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Natalia

You are so right that Skype, as well as other technological inventions, makes our lives and connections much easier. Personally I do not only communicate with my friends who are all over the globe, family who are in Russia, and former students from all over the world but also help teachers of English in Russia make their lesson more interesting and authentic. For instance, in December I organized a Skype lesson for my friend who teaches English in a remote village in Siberia. They do not have any opportunity to meet a native speaker there, but Skype made it possible. It is a great tool for making our life more interesting!

Acai Optimum

very informational... educative as well, i've been a very good follower of your blog... all am gonna say is good job!

Amponsah

what is your skype name Helen Benedict

Dave

dave.landers66 but if you are interested in Skyping with me please let me know a time when you might be available as I have classes and perhaps too many meetings as our semester ends in three weeks. :)

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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.

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