Otrobonita/noicy-space-talks huggingface dataset:
CDR-EVA: As long as the brakes hold out - -
CDR-EVA: It should be easy, Charlie.
LMP-EVA: Have you got the brakes on?
CDR-EVA: Partially.
LMP-EVA: Isn't that something?
CDR-EVA: Have to.
CDR-EVA: Okay. What was the heading and distance for that - to that?
LMP-EVA: 354 for 3.4.
LMP-EVA: You know, it didn't really - It was really not apparent we were climbing this steep a slope.
CDR-EVA: 354 for 0.4?
LMP-EVA: 3.4.
CC: Okay, that's the bearing and range that - - and
LMP-EVA: Okay, Tony, was that bearing ran - was that at stop 5?
CC: Okay, the heading and distance - -
LMP-EVA: Okay, stop 5. Roger.
CC: - - is 352 at 0.7.
LMP-EVA: Okay, we - we've got a 354 bearing back to the LM right now, so we'11 Just keep on that.
LMP-EVA: Man, John. You're doing a great Job. Okay, Tony, coming back downslope 354 at 3.8 is about the same stuff.
LMP-EVA: Okay. We' re about to cross our tracks. 95/17 Tape
LMP-EVA: We're going back down our tracks, Tony.
CDR-EVA: Only way to fly, Tony.
CDR-EVA: Charlie, you said you were going to see some other tracks on the Moon.
LMP-EVA: Yeah. That - that big crater I was thinking about is right back there - it looks like. \\
CDR-EVA: No wonder we broke the pitch meter. Just as well we did.
CDR-EVA: Ya-ho-ho-ho-ho. Look at this baby. I'm really - I'm really getting confidence in it now. It's
UNKNOWN: Oh, this machine is super.
CC: Probably a good idea you couldn't see how steep it was going up.
CDR-EVA: Darn right it was.
CDR-EVA: Okay. I've got the power off, and we're making 10 kilometers an hour. Just falling down our own tracks.
LMP-EVA: Hey, Tony. I'm keeping my eye out for a blocky rim one.
LMP-EVA: Almost spun out.
CDR-EVA: How about this one right here, Charlie?
LMP-EVA: Yep, that - that's it, John. That's a good one.
LMP-EVA: Okay. It's stop 5. We're supposed to park at -
CC: 180.
UNKNOWN: 180. Say again, Tony.
CC: Roger. I was just saying 180.
LMP-EVA: That doesn't look like a secondary, John.
CDR-EVA: It doesn't look like one to me either. Well?
LMP-EVA: It might be a primary impact, but I - I - I think those blocks are or - the rocks there are from South Ray. We'11 - I think we ought to get a rake sample he re.
CC: How big is that crater?
UNKNOWN: 15 meters across.
CC: Okay. Understand 15 meters.
CDR-EVA: Okay. We're parked right on the rim of it. We'11 let you see.
LMP-EVA: The biggest - the biggest blocks we see, Tony, are about 50 centimeters, or bigger; and they're in the bottom and all over the crater - no cert - preferred orientation. Okay. We're parked at 174, 353, 5.9, 3.5, 100, 100 -
LMP-EVA: Excuse me, John. 65, 65, 100 - 90, 105, off-scale low, and off-scale low - Wow!
CDR-EVA: In the - in a hole?
LMP-EVA: No, it's downslope for me over here. 95/19 Tape
CDR-EVA: It is?
CDR-EVA: Me too, Charlie. Fact is, let's bring the Rover back up here.
LMP-EVA: Well, I'm out - I'm not getting out again, and getting hack in.
CDR-EVA: No, I don't mean that. I mean let's bring the Rover back up here.
LMP-EVA: Oh, you want to pick it up, huh?
CDR-EVA: Okay, now. We've got to swing it around.
CDR-EVA: That's more like it.
LMP-EVA: Didn't run.
CDR-EVA: What did you say?
LMP-EVA: Didn't run - the camera didn't run. X is still there. The film looks good.
CDR-EVA: Okay. MODE switch to 2.
LMP-EVA: Okay, now it's working.
CC: Okay. We've got a picture.
CDR-EVA: Got the Earth in the tube. Okay.
CC: 04ay. And while you're brushing off the LCRU there, make sure you do a good job. We notice it seems to be heating up.
CDR-EVA: I've been doing a good job.
LMP-EVA: I'11 vouch for that, Tony; honest.
CC: We believe you. Our best bet here at this crater is to look for - -
CC: - - a rounded, as well as angular - the angular boulders are probably from South Ray. And maybe the rounded ones are - are working their way out of the regolith here. So that may be a cue to our - to our getting Descartes.
LMP-EVA: Good point.
CDR-EVA: Roger. Well, I'11 tell you what. If we do a rake sample in the wall, would probably be our best bet.
LMP-EVA: That's what I would like to do.
LMP-EVA: You know, John, looking back, I can't even see our tracks.
CDR-EVA: They're back there - I guarantee.
LMP-EVA: I know it. Man, we come a long way. I thought this thing was just right next door to us.
LMP-EVA: That rake is sure a great way to get a lot of rocks - in a hurry.
CDR-EVA: Yep, it sure is. Boy, I tell you, even South Ray looks like it's accessible. I'd - I'd hesitate to say, though. There may be blocks down there that won't quit.
LMP-EVA: There's some big black ones. See those big black blocks there, John?
CDR-EVA: Yeah. 95/21 Tape
LMP-EVA: On - on the side of it. And there's some - there's some big white ones there, too. The black ones are the biggest.
CDR-EVA: It almost looks like we could just go right down there and right up on South Ray, doesn't it? No, we couldn't (laughter).
LMP-EVA: I don't believe they're going to let us, but it looks it. I agree with you.
CDR-EVA: I don't think we could.
CC: Judging by the blocks here, I sure don't know.
LMP-EVA: Aw, Tony, this is - they aren't bad here. This Rover takes them like - I don't think we're going to need 40 minutes here, I'11 tell you. We ought to spend some more time somewhere else.
CDR-EVA: Let me get the rake sample here.
