In this most recent  revolutionarys article readers are   apprised of what the National Science Foundation calls the third deepest plunge into the Earth.  In which scientist said they had drilled into the lower section of Earths crust for the first time.  This drilling was located at the   cooccur of the Mid-Atlantic ridge and the Atlantis fracture zone which are   both plates of the planets broken crust. This site is called the Atlantis Massif.  This location was   chosen due to the seafloor being shallower at the center and logically  do the drilling easier.  These new developments might allow scientists to break  with the  diffuse in coming years.  I am  non sure what the expect result of the penetration of the mantle is  unless it is unsettling to me.  A new  articulate was added to my vocabulary Moho which is a  leap formally kn feature as the Mohorovicic discontinuity. This marks the division  betwixt Earths  brittle outer crust and the hotter, softer mantle. My own research on    The Mohorovicic discontinuity  embed  the Mohorovicic discontinuity was first identified in 1909 by Andrija Mohorovicic when he  sight the abrupt increase in the velocity of earthquake waves at this point. The location of the Mohorovicic discontinuity varies between  active 5 km  infra the mid-oceanic ridges to approximately 75 km beneath continents.  The Integrated  oceanic Drilling Program or IODP seeks this Boundary.

  This hole took about  8 weeks to drill and brought back new information about the planets composition. Drillers  apply the watercraft JOIDES Resolution. The 10-year, $1.5 billion  plan is funded by the NSF and Japans Minist   ry of Education, Culture, Sports, Science, a!   nd Technology. , I researched the vessel JOIDES resolution because The article did  non provide additional information. The JOIDES Resolution was  erstwhile known as the B.P. Sedco-Explorer. The vessel is specially equipped with multiple...                                        If you  pauperization to get a full essay, order it on our website: 
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