News aggregator

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.  

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 

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!

Tiny Architects

Geopoetry - Fri, 07/10/2015 - 11:00
 Kelly Strzepek.

Foraminifera are tiny plankton that typically build elaborate shells of calcium carbonate. Their kind have lived in the ocean for millions of years. Photo: Kelly Strzepek.


Heaved upwards from your deep and watery grave,

From the quiet murk onto a chaotic, brine-encrusted ship deck,

You’re ever so carefully washed free from the mud,

From all the rinsings of continents that settled out of the sea with you

Like snow, softly entombing your remains.

Now through my looking glass, you lie scattered

Like discarded Christmas ornaments,

Lying in broken glory, shards of a former world;

Tiny fossils, utterly bewitching.

Some people say there must be a knowing architect behind all this design;

Looking at your tiny turrets, buttresses, embellishments,

I understand the sentiment.

How is it, and why is it, that you craft such castles

Smaller than a grain of sand?

I know it is your work, not that of some artful watchmaker;

I’ve watched your live descendants raise their miniscule arches,

Lay down their mortar and stone, precisely and perfectly.

Still, it’s hard to believe my eyes. I am desperate to ask you,

Clever protist with no brain, to tell me all your secrets.

I wonder if some life-form, eons hence,

Will ever find my ancient bones,

Marvel at their beauty,

And imagine the life of the mysterious being that grew them.



This is one in a series of posts by Katherine Allen, a researcher in geochemistry and paleoclimate at the Lamont-Doherty Earth Observatory and the Department of Marine and Coastal Sciences at Rutgers University.

Finding Pluto

Geopoetry - Fri, 06/26/2015 - 11:00

This summer, a space probe that has been traveling for 9 years will finally reach Pluto. Image: JHUAPL/SwRI


Far away, a beloved dot

Arcs through cold and shrouded spaces,

Not lonely, as we had once thought,

But circled by more rocky faces:

Charon, Nix, and Hydra found,

Classified as “dwarf” or pseudo,

And though such bodies now abound,

None sparks wonder quite like Pluto.

On the hunt for Planet X,

Tombaugh found a ball of light,

Among a crowd of tiny specks;

Imaginations soon took flight.

Elusive is this outerworld;

Nine years ago we took a dare –

To deepest space, a scouter hurled

… and soon it will be there!



Further reading:

Pluto-bound probe faces its toughest challenge: finding Pluto, Witze (2015) Nature

NASA Mission: New Horizons to Pluto

This is one in a series of posts by Katherine Allen, a researcher in geochemistry and paleoclimate at the Lamont-Doherty Earth Observatory and the Department of Marine and Coastal Sciences at Rutgers University.


‘Faux pause’

Geopoetry - Fri, 06/12/2015 - 10:30
 Maintenance workers on an ocean buoy, NOAA.

The global ocean buoy network has been expanding in recent years. Accounting for small, consistent offsets between temperatures measured by buoys and by ships reveals a greater global warming trend than previously calculated for the past 15 years. Image: Maintenance workers on an ocean buoy, NOAA.


New data support the conclusion

The “hiatus” was mostly illusion.

They say that the keys

Are the poles and the seas …

The next job: reduce the confusion.



Further reading:

Global warming “hiatus” never happened, study says, Wendel (2015) EOS

Possible artifacts of data biases in the recent global surface warming hiatus, Karl et al. (2015) Science

This is one in a series of posts by Katherine Allen, a researcher in geochemistry and paleoclimate at the Lamont-Doherty Earth Observatory and the Department of Marine and Coastal Sciences at Rutgers University.


Geopoetry - Fri, 05/01/2015 - 12:19


MESSENGER's last image of Mercury. (NASA)

MESSENGER’s last image of Mercury. (NASA)


Alien orbits you plied,

While we vicariously spied

A distant globe …

Oh, tough little probe!

It’s been a wonderful ride.




Further reading:

MESSENGER’s last image

This is one in a series of posts by Katherine Allen, a researcher in geochemistry and paleoclimate at the Lamont-Doherty Earth Observatory and the Department of Marine and Coastal Sciences at Rutgers University.

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.

An Earth Epic

Geopoetry - Fri, 04/10/2015 - 10:30
 Ricardo Ramalho

Photo: Ricardo Ramalho

I hear that the Archean Earth

Spewed lava and was hot,

(While much later, “Snowball Earth,”

Apparently was not),

Some have said that life sprung out of

Spreading-ridge-type stew,

Photosynthesis seems likely

Based on carbon records, too.

Crust was forming, oceans warming,

Stromatolites came later,

(We have to wait a long, long time

for T-Rexes, Fish, and Gators)

The Prot’rozoic was really wild,

Stromatolites went crazy,

Our atmosphere gained oxygen,

The rest is a bit hazy.

Super-duper continents

and Banded-Iron formed;

Glacial stuff beneath cap carbs

Say Earth cooled and warmed.

Half a billion years ago

Is when it gets exciting …

Suddenly, life took a leap!

All living, breeding, fighting.

Brachs and Crinoids, Bryozoans,

Weirdo shells galore,

Nautiloids (like giant dunce caps)

Roamed the ocean floor.

