Standing motor cars rocked noticeably. Build floors with a light material similar to the roof. The main cause is that when tectonic plates, one rides over the other, causing orogeny collide (mountain building), earthquakes. Measured 7. The correct answer is option ”c”. You can find these kinds of faults in California. The plates under the oceans are called oceanic plates and the rest are continental plates. The most obvious indication on a seismogram that a large earthquake has a deep focus is the small amplitude, or height, of the recorded surface waves and the uncomplicated character of the Pri­mary and Secondary waves. The earthquake originates from the entire fault – which may be 1000 km long. About 50,000 quakes of magnitudes 3 to 4 occur each year, and only about one of magnitude 8 to 9 each year. Join steel beams together by the feet and allow them to go outside the line of the building to decrease the chance of the structure overturning. (V) Felt by nearly everyone; many awakened. Comprehensive listing of seismic events are held by several agencies such as the International Serological Centre (ISC) in Newbury, UK, and the National Earthquake Information Centre at the World Data Centre A in Boulder, Colorado, USA. This is based on the Richter magnitude but also depends on the frequency of the wave, distance from the source, etc., and is of the form log E = aM + b. Earthquakes can range in size from those that are so weak that they cannot be felt to those violent enough to toss people around and destroy whole cities. The plates are moved around by the motion of a deeper part of the earth (the mantle) that lies underneath the crust. The distortion builds up very slowly, over tens or hundreds of years. The bronze ball would fall into the open mouth of one of the toads, making enough noise to alert someone that an earthquake had just happened. (VIII) Damage slight in specially designed structures. The Richter scale was named after the American seismologist Charles Francis Richter. These fires can be started by broken gas lines and power lines, or tipped over wood or coal stoves. Identifying the pattern can provide a clue to the size of the next earthquake. However, fool-proof prediction of large earthquakes is still not possible. By studying the seismogram, the seismologist can tell how far away the earthquake was and how strong it was. (III) Can be felt by persons indoors, especially on upper floors of buildings. The magnitude of a particular earthquake is a single number which does not vary from place to place. Dishes, windows, doors disturbed. Have a doubt at 3 am? They occur on lakes that are shaken by the earthquake and are usually only a few feet high, but they can still flood or knock down houses, and tip over trees.

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