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Strategies to tackle natural and man made disaster
Mitigating the impact of disaster
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Landslides Warning System
INTRODUCTION
Landslides are the down slope movement of mass of land, rock, soil, or
related debris. In most mass movement, water plays a pivotal role by
assisting in the decomposition and loosening of rock, lubricating rock
and soil surfaces to enhance the beginning of movement, adding weight
to an incipient landslide, and imparting a buoyancy to the individual
particles, which helps overcome the inertia to move.
Landslides can also be triggered from volcanic eruptions and
earthquakes, which initiate earth movement on a grand scale.
Landslides are frequently the direct consequence of human activity.
They are predominant in highland areas where Agricultural irrigation
and forestry practices such as clear-cutting and stripping vegetation
from naturally oversteepened slopes are eminent. Highway construction
on similar slope conditions awaits only the first good rain to provoke
earth movement. In an urban setting, improper drainage most often
induces disastrous sliding.
The goal of early warning is born from a hope to head off conflict
before it becomes costly. Landslides cause significant economic damage
and hazard to environment all over the world. Apart from preventive
measures, early warning and fast extinction of Landslides are the only
chance to avoid major casualties and damage to nature, especially in
regions with dense population.
ABSTRACT
Landslides are often recurring phenomena, the systems which meant to
deal with the same must meet the domain requirements, be effectively
developed and flexible to changes. What is needed to make these new
warning sensors available is money fo...
... middle of paper ...
... automatically
interrupt local radio and television broadcasts, would be broadcast to
radio alert systems and broadcasts
To personal landscape warning beeper system.
ARCHITECTURAL DESIGN
SUBYSTEMS AND THEIR COMPENENTS
Sensors: detects the movement of rocks below the surface through the
gauge wires.
Computation components: receives signals from sensors, determine the
risk and produce some output. The system uses computers.
Communication systems: allow system components to communicate. Optical
fibers are
Used in this case.
Siren: emits an audible warning when a threshold is reached.
Alarm controller: Controls the operation of the system.
External control center: receive commands from the control center and
connects to radio stations and personal landscape warning beeper
systems.
There are three clear landslides; the southwest landslide is stream-laid sand and gravel from the quaternary that was located on a steep slope resulting in gravity pulling sediments down the steep slope. The northeast landslide appears to be tuff sediments that have fallen upon biotite-quartz diorite rocks. The northwestern landslide is the largest of the landslides. The landslide occurred just south of the creek; erosion must have lowered the creeks elevation creating a steep decline resulting in Bena gravel to fall.
Regina:The Early Years. (2014). Cyclone of 1912. Regina: The Early Years 1880 -1950. Retrieved March 7, 2014, from http://scaa.usask.ca/gallery/regina/central/cyclone.html
Avalanches kill back country recreationalists every year, including skiers, snowboarders, snowshoers, and snowmachiners. All back country users should have knowledge of the basic physics of avalanches to help them evaluate local and regional potential for slides. The foundation of this knowledge comes from understanding how the surrounding environmental conditions in previous weeks, previous days, and the day in question all contribute to snow stability or instability, and how specific factors affect snow on a micro-scale, which determines how snow slopes will behave on a macro-scale. There are two major types of avalanches (excluding debris avalanches from broken cornices and ice formations). These are point releases, or loose snow slides, and slab avalanches. While point releases can be dangerous and should be avoided, slab avalanches are much more catastrophic and account for most of the backcountry avalanche disasters involving humans. Basic physics of point releases are discussed here, followed by a discussion on the basic physics of slab avalanches, and how external factors contribute to the stability or instability of a snow covered slope.
New Madrid earthquake of 1811-1812 was known to be “one of the most powerful earthquake felt throughout the Eastern United State”(2,75) . “December 16, 1811 at 2 a.m”(1). , the first earthquake had struck in the Northern part of Arkansas through Missouri. “This earthquake occurred in Central Mississippi Valley”(2,2) . New Madrid fault is located in the northern part of Missouri and southern part of Illinois. On the morning of December 16, 1811, when the earthquake struck; “people were scared”(10,26) , they ran out of their houses as the trees were falling onto the ground and the ground was breaking up. After the earthquake ended, around 7 a.m., one of the largest aftershock occurred and it was known to be a destructive shock because
Mill also addresses the idea of governments interfering in an individual’s life in some form of help or benefit without infringing on any liberties by presenting his three objections. The first of which being the idea that “… when the thing to be done is likely to be better done by individuals than by the government.” (Mill p.121). He believed that individuals can best decide matters which pertain to their own life because they are the ones who are most “personally interested in it.” (Mill p.121) and because the individual is indeed usually the one who possesses the most intimate knowledge of their own life that they should not allow others to decide what is best for them personally. The second of Mill’s objections is that even when the individual
D.J. Dowrick (”Earthquake Risk Reduction”in Wiley) explains that seismic hazard is any physical phenomenon associated with an earthquake that may produce adverse effects on human activities. Earthquakes occur very suddenly without any warning. Thus, earthquake not only destructs people’s living environment, but also affects people’s mental health. People are more scared of earthquake. In 2010, there are two severe earthquakes, which are Haiti Earthquake and Chile Earthquake. Both of these two earthquakes produced the various impact considerably across countries and regions. The purpose of this essay is to analyse those two earthquakes according to knowledge such as why they occur, how strong they are, and what the impact they made. Even though people still can not predict earthquake, through analyse earthquakes, they can prevent it bring huge losses.
