من يعرف الانجليزية اريد ان يساعدني للثانية ثانوي

عنوان الموضوع : من يعرف الانجليزية اريد ان يساعدني للثانية ثانوي
مقدم من طرف منتديات العندليب

اريد فقرات عن جميع الكوارث بالانجليزية مثل الزلااوزل او الفيضانات او البراكين مع كيفية الاحطياطات
اريد فقرات لا تتجاوز 6 او 7 اسطر فقط
بلييييييييييييييييييييييييييييز مساعدة

>>>>> ردود الأعضـــــــــــــــــــاء على الموضوع <<<<<
==================================

>>>> الرد الأول :

لم اجد اية مساعدة مشكورين

=========

>>>> الرد الثاني :

اتمنى انك تستفيدي من هذا البحث


An earthquake (also known as a tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. Earthquakes are recorded with a seismometer, also known as a seismograph. The moment magnitude of an earthquake is conventionally reported, or the related and mostly obsolete Richter magnitude, with magnitude 3 or lower earthquakes being mostly imperceptible and magnitude 7 causing serious damage over large areas. Intensity of shaking is measured on the modified Mercalli scale.

At the Earth's surface, earthquakes manifest themselves by shaking and sometimes displacing the ground. When a large earthquake epicenter is located offshore, the seabed sometimes suffers sufficient displacement to cause a tsunami. The shaking in earthquakes can also trigger landslides and occasionally volcanic activity.

In its most generic sense, the word earthquake is used to describe any seismic event—whether a natural phenomenon or an event caused by humans—that generates seismic waves. Earthquakes are caused mostly by rupture of geological faults, but also by volcanic activity, landslides, mine blasts, and nuclear experiments. An earthquake's point of initial rupture is called its focus or hypocenter. The term epicenter refers to the point at ground level directly above this.


Naturally occurring earthquakes


Tectonic earthquakes will occur anywhere within the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane. In the case of transform or convergent type plate boundaries, which form the largest fault surfaces on earth, they will move past each other smoothly and aseismically only if there are no irregularities or asperities along the boundary that increase the frictional resistance. Most boundaries do have such asperities and this leads to a form of stick-slip behaviour. Once the boundary has locked, continued relative motion between the plates leads to increasing stress and therefore, stored strain energy in the volume around the fault surface. This continues until the stress has risen sufficiently to break through the asperity, suddenly allowing sliding over the locked portion of the fault, releasing the stored energy. This energy is released as a combination of radiated elastic strainseismic waves, frictional heating of the fault surface, and cracking of the rock, thus causing an earthquake. This process of gradual build-up of strain and stress punctuated by occasional sudden earthquake failure is referred to as the Elastic-rebound theory. It is estimated that only 10 percent or less of an earthquake's total energy is radiated as seismic energy. Most of the earthquake's energy is used to power the earthquake fracture growth or is converted into heat generated by friction. Therefore, earthquakes lower the Earth's available elastic potential energy and raise its temperature, though these changes are negligible compared to the conductive and convective flow of heat out from the Earth's deep interior.

Earthquake fault types

There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other ; transform boundaries are a particular type of strike-slip fault. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip; this is known as oblique slip.

Earthquakes away from plate boundaries

Where plate boundaries occur within continental lithosphere, deformation is spread out a over a much larger area than the plate boundary itself. In the case of the San Andreas fault continental transform, many earthquakes occur away from the plate boundary and are related to strains developed within the broader zone of deformation caused by major irregularities in the fault trace (e.g. the “Big bend” region). The Northridge earthquake was associated with movement on a blind thrust within such a zone. Another example is the strongly oblique convergent plate boundary between the Arabian and Eurasian plates where it runs through the northwestern part of the Zagros mountains. The deformation associated with this plate boundary is partitioned into nearly pure thrust sense movements perpendicular to the boundary over a wide zone to the southwest and nearly pure strike-slip motion along the Main Recent Fault close to the actual plate boundary itself. This is demonstrated by earthquake focal mechanisms.
All tectonic plates have internal stress fields caused by their interactions with neighbouring plates and sedimentary loading or unloading (e.g. deglaciation). These stresses may be sufficient to cause failure along existing fault planes, giving rise to intraplate earthquakes.

