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More updates from our field teams...

Sugar - Sun, 08/09/2015 - 12:35

Seventeen teams are rounding up 1953 small seismic stations along our 350-mile-long line across eastern Georgia, and they continue to send texts and pictures with updates on their work…

“21757. Still kickin”
Kevin hunts for missing texans with the metal detector....
“Team 11 is all done and headed home to the mother ship”

“We’re not coming back unless we have all of them!”

“We had a helper at site 20431!”

“Hello Donna Rach and I are crushing it right now”

“Daily check in, we’re making good time so we should see the puppies soon enough”


Making metadata...
“Recovered a Texan at stop 20858. This one doesn’t seem to be working correctly, whenever I press it it just tells me things like “The Cowboys are America’s team” and “Bush was an American hero”. Weird.



“We got to 20170 the one with the ant colony”

Loaded up with Texans and geophones
“Stop 20804. Everything’s fine, except some guy came out of the woods and bit Brent. All he’s saying now is “brains” and is acting super creepy. I’ll keep an eye on it and only use the shovel if necessary”




“Will do! I will let you know if we become stuck… Looks likely”

Unearthing another Texan

“Just beat the downpour and headed for base”

“Stop 20879. Found the Texan disconnected from the geophone on top of where we buried it with pieces of bag around it, looked everywhere for the geophone. Found it about 5 m down the hill near the tree line with bite marks all along it. Either an animal dug it up or a very hungry confused thief”



Picking up litter?
“Found 2 dollars at 21058! Who says geology doesn’t pay well?”

Was not seen on the line...
Was seen on the line... yikes.

Best texts from the field (so far...)

Sugar - Thu, 08/06/2015 - 07:43
Seventeen teams have been out deploying small seismographs and geophones along a 300-mile-long profile across eastern Georgia, and they have been checking in with me regularly by text message. Some highlights from texts and pictures from our groups:



“Team4 is Done! I repeat again, 4 is done! Heading back to the sweet onion city! ☺”

“Still alive”



“Team gruesome twosome on our way back to the hub”

“We are gonna skip installing 21520 because both sides of the streets are well maintained yards and there’s not a great place to put a Texan”

“We’re done! Just kidding haha. We’re on our second!”

“We’re in the zone”

“All geophones buried --- I am beat. Where’s a can of spinach when ya need one, lol”

“It's a long way to the top if you want to study rocks”
"Sunrise at station 21779"
“We’re dirty but doing well!”


“Still digging. Still have not reached China. Will attempt again on next hole”


“On 20186 and we lost our bubble level. We even dug up the last geophone to see if I accidentally buried it”

“We just deployed our last station, 20224. Can we go to Jekyll Island?”



Donna Shillington, LDEO

Digging Holes and Filling Batteries -- A party in Vidalia, Georgia

Sugar - Tue, 08/04/2015 - 07:52

The SUGAR deployment team arrived en-masse on Saturday bringing the Line 2 personnel total to a whopping 45! The day started off with science and overview lectures by the SUGAR principle investigators Donna Shillington and Dan Lizarralde.  Students diligently rearranged the ten’s of Texan boxes into a makeshift lecture hall, complete with a projector and a Bluetooth sound system. 

With the science lecture complete and stomachs full of pizza, the entire group ventured out to conduct a practice deployment under the watchful eyes of the PASSCAL instrument team.  All 17 teams participated in the activity, standing in a single file line in front of our hotel digging practice holes, connecting the Texans to the geophones, and mindfully orientating them with their handy-dandy bubble levels. 

After a sweat filled hour under the Georgia sun, we caravanned back to the instrument center for a “battery party”. I call it a battery party in honor of the “streamer parties” that students will often participate in on active source seismic research cruises in which kilometers of cable need to be reeled off and rearranged.  In our case a battery party consisted of the 32 students placing 2 D-cell batteries inside each of the 2,000 Texans.  The instrument center quickly transformed from an orderly lecture hall into a mass of empty battery boxes and disassembled Texans though despite the apparent chaos, we got the job complete and the Texans filled in only a few short hours. 

Next up will be flagging the instrument locations and the actual deployment.  We have our fingers and toes crossed for dry weather and safe road conditions as the student teams prepare to set off on their flagging and deployment expeditions. 

Natalie Accardo - Columbia University, LDEO


The SUGAR2 deployment team hails from all across the United States
covering more than 15 states and 21 different universities/institutions.   

The deployment team sits with rapt attention listening to
the science and overview lecture.