Stokoe II and Nazarian (1983) created method termed spectral analysis of surface waves (SASW) and its purpose is to scrutinize dispersion curves of ground roll to yield near surface S-wave velocity profiles. In the spectral analysis of surface wave technique, we use the spectral analysis of ground roll created by an impulsive source, such as a weight drop, and the resulting waves would be recorded on a pair of receivers, also called geophones on land surveys. The data will be examined in the frequency domain in order to create a dispersion curve by calculating the phase difference between each deployment of receiver pairs (Park et. al,
Information is perhaps one of the most crucial elements in regards to disaster preparedness. Resultantly, it is vital that individuals understand what information is relevant to the local area and how to obtain information in the event of a disaster or emergency. Furthermore, it is essential that individuals stay informed prior to, during, and after a disaster. Described below are some of the key elements to consider in regards to being and staying informed:
Earthquake is the earth tremor that results from the sudden release of the pent-up energy in the earth’s crust. This released energy creates the seismic waves that determine the frequency, type and size of the earthquakes. Any earthquakes whose magnitude is bellow 5 on the Richter scale is considered weak, while the earthquakes whose magnitude is above 7on the Richter scale is considered potentially dangerous. The largest earthquake ever register in the history of man is the earthquake in Japan in 2011 which had a magnitude of 9.0 on the Mercalli scale(Seeram, pars. 4-5). While most earthquakes are causes by seismic events on the earth’s crust, these can be accelerated by natural events, or the activities of the human beings. For example, when the geological faults lines rapture, pressure is created in the earth’s crust forcing its way out thereby causing a break or sliding along the fault line. Volcanic activities are also known to cause earthquakes and so are nuclear test, bombs and landslides. The hypocenter is the initial point from which the raptures occur, while the epicenters is the ground directly above the hypocenter (Zacharias,, sec. A)
This leads to formulating certain survival procedures, researching new technology and preparing and for an earthquake and volcanic eruptions. To overcome the effects of earthquakes, scientists and engineers have designed earthquake resistant infrastructure. This was created because common infrastructures fail in earthquakes as there are heavy and can 't stand seismic waves. The major cause of death during earthquakes is being killed by a falling building. However, in earthquake resistant building the main concept is to make the building as rigid, strong and out of the lightest material possible so if it does fall individuals have a possibility of surviving. At the bottom of earthquake resistant building, there would be some sort of shock absorber, so it can absorb the seismic waves reducing the impact. Then, the building will incorporate a sheer core and sheer walls, to reduce the rocking movements of an earthquake. Along with this, walls will have two steam beams for added security. In developing countries, a similar type of plan is used but the building is made out of more cheaper and everyday objects. Another defence systems humans use to adapt to earthquakes and volcanoes is monitoring and warning systems. Monitoring and warning systems are usually controlled by local or national governments. In earthquake situations, sensors (which are distributed in the region prone to earthquakes) send information to the alert centre when a seismic wave is detected, there the information is investigated. Afterwards, the information from the alert centre is immediately transmitted to the individuals of the region warning them about the expected intensity and arrival time of earthquake by text message or call. After that, it is advised that individuals turn off all electrical appliances and follow their local earthquake
Living in Bangladesh, we have seen quite disastrous mudslides from the past few years. Mudslide is also called a landslide or a land slip. It is a downward mass movement of earth or rock on unstable slopes, including many forms resulting from differences in rock structure, coherence of material involved, degree of slope, amount of included water, extent of natural or artificial undercutting at the base of the slope, relative rate of movement, and relative quantity of material involved. There are numerous facts that can cause a mudslide and there are also numerous effects that it can cause us.
...strous. These landslides were caused by the heavy rainfall which often caused the hills being dug to give way, resulting in massive landslides. The workers cut their way through the continent with dynamite and steam shovels. These engineering maneuvers were slow and time consuming but were completed successfully (McCullough 106-108).
Authorities have attempted to implement codes or regulations, but that has proved to be very difficult tasks becasue there are many variables that effect the dynamic response of buildings. One way to try to avoid disaster is to evaluate seismic risk is to look at a buildings hazards, exposure, vulnerability, and location. Hazards are, for example, landslides ad soil type. Exposure is a building's occupancy and function. Vulnerability is the expected performance of a building's system, and location is how often earthquakes occur in the area. (Lagorio)
Johns Hopkins University. (2009, March). In disaster-prone areas, construction needs a new approach. Retrieved from http://phys.org/news157051992.html
Earthquakes belong to the class of most disastrous natural hazards. They result in unexpected and tremendous earth movements. These movements results from dissemination of an enormous amount of intense energy in form of seismic waves which are detected by use of seismograms. The impact of earthquakes leaves behind several landmarks including: destruction of property, extensive disruption of services like sewer and water lines, loss of life, and causes instability in both economic and social components of the affected nation (Webcache 2).