Shallow-focus and deep-focus earthquakes

The majority of tectonic earthquakes originate at the ring of fire in depths not exceeding tens of kilometers. Earthquakes occurring at a depth of less than 70 km are classified as 'shallow-focus' earthquakes, while those with a focal-depth between 70 and 300 km are commonly termed 'mid-focus' or 'intermediate-depth' earthquakes. In subduction zones, where older and colder oceanic crust descends beneath another tectonic plate, deep-focus earthquakes may occur at much greater depths (ranging from 300 up to 700 kilometers). These seismically active areas of subduction are known as Wadati-Benioff zones. Deep-focus earthquakes occur at a depth at which the subducted lithosphere should no longer be brittle, due to the high temperature and pressure. A possible mechanism for the generation of deep-focus earthquakes is faulting caused by olivine undergoing a phase transition into a spinel structure.
Earthquakes and volcanic activity

Earthquakes also often occur in volcanic regions and are caused there, both by tectonic faults and by the movement of magma in volcanoes. Such earthquakes can serve as an early warning of volcanic eruptions, like during the Mount St. Helenseruption of 1980.

Earthquake clusters

Most earthquakes form part of a sequence, related to each other in terms of ******** and time.

Aftershocks

An aftershock is an earthquake that occurs after a previous earthquake, the mainshock. An aftershock is in the same region of the main shock but always of a smaller magnitude. If an aftershock is larger than the main shock, the aftershock is redesignated as the main shock and the original main shock is redesignated as a foreshock. Aftershocks are formed as the crust around the displaced fault plane adjusts to the effects of the main shock.

Earthquake swarms


February 2008 earthquake swarm near Mexicali



Earthquake swarms are sequences of earthquakes striking in a specific area within a short period of time. They are different from earthquakes followed by a series of aftershocks by the fact that no single earthquake in the sequence is obviously the main shock, therefore none have notable higher magnitudes than the other. An example of an earthquake swarm is the 2004 activity at Yellowstone National Park.

Earthquake storms

Sometimes a series of earthquakes occur in a sort of earthquake storm, where the earthquakes strike a fault in clusters, each triggered by the shaking or stress redistribution of the previous earthquakes. Similar to aftershocks but on adjacent segments of fault, these storms occur over the course of years, and with some of the later earthquakes as damaging as the early ones. Such a pattern was observed in the sequence of about a dozen earthquakes that struck the North Anatolian Fault in Turkey in the 20th century and has been inferred for older anomalous clusters of large earthquakes in the Middle East.

Size and frequency of occurrence

Minor earthquakes occur nearly constantly around the world in places like California and Alaska in the U.S., as well as in Guatemala. Chile, Peru, Indonesia, Iran, Pakistan, the Azores in Portugal, Turkey, New Zealand, Greece, Italy, and Japan, but earthquakes can occur almost anywhere, including New York City, London, and Australia. Larger earthquakes occur less frequently, the relationship being exponential; for example, roughly ten times as many earthquakes larger than magnitude 4 occur in a particular time period than earthquakes larger than magnitude 5. In the (low seismicity) United Kingdom, for example, it has been calculated that the average recurrences are: an earthquake of 3.7 - 4.6 every year, an earthquake of 4.7 - 5.5 every 10 years, and an earthquake of 5.6 or larger every 100 years. This is an example of the Gutenberg-Richter law.
The number of seismic stations has increased from about 350 in 1931 to many thousands today. As a result, many more earthquakes are reported than in the past, but this is because of the vast improvement in instrumentation, rather than an increase in the number of earthquakes. The USGS estimates that, since 1900, there have been an average of 18 major earthquakes (magnitude 7.0-7.9) and one great earthquake (magnitude 8.0 or greater) per year, and that this average has been relatively stable. In recent years, the number of major earthquakes per year has decreased, although this is thought likely to be a statistical fluctuation rather than a systematic trend. More detailed statistics on the size and frequency of earthquakes is available from the USGS.
Most of the world's earthquakes (90%, and 81% of the largest) take place in the 40,000-km-long, horseshoe-shaped zone called the circum-Pacific seismic belt, also known as the Pacific Ring of Fire, which for the most part bounds the Pacific Plate. Massive earthquakes tend to occur along other plate boundaries, too, such as along the Himalayan Mountains. Humans can cause earthquakes for example by constructing large dams and buildings, drilling and injecting liquid into wells, and by coal mining and oil drilling.
With the rapid growth of mega-cities such as Mexico City, Tokyo or Tehran, in areas of high seismic risk, some seismologists are warning that a single quake may claim the lives of up to 3 million people.