CDR-EVA: f/11 and 11.
LMP-EVA: We could go out to - Okay, go ahead, pick a place. I'11 get the gnomon. You going to get it? Okay.
LMP-EVA: Okay. Our little note here in the checklist, Tony, doesn't mean too much. We seem to be on a bench here that'S about 50 meters wide, and then it's - and the slope here on the bench is only about 2 degrees - maybe 3 or 4 degrees - maybe 10 - no, about 5 degrees, I'd say. And -
CDR-EVA: Houston, here's about a foot and a half across secondary - pri - looks like a primary that cut into the rim - the upper rim of this 10- or 20-meter see - this - yeah, this 20-meter secondary. How about sampling out of the wall of that one?
LMP-EVA: John, I don't think this is - this big crater is a secondary.
CDR-EVA: That's what I mean. But this - -
LMP-EVA: That little one is.
CDR-EVA: This little bitty one is probably a primary, too because look how the - look at the glass on the bottom. Man, you've got to have velocity to do that.
LMP-EVA: Yeah, I agree.
CC: Okay, does it look like it knocked out any rocks?
CDR-EVA: Charlie. Okay.
LMP-EVA: Yeah, there is - -
CDR-EVA: Yeah. I don't think the rocks that are there were there because of -
LMP-EVA: Yeah, it does, John. There's some rocks right in that corner there, right by your footprint.
CDR-EVA: Oh, yeah, right by my footprint.
LMP-EVA: See that one right there - by the rake?
LMP-EVA: And here's one right in the very bottom. Why don't you get that scoop going? And I'11 go over here and get a - get a locator.
CC: Okay. Sounds like a good plan. And we'd like a documented sample of a glass-covered rock, if you can find one.
CDR-EVA: Okay. Well, we've got several - We've already picked up a couple of beads for you, but we didn't document them.
LMP-EVA: Now, that's a good bagfull.
LMP-EVA: One - one scoop.
CDR-EVA: Want me to do it again?
LMP-EVA: Well, we got a bagful.
CDR-EVA: Notice the color of the material, Chartie, in the bottom of it - it's white. We get a kilo of soil.
LMP-EVA: That's what this is. This isn't rocks.
CDR-EVA: Friable soil?
CDR-EVA: That could be Descartes, Charlie.
LMP-EVA: Hey, Tony, that rake soil - sample was in 332, and I just, by - with an experiment, pinched one of the rocks, and it all - it broke.
LMP-EVA: It's probably going to be a bagful of soil when we get it back.
CC: Well, that may still be Descartes.
CDR-EVA: It may be.
LMP-EVA: I think it is.
CDR-EVA: The lower - the lower material in the - in the cra - in the crater is -
LMP-EVA: Want - want another one?
CDR-EVA: Yeah. Lighter albedo - much lighter albedo. And if I had my druthers, it's somewhere between the gray and the white out on the plains.
LMP-EVA: That's good, John. It's about a kilo.
CDR-EVA: It's somewhere between the gray of the surface and the white material that we picked up out on the plains. About - and we got a bagful of most of that - under - from scooping underneath the rock samples.
CC: Okay. And, after this, we'd like you to move to the rim of the main crater, and spend some time just describing the rocks you see, and then sample the rim.
LMP-EVA: Okay. I think - okay. I think -
CDR-EVA: There's one of those glass jobs, Charlie, right there.
LMP-EVA: I don't see it.
CC: Okay. We'd like a documented glass sample, if you have a chance.
CDR-EVA: That wasn't big enough to document.
LMP-EVA: But we'11 look for a rock that's glass-coated, Tony.
CDR-EVA: If we were to sample on the upslope side of this crater where it shield - I mean shielded toward South Ray and the wall - if - if - if it wasn't caused by South Ray, then - then we ought to be looking at the - the - the real Descartes.
LMP-EVA: That's a good plan.
LMP-EVA: Hey, Tony - the - the - }iere's a glass-covered one, John, right here.
UNKNOWN: that right by this - right by that foot- print. Right where I stopped walking. Man, you're going to get me down in that crater.
CDR-EVA: No, I'm not.
LMP-EVA: I'm not going to get a down-Sun of that.
CDR-EVA: I don't think you ought to.
CC: No, let's forget the down-Sun.
LMP-EVA: I'11 get the cross-Sun, okay?
CDR-EVA: Yeah. Now, the only rocks we see are really angular, and they're on this rim. And I - I guess the problem is - it was a cratering event was just no probably so long ago. There's - not even a hint of any ledges or bedrock in this rascal.
LMP-EVA: John, why don't you take the rake right here in front of the - the - gnomon - I've already docu- mented that area - and see what you get?
CDR-EVA: Take the rake what, Charlie?
LMP-EVA: And Just right here in front the gnomon and see what you get. One scoop and - it might be -
LMP-EVA: I got - I got the pictures.
CDR-EVA: You do, huh?
CDR-EVA: I don't think you're going to get anything but soil. One or two.
UNKNOWN: there's some rocks. Two.
LMP-EVA: Hey, there we go. Why don't you hold the bag and let me pour it in? Okay.
LMP-EVA: I bet we'd be in a better position.
LMP-EVA: Well, we've got a few of those. Let me try one more scoopful.
CC: Okay, do those look like clods, too?
CDR-EVA: No, they don't. There is at least one of them that's glass-coated.
UNKNOWN: there's some.
CDR-EVA: These are whitish -type rocks, very small - They may have come from South Ray.
UNKNOWN: Let's try one more scoop, John.
CDR-EVA: Okay. R_ere's one right under there. It looks like a good - a good samp - a good bet.
LMP-EVA: Man, you can get a bunch of stuff with this rake. See s if this was - if this was from South Ray - -
CDR-EVA: Hey, look at that -
LMP-EVA: And all of those are rounded.
CDR-EVA: I know it. That - Charlie points - the - the different characteristics of these rocks that we're Just getting right now, and maybe that's the key is that all - they're more rounded than the South Ray crater rocks are. 95/27 Tape
CDR-EVA: There are a few angular in there, but they - these are mostly rounded; and I see some little black glass on one, but they're mostly rounded, whitish rocks covered with dust, of course.
