NOVA; To the Moon; Footage of Monterey Conference, part 1 of 2

You Marker I don't like any particular

one This was Paul Gass, Jerry Barserberg, Bob Walker, and Jerry Barserberg. Yes, it was a lot after that.

These were the poor horsemen that would be a pocket lift, just in your own way. I had accused you of being one of those, but you were the... I was in the trenches, actually, doing the hard work. That's the phrase I just used with them. Okay, I said you were on the trenches, yes. This was in the lunar receiving lab at 1969 till I 20th when the samples came back. And my job was to analyze them, and this was the roughest work I ever had to do in my life, I think. I'm sorry, we're done putting up the poster. I don't know, do you just want to shoot us at a distance or something, we're not actually seeing anything at that point.

Oh, this is an anine, this is terrible. And I mean, I don't even know if I can see Jim was down in the road. Yeah, he doesn't even know if I can see him. That was Jim. Not that you can see, so it's weird because the really un-mice topic or composition is not solid as you can expect. What is the reason of the un-mice topic? I'd be, uh, sorry.

I'll check that Count Day's that business of the led evolving. Her business of the led evolving is very interesting. It's pretty easy to do. I mean, I just didn't have the numbers. Yeah. I mean, that was extremely important. Yeah. Now, I can give you those initial values. I mean, the initial from the end day line, you know, can. The question is, how big the mu has to be in order to get there and say... For a different time. But it must be... It's got a pretty high. Well, it has a point of view. How high? I do not know the answer. Yeah, that's good. Could have done the calculations 10 years ago, but today... But, you know, the one pretty high up on the line is, for instance, C1. And C1 is hellishly unusually in all isotopes. You know that, right? Yeah, but so it won't be very surprising. The magnitude of the led effect there is one he presented on the led. But what is the led carrier in those un-radigenic led CII?

I don't know. And C1, you remember you have Zinks Benels, huh? You remember it's C1, you have Zinks Benels. Yeah. It's C1, it's C1. It's C1. It's C2. It's so evolved on a rich phase. Well, the Uper is C1, and the Uper is C1. It's C1, and you're going to try to come back and start on the scale. But there's a gas pressure from the vaporized portioning material, which is small in a amount, but it's enough to perturb the orbits. And essentially, it feeds in the rock rock, but at least where these things are being formed, this is consistent with the trace element data also for water-rich granite, and even towards granite pectetite feed. Now, furthermore, the other question that I need to ask you, is that these are compounds or so?

This is just a depletion diagram for tungsten. And if you start off with a condritic tungsten formed the earth and have early core formation, as long as you wait, then you wait in 50 million years until all the half of the way, actually, in this case, we're going to have a quality of stench of the criminal extraction, in this case of drugs. And here, this is a real problem. You have excess the derivation. And we're already particles because of that, there would come back. Yeah, well, this is not a surface, so this is in velocity. This means zero velocity. So this is all negative velocity, that is velocity going down. And the vector velocity is straight down. It's very long for it to carry it out for years. I have no idea.

I have no idea. Did you apply? No, almost did. Did you like to live in Denmark? Yes, I wouldn't mind. I wouldn't mind. I wouldn't mind almost doing it. Which actually says that the wound in a war is, this is traditionally depleted. Exitally depleted. And the solid, I mean, it's head straight. It's all flat out of it. So what about the adenium? This is porous tail, okay. Now you go to an anti-tide and you see the whole rock is off the metal C3C2. Let me just look a second.

That's far, I don't know. And this is no metal or metal, non-metallic, and this is a metal. So in the corn, everything is on it, right? And now you go to Indark, it has the same slope, right? But the whole rock is off. The metals are lying there. It silicates obviously not, because the whole rock. Now when you look at the metals here, well, the metal is lying up pretty well. It's perfectly in the large form of this, right? And then you come over to AB, you see the same thing. AB is horribly heterogeneous, we know that, right? Now, and you go on and on and on. And the conclusion is that silicates form 20 million years later, which is full. I mean, if all it shows is the silicate metal rock, and then take it, it's better. In the sense that you can't get the silicate in the silicate, it's taking a lot of pressure.

I don't know if I can do it. I'm not sure if I can do it. The camera is talking about it. And if that equation stays, so I'm poorly known. Then all bets are off, basically. It says the basic cartoon on what's going on is probably correct. But the details cannot be possibly well understood. Which means it's not meaningful to talk about whether the earth was half grown, record is grown. No, that's right. I'd say think of that as a free parameter. And then start saying, well, if you don't have to have 100% of the earth, and you only have to have 90 or 80 or 70%, can you make the whole system look more like it really is by adding stuff from the asteroid belt or comments? Well, then again, the difference. The problem with the earth at that point is that if it's really that small, then you'd be deducted to find a way of adding relatively oxidized stuff, but not like the late veneer, but maybe up to 20, 30, 40% of the remaining mass of the earth.

Or else you don't satisfy the metal-seeking element of the bonuses in the earth's metal. Likewise, in the case of the moon, you're going to melt that. That moon is going to melt roughly coincident with the large impact, I think. And so you've got to find a way of keeping it... Going there with Christmas. Oh, nice. Amsterdam is just nice. It is open here. You can just wear whatever you need and wear.