Printer Friendly

Drilling exposes ocean's underside.

It ranks as one of the most expensive fishing trips of all time, but this recent international expedition didn't hook any deep-sea delicacies. Instead, crew members hauled up broken pieces of drilling equipment, and in doing so, they rescued a 12-year effort to bore deep beneath the seafloor, opening a window into Earth's internal workings.

The machinery had been clogging the deepest hole ever cut in the ocean floor and had threatened to end all drilling at this hole, known as 504B and located near the Galapagos Islands. But hours before they had planned to abandon 504B for another site, members of the Ocean Drilling Program (ODP) freed the offending pieces. They tehn went on to deepn the prized hole, eventually reaching a depth of 2 kilometers below the ocean floor.

"This is a landmark," says marine geologist Henry Dick of the Woods Hole (Mass.) Oceanographic Institution, who served as a co-chief scientist on the cruise, which ended last week. "We went out there and demonstrated that deep crustal drilling in the oceans is possible."

Ocean crust covers roughtly two-thirds of Earth's surface; but because it lies hidden beneath the waves, often at great depths, it has resisted the kinds of detailed investigations possible on land. It was not until the 1960s that oceanographers discovered how ocean crust originates through the process of seafloor spreading. Hole 504B will help illuminate this process by giving scientists their first real look at the interior of normal ocean crust, Dick says.

Seafloor spreading occurs at the junction of two lithospheric plates -- large sections of the Earth's broken outer shell. As the plates pull apart, molten magma escapes from deeply buried chambers and squits up to the surface, where it flows out and hardens. Over millions of years, these episodes create new crust as older crust moves away from the plate junction.

The spreading process builds a layered crust tha resembles a complex cake. The "icing" on top consists of sediments and hardened lava. The middle layer is made of sheeted dikes -- thin, vertical structures that form when magma solidifies in the crack between the plates. Shaped like giant sheets of paper, individual dikes ofte measure only 1 meter thick, yet they may stretch 1,500 meters vertically and 5,000 meters horizontally. Hole 504B is the only drillhole to reach into the sheeted dikes. Beneath the dikes lies a third layer consisting of huge deposits of gabbro rock -- the fossilized remains of ancient magma chambers.

The ODP and its predecessor program have drilled at 504B on and off since 1979. But as the hole deepened, conditions grew more difficult, sparking a string of technical frustrations, caused in part by temperatures that topped 150 [degrees]C at the bottom of the hole. With scores of other potential drill sites around the world, scientists debated whether to risk spending more time on this valuable but problematic hole.

In September, the ODP drillship headed back to 504B for one last try. Crew members spent nine days trying to fish broken drill pieces out of the bottom of the hole, which lay 4.5 kilometers below the deck of the ship. Success came with less than one day remaining before cruise leaders had planned to abandon the hole. Using improved techniques, they then proceeded to deepen the hole by 378 meters.

Although the recent drilling effort fell short of its goal -- the gabbro deposits -- several signs indicate that this long-sought layer may lie within a few hundred meters of the bottom of the hole, says Dick. The density and grain size of the rock pulled up in the drillcore has increased as expected, he notes, and the mineral chemistry suggests that the ancient magma chambers are near.

Because of previously scheduled cruises, the drillship cannot return to 504B before mid-1994. But given last month's success, ODP will place a high priority on resuming drilling there as soon as possible, says James Austin of the University of Texas at Austin, who chairs the ODP planning committee.

Recent studies on land have highlighted the importance of drilling at such sites. In the past, scientists have used ophiolites -- slivers of ancient seafloor that have been pushed up onto the continents -- as an accessible analog for studying ocean crust formation. But in the Nov. 14 NATURE, Don Elthon of the University of Houston suggests that ophiolites differ from most ocean crust. "We can learn a lot of general things about ocean crust by studying ophiolites," he told SCIENCE NEWS. "But for the details, the particulars, we really need to go out and drill in the ocean."
COPYRIGHT 1991 Science Service, Inc.
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 1991, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

Article Details
Printer friendly Cite/link Email Feedback
Author:Monastersky, Richard
Publication:Science News
Date:Nov 23, 1991
Words:765
Previous Article:Desalinization, the microbial way.
Next Article:Emergency repair for the ozone hole?
Topics:


Related Articles
Deep source of magnetic stripes.
Leg 104: rifting, currents and climate north of the Arctic Circle.
Leg 106 treats: heat vents, sea creatures, engineering feats.
Connect the dots in the ocean crust.
Drilling discoveries in the Pacific.
Drilling hits birthplace of Pacific plate.
Drilling shortcut penetrates Earth's mantle.
Liberia offers opportunities as a new source of wood supply. (From the Archives).
Oil booms: whales don't avoid noise of seismic exploration.
Pregnant in America: a nation's miscarriage.

Terms of use | Copyright © 2016 Farlex, Inc. | Feedback | For webmasters