LMP-EVA: These are a couple of good ones.
CC: Okay. That sounds real good.
UNKNOWN: Bag 334.
CDR-EVA: Okay. ....
UNKNOWN: That's bag 334, Tony.
CC: Okay; 334.
LMP-EVA: Houston, do you want us to go sample the rim of this thing again - some more?
CDR-EVA: They want us to get a glass-coated one, and there's a good one right up on the -
CC: Okay, did you get - -
CDR-EVA: Let's go up there and get it.
CC: Did you get your soil there?
LMP-EVA: Do what? Huh? Say again.
CC: Okay. You got your soil there?
CDR-EVA: No. We didn't. I'11 get a scoopful.
CC: Okay. And you're doing so well inside the rim there, we'd kind of like you to stay inside the rim and just kind of work around and see what you can find.
UNKNOWN: Let me get a sa - some soil here.
CDR-EVA: Wait a minute, Charlie.
LMP-EVA: This ain't - you really feel like you're on the verge of instability, don't you?
CC: That's probably only because you are.
CDR-EVA: I've got the gloves so dirty. There's a - 100 kilos. Okay. That's 100 kilos that's going into bag 402.
CC: Okay; bag 402.
CDR-EVA: Hope you're able to document it with the T - TV, because we've stepped all over it.
LMP-EVA: Tony, these after pictures are going to be - on this kind of terrain, you're - you - you're bouncing so much trying to keep your balance, that you just sort of obliterate whatever you've picked up - the place you picked it up.
CC: Okay. When you dig down there, you're not getting - -
CDR-EVA: Okay. We'11 go down about a f - wait a minute.
CC: - - any of that white soil. Is that right?
CDR-EVA: That's correct; we're not. I kicked some of it away to see just'how -
LMP-EVA: Hey, John?
LMP-EVA: Here's an old, old rounded rock that's - that's fractured, badly beat up. Let's - let's get that one. Give me - Can you give me the - get your - get your -
CC: That's what we're looking for, Charlie.
LMP-EVA: I was going to say take a - take a picture of that. This gnomon is worthless. It's against the stops.
CDR-EVA: That one right there?
LMP-EVA: Yeah. That one right there.
CDR-EVA: Okay, I'11 get it. I'11 get a - cross-Sun.
UNKNOWN: That's all we're going to be able to get.
CDR-EVA: Well, it's - it's sort of an up-Sun.
LMP-EVA: Man, I'm feel like I'm -
CDR-EVA: I'11 shoot these at 5.6, Houston. Stereopair l_-Sun. You can doc - I can get the location all right.
LMP-EVA: Oh, don't work at that, John.
CC: Okay. We can get the location off the TV.
CDR-EVA: Okay. Was an old rock, wasn't it? ... it crumbled to pieces.
CDR-EVA: That was fruitless there.
LMP-EVA: Get it - get that - that right there.
CDR-EVA: I am. I'm trying to get upslope on it.
LMP-EVA: Here let me - hand me I can get it.
CDR-EVA: Careful, Charlie. There we go.
LMP-EVA: Uh-oh. Okay. I got it.
CC: Okay, and the white rock that you picked up and the ones you just have here, can you see any crystals in it?
LMP-EVA: Yes, sir. I sure can. It's a bluish crystal, a couple of millimeters size.
CDR-EVA: Bluish?
LMP-EVA: Well, that's what it looked - Grayish maybe - and it's got - one corner of it's got a glass rind [?] on it about a cent - about half a centimeter thick. k
LMP-EVA: It looks like - it doesn't look like a breccia, Tony. It looks like a crystalline rock.
CC: Outstanding ....
CDR-EVA: Yeah, it's got a lot of - it's fine grained - it seems to be a fine-grained crystalline rock any- way, the part that we can see. The particles in it are millimeter size, though. I see some millimeter-size sparklies flashing at me. That's going in bag 403.
CC: Okay, 403.
LMP-EVA: Hey, John, let's - why don't just - let's keep that ... - I'm having about strike out on this rake here. I can't - get a couple of little ones each time, but - -
LMP-EVA: - - about it.
LMP-EVA: Want to move on around there about 10 feet or so?
LMP-EVA: Pick a spot. I'11 follow in your tracks. You're sliding downhill about 2 inches every time you - I can't get going, here (laughter). There's a - Look at that glass-covered one right there, John.
CDR-EVA: Okay. Let's get it, Charlie.
LMP-EVA: Okay. I'11 back off and get the - cross-Sun here.
CDR-EVA: Yeah, I'11 have to get an up-Sun here, or else do a lot of work.
LMP-EVA: Gonna be just one rock and one bag here.
LMP-EVA: Hey, Tony. We just picked you up a glass rin - lin - rind rock - at least a quarter of it's got glass on it, and it's so ra - it's so dust covered that it - - 95/31 Tape
CDR-EVA: - - defies description.
LMP-EVA: Defies description. (Laughter) Yeah.
CDR-EVA: 404 is the bag number - -
CC: Okay, bag 404.
LMP-EVA: Y'all got us on the big eye?
CC: We sure do.
LMP-EVA: Yeah. They do.
CDR-EVA: Close the top, Charlie.
LMP-EVA: Okay. Let me try a rake here - let me get an after here.
CDR-EVA: Get an after, Charlie.
LMP-EVA: Okay. Got it. Here, let me rake up here. Here's some - these are either clods or - -
CDR-EVA: Be careful, Charlie.
LMP-EVA: Uh-oh. That was a whitish rock. That one probably came from South Ray. Wait a minute. Here - here's some good ones - dusty ones.
CC: Man. It sure looks like a good thing we had that rake along.
CDR-EVA: Yeah, most of those are either little rocks - -
CDR-EVA: Well, I don't - I don't - there's a round one, Charlie.
LMP-EVA: Hey, there's a great one, John. There's a good rock right there.
CDR-EVA: I don't think this is going to be a simple problem, even after you - -
CC: We concur, John.