Students practice digging holes and deploying Texans
near our hotel in Vidalia, Georgia.
Students and PASSCAL personnel take over the instrument center
filling 2,000 Texans with D-cell batteries.
The "battery party" comes to an end as the last Texans are filled and
the boxes are rearranged for easy late-night programming by the PASSCAL team.  



2000 “Texans” with all the fixin’s….

Sugar - Sun, 08/02/2015 - 09:21
During our project, we plan to record sound waves generated by a series of controlled blasts on two profiles, one with 2000 instruments (“Texans”) deployed along a 350-mile-long profile across Georgia and another with 700 Texans deployed along an 80-mile-long profile.  In total, that’s 2000 instruments and 2700 deployments!! Lot of instruments means lots of stuff.   The basic components of the instruments themselves were shipped in ~160 big plastic boxes arranged into ~18 pallets.  Each of these instruments will be powered by two D-cell batteries. To power the instruments for both lines, we needed 5500 D-cell batteries.  We picked them up from the Lowes in Vidalia as a 2000-lb pallet.  For each station, we also need flags to mark the locations, and bags and tape to protect the data recorder.  We very quickly filled up our 1800-square-foot field center in Lyons, GA with all these goodies…

Donna Shillington,  LDEO

Freshly delivered pallets of boxes holding all the science equipment
The PASSCAL team re-arranged the boxes into a T for their own devious reasons :)The trusty Silverado loaded down with 2000 pounds of batteries! (Dan for scale).



Drill, Baby Drill! Drilling and filling for the SUGAR seismic shots

Sugar - Fri, 07/31/2015 - 12:14
We are using sound waves to image the subsurface of Georgia along two long transects.  It is like creating a huge x-ray of the geology in the region. Thousands of instruments (termed “Texans”) will record sound waves that are generated from a series of controlled seismic sources (“shots”) that we will set off along the line. 

For the last few weeks, the seismic source team, based at the University of Texas – El Paso, and the drillers have been hard at work drilling twenty-six 60- to 100-foot-deep holes that will contain the explosives used to create the sound waves.  Once the holes are drilled (the first stage of which is termed spudding), emulsion explosives with boosters and caps are carefully installed in the base of the hole and the remaining height is filled in with dirt and gravel (“stemming”). 

Now with the 26 shots drilled and patiently waiting for the electronic signal to blow, all we have left to do is deploy the 2,000 instruments that will record the sound waves … An easy feat for the 50+ scientists, students, and engineers descending on Vidalia, GA over the next few days.  Stay tuned for our progress and adventures as we continue on this epic scientific undertaking.

Natalie Accardo - LDEO

The SUGAR seismic source and science team from left to right:
Steve Harder, Dan Lizarralde, Ashley Nauer, and Galen Kaip
The drill rig set up and drilling a shot on SUGAR Line 2.

Galen Kaip prepares the source charges (white tubes) on the truck bed as
the drillers complete a shot hole.
The source team carefully lowers the prepared seismic charges into the complete shot hole.
Ashley Nauer (red hat) stands waiting with shovel in hand to fill the remaining height of
the hole with sand and gravel.   
The drill team monitors the process of spudding, the very first stage of drilling the
shot hole, for SUGAR line 2.
The source team and drill team push on late into the night to ensure the completion of the
final shot for the entire SUGAR experiment.  

Ocean Currents Could Shed Light on Flight 370 Mystery - Business Insider

Featured News - Fri, 07/31/2015 - 12:00
Ocean currents could have carried debris from a missing Malaysia Airlines flight around the Indian Ocean to Reunion Island, says Lamont's Arnold Gordon.

Ramping up for bigger, badder SUGAR Part 2

Sugar - Tue, 07/28/2015 - 23:11
We are in Georgia gearing up for the second phase of field work for the SUGAR project, which will involve collecting seismic refraction data along two profiles spanning eastern Georgia. In the coming weeks, we’ll deploy thousands of small seismometers along county and state roads across the region, which will record sound waves generated by a series of controlled blasts. We can use the sound waves to make pictures of geology beneath the surface. Geological structures beneath Georgia record the most profound events involved in the formation and evolution of the eastern North America continent. In particular, we want to image an ancient suture between Africa and North America that formed when these continents collided to create the supercontinent Pangea, frozen magma bodies from one of the biggest volcanic outpourings in Earth’s history, and continental stretching and thinning that lead to the breakup of Pangea and formation of the Atlantic Ocean.


