Blog Posts Tagged "expedition 330"
I Flew Into a Burning Ring of Fire
If, like me, you had just spent thirty hours traveling from the east coast of the United States to Auckland, New Zealand, then while you were riding in the shuttle from the airport to your hotel, you also may have noticed that Auckland looks like it could be a city found on the east coast of the United States (well, except for the fact that the trees
What is a Seamount?
Core Describers
Hello. I’m sailing on the Louisville Expedition 330 and I’ll be blogging about what I do, the science onboard the ship and life at sea in general. This first blog will be an introduction to what I do.
Find Out Which of the World’s Volcanoes are Erupting Today, Today!
One of our main research objectives for drilling the Louisville seamount trail is to try to better understand what is happening in the mantle underneath it. Volcanoes and earthquakes are our most dramatic reminders that the inside of the Earth is not a static ball of rock: there is a fluid mantle that is causing the seemingly solid crust beneath us to move and change.
What do Hawaii, Yellowstone National Park and the Louisville Seamount Trail all have in common?
What's so cool about Louisville?
Deck the Labs With Cores of Basalt
Santa Claus, reindeer and gas station attendants are not the only people working on Christmas Day this year. Everyone onboard the JOIDES Resolution is working today as well. The captain and crew are making sure the ship is running smoothly. The engineers and roughnecks are continuing to drill into the seamount to bring up more cores of volcanic rocks.
Why Paleomagnetists Rule!
Meet Nicola Pressling, one of the scientists on board, and find out why paleomagnetists have the coolest job you probably never heard of before.
Make a Seamount Trail in the Classroom
Why Starting a Relationship with a Hotspot is Going to be Complicated
Hotspots are like the strong, silent type. On the surface it is obvious they are very powerful, but it is difficult to find out what is going on with them underneath the surface, because there is no way to force your way down there.






