|
|
|
|
|
|
|
|
|
|
Here you can find daily updates and news of our progress. Check back in for new information!
|
|
Day 48 - December 5, 2018
We arrived in Montevideo! Well, almost--at the time of writing this, we still need to pilot into port and go through customs. That should happen soon, though.
Read more
|
|
Day 47 - December 4, 2018
We have finished up packing! We should be arriving in port tomorrow around noon. It’s been a pleasure participating in this cruise with everyone, and I for one cannot wait to see what exciting discoveries will be rooted in the samples and data we collected.
Read more
|
|
Day 46 - December 3, 2018
We finally reached the EEZ this morning. The multibeam is off and we are not logging anymore. Our shifts are technically done, but it may take some people a bit to fully change their sleep schedule back.
Read more
|
|
Day 45 - December 2, 2018
The storm really started to pick up today. We had 50 knot winds for a short bit as the front hit us, but it “died” back down to around 40. We’re still heading for the EEZ.
Read more
|
|
Day 44 - December 1, 2018
We’ve started another ping pong tournament to pass our free time while we finish processing samples and start packing everything away. In a nice bit of parallelism to the beginning of our cruise, there’s another storm brewing as we head back to Montevideo.
Read more
|
|
Day 43 - November 30, 2018
Today was a busy day! We had our final day of student presentations. Kaya gave a talk about geothermobarometers, or methods to determine the original formation pressures and temperatures of metamorphic and igneous rocks.
Read more
|
|
Day 42 - November 29, 2018
A bit of somber news…we lost our dredge basket at Tseenkee Escarpment this morning. This is an accepted risk while dredging since these wires can reach very high tensions very quickly, but it’s always stressful when it happens.
Read more
|
|
Day 41 - November 28, 2018
The Suhail Escarpment dredge came up and gave us a nice mix of basalts, sediment, and corals. We spent the rest of the day transiting to the next dredge site BUT we were treated to the beginning of our student presentations!
Read more
|
|
Read All News Updates |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Read short reports presenting some of the science behind the cruise, as well as blog stories about life on the RVIB Nathaniel B. Palmer. Don’t worry about having to do extra reading—the reports are written with a general audience in mind, and will cover topics mentioned in the Scientific Objectives as well as other basic geology topics.
|
|
Science Report 7 - Multibeam and Sub-bottom profiling
On our exploration of the Rio Grande Rise, we aimed to dredge rock samples from seamounts and escarpments on the seafloor. In order to dredge the ocean floor effectively, we need to be able to map what’s down there in detail. The existing maps of the ocean floor are based on satellite bathymetry.
Read more
|
|
Science Report 6 - An Intro to Satellite Altimetry
An important aspect of our cruise has been collecting multibeam sonar data to map the ocean floor. Why is this important? Don’t we already have a map of the ocean? Hasn’t Google already done that?
Read more
|
|
Science Report 5 - Green flash – a rare and spectacular sight at sunset, Rio Grande Rise, South Atlantic
Some of you might have heard of the “green flash”—an upward flash of emerald-green light that appears for a few seconds just after the sun disappears beneath the horizon. It has a certain “wow effect” as this green light is a big surprise in a typical red-toned sunset.
Read more
|
|
Science Report 3 - Isotopes crash course!
When people think of isotopes and radiation, images of nuclear plants and catastrophes sometimes go through their minds. Those are just one part of the story, however. Isotopes are actually very important to us geochronologists and geochemists when it comes to getting information out of rocks we have collected—such as the ones we’ve gotten on this science cruise.
Read more
|
|
Science Report 2 - Rock Descriptions: Demystified
Identifying and describing the rocks collected by a dredge is one of the most important steps of a cruise. The scientists do their sample selection for geochronology and geochemistry based on these rock descriptions in order to address the research questions summarized on the main page of this website.
Read more
|
|
Science Report 1 - Reconstructing Earth: Magnetics and Magma
One of the scientific goals of the NBP1808 cruise to the Rio Grande Rise is to collect measurements that will improve the plate tectonic reconstruction of the opening of the South Atlantic. How is this done? We are able to measure magnetic anomalies originating in the oceanic crust, which lies 1000-4500 m below the ship.
Read more
|
|
Read All Science Reports |
|
|
|
|
|
|
|
| |
|
|
|
|
|
|
|
Rio Grande Rise 2018 Expedition
Browse through a gallery of pictures from the NBP1808 cruise, showing life aboard the RVIB (Research Vessel Ice Breaker) Nathaniel B. Palmer as we explore the Rio Grande Rise off the coast of Brazil in the South Atlantic.
|
Co-PIs on the Rio Grande Rise project: (From left to right) Cornelia Class, Anthony Koppers (Chief Scientist), William Sager.
|
The members of the NBP1808 science team.
|
|
View Image Gallery |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Planned Cruise Track
This map shows the planned path of the ship as we make our way around the Rio Grande Rise. This map includes our detour to avoid the storm.
|
|
See Larger Version |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
- Use 40Ar/39Ar geochronology to determine whether the Rio Grande Rise formed along micro-plates, as an age-progressive feature like most of Walvis Ridge, or from a short-lived large eruptive event
- Investigate whether the Rio Grande Rise displays three geochemically distinct zones similar to the triple-zoned younger part of Walvis Ridge using major-trace element and Sr-Nd-Hf-Pb isotope data
- Collect magnetic anomaly data to help strengthen the age model for the South American tectonic plate
- Explore the formation of the Rio Grande Rise as shaped by plume dynamics and/or shallow tectonics
- Determine whether the geochemical mantle sources are related to a zone of probably dense material at the base of the mantle called the African Large Low Seismic Velocity Province (LLSVP)
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
The NBP1808 editors:
(left to right) Malik, David, Ellyn, and Matt.
|
A team of 17 students and scientists led by Chief-Scientist Anthony Koppers will be at sea for seven weeks, mapping and dredging troughs, cliffs, and seamounts in the Rio Grande Rise region off the southeast coast of South America. The team consists of 11 graduate students in geophysics, geochronology, and geochemistry; 4 undergraduates; 1 post-doc; and 3 professors from Oregon State University, Lamont-Doherty Earth Observatory of Columbia University, and University of Houston. Over the next few weeks we will keep you updated as we map and dredge the Rio Grande Rise and expand the knowledge of the general area.
|
|
|
|
|
|
|
|