CDR-EVA: - - you - -
CDR-EVA: - - get the rocks back because they're so dark - so darn - dark - it's 405.
CDR-EVA: Go in bag 405. That's a big round - round rock that's dust covered. I see white streaks through it, and I can't tell from the clasts showing through that I can see whether it - it seems - no, I don't know whether I can see any glass on it or not. But it's a friable white rock, and it's rounded.
CDR-EVA: Going into bag 405 with Charlie's ric - with Charlie's rake sample.
CDR-EVA: You see because there is so - so doggone many craters around here, I mean - -
CC: Right. Understand. We'd like you to find the steepest slope that you can work on there, and dig as deep as you can with that rake.
CDR-EVA: Let me do that, Charlie.
LMP-EVA: We were dig - we're on it right now, babe. I'11 tell yOU.
CC: Okay, can you dig into the face of the slope a bit?
CDR-EVA: Let me dig. Let me - Charlie, let me do that.
LMP-EVA: Okay. I'11 swap with you.
CDR-EVA: Hold the gnomon.
LMP-EVA: Okay. i-
CDR-EVA: Watch it now.
LMP-EVA: Hey, how about right up here, John. Here's a deep - sleep - steep part, or right over there where we walked from. Where you going?
CDR-EVA: On a steep slope.
UNKNOWN: OKay, right to your left is a good one. Right where we been.
CDR-EVA: Steepest is closest to the rim.
LMP-EVA: That's right. Right up there.
CDR-EVA: Man, you don't make much headway.
UNKNOWN: Great job.
UNKNOWN: Okay, Tony. We've gone vertically into the wall, about a foot, and it all looks the same. Occa- sionally, you see a white splotch.
CC: Okay. Can you - will the rake pull out any rocks - in there? Take a rake sample down in the - the hole there.
LMP-EVA: Just a minute. Hey, John, I tell you what. Let me get upslope.
CDR-EVA: Move out of the shadow, Charlie. I can't see it.
LMP-EVA: Okay, that - there you go.
CDR-EVA: Whoop. One thing about being on a 20-degree slope. You can get down on your knees.
CDR-EVA: Well, I - I think that's gonna be the name of the game until we get a -
LMP-EVA: Looks like just indurated regolith, doesn't it.
CDR-EVA: Uh-huh.
LMP-EVA: Don't see any rocks. Here let me - let me do this. I
CDR-EVA: There's one.
CDR-EVA: There's some.
UNKNOWN: Yeah, they're rocks all right. Going in bag 335, three little ones, Tony.
LMP-EVA: No, they aren't; they're clods. And they're clods, not - not rocks.
LMP-EVA: But, anyway, 33 - 335, did I say 331, 335?
CC: You said 335.
LMP-EVA: Here, let me have the rake a minute. Let me try something.
CC: Well, you think the rock concentration near the surface is a lag surface, then?
LMP-EVA: Apparently so because, in this - in this wall here, we're not getting a thing.
CC: Okay, why don't you take a soil right there - -
LMP-EVA: And there looks like - -
CC: - - fill up a soil bag.
LMP-EVA: Okay. And there's less soil here - I mean less rocks here than on the other side of the crater. The side towards the Rover is - -
CDR-EVA: - - is - this could be a south - south - South Ray, course, that's downslope too.
LMP-EVA: Now there is a pure - there are two rocks, right there. 95/35 Tape
CDR-EVA: Hey, Charlie, I got to put this one in your bag before I can get it.
CC: And, we're going to have to press on after this sample.
CDR-EVA: Yeah. Okay; 20 minutes to get back to the Rover.
UNKNOWN: Oh, you need this, don't you?
LMP-EVA: Get you a soil - they want a soil bag full. Hate to waste a bag on that one, but - -
CDR-EVA: Okay. What? Let's put the - let's put the soil in there with the ...
CDR-EVA: Bag 406 will have one rock in it and a soil sample from this low area.
LMP-EVA: Let's fill up the bag.
LMP-EVA: And, Tony, a lot of this soil is coming out from about 6 - 6 inches down - -
LMP-EVA: - - out of this crater. You know, John, I think if we got a running start straight at the Rover, we'd make it up the other side.
CC: Go the other way.
CDR-EVA: Let's go around the rim.
CC: Okay, the plan back at the Rover is now we'd like John to take an LPM measurement and, Charlie, if you could sample around the rim there near the Rover and take both angular and round whatever you find.
LMP-EVA: Do they want - Okay.
CC: Yep, we'd like an LPM. Incidentally, your magnetic field there is about 130 gammas back at the LSM.
CDR-EVA: How is it at - how is it at the site measurement. Does it agree with that?
CC: Okay. I believe it was about 20 g_mmas less, something like that 110 gammas.
CC: Plunging pretty steeply.
LMP-EVA: Hey, John. It's easier to go straight across. That was fun.
CDR-EVA: I haven't had any trouble.
UNKNOWN: I had a tough time walking up there, on the side - -
CDR-EVA: I got big feet today, Charlie.
UNKNOWN: - - like that. Uh-uh.
CDR-EVA: Going 45 feet on an LPM re - (laughter) gonna put me over the edge here. I'm gonna go out at right angles to the Rover, around this crater rim, for this measurement, Houston. It may not be exactly 45 feet, but it'11 be close.
CC: Okay. That sounds good, John. And, Charlie, we'd _-_ like some fist-size samples here.
LMP-EVA: Okay, we've got a ton of the_. We'11 get them for you.
CDR-EVA: Okay. Lots of luck with that LPM.
CC: And, John, why don't you take a pan when you document the location of that LPM tripod. That'11 take care of our pan.
CDR-EVA: That's a good idea. Ail right, fine, good - good head.
LMP-EVA: I already took one pan.
CDR-EVA: Well, they want another one.
CDR-EVA: Okay. The READ switch is going on. Not the READ switch, the - the ON switch, the power swit ch.
CC: Okay. We got it. Charlie, where did you take your pan from?
LMP-EVA: H_mm_ on the south rim of that crater.