Then disaster strikes them down,

(This happens four more times)

And we soon approach some names

That are difficult to rhyme.

Gondwana drifts to the South Pole,

and glaciers spread like malls,

The world was likely colder,

and sea level took a fall.

So ends the years of trilobites

(and the Ordovician)

But soon we get new forms of life,

And we can all go fishin’!

Finally the land joins in,

And starts to grow green stuff,

(are you still enjoying this,

or have you had enough?)

More death, more life, more death again,

While giant mountains grow,

(we think this lowered CO2,

but no one really knows).

The Carboniferous was lush,

(that’s where our coal is from!)

Amazing bugs and dinosaurs,

(though some say they were dumb).

Gymnosperms and vertebrates,

Then the grimmest death so far,

Then Triassic life recovered,

with reptiles big as cars.

We leave aragonitic seas behind

And move towards today,

Though continents were not in place,

(that great Tethys seaway).

About 100 million years ago

Deep sea carbonates abound,

So now the ocean’s buffered well,

(and planktics can be found!)

And THEN Earth has a real bad day,

An asteroid hits hard,

Fire-balls and darkened skies,

Life is burned and charred.

(Holy cow, this is quite long,

let’s finish it already!) …

Cenozoic history

was anything but steady.

It started hot, they also say

that CO2 was high;

Wimpy mammals take the lead,

(I hear that bats could fly).

Himalayas cause a ruckus,

Gateways open/close,

We start to get some glaciers,

And cold, deep water flows.

From the Greenhouse to the Icehouse

Now we’re really getting chilly,

Then humans come along (that’s us)

and everything gets silly!

So there you have it, Earth through time,

History deep and long,

I surely skipped a lot of stuff,

And may have got some wrong.

I hope if you’re still reading

that your brain is not too vexed,

Now it’s time to face the future,

…. I wonder what is next!



Further reading:

See the geologic record.

This poem was first published on the author’s website on May 22, 2009.

This is one in a series of posts by Katherine Allen, a researcher in geochemistry and paleoclimate at the Lamont-Doherty Earth Observatory and the Department of Marine and Coastal Sciences at Rutgers University.

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.


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

Go Endeavor Go! Nighttime Adventures...

The ENAM Seismic Experiment - Sun, 04/05/2015 - 02:25
A unique low light vantage point of the Endeavor

A look at all the instrumentation on the bridge of the R/V Endeavor. 

The full moon as it shines over the ocean water! Creepy!

The OBS retrieval at night! One of the crew members installed a light at the end of the hook to aid in the equipment capturing process. 

This picture was take from the bridge of the Endeavor. It is the Quantum of the Seas cruise ship at ~0300 during an OBS retrieval. 
This picture is ~2 miles away from the Quantum of the Sea cruise ship and is as close as the Endeavor can legally pass another large ocean vessel under maritime law. The bright celestial object overhead is Jupiter.

This photo shows the Endeavor docked at port just before we embarked on this high seas adventure. The first evening we went to a chinese restaurant called 7 moons. By the time we arrived back at the shipyard the gate had been pulled shut and appeared to be locked and was topped with plenty of barbed wire. After some deep thought our highly intelligent group realized that it was pulled closed and all we had to do was roll it open haha. There is a geophysicists joke embedded in that experience. 

This is the WHOI crew carefully bringing the OBS back onto the ship. Hard hats and life preservers are required when on deck during retrieval operations. The OBS in this photo is hanging down beneath the orange apparatus.  

As the Endeavor aligns itself with the OBS in the ocean currents at night the WHOI crew get in position to capture the Ocean Bottom Seismometer. 

After a successful OBS capture the WHOI crew quickly disassembles the OBS and prepares it to be stacked with the other equipment that is strongly secured to the surface of the deck. 

This shows the spotlight at night. It is used to help orient the ship alongside the OBS in the pitch black darkness of the night at sea. We have also thankfully had the full moon over the last few days to assist us in finding the OBS once it pops up to the surface.

This lovely burry image is the spot light as it tracks the OBS. The spotlight is extremely useful once the OBS is within several ship lengths of distance. 

The OBS is starting to get closer now....

Full moon over a perfect OBS recovery.

Hammock in the middle of the night!

You can really get a good feel for spotting the OBS at night in this picture. It is obviously a ship length or two off the starboard bow. 

Terry Cheiffetz


Survival Suits to the Rescue!

The ENAM Seismic Experiment - Sat, 04/04/2015 - 16:20
Before the R/V Endeavor embarks on its research voyage the new crew/scientists get to enjoy the challenge of a mock sinking scenario where they have ~2mins to jump out of their shoes and wiggle into these fashionable lobster costumes.  

Dr. Maureen Long and one of the crew members race each other to safety!

Graduate Student intern Colton Lynner is almost unrecognizable once the survival suit is fully on. Only the last troublesome step up zipping up to go before full emersion can take place. 

Graduate Student intern Terry Cheiffetz struggles with the final zipper step as well. 

Dr. Maggie Benoit looks like she wants to really know how to put on the survival gear in case of emergency or... she can't believe she has to participate in these fun shenanigans.

The final product appears to be both fashionable and comfortable. We would interview the model in this photo but he declined to comment....hopefully next years model will have a mouth hole haha!



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