Map of SUGAR lines, showing two possible locations of the ancient suture (red dotted lines)

We collected similar data in western Georgia last year during the first phase of the SUGAR experiment imaging these same features. During that field program, we deployed 1200 seismometers and set off 11 controlled blasts along a 250-mile-long line, which felt like a big project at the time. But this year, we will go even bigger! In eastern Georgia, we need to span an even larger area to encompass our geological targets. One of the reasons that we need to look at a bigger swath of the earth is that there is a debate about the location of the suture here – it could be as far north as Milledgeville, GA or as far south as Baxley, GA. (In case you are not up on your Georgia geography, those towns are ~100 miles apart). This means longer profiles, more instruments and more blasts! We will deploy a total of 2700 seismometers and detonate 26 blasts along two profiles. The longer profile spans 350 miles from Winder, GA to the Florida-Georgia state line near St Mary’s Georgia. Stay tuned!

Donna Shillington, LDEO 



Interview: Climate Change in Central Asia - The Diplomat

Featured News - Thu, 07/23/2015 - 12:00
Lamont-Doherty's Benjamin Orlove discusses the repercussions of climate change in Central Asia.

Stay Tuned for SUGAR 2!!

Sugar - Wed, 07/22/2015 - 21:57
In just a few short weeks a mass of students and scientists will descend on southern Georgia with work boots and sunscreen in hand to take part in the second portion of the SUGAR active source experiment.  Make sure to stay tuned for regular updates on our progress and to learn more about the exciting science that motivates this amazing field expedition!

What's Inside the Earth? - PBS News Hour

Featured News - Thu, 06/25/2015 - 12:00
Lamont-Doherty's Christine McCarthy discusses some of the ways scientists study what is inside the Earth.

The True Face of Mercury - BBC

Featured News - Thu, 06/11/2015 - 12:00
Almost 20 years ago, NASA researchers began developing the Messenger probe, which would photograph the entire surface of Mercury. Lamont-Doherty Director Sean Solomon discusses the mission he led.

How Does Oil Form? - NBC News

Featured News - Wed, 06/10/2015 - 12:00
Lamont-Doherty's Peter Kelemen breaks down the process of oil formation for NBC News.

California's Vanishing Clouds Could Intensify Drought - KQED

Featured News - Mon, 06/08/2015 - 12:00
Fog and clouds play a vital role in keeping coastal temperatures down. But that benefit could be disappearing. Lamont-Doherty's Park Williams explains.

New Estimates of the Deep Carbon Cycle - Deep Carbon Observatory

Featured News - Fri, 06/05/2015 - 12:00
In a new study, Lamont-Doherty's Peter Kelemen assesses how much carbon is taken up by the Earth’s crust during hydrothermal processes at or near mid-ocean ridges, and how much carbon is released into the atmosphere through volcanic degassing and diffuse venting.

Smooth Sailing Back to Tasmania

Melting Glaciers-Tracking Their Path - Fri, 05/01/2015 - 10:12
Antarctica, NBP1503 science team

The NBP1503 science team.

After a surprisingly smooth crossing of the Southern Ocean, with favorable winds we arrived back in Hobart, Tasmania. The weather maps show that we just got ahead of another big storm system.

Once the equipment is stored away and the samples are loaded off, we will all head back to our offices and labs to further process and analyze our data and eventually put all the results together.

Taking a 4,000-Meter-Deep Profile of Antarctic Waters

Melting Glaciers-Tracking Their Path - Mon, 04/27/2015 - 10:47
NB Palmer, West Antarctica, CTD system

The CTD system is lowered over the side from the NB Palmer. It measures temperature, salinity, and oxygen with depth.

In addition to understanding potential pathways for “warmer” circumpolar deep water to reach the ice shelf, we are also measuring what the structure and properties of the water column are and determining if there is already warmer water on or near the continental shelf that could already interact with the glaciers of East Antarctica today.

To measure water properties, we are using an instrument that can be lowered through the water column that measures conductivity, from which we calculate the salinity of the water, temperature, pressure (i.e. water depth), oxygen, and fluorescence, which is an indicator for phytoplankton or algae in the water. This system is called a CTD for short.

This system can also take water samples from different depths that can be used for further analysis or for calibration and verification of the sensors. When we lower this system in deep water, e.g. 4000 meters, (about 2.5 miles), the measurements take over three hours.

We have measured the water properties at 42 different locations during our expedition and will analyze the results carefully when we are back.

Follow @FrankatSea for additional updates and images from the Southern Ocean.