LMP-EVA: About 10 feet be - to the 4 o'clock position of the Rover.
CC: Okay, John. I guess we won't need a pan, if you can just get the LPM.
CC: Okay, John. A minute.
CDR-EVA: Wait a minute; I'm deploying it.
CC: Oh, I thought you gave a mark. Ail right. I understand.
CDR-EVA: - - turning ...
CDR-EVA: Yeah, I did - for turning on.
CDR-EVA: Hey, I got it out to the white line now.
LMP-EVA: Okay, Tony. I'm sampling right in front of the Rover. - about 10 feet. I got a fist-size rock out here.
UNKNOWN: It's captured in the old tongs. Was captured in the old ton_s.
CDR-EVA: Okay, that's aligned perfectly. Here we go.
CDR-EVA: Okay. Now start your minute, Tony.
LMP-EVA: Okay. That rock's going in 336. It's a - a rounded rock and it's dusty, and all I can see is - is some streaks on it, Tony - white streaks.
LMP-EVA: Hey, John. Could you throw - throw me the bag that's under your seat. I'11 get it. I'11 get it. I'11 get it.
CDR-EVA: I'm about to - I'm gonna knock ... - -
LMP-EVA: Well, I'11 get it.
CDR-EVA: It's under my seat?
LMP-EVA: I thought so. The one that we were - -
CC: Okay, John -
CC: MARK. __
LMP-EVA: No, it's not there; it's under my seat. Excuse me. Page llll
CDR-EVA: Okay. The READ switch is going on. 563, 415, 3 - wait a minute. 563, 415, 356, 570, 424, 357, 571, 425, 357, off. Okay. The RE - the off - the POWER switch is coming OFF.
LMP-EVA: Did you get those, Tony? '
CDR-EVA: Did you get those? I forgot to ask you. Okay.
CC: And visors down.
CDR-EVA: ... Visors do_m. Hey, Charlie, where I tripped over here is a lot of white rock.
LMP-EVA: I got some over here, too. Boy, I'm going to grab that one. That's a fresh, sharp, white rock, Houston, that I have never seen the like of. Very angular.
CDR-EVA: Ouch. Boy, Charlie, look at this rock. That has got to be plage.
LMP-EVA: Whereabouts did you find it, John?
CDR-EVA: Bight down there in that - that hole - -
LMP-EVA: Oh, yeah.
CDR-EVA: - - with all that white rock - -
LMP-EVA: Uh-huh.
CDR-EVA: Look at these little crystals in it. No, that couldn't be. A big, white, angular rock and it's - but all the crystals in it are very small. ·That - that is a crystal rock. We're gonna get that one. That's the first one I've seen here that I really believe is a crystal rock, Houston.
LMP-EVA: Want to put it in a padded bag?
CC: Outstanding - - I
CDR-EVA: I believe we'd have to break it in two, so - -
CC: No, we don't need that in a padded bag.
CDR-EVA: It's about 6 centimeters - 12 centimeters long, and it's got a head on it like - it looks like the head of a - maybe a viper or diamondback, if you lay it down flat. You won't have any trouble recognizing it. And it's white, and when I hold it up to the Sun, it has a greenish cast to it. A greenish-bluish cast.
CDR-EVA: Oh shoot! I see some - I see some striations in it, too. They may be my imagination.
LMP-EVA: Okay, Tony. I've got two more documented samples in bag 33 - two more rocks documented in 337.
CC: Okay, 337. And we're gonna have to press on here.
CDR-EVA: Okay, I'm putting this rock under your seat.
LMP-EVA: I'm in. Okay, John.
CDR-EVA: ... I wouldn't do that.
LMP-EVA: I don't blame that pitch meter for falling down. Man, I've fallen down twice. (Laughter) I'm deadly. The Rover wheels are covered with dust, John.
CC: And, John, do you have a bag number for your white rock, or have you collected it yet?
CDR-EVA: I made a grab sample out of it, Houston.
LMP-EVA: Too big for a bag, wasn't it, John?
CDR-EVA: Yeah, it was too big for a bag.
LMP-EVA: It's - amazing how you can trip over - how you can be going along and trip over a rock, and I'm one of these guys that always looks down and it's - and still seem to be able to trip them going forward.
LMP-EVA: Okay, Tony. The samples are complete here. I'm leaving with frame count number - looks like about 170, Tony. I'd better change mags before I start out on - we start out here. Over.
CC: Okay. And, while you're up there, you might adjust the DAC. Maybe you can get it running.
LMP-EVA: I already did, and it's running. It'11 be running.
LMP-EVA: That is the best sample we've got.
UNKNOWN: I'11 tell you. That is a crystalline rock if I've ever seen a crystalline rock.
CDR-EVA: First one today.
CDR-EVA: I ... (laughter) at least the first one you could say was one, maybe .... - -
LMP-EVA: That is a great rock. Okay, John, could you - when you get around there, could you give me a film mag, black and white?
CDR-EVA: Okay. I guess we could - -
LMP-EVA: Which one do you want me to use, Tony?
CC: Call that one the "Great Young."
CDR-EVA: Oh. Come on.
LMP-EVA: It's not very big, but it's just a nice rock.
LMP-EVA: Yeah, it was made about - it looks like it's about 3 days old. No, it must be on the order of 4 billion.
CDR-EVA: Which one do you want, Charlie?
LMP-EVA: The black and - any black and white. It doesn't matter. Wrong pocket.
CDR-EVA: Any black and white?
LMP-EVA: Yeah, ain't but one - -
LMP-EVA: - - magazine I.
CDR-EVA: You already shot up a roll of black and white?
LMP-EVA: Yeah. 170.
LMP-EVA: Uh-oh. I got it. There you go.
CDR-EVA: Okay. Start sliding it in the camera box .... I got dust on it. *** put him *** we *** got the *** Baker 2.
CC: Okay, we can - -
CDR-EVA: Yeah, ...
CC: - - see it works.
LMP-EVA: Okay, Tony. Maga - yeah, magazine India.