Effects/impacts of earthquakes


1755 copper engraving depicting Lisbon in ruins and in flames after the 1755 Lisbon earthquake. A tsunami overwhelms the ships in the harbor.


There are many effects of earthquakes including, but not limited to the following:

Shaking and ground rupture

Shaking and ground rupture are the main effects created by earthquakes, principally resulting in more or less severe damage to buildings or other rigid structures. The severity of the local effects depends on the complex combination of the earthquake magnitude, the distance from epicenter, and the local geological and geomorphological conditions, which may amplify or reduce wave propagation. The ground-shaking is measured by ground acceleration.
Specific local geological, geomorphological, and geostructural features can induce high levels of shaking on the ground surface even from low-intensity earthquakes. This effect is called site or local amplification. It is principally due to the transfer of the seismic motion from hard deep soils to soft superficial soils and to effects of seismic energy focalization owing to typical geometrical setting of the deposits.
Ground rupture is a visible breaking and displacement of the earth's surface along the trace of the fault, which may be of the order of several metres in the case of major earthquakes. Ground rupture is a major risk for large engineering structures such as dams, bridges and nuclear power stations and requires careful mapping of existing faults to identify any likely to break the ground surface within the life of the structure.

Landslides and avalanches

Landslides are a major geologic hazard because they can happen at any place in the world, much like earthquakes. Severe storms, earthquakes, volcanic activity, coastal wave attack, and wildfires can all produce slope instability. Landslide danger may be possible even though emergency personnel are attempting rescue.

Fires


Fires of the 1906 San Francisco earthquake


Following an earthquake, fires can be generated by break of the electrical power or gas lines. In the event of water mains rupturing and a loss of pressure, it may also become difficult to stop the spread of a fire once it has started. For example, the deaths in the 1906 San Francisco earthquake were caused more by the fires than by the earthquake itself.

Soil liquefaction

Soil liquefaction occurs when, because of the shaking, water-saturated granular material (such as sand) temporarily loses its strength and transforms from a solid to a liquid. Soil liquefaction may cause rigid structures, as buildings or bridges, to tilt or sink into the liquefied deposits. This can be a devastating effect of earthquakes. For example, in the 1964 Alaska earthquake, many buildings were sunk into the ground by soil liquefaction, eventually collapsing upon themselves.

Tsunami


The tsunami of the 2004 Indian Ocean earthquake



Tsunamis are long-wavelength, long-period sea waves produced by an sudden or abrupt movement of large volumes of water. In the open ocean, the distance between wave crests can surpass 100 kilometers, and the wave periods can vary from five minutes to one hour. Such tsunamis travel 600-800 kilometers per hour, depending on water depth. Large waves produced by an earthquake or a submarine landslide can overrun nearby coastal areas in a matter of minutes. Tsunamis can also travel thousands of kilometers across open ocean and wreak destruction on far shores hours after the earthquake that generated them.

Ordinarily, subduction earthquakes under magnitude 7.5 on the richter scale do not cause tsunamis. However, there have been recorded instances, yet most destructive tsunamis are caused by magnitude 7.5 plus earthquakes.
Tsunamis are distinct from tidal waves, because in a tsunami, water flows straight instead of in a circle like the typical wave. Earthquake-triggered landslides into the sea can also cause tsunamis.

Floods

A flood is an overflow of any amount of water that reaches land Floods usually occur because of the volume of water within a body of water, such as a river or lake, exceeds the total capacity of the formation, and as a result some of the water flows or sits outside of the normal perimeter of the body. However, floods may be secondary effects of earthquakes, if dams are damaged. Earthquakes may cause landslips to dam rivers, which then collapse and cause floods.
The terrain below the Sarez Lake in Tajikistan is in danger of catastrophic flood if the landslide dam formed by the earthquake, known as the Usoi Dam, were to fail during a future earthquake. Impact projections suggest the flood could affect roughly 5 million people.