Mapping the Seafloor

Melting Glaciers-Tracking Their Path - Mon, 04/20/2015 - 11:53
In addition to depth, we can identify many features in the high-resolution multibeam data that we produce. Most of the seafloor near the shelf break (where the water is between 300 and 500 meters deep) is covered with these irregular furrows that are created when large icebergs are grounded here.

In addition to depth, we can identify many features in the high-resolution multibeam data that we produce. Most of the seafloor near the shelf break (where the water is between 300 and 500 meters deep) is covered with these irregular furrows that are created when large icebergs are grounded here.

One of the goals of this expedition is to investigate if water from the Southern Ocean with temperatures above the melting point of glaciers could reach the glaciers in East Antarctica, and if there are any obstacles on the seafloor of the shelf that impact the ability of such water to reach the glaciers and ice streams.

The continental shelf in our study areas along the East Antarctic margin has been mapped in the past, but the existing data are very sparse and have many gaps. However, it is important to know the actual water depth of the continental shelf if we want to understand if water from the Southern Ocean with temperatures above the melting point could reach any glaciers and ice streams in this part of Antarctica.

We use a multibeam echosounder system installed on the Nathaniel Palmer to map the depth of a wide swath of the seafloor along our ship track. Access to the continental shelf is often limited by dense ice cover, but using the multibeam, we have managed to determine detailed depths in several areas. We will later analyze the depth data together with measurements of water column properties that will tell us exactly how deep the “warmer” Southern Ocean water is.

Follow @FrankatSea for additional updates and images from the Southern Ocean.

In the Ice

Melting Glaciers-Tracking Their Path - Fri, 04/10/2015 - 09:12
 The Nathaniel B. Palmer steaming through dense sea ice cover.

Some examples of the sea ice that we have encountered so far. Top left: bands of grease ice. Top right: small pancake ice merged together. Bottom left: larger pancake ice; bottom right: our ship, the Nathaniel B. Palmer, steaming through dense sea ice cover.

Several days ago we reached our main work areas along the margin of East Antarctica. Our expedition is relatively late in the season and the seas around Antarctica are starting to freeze. While the abundance of sea ice makes it more difficult to get to all of our research areas, the different shapes and forms of newly forming sea ice are a great visual experience. We also have a group of Australian scientists aboard the Palmer who are studying sea ice and sea ice formation using an unmanned aerial system or drone, so they are especially pleased by our icy experience.

Follow @FrankatSea for additional updates and images from the Southern Ocean.

Closing in on Antarctica

Melting Glaciers-Tracking Their Path - Mon, 04/06/2015 - 11:29
During our transit south to Antarctica we deployed seven ARGO floats (yellow device in picture) for the University of Washington. They drift with the currents in the oceans, measure profiles of salinity and temperature and send those via satellite to researchers on land. They are part of an international effort to better monitor the conditions of the oceans.

During our transit south to Antarctica we deployed seven ARGO floats (yellow device in picture) for the University of Washington. They drift with the currents in the oceans, measure profiles of salinity and temperature and send those via satellite to researchers on land. They are part of an international effort to better monitor the conditions of the oceans.

We are less than a day away from our first study area on the continental shelf in front of the Dibble Glacier. As we approach Antarctica we are starting our science program with a 4500 meter deep CTD and multibeam acquisition. The CTD is used to determine the conductivity, temperature and depth of the ocean, while the multibeam maps large swaths of the seafloor from the ship.

The main goal of our project is to investigate the continental shelf in front of different glaciers along East Antarctica. We want to find out what the water depths and the water properties are in front of these glaciers and ice streams. Deep troughs and connections between the glaciers and the open ocean could allow “warmer” ocean waters to reach the ice front and result potentially in melting of the ice. We are especially interested to compare the situation in front of different glaciers along East Antarctica to better understand the differences between them. Many of these areas are poorly charted, if at all. So we are all excited to discover what is there!

Follow @FrankatSea for additional updates and images from the Southern Ocean.

Sunrise...Sunset...Sunrise...Sunset...

The ENAM Seismic Experiment - Sun, 04/05/2015 - 03:46
A compilation of sunrise and sunset photos aboard the R/V Endeavor. 

Day 3 sunset

Day 4 sunset

There is a bizarre foggy mist across the entire surface of the ocean.

This was a huge cargo vessel off in the distance. I know it isn't a sunrise or sunset but its a sweet pic.

Day 6 sunrise with a storm front in the distance.

Panorama of Day 6 sunrise.

Porthole sunset with my refection.

First bit of sunset color directly off the bow of the Endeavor.

about 20mins later....





Terry Cheiffetz




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