LMP-EVA: And starting with fr_m_ count number - about number 3. I guess I fired off a couple. 95/43 Tape
CDR-EVA: Okay, we're ready to press here.
CC: Okay, and just to make sure you didn't get any dust on that LCRU while you're working around there, we would like you to brush it off again. We're really heating up on that.
LMP-EVA: It's clean.
CDR-EVA: It is clean.
LMP-EVA: It's clean. Honest.
LMP-EVA: Want to shut it down for a while?
CC: No. That's all right. And, Charlie, on your LRV read-outs, we won't be needing VOLTS, so why don't we just leave that switch in AMPS?
LMP-EVA: Okay. Got it in AMPS.
LMP-EVA: Okay. It - it's dusted. Going downhill, it doesn't get near as much dust as it did coming up - for some reason.
CDR-EVA: Maybe that's because (laughter) it was 4 kilometers one way and half of one the other. That's probably the reason.
LMP-EVA: I hope I can get back in this beauty here now.
CDR-EVA: You're in.
LMP-EVA: Okay. Dadg?mmit.
CC: Okay, we've got the - the - -
CDR-EVA: Don't - don't do anything with the -
CC: - - magnetometer reading. Station 5 there is 125 g_unma down; the ALSEP site was 230 g_mma - correction - up; the ALSEP site was 230 gamma down; and Spook was 180 down. Hey, John. Do you have switch position 17
CDR-EVA: No, it's - no, I'm going to 1 right now.
CDR-EVA: ... the TV?
CC: We thought maybe you were getting on - -
CDR-EVA: TV's on CCW.
CDR-EVA: TV is CCW. Heading for 6.
CC: That was a very interesting magnetometer reading.
CDR-EVA: Yeah. I didn't think I'd ever - Well, give you a good alignment and read the numbers right, hut (laughter) other than that I - And,
CC: John - -
CDR-EVA: Okay. Station 6 - -
CC: - - We'11 need your ...
CDR-EVA: - - should be about - You'11 have to wait. Oh, no, I can see it. It's - 96, Tony, 96.
CC: And, Charlie, DAC on as you start back - -
CDR-EVA: Okay. We're in and we're on our way.
LMP-EVA: It's already on.
CC: Okay. That station 6 will be completely nominal. 95/45 Tape
LMP-EVA: Okay. Ahh. Okay. This is 3.60 at 2.9. Why don't we just make it 3.5 at - at 2.9.
CDR-EVA: Okay, Charlie. I want to follow n_ tracks down this thing.
LMP-EVA: That's fine. and
CDR-EVA: Okay, we're riding at idle, she's picking up speed. And
CC: Okay. we would like station 6 at the lowest terrace on Stone Mountain and a blocky crater, if possible. Understand. and
CDR-EVA: The lowest terrace a blocky crater.
CDR-EVA: Charlie, where do you think Stone Mountain takes off in the - -
LMP-EVA: ... I can see a place down here. See that - off to the left, John, by our - where your tracks came up there - -
LMP-EVA: There's a pretty big crater, with some blocks around it. I think that might do.
LMP-EVA: Hey, Tony, where do you estimate a - one would be?
CC: Okay. You'11 be at - -
LMP-EVA: Look, there's one right down there, John; 12 o'clock, there's one, about 200 meters. t
CDR-EVA: Twelve o'clock, 200 meters?
CC: Okay. You'11 be in the neighborhood and range of 3.0 or a little bit greater.
CDR-EVA: Okay. I'm just glad that we don!t have that - watch the Rover go TV. Or (laughter) I don_t t_nk- we'd be going.
UNKNOWN: Hey, Tony, look in that -
LMP-EVA: Just to the left there, John. See those blocks over there in that crater.
CDR-EVA: Say, where.
LMP-EVA: Okay, you're 10 o'clock position.
CDR-EVA: That big block there?
LMP-EVA: No, well, on over farther than that.
CDR-EVA: You want to take off and go that way now? I can't see nothing. I got my blinder down.
LMP-EVA: Oh, I'm sorry. Okay, now hook a left. No, not through this crater. (Laughter).
LMP-EVA: Right on the other side of this crater.
CDR-EVA: Kind of expect trouble from backseat drivers.
CC: Yeah, I've noticed that.
LMP-EVA: Well, that's only 3 - that's only 3.3, John. Why don't we go down a little bit further.
CDR-EVA: This one right here?
UNKNOWN: that one's only 3.3 down. They think about 3.0. anyway. Turns out it's not a crater at all It's just a swale.
LMP-EVA: Yeah. Really some interesting angular blocks here. Okay, Tony. It's still apparently - well, it's - we veered - we're steering about 3.40 now, and - we're getting some angular blocks and cobbles just as we described before - 20 percent of the surface, perhaps. 95/47 Tape Page lll9
CC: Okay. The nominal station 4 would be on a bearing of 3.56. But you're going to have to use - -
LMP-EVA: Okay. That's pretty good.
CC: - - your own judgment.
LMP-EVA: We'11 veer over that - -
CDR-EVA: 3.56 at what, Charlie?
LMP-EVA: At ... says.
CC: At 3.0.
LMP-EVA: 3.0. Okay?
CDR-EVA: Like driving a camel.
UNKNOWN: And, Tony, over on - Smoky, it doesn't appear - I can see the lineations over there, but the - they are more widely spaced than - than on Stone here and mostly parallel to the Cayley. Bear - bear left a little bit, John, if you can. can There's a - okay, we're at 3. We start looking for a place now.
CDR-EVA: Here's the bench right down here, I think.
LMP-EVA: Yeah, I see it.
LMP-EVA: Yeah. Now if we drive along the bench, maybe we'11 find a blocky crater.
CDR-EVA: Want to go right or left?
LMP-EVA: Left. Because then station 8's on over to the left.
CDR-EVA: Look at that block there, Charlie.
CDR-EVA: That big block right over there.
LMP-EVA: I know it. That's the one I described. It's a giant size.
LMP-EVA: Okay, Tony. We're at 3.0 at 3.55. Driving west, along a bench, trying to find a blocky crater.
LMP-EVA: Passing these big glass-splattered rocks that apparently came out of South Ray. Think every one of them did, frankly.
CC: Hello. Did you have a busy rev?
CMP: (Laughter) Yeah. That was a little tight. I went to a - to a - half degree per second, and we made it. Seems like I had some things I needed to bring you up to speed on. Let me see if I can find out where I wrote them down.
CMP: I feel like one of the most - one of the most interesting things I've seen on the back side here is in the crater Guyot. Up on the side, there's a big hole, and it sure looks like there is some big, black blob running out of it.
CC: What's the name of that crater again, Ken?
CMP: Guyot. Just to the north and west of King.
CC: Ken, do you have any film reports for us?
CMP: Oh. Let's see. Magazine Papa Papa, I've got 77 showing, and - I'11 get you that 35~millimeter mag here somewhere.
CMP: Okay. On 35, magazine Zulu Zulu, I'm reading 22 frames. I had to retake one of the frames; I knocked nry flashlight, and it came on while I was in the middle of one of the sequences.
CC: Roger. Understand. And if you'11 give us AUTO on the HIGH GAIN and ACCEPT, we'11 send you up a state vector.
CMP: You have AUTO and ACCEPT.
CMP: And the PAN CAMERA POWER is on.
CC: Casper, the computer is yours.
CC: Casper, we're ready for POWER OFF on the PAN CAMERA.
CMP: Okay. I'11 get that in Just a second.
CMP: Okay. The POWER is OFF.
CC: Casper, you're awful quiet.
CMP: Yeah. I'm doing a little housecleaning.
CC: Roger. And I hear your radio running while you're doing it.
CMP: Oh, yeah. And this one is kind of appropriate. Are you familiar with Mr. Holst's suite "The Planets ?"
CC: No, I'm not. bring along.
CMP: Well, seemed that was an appropriate thing to
CMP: You know, Hank, you wouldn't think you could lose something in only 12 feet. Right now, I've probably got more things lost than I've got found.
CMP: Somewhere, I lost the ring sight that goes on the TV camera and the Hasselblad. And it's probably wherever I put it. (Laughter) But, unfortunately, I Just don't happen to know where that is. I guess that's really the only piece of operating equipment that I've misplaced. Well, that's pretty good, considering the shambles that this place generally stays in.
CMP: It's really puzzling. I've been sitting here - one of the reasons I'm not saying an awful lot is I'm trying to get some kind of an idea in my head as to how you describe the differences between the front and the back materials. And that's really hard. Because every time you look for a - an objective thing, you really kind of find that there's a lot of similarities, when you get down to the details. It's not clear that the back side is - would be that much different from the front if we put a few mares in there and a couple of - of the big rilles.
CMP: One of the things that I noticed about - most of the craters on the back side, the larger ones - even the ones with the steep interiors - do not have any kind of a - a block ejecta around the outsides. You know. I shouldn't say none, but it's very seldom - You have to stop and look for each block. But there are a few craters like - Chaplygin, and - a couple like that that - in fact, have large blocks around the outside. King is another one that has - The outer flanks of King look very much like the central feature in the interior.
CMP: And I got North and South Ray again and -
CC: John and Charlie are at station 5 now, Ken.
CMP: Okay. I guess I really can't say I see them.
CC: They're packing up to move on down to station 6 now.
CMP: Okay. I can see one, two, three distinct layers and it looks like several stre_m_ of material that go from the interior of South Ray over to - One of them points out, goes in South Ray and over the lip and down the outside. And it points over to- wards Baby Ray. And I'm trying to look at the material - All those things we said we could see, all those lineaments and things that we looked at back in the furrow of Descartes Just don't show, Hank.
CMP: And I'm looking down into the floor of Dollond T, and it looks like Dollond T has two different units: one that kind of floods in from the west - looks like it sort of fills the floor there. All that stuff that we talked about and all those things we looked at on the plotter are apparently below the resolution of what I can see with these binocu- lars. And, in general, as the Sun comes up, my first impression at the lower Sun was that the ma- terial to the - of Stone and Smoky were the s_e and that the Descartes furrowed material was also part of the same thing. As the Sun angle comes up, it starts to change its character a little bit, and it's looking more like the plotter photos.
CC: Roger. It sure seems that the Sun angle really affects what - what you're able to see. And - I guess you're about ready to look at Alphonsus. Is that correct?
CMP: Okay. We're just coming up on Albategnius and Klein now. Boy, I wish we could get a couple more of those - forward oblique photo passes. That was the one time when the windows were really pointing in the direction you'd like to have them. Other than that, you have a permanent crick in your neck.
CMP: I've looked at Alphonsus on quite a few of our revs; and, at the lower Suns, there was absolutely no - nothing I could say about dark halos around those little craters. Now, this time, I look at them, a_ld there's a very obvious dark halo. It looks exactly like the dark halos you see around the two craters to the south of Theophilus. I've looked for some topographic or - or surface fea- ture that might he different between the northern and southern halves of Alphonsus, and I've had absolutely no luck at all with that. I see now one, two, three distinct, dark halo areas and probably a fourth one. The rim of Alphonsus and the rim of Ptolemaeus are inseparable - where I am right now. I haven't quite gotten to it yet. The long, north-south trending lineament that runs through Alphonsus looks Just like the photographs. It does indeed run up there, and it runs through the wall, and looks like it's an extension of the little crater chain that runs through Ptolemaeus. Halley fill in the floor of Ptolemaeus looks just like it does in Alphonsus. I don't see any - any really significant difference. The only thing I can say about the dark halo areas in Alphonsus - is that - Well, I can't get the binoculars on them because I can't get close enough to the window.
