a solid short-term day to month forecasting in order to identify the places at risk, still is an insoluble problem. Although this may be true, some scientists in diverse fields choose to follow a different and a rather controversial approach on the subject by studying the unusual animal

Steel frame structures are made as the name suggest from steel, the material is strong and flexible. When weight is added it bends without cracking. Another characteristic of steel is that its plasticity or ductility, meaning that when force is added it won’t crack however it will lose shape therefore giving warning for people to evacuate the building. A disadvantage of steel is that is loses strength when subject to fire. Studies have shown that it can loose up- to half its strength when subject to fire, therefore making it imperative to cover the steel with boards or spray on.

Earthquake early warning systems alert devices and people when shaking waves generated by an earthquake are expected to arrive at their location. The seconds to minutes of advance warning allow people and systems to take actions to protect life and property from disastrous shaking. Devices such as isolation systems and dampers are designed to reduce vibrations of structures being effected in an earthquake and are added to the design of some modern buildings mainly in Japan. Advanced radar and infrared cameras take a series of images collecting data to identify signs of earthquakes. Advanced Interferometric Synthetic Aperture Radar shows fault movements over a period of years. Modems and Data Processing centres receive data collected by satellites to analyse the trends recognised in the electromagnetic emissions, radar pictures, infrared readings and elf

A ‘hazard’ can be defined as a geophysical process operating within the lithosphere, atmosphere, hydrosphere or biosphere which could potentially lead to the loss of human life or property. However, an earthquake only becomes hazardous and therefore needs management if it occurs within close proximity to a vulnerable population. To some extent, any human settlement around the world situated close to or on top of an area of seismic activity is vulnerable. However, not all nations suffer equal devastation.

Over more than 50 decades there has been multiple earthquakes that have been caused by the activity that takes place beneath and above the surface of the earth. For every earthquake there are various effects and consequences, these are generally not preventable but teachable moments. As we study and explore landforms we learn and better understand how today 's structures came about, what took place decades ago and where do we go from here. Thanks to the technology and inquiring minds we are able to study past events like the 1906 San Francisco earthquake and the 1964 Alaska earthquake. In comparing these two events we can get an overview of what happened and better prepare ourselves for something like that in the future.

Earthquakes have been recorded throughout history for thousands of years. Even before seismographs in early times, there are records and accounts of mysterious ground shaking. Earthquakes occur when rocks break along an underground fault (UPSeis, 2007). This, in return, causes vibrations through the earth which causes ground shaking. The magnitude of the shaking varies depending on how great the movement along the fault is; the greater the movement, the bigger the earthquake. Some earthquakes are huge and cause significant damage, while others are small and cause little or no damage what-so-ever. Earthquakes are unpredictable, and can happen at any time. It is uncertain where an earthquake will strike, but there is a greater risk

According to Brillinger (2011), earthquakes were recorded after happening to get an earthquake statistics. Earthquakes may be large or small, serious or trivial; however, the higher the magnitude, the greater the damage to a particular location and the surrounding area. Earthquakes can also create other natural disasters, like tsunamis and volcanic eruptions, which bring more dangerous disasters than earthquakes. Statistics of earthquakes can be extremely important for it can give governments plans to do rebuilding after earthquakes, can help scientists better detect and anticipate earthquakes, and can provide more information to public to learn about earthquakes. It is helpful to take a look at existed statistics; from the website of US government,

The earthquakes above give a brief glimpse into the importance of analyzing past and present fault configurations. If scientists could make a breakthrough in this area perhaps we could better predict earthquake activity and better prepare ourselves if it is deemed a potential disaster is looming.

Earthquake Hazards occur when there are adverse effects on human activities. This can include surface faulting, ground shaking and liquefaction. In this essay I will be discussing the factors that affect earthquakes, whether human such as population density, urbanisation and earthquake mitigation or physical such as liquefaction, magnitude, landslides and proximity to the focus.

When and Earthquake occurs it generates seismic waves in a pond by the ripples and the wind, but also travelling downwards through the earth. Scientists can detect and measure the vibrational waves at great

The earthquake was felt from southern Oregon to south of Los Angeles and inland as far as central Nevada, an area of approximately 200,000 square miles. The ground motion caused by the earthquake source is recorded by instruments called seismographs. The zigzag trace made by a seismograph, called a "seismogram," reflects the changing amplitude and frequency content of the ground shaking beneath the instrument (usgs.gov). Using seismograms, scientists can determine the time, the epicenter, the depth, and the type of faulting of an earthquake as well as estimate how much energy was released by it.

In the U.S. alone, the average annual cost to repair damage caused by earthquakes is $4.4 billion USD. The worldwide figure is much larger than this but unquantifiable due to poorer countries unable to accurately determine the amount of damage that occurred. Year after year the cost of damages barely fluctuates from these ridiculously high figures and money must be pumped into repairing the damage done. Although a lot is being learnt about earthquakes and the fact that humans are now normally able to be alerted in time to evacuate the area the earthquake will affect, there have been no breakthroughs into reducing the amount of damage earthquakes cause to buildings and infrastructures.

Thesis statement: In the speech, I will continue to improve the earthquake’s knowledge of my audience by analyzing cases; introduce the significant idea of earthquake prediction; deeply develop rescue methods.

There are other ways to improve buildings to reduce the impact of earthquakes. In some Japanese buildings, there’s a base isolation built. The “Base Isolation” is a system that is made of steel disks. These steel disks are made of soft materials to soften the transmission of seismic movement from the ground

     An Earthquake is the shaking of the earth's surface caused by rapid movement of the earth's rocky outer layer. The sudden shaking of the ground that occurs when masses of rock change position below the Earth's surface is called an earthquake. The shifting masses send out shock waves that may be powerful enough to alter the surface of the Earth, thrusting up cliffs and opening great cracks in the ground.