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Large Quantity of energy is released during an earthquake with a combination of radiated elastic strain seismic waves frictional, heating of the fault surface and cracking of the rock, thus causing an earthquake. When two plates of earth interact at their boundaries they develop stress of earth's crust. When this stress exceeds a critical value, a sudden failure happens and stress is released, as energy. This process of gradual build-up of stress and strain punctuated by occasional earthquake failure is known as elastic-rebound theory.
Seismic energy is only 10% or less of the earthquake's total energy. Most part of the earthquake energy is used to power the earthquake fracture growth or is converted in to heat generated by friction. Therefore, earthquakes lower the earth's available elastic potential energy and raise its temperature.
Prophase This is the first and longest phase of mitosis .At its beginning all 10 nm segments of chromatids (= chromonemata) of the duplicated chromatin fibres of interph
A 62 year old white male develops pitting edema of both feet. Put on Lasix and metoprolol. Develops hallucinations and confusion. Tapered off. Dies 3 weeks later of lymphatic o
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Major Criteria 1) Positive blood culture • Typical microorganism for infective endocarditis from two separate blood cultures Viridans streptococci, Streptococcus bovis, HAC
What are the physical propertie of sol Sols resemble liquids in their main physical properties - that is, they flow and they do not show rigidity of form. However, when a sol a
To verify the effect of intra-specific competition on the growth of saplings of Eucalyptus dives, an experiment was designed in which two sets of pots were used. In the first set o
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