Expedition 354: Bengal Fan

Dates: 29 January - 31 March 2015

Ports: Singapore to Colombo, Sri Lanka

Co-chief Scientists: Christian France-Lanord & Volkhard Spiess

Staff Scientist: Adam Klaus

Onboard Education Officers: Diane Hanano & Lisa Strong

Science Party & Crew: Click here for profiles<

Live Video Broadcasts: Sign-up now!<



Expedition Summary

On this expedition we’ll be exploring the connection between mountain formation and climate. The mountains we’re studying are the highest on earth – the Himalaya. But we’ll be studying them at the bottom of the ocean, in the Bay of Bengal, by looking at eroded sediment. These large and small bits of the mountains get washed into rivers and carried to the sea. The outflow of sediment into the Bay of Bengal is called the Bengal Fan. It’s called a fan because the sediment fans out, and it looks a little like a ladies’ fan. We’ll drill sediment cores on a transect – six different sites in a line, across the middle of the Bengal Fan.

Check out our 2-minute Expedition Trailer< – a video that will introduce you to our lead scientists and tell you more about our mission.

The video (with music!), Aboard the JOIDES Resolution<, ponders the question: why come this far to sea? 

Our most recent 6-minute video Source to Sink< features interviews with three of our scientists and explains why studying the Himalayas at the bottom of the Bay of Bengal is so important.


What is the Bengal Fan?

The Bengal Fan is the largest submarine fan in the world. It is ~3000 km long, ~1000 km wide and up to 16.5 km thick. It covers the floor of the entire Bay of Bengal, bordered to the west by India, to the north by Bangladesh and to east by the Andaman Islands.

The fan began forming tens of millions of years ago when the Indian Plate collided with the Eurasian Plate, causing the uplift of the Himalaya and Tibetan Plateau, and with that, the subsequent erosion


How are mountains and climate related?


The extreme height of the Himalaya make them very effective storm catchers. When moist tropical winds run into the mountains, the air is pushed up the wall of mountains. The air expands and cools, forming clouds and rain. This process is the primary cause of the Asian monsoon rains, which can drop 1-5 meters of water per year. All that water scours the mountains and erodes them. That sediment washes into mighty rivers, two of which, the Ganges and the Brahmaputra, drain into the Bay of Bengal. They transport a billion tons of formerly Himalaya material a year. When the Himalaya loses a billion tons of weight, the remaining mountain rises up slightly in a process called isostatic rebound. The mountains get reduced by erosion, but rebound and get slowly taller, creating that effective storm barrier, causing more erosion, and the cycle continues.

Because sedimentation in the Bengal Fan responds to both climate, in the changing intensity of the Asian monsoon, and tectonic processes, like isostatic rebound, its sediment records the past evolution of both the Himalaya and regional climate.


Want all that in simple terms?

Here is an explanation of our expedition using only the most common 1000 words (note: mountain, ocean, and drill are not included!):

We are trying to understand how the tallest land in the world breaks down into small pieces and moves down to lower places. The tall land is very good at catching rain going by. The rain is good at carrying small pieces of the tall land to lower places. The rain can make the tall land shorter. We will study the small pieces in the lower places to learn more about the rain.

We will spend two months out on the water with people from all over the world. Using a long stick, we will break the ground and pull up small pieces of rock from the bottom of the water.  By studying what these small pieces are made of, we can learn about what the air and water were like many many years ago (like ten hundred hundred hundred years). The pieces also have tiny animals (and other things that used to be living) inside that can tell us how old the pieces were when they were put there.

It's not easy - try it yourself here<!


How to get Involved

Talk to us!

Sign-up for a live video broadcast with the ship.  We will take you on a tour of some of the key places onboard, and then give you a chance to talk to one of the scientists, technicians or education officers.

Sign-up now!<

Follow us!

Facebook icon 01   Facebook: JOIDES Resolution<

twitter-logo-icon   Twitter: @TheJR<

instagram-icon   Instagram: @joides_resolution<