Earthquake

On January twelfth 2010, a deadly earthquake with a magnitude of 7.0 hit the coast of Port au prince, Haiti for 35 seconds, killing around 200,000 and leaving approximately to 1.5 million of the population homeless including kids who became orphans and vice versa in a matter of less than a minute. Before the earthquake, the way of life was not as bad as portrayed back at home, most of the news broadcasted in the mainstream media were exaggerated news, negative light and unfair tales to make Haiti

Body One: To begin with, London goes through the story by just giving people the gist of the people who met the violence of the earthquake while Anderson focuses on one discrete person even though many have had contact with the disaster we call Katrina. London informs us of the victims but doesn’t name them in detail. “With me sat Japanese, Italians, Chinese, and Negroes-- a bit of the cosmopolitan flotsam of the wreck of the city”( London 416). London clearly gives the race of the victims that surrounded

structures below the surface of the water and shielding the plates from rifting and pulling the islands into the rift (Abbott, 2013). Multi-story parking facilities have been proven to be problematic and very susceptible to collapse during an earthquake. Multi-story

2010 Haiti Earthquake and 1989 Loma Prieta Earthquake. The type of plate boundary for the Haiti Earthquake is a transform plate boundary. However, for the Loma Prieta Earthquake, it is a divergent plate boundary. The tectonic plates that were involved for both were the North American Plates, but the second plates are not the same. The Caribbean plate was the second plate for the Haiti earthquake and Pacific plate was the Loma Prieta earthquake. The depth and magnitude of the earthquake is related

A 6.9-magnitude earthquake struck northeastern Japan on Tuesday morning at about 6 am local time (GMT 9 pm Monday), which triggered a minor tsunami wave. The earthquake was initially approximated at 7.3 in magnitude, but later downgraded to 6.9 by US Geological Survey. Its epic center was located off the coast of Fukushima prefecture in Honshu island at a depth of about 9 miles. The height of waves triggered by the quake varied in different coastal regions, from 1.4 meters at Sedai port in Miyagi

Earthquake survivors in Iran complained about the slow relief efforts as they asked for authorities to provide them food and shelter while they brave the cold weather. Iran's earthquake, which occurred on November 12, registered at least 530 fatalities and thousands of injuries, and it was also recognized as the country's deadliest quake in more than a decade as it was recorded to possess a 7.3 magnitude. In response to these insights, Iranian Supreme Leader Ayatollah Ali Khamenei urged the agencies

The earthquake affected nearly one-third of the country’s total population which was three million people. Over one million people was left homeless in the immediate aftermath. In the devastated urban areas, the displaced were forced to squat in ersatz cities composed of found materials and donated tents. Looting—restrained in the early days following the quake—became more prevalent in the absence of sufficient supplies and was exacerbated in the capital by the escape of several thousand prisoners

The Haiti earthquake of 2010 challenged the way the international humanitarian community had been collecting data for and during an emergency crisis. After any large-scale disaster, there is always a period of chaos where NGOs are trying to gather and analyze as much critical information as possible that would be required to establish the essential needs of the affected persons most efficiently, this comes as a result of humanitarian organizations failure to develop adequate preparedness for disaster

The 2010 Haiti Earthquake Location: The epicentre was located near the town of Léogâne, which is approximately 25 kilometres west of Haiti’s capital, Port-au-Prince. (See figure 1.1) Date/time: 16:53 local time on Tuesday, January 12th, 2010. Description of the event The earthquake was caused by a “blind thrust” fault action along the Enriquillo-Plantain Garden fault system, which had been building up stress for the past 250 years. A blind fault is a rupture in a lithospheric plate that does not

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