Understanding Earthquakes and Tsunamis

  • Thread starter PRINCESS NOOR
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In summary, the earthquake that occurred in 2004 was unusually large in geographical extent, occurred in two phases, and was caused by the movement of plate magma.
  • #1
PRINCESS NOOR
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Dear Sir,

this an interruptions i would like to share and discuss with you.

1.is right that the main reason behind an earthquake is the plate's movements?
is there any reason other than the one which mentioned above.

2.i want i full explanation for the earthquake that occurred in tsunami and how it occurred?

with my regard
 
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  • #2
http://en.wikipedia.org/wiki/2004_Indian_Ocean_earthquake

The earthquake was unusually large in geographical extent. An estimated 1200 km (750 miles) of faultline slipped about 15 m (45 ft) along the subduction zone where the India Plate dives under the Burma Plate. The slip did not happen instantaneously but took place in two phases over a period of several minutes. Seismographic data indicate that the first phase involved the formation of a rupture about 400 km long and 100 km wide, located 30km beneath the sea bed. The rupture proceeded at a speed of about 2 km/s, beginning off the coast of Aceh and proceeding north-westerly over about 100 seconds. A pause of about another 100 seconds took place before the rupture continued northwards towards the Andaman and Nicobar Islands [7] (http://www.guardian.co.uk/life/feature/story/0,13026,1383675,00.html).

The India Plate is part of the great Indo-Australian Plate, which underlies the Indian Ocean and Bay of Bengal, and is drifting northeast at an average of 6 cm/year (2 inches/year). The India Plate meets the Burma Plate (which is considered a portion of the great Eurasian Plate) at the Sunda Trench. At this point the India Plate subducts the Burma Plate which includes the Nicobar Islands, the Andaman Islands and northern Sumatra. The India Plate slips deeper and deeper beneath the Burma Plate until the increasing temperature and pressure turns the subducting edge of the India Plate into magma which eventually pushes the magma above it out through the volcanoes (see Volcanic arc). This process is interrupted by the locking of the plates for several centuries until the build up of stress causes their release resulting in a massive earthquake and tsunami. The volcanic activity that results as the Indo-Australian plate subducts the Eurasian plate has created the Sunda Arc.
 
  • #3
PRINCESS NOOR said:
1.is right that the main reason behind an earthquake is the plate's movements?
Is there any reason other than the one which mentioned above.
Yes, there are some other causes :

1. Some earthquakes are caused by the movement of magma in volcanoes, and such quakes can be an early warning of volcanic eruptions.

2. A rare few earthquakes have been associated with the build-up of large masses of water behind dams, (such as the Kariba Dam in Zambia, Africa) and with the injection or extraction of fluids into the Earth's crust (e.g. at certain geothermal power plants and at the Rocky Mountain Arsenal).
 
  • #4
PRINCESS NOOR said:
2.i want i full explanation for the earthquake that occurred in tsunami and how it occurred?

You realize that a tsunami is an event, not a place, right?
 
  • #5
You realize that a tsunami is an event, not a place, right?


loooooooooool :rofl:
 

What causes earthquakes and tsunamis?

Earthquakes are caused by the sudden release of energy along fault lines in the Earth's crust. Tsunamis are caused by underwater earthquakes, landslides, or volcanic eruptions that displace large amounts of water.

How are earthquakes and tsunamis measured?

Earthquakes are measured using a seismograph, which records the seismic waves produced by the earthquake. The magnitude of an earthquake is measured using the Richter scale, which assigns a numerical value based on the amplitude of the seismic waves. Tsunamis are measured using a tide gauge or a buoy, which records the height of the waves.

Can we predict earthquakes and tsunamis?

Currently, we do not have the technology to predict earthquakes and tsunamis with accuracy. However, scientists can monitor seismic activity and ocean conditions to issue warnings and prepare for potential disasters.

What are the potential impacts of earthquakes and tsunamis?

Earthquakes and tsunamis can cause widespread destruction and loss of life. The shaking from earthquakes can damage buildings and infrastructure, while tsunamis can flood coastal areas and cause damage from strong currents and debris. Secondary effects, such as fires and landslides, can also occur.

How can we mitigate the effects of earthquakes and tsunamis?

There are several ways to mitigate the effects of earthquakes and tsunamis. Building codes can be implemented to ensure structures are designed to withstand seismic activity. Early warning systems can also be put in place to give people time to evacuate in the event of a tsunami. Education and preparedness also play a crucial role in reducing the impact of these natural disasters.

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