New instruments hook to the underwater lab.
Credit: David Fierstein © 2005 MBARI

We heard about the Monterey Bay Aquarium Research Institute's new underwater laboratory in a radio story last fall. When that story aired, the lab (known as the Monterey Accelerated Research System, or MARS) was just getting going, with lots of neat experiments planned. Now, few of those have become a reality.

In case you missed the first story, the MARS is essentially an underwater data hub, perched on the ocean floor almost 3,000 feet below the surface of Monterey Bay. A 32-mile cable connects the system to land, acting as a power cord and data link. Several "underwater extension cords" allow a variety of instruments to plug into the hub, getting power from land and sending back data via the cable. That constant connection is a big step forward in undersea science; without it, researchers have had to use boats to stay physically close to their instruments (something hard to do for very long), or have sent the instruments off on their own, relying on batteries to keep them running and collecting data.

Until late February, earthquake scientists at the UC Berkeley Seismological Laboratory had been using that second method with their seafloor seismic station, the Monterey Ocean Bottom Broadband (MOBB). "We had to wait three months to even know if the instruments were alive," said Barbara Romanowicz, the lab's director. But the MOBB is now plugged in to the MARS system, and is transmitting its information about earthquakes in real-time.

That new stream of information could be especially valuable in California, because the MOBB provides a unique view of the main fault system, the San Andreas, which runs along the Northern California coast. Most seismometers are land-based, and therefore positioned on the east side of the fault. The MOBB is on the west side of the fault, offering a helpful perspective on the fault's shifts and shakes.

The researchers hope that the MOBB's new stream of real-time data will improve their earthquake models, and perhaps eventually help provide early warnings about impending quakes (for more on that topic, see the TV story, Earthquakes: Breaking New Ground).

The MOBB is just one instrument using the MARS hub. A tool that uses sound waves to track fish is currently attached, and within the next six months you can expect to see a robotic DNA lab and a robot that crawls along the seafloor, collecting data on animals that live in the mud.

I met Mary Lou Zoback out at the Fremont Bart station, which sits right on top of the Hayward Fault. She pointed out cracks in the parking lot from the creeping fault. Zoback is a geophysicist who worked 28 years at the U.S. Geological Survey and who has done catastrophe modeling of risky residential buildings. Her company estimates that a 6.8 quake, or bigger, on the Hayward Fault could cause a disaster on par with Hurricane Katrina, causing 168 billion dollars in damage and leaving at least 200,000 homeless.

A number of public buildings in the east bay are undergoing retrofitting to make them more structurally sound. Area hospitals have until 2013 to meet seismic safety standards. There is a state inventory of public schools prone to collapse in a major quake, but no such list exists for private schools. And retrofitting standards for risky residences are confusing. I talked with Jim Cook, of Bay Area Retrofit. He says existing codes are unclear and there really is no specific licensing for seismic home retrofitters. Cook has been fighting local governments for years to improve seismic safety standards.

Homeowners can have their home evaluated but what if you are a renter? Many apartments and condos can collapse in earthquakes because they have parking or open commercial space on the first floor making this story weak or "soft." According to the Association of Bay Area Governments Earthquake and Hazards Program, soft-story apartment buildings were responsible for about two-thirds of the 46,000 uninhabitable housing units in the 1991 Northridge earthquake. In the Bay Area, unreinforced masonry (older buildings constructed of brick, stone or cement blocks) continues to be a threat.

The thought of a big earthquake is scary enough, never mind the chaos that can happen in the aftermath. But the damage from a large earthquake has repercussions that can last for a very long time. We can still see the scars from the 1989 Loma Prieta earthquake. Downtown Santa Cruz is not yet fully rebuilt and retrofitting continues on the Bay Bridge. We can prevent a lot of damage up front by shoring up our buildings and creating a family disaster plan and an earthquake kit. The Hayward Earthquake Alliance has put together some really helpful information on how to prepare for a major quake.

Listen to the Hayward Fault Radio Report and view the recent QUEST TV segment on the fault online.

Can elephants feel seismic waves?

Scientists have known for years that elephants can communicate. By using low frequency vocals, called rumbles, elephants can 'talk' with eachother, sometimes communicating from very long distances.

But the new question being asked by some scientists is: can elephants feel those rumbles in the earth?

Biologist Dr. Caitlin O'Connell-Rodwell from the Oakland Zoo wants to find out. After studying elephant activity in Africa, she noticed that elephants would raise and lower their feet when interacting with one another. She realized that these elephants were using seismic waves felt through their feet to send messages.

O'Connell-Rodwell and her team have been creating mini-earthquakes for an elephant (named Donna) at the Oakland Zoo to monitor her responses to different seismic activities.

Check out this National Geographic video about the study on YouTube: