by Teresa » Mar 2, 2007 5:13 pm
There are other mantle rocks at the surface. These are within ophiolite sequences, and are olivine rich rocks like perioditite, dunite and eclogite, with lots of garnet, spinel and pyroxenes. Because of the low pressures on the surface, they often decompose fairly fast. Under the ocean, pressures remain high (though not as high) as in the mantle.
What is cool about this 'scab' is that around 1960, there was a proposal to drill through the Mohorovicic discontinuity-- the layer between the crust and mantle.
Now it looks like all you have to do is send a drilling rig right to the site, slide through the water and voila, you are there!
I will be waiting for their results.