Human impacts

Earthquakes may result in disease, lack of basic necessities, loss of life, higher insurance premiums, general property damage, road and bridge damage, and collapse of buildings or destabilization of the base of buildings which may lead to collapse in future earthquakes. Earthquakes can also lead to volcanic eruptions, which cause further damages such as substantial crop damage, like in the "Year Without a Summer" (1816).
Most of civilization agrees that human death is the most significant human impact of earthquakes.

Preparation for earthquakes

Today, there are ways to protect and prepare possible sites of earthquakes from severe damage, through the following processes: Earthquake engineering, Earthquake preparedness, Household seismic safety, Seismic retrofit (including special fasteners, materials, and techniques), Seismic hazard, Mitigation of seismic motion, and Earthquake prediction.

Earthquakes in culture


Mythology and religion

In Norse mythology, earthquakes were explained as the violent struggling of the god Loki. When Loki, god of mischief and strife, murdered Baldr, god of beauty and light, he was punished by being bound in a cave with a poisonous serpent placed above his head dripping venom. Loki's wife Sigyn stood by him with a bowl to catch the poison, but whenever she had to empty the bowl the poison would drip on Loki's face, forcing him to jerk his head away and thrash against his bonds, causing the earth to tremble.
In Greek mythology, Poseidon was the god of and cause earthquakes. When he was in a bad mood, he would strike the ground with a trident, causing this and other calamities. He also used earthquakes to punish and inflict fear upon people as revenge.

Popular culture

In modern popular culture, the portrayal of earthquakes is shaped by the memory of great cities laid waste, such as Kobe in 1995 or San Francisco in 1906.[34] Fictional earthquakes tend to strike suddenly and without warning.[34] For this reason, stories about earthquakes generally begin with the disaster and focus on its immediate aftermath, as in Short Walk to Daylight (1972), The Ragged Edge (1968) or Aftershock: Earthquake in New York (1998). A notable example is Heinrich von Kleist's classic novella, The Earthquake in Chile, which describes the destruction of Santiago in 1647. Haruki Murakami's short fiction collection, After the Quake, depicts the consequences of the Kobe earthquake of 1995.
The most popular single earthquake in fiction is the hypothetical "Big One" expected of California's San Andreas Fault someday, as depicted in the novels Richter 10 (1996) and Goodbye California (1977) among other works.[34] Jacob M. Appel's widely-anthologized short story, A Comparative Seismology, features a con artist who convinces an elderly woman that an apocalyptic earthquake is imminent. In Pleasure Boating in Lituya Bay, one of the stories in Jim Shepard's Like You'd Understand, Anyway, the "Big One" leads to an even more devastating tsunami

=========

>>>> الرد الثالث :

انا اريد علي ما درسناه فقط ومن استطاع ان يحل لي هذه ومشكور اختي انا ضعيفة فيها ومن استطاع لا شكر علي واجب
using the following notes , write a paragraph on the 1980 earthquake of El Asnam
- October 10th ,1980
-seven on richter scale
-buildings and houses collapsed
-many casualties
-quick arrival of rescuers
-solidarity among Algerians
-foreign aid
-government program to reconstruct towns / villages.
وهذه
: write a piece of advice about the precautions that people should take before, during and after an earthquake
و هذه
: Write a short announcement to state the different safety measures that should be taken before,
durig and after an earthquake.
Use these notes:
a- Plan emergency procedures.
b- Don't panic.
c- Provide first aid.
d- Check for injuries
وهذي الاخيرة
Describe a disaster you have witnessed in your life

=========

>>>> الرد الرابع :

اوكي اختي السؤال عن زلزال شلف (الاصنام سابقا) يوم 10 اكتوبر 1980 ويطلب منك ان تكتبي حول نتائجه ومذا فعلت او برنامج الدولة لاعادة بناء المدن واالقرى



1980 El Asnam earthquake is located in Algeria

The 1980 El Asnam earthquake was an earthquake that occurred in the Algerian town of El Asnam, now known as Chlef, within the central part of the Chelif valley. The earthquake - at 7.3 on the Richter scale the largest earthquake in Algeria - was followed 3 hours later by an aftershock measuring 6.3 on the Richter scale, and these two quakes caused considerable damage and a high death toll.

