Part 2 (1/2)
”Good.”
”They ought to promote you.”
”I hope not.”
”Why not?”
”I don't like responsibilities.”
”But you take them on yourself, and you handle them well.”
”I was lucky, once. Who knows what will happen, next time ... ?” He gave me a furtive look.
”What do you mean, 'next time'?”
”I mean, if it happens again,” I said. ”I just happened to be in the control room ... ”
I knew then that he was trying to find out what I knew, so neither of us knew much, though we both knew that something was wrong. He stared at me, sipped his beer, kept staring at me, then nodded. ”You're trying to say that you're lazy?”
”That's right.”
”c.r.a.p.”
I shrugged and sipped mine.
Back around 1957, fifty years ago, there was a thing called AMSOC, and it was a joke. It was a takeoff on the funny names of alphabetized scientific organizations. It stood for the American Miscellaneous Society. It represented something other than a joke on the organization man, however. This was because Doctor Walter Munk of Scripps Inst.i.tution of Oceanography and Doctor Harry Hess of Princeton were members, and they had come up with a strange proposal which later died for lack of funds. Like John Brown, however, while it lay moldering in its grave, its spirit kept churning its feet.
It is true that the Mohole Project died stillborn, but that which eventually came of the notion was even grander and more creative. Most people know that the crust of the Earth is twenty-five or more miles thick under the continents, and that it would be rough drilling there. Many also know that under the oceans the crust is much thinner. It would be quite possible to drill there, into the top of the mantle, penetrating the Mohorovicic Discontinuity, however. They had talked about all kinds of data that could be picked up. Well, okay. But consider something else: sure, it's true that a sampling of the mantle would provide some answers to questions involving radioactivity and heat flow, geological structure and the age of the Earth. Working with natural materials, we would know boundaries, thicknesses of various layers within the crust; and we could check these against what we had learned from the seismic waves of earthquakes gone by. All that and more. A sample of the sediments would give us a complete record of the Earth's history, before man ever made the scene. But there is more involved than that, a lot more.
”Another one?” Martin asked me.
”Yeah. Thanks.”
If you study the International Union of Geology and Geophysics publication, Active Volcanoes of the World, and if you map out all those which are no longer active, you will note certain volcanic and seismic belts. There is the ”Ring of Fire” surrounding the Pacific Ocean. Start along the Pacific coast of South America, and you can follow it up north through Chile, Ecuador, Colombia, Central America, Mexico, the western United States, Canada, and Alaska, then around and down through Kamchatka, the Kuriles, j.a.pan, the Philippines, Indonesia, and New Zealand. Forgetting about the Mediterranean, there is also an area in the Atlantic, near Iceland. We sat there.
I raised mine and took a sip.
There are over six hundred volcanoes in the world which could be cla.s.sified as active, though actually they don't do much most of the time. We were going to add one more.
We were going to create a volcano in the Atlantic Ocean. More specifically, a volcanic island, like Surtsey. This was Project RUMOKO.
”I'm going down again,” said Martin. ”Sometime during the next few hours, I guess. I'd appreciate it if you would do me the favor of keeping an eye on that G.o.ddam machine next time around. I'd make it up to you, some way.”
”Okay,” I said. ”Let me know when the next time is, as soon as you know it, and I'll try to hang around the control room. In case something does go wrong. I'll try to do what I did earlier, if there's no one around who can do any better.”
He slapped me on the shoulder.
”That's good enough for me. Thanks.”
”You're scared.”
”Yeah.”
”Why?”
”This d.a.m.ned thing seems jinxed. You've been my good-luck charm. I'll buy you beers from here to h.e.l.l and back again, just to hang around. I don't know what's wrong. Just bad luck, I guess.”
”Maybe,” I said.
I stared at him for a second, then turned my attention to my drink.
”The isothermic maps show that this is the right place, the right part of the Atlantic,” I said. ”The only thing I'm sacred about is none of my business.”
”What's that?” he asked.
”There are various things about magma,” I said, ”and some of them frighten me.”
”What do you mean?” he asked.
”You don't know what it's going to do, once it's released. It could be anything from a Krakatoa to an Etna.
The magma itself may be of any composition. Its exposure to water and air could produce any results.”
”I thought we had a guarantee it was safe?”
”A guess. An educated guess, but only a guess. That's all.”
”You're scared?”
”You bet your a.s.s.”
”We're in danger ... ?”
”Not us so much, since we'll be the h.e.l.l out of the way. But this thing could affect world temperatures, tides, weather. I'm a little leery, I'll admit it.” He shook his head. ”I don't like it.”
”You probably had all your bad luck already,” I said. ”I wouldn't lose any sleep ... ”
”I guess you're right.”
We finished our beers and I stood.
”I've got to be running.”
”Can I buy you another?”
”No, thanks. I've got some work to do.”
”Well, I'll be seeing you.”
”Yes. Take it easy,” and I left the lounge and moved back to the upper decks.