2 weeks 23 hours
Exp 362: Sumatra Seismogenic Zone
Expedition 362: Sumatra Seismogenic Zone
Dates: 6 August – 6 October 2016
Ports: Colombo, Sri Lanka to Singapore
Co-Chief Scientists: Lisa McNeill and Brandon Dugan
Staff Scientist: Katerina Petronotis
Onboard Education Officers: Naomi Barshi and Agnès Pointu
Science Party and Crew: Meet them here, and check out where we're from all over the world!
We want to know why earthquakes happen where and when they do. When earthquakes happen in the ocean, they can displace huge volumes of water and cause tsunamis, such as the 26 December 2004 Sumatra earthquake and the 11 March 2011 Tohoku-Oki (Fukushima) earthquake. The combination of ground shaking and flooding is destructive and deadly. Very large earthquakes like these are typically at subduction zones, places where tectonic plates converge and one plate gets pushed down beneath the other. Yet these earthquakes, as well as several others in the past 15 years, surprised earth scientists in terms of their size and the amount and location of the fault slip during the earthquake. Subduction zone earthquakes can happen many tens or even hundreds of kilometers below Earth’s surface. The shallower and larger the earthquake, the more damage it can cause by shaking. It is even more dangerous if it occurs under the ocean floor because it can trigger a tsunami.
We can’t predict earthquakes, but we can learn more about what happens below the Earth’s surface and why rocks break and cause earthquakes that trigger tsunamis.
Where are we going?
We’ll spend two months drilling into the ocean floor west of Indonesia (see map above) trying to figure out everything we can from the sand and silt and clay and fossils at the bottom of the ocean! In particular, scientists want to know if the sediments on the Indo-Australian plate have specific characteristics which can explain why the earthquake of 2004 took place under the accretionary prism (see red line in figure below) rather than deeper along the plate boundary. (An accretionary prism is the pile of sediments scraped off the down-going plate at the subduction margin.)
Several kilometers of sediments have settled to the ocean floor at the drill sites. These sediments get transported to the Sunda subduction zone by the tectonic plate on which they rest (the Indian Plate, in this case). The thickness of the sediments stacked on the seafloor increases toward the subduction zone, where the thickness reaches as much as 5 km. The Sunda subduction zone is a place where two tectonic plates meet: the fault between the two plates is where the big earthquakes happen. We want to sample the sediments before they develop into the faulted plate boundary region so that we can learn about their physics, chemistry, temperature, and pressure. These variables change as the sediments become more deeply buried and eventually turn into brittle rocks. Under stress, the rocks break along faults and cause earthquakes.
What will we do when we get there?
We plan to drill through 1.5 km (about 1 mile) of sediment to sample the sediments that get scraped off the seafloor before they get caught in the faults were these earthquakes happen. Scientists on board will describe what the sediments are made of, identify fossils to tell when and where the sediments formed, and work out how they might deform when pressures and temperatures get much higher. In addition to finding out the “recipe for disaster” that makes these sediments turn into earthquake-prone rocks, we can learn about Earth’s climate in the past and the history of the Himalaya mountains. Stay tuned for more details as the expedition gets underway! Follow the blogs and updates on Social Media!
What do we hope to do when we get home?
The JOIDES Resolution is a floating laboratory where scientists can do many different types of analyses. Two months may seem like a long time, but it’s a very short time for the scientific process! We will need to take samples back to shore to do more analyses and experiments to see how the sediments behave under different conditions. We can recreate the types of pressures, temperatures, stress, and chemical conditions that the sediments would experience in the Sunda subduction zone to learn more about when, why, and where the earthquakes happen.