The initial earthquake occurred at 12.24 GMT. Reports initially put the death toll much higher at around 20,000. The final death toll, however, ended up being around 3,500. The town's main hospital, a big department store, the central mosque, a girls' school and two housing complexes were destroyed.[1] Around 300,000 people were left homeless. The earthquake was the largest in the Atlas range since 1790.[2]

اما بالنسبة لاخر عنصر وهو"" ماهو برنامج الحكومة لاعادة بناء المدن والقرى"" لم اجد بحثت لكي لكن لم اجد اي معلومات

=========

>>>> الرد الخامس :

write a piece of advice about the precautions that people should take before, during and after an earthquake:
اكتب مجموعة نصائح حول الاحتياطات التي يجب على الناس القيام بها قبل و اثناء وبعد الهزة الارضية(الزلزال)

What to Do Before an Earthquake///ما الذي يجب فعله قبل الزلزال


Make sure you have a fire extinguisher, first aid kit, a battery-powered radio, a flashlight, and extra batteries at home.
Learn first aid.
Learn how to turn off the gas, water, and electricity.
Make up a plan of where to meet your family after an earthquake.
Don't leave heavy objects on ****ves (they'll fall during a quake).
Anchor heavy furniture, cupboards, and appliances to the walls or floor.
Learn the earthquake plan at your school or workplace.

What to Do During an Earthquake//مالذي يجب فعله اثناء الزلزال

Stay calm! If you're indoors, stay inside. If you're outside, stay outside.
If you're indoors, stand against a wall near the center of the building, stand in a doorway, or crawl under heavy furniture (a desk or table). Stay away from windows and outside doors.
If you're outdoors, stay in the open away from power lines or anything that might fall. Stay away from buildings (stuff might fall off the building or the building could fall on you).
Don't use matches, candles, or any flame. Broken gas lines and fire don't mix.
If you're in a car, stop the car and stay inside the car until the earthquake stops.
Don't use elevators (they'll probably get stuck anyway).

//What to Do After an Earthquake// مالذي يجب فعله بعد الزلزال

Check yourself and others for injuries. Provide first aid for anyone who needs it.
Check water, gas, and electric lines for damage. If any are damaged, shut off the valves. Check for the smell of gas. If you smell it, open all the windows and doors, leave immediately, and report it to the authorities (use someone else's phone).
Turn on the radio. Don't use the phone unless it's an emergency.
Stay out of damaged buildings.
Be careful around broken glass and debris. Wear boots or sturdy shoes to keep from cutting your feet.
Be careful of chimneys (they may fall on you).
Stay away from beaches. Tsunamis and seiches sometimes hit after the ground has stopped shaking.
Stay away from damaged areas.
If you're at school or work, follow the emergency plan or the instructions of the person in charge.
Expect aftershocks.

=========

Write a short announcement to state the different safety measures that should be taken before,
اكتب اعلان صغير لتبيين تدابير السلامة المختلفة التي ينبغي اتخاذها قبل وخلال وبعد الهزة الارضية
هذا السؤال مثل الذي قبله

اخر سؤال Describe a disaster you have witnessed in your life؟
وصف كارثة شاهدتها في حياتك

مشكورة اختي zahra علي جهودك هذي الفقرة راح يجبهنا في الامتحان وحدا منهم و مشكورا مرة تانية

المشاركة الأصلية كتبت بواسطة chouchoulaila https://3andlib.xplainer.net/images/...s/viewpost.gif مشكورة اختي zahra علي جهودك هذي الفقرة راح يجبهنا في الامتحان وحدا منهم و مشكورا مرة تانية

العفو أختي...في أي وقت

بالتوفيق ان شاء الله

WRITTEN COMPOSITION
A monthly magazine has invited readers to contribute some ideas on how to increase solidarity among people in case of a natural disaster (earthquake, tsunami, floods, hurricanes, etc.). Write a proposal on how you will deal with the problem and what solutions you will suggest.
أنا أحتاجها غدا أرجوكم ساعدونيييييييييييييييييي https://3andlib.xplainer.net/images/smilies/sdf.gif https://3andlib.xplainer.net/images/smilies/sdf.gif https://3andlib.xplainer.net/images/smilies/sdf.gif https://3andlib.xplainer.net/images/smilies/sdf.gif