CMP: If you remember that one we looked at the blowups of, I'm looking at that now, and - Yeah, there's a slight albedo difference or a darkening of the material around the - It doesn't look any different than any other crater down there. It's filled in on the western flank. It has a slightly raised rim around the eastern side. It's very subtle. It looks very subdued. It looks just like all the rest of the craters that you see all over the rest of the Moon. Nothing significant about it - except in its setting. I really don't see any relation- ship between Davy and Davy's chain with any other feature that shows in either Ptolemaeus or the sur- roundings. The main token - I can't even get over far enough to take a good look at - at Alpetragius. ... is Just about out of the field of view. And one thing I am gonna try to take a look at, and I don't know if we have enough Sun yet, and I'm gonna use these light level - red and blue filters, and take a look at Lassell C. And see whether or not there's any enhancement that's comparable to what we've seen with the photographs with the red and .... blue filters.
CMP: And just looking at these things directly through the filters, you don't - you don't see anything there at all. I didn't really think you would, but I thought it was an interesting thing to try.
CMP: And I can see a lot of the - that little crater that's out to the west of Lassell C, the one that looks like it has a little cone ***, is very obvious now that the Sun's come up higher; and it's - it does look a little different, but there's so many of these little craters and little mountain things that stick up through the floor of the mare that it's not real obvious that that's anything out of the ordinary.
CC: Can you see the little bright ray there?
CC: There should be a little bright ray, I think. Isn't it? Near the suspected dark cone?
CMP: I didn't see any bright ray around it. No sir.
CMP: And you can see all the Fra Mauro area now. And Rima Parry system stands out, and you can see Parry and Bonpland. And most of the highlands material that's over to the east of - of Fra Mauro itself all has the same appearance as though it's - belongs to the same pattern.
CC: You ought to be approaching the terminator now. Is that right?
CMP: And I have been rather impressed with the fact that, in most of these little ... or rilles, in the iow Sun, it appears to me that the - - 96/1 Tape
LMP-EVA: Hey, here's a crater here, John, that's about 10 meters, that - fairly blocky rim, angular. Want to stop here? It's a secondary on this side.
CDR-EVA: Yeah. What do you think?
LMP-EVA: Tony, it's a secondary. We're at 357 at 3.1, and we got a secondary that's fairly blocky rim. There's one up Just to the up - a little upslope from us that might be better. But there's not as mnny blocks on the rim. Same size crater.
CC: Okay; we'd like some more blocky ones.
LMP-EVA: Okay, I think it's a secondary.
CC: Right, but it might - -
LMP-EVA: Okay, you can park a 180 here, John.
CC: - - have punched through.
CDR-EVA: Okay, but - I can't park 180. If I park 180, we'11 be downslope from it.
LMP-EVA: No, the crater's over to the left.
CDR-EVA: I know where the crater is.
LMP-EVA: Why, don't you Just park north? I can point that antenna north.
LMP-EVA: You ought to get over here to the right a little bit so the TV won't be looking into the Sun. Okay, this is good; yeah.
CDR-EVA: Now I'11 just swing around and point it north. How will that be? There.
LMP-EVA: That's great.
LMP-EVA: Okay, Tony; 180, 357, 6.7, 3.1, 100, 95; amps 0, 0 - maybe - well, maybe 2 amps each. Bats are 95 and 110; off-scale low, off-scale low, and off- scale low, off-scale low. Over.
CC: Okay; we copy that, and verify DAC off.
LMP-EVA: Soon as I get out.
CC: Okay, and we'11 also need EMU checks here.
LMP-EVA: Okay, I don't have any flags; I can't see my quant ity.
CDR-EVA: You got about 65 percent.
LMP-EVA: Sixty-five percent and - my pressure's good, and I'm Just - I haven't changed my cooling.
LMP-EVA: _.
CDR-EVA: Okay. Now this is harder ...
CDR-EVA: Boy, Charlie.
CDR-EVA: This is ... hard ... - -
LMP-EVA: It's a lot harder.
CDR-EVA: Yeah, I didn't - we didn't sink near - Of course, we're not standing on the rim of a crater. - But this is harder, because we're Just sort of bouncing here.
LMP-EVA: Yeah, it's a lot more - Tony, the regolith charac- ter - as John said, it's really changed.
CDR-EVA: Okay, let me get the -
LMP-EVA: When we walk, we don't bounce as much - I mean, we don't sink in as much.
CDR-EVA: *** at 2.
CDR-EVA: ... - Charlie -
CC: Okay; we've got a picture.
CDR-EVA: Roger. And you hardly got any dust on you, but I'm going to do you a favor and dust you off.
CDR-EVA: What you doing there, Charlie?
LMP-EVA: *** what this rock's made out of. I'm trying to get a fresh surface.
CDR-EVA: I wouldn't do that. It's not worth doing.
CDR-EVA: *** help you there. That okay?
CC: Ah, thank you much there, John.
CDR-EVA: Man, that is some rock.
LMP-EVA: That matrix there's pure white, John, with black pheno - phenocryst in it. It might be clast. It might be a breccia. And it's got some lathlike crystals in it.
LMP-EVA: That's the one I'm talking about. See, I Just broke that open.
CDR-EVA: Yeah, that's a two-rock breccia. Let me get a bigger piece of it, Charlie.
LMP-EVA: I think - Okay, I don't know whe - You can't whack it off.
CDR-EVA: Too hard to whack?
LMP-EVA: Yeah, I've whacked about five times, as hard as I could.
CDR-EVA: Okay, Houston, it has a white matrix with square clasts and elongate clasts in it.
CDR-EVA: That - that might be - and it's round - and it's rounded, too.
CC: Very good, and we understand it's a two-rock breccia.
LMP-EVA: Looks like some more of them right down here, John, that are -that are sample - -
LMP-EVA: - - that are sample size.
CDR-EVA: Okay, let's get some of those.
LMP-EVA: We only got 20 minutes here. I'11 start the pan.
CC: And, John, we'11 need an EMU check.
CDR-EVA: Okay. I'm reading 385, and - no flags.
CDR-EVA: Every time I read my oxygen gage I, get a - (laughter) get an earful of orange Juice.
LMP-EVA: Yeah, mine, too.
CDR-EVA: Fifty-eight percent, and I'm on - between INTER- MEDIATE and MINIMUM cooling.
LMP-EVA: Okay, pan's complete, Tony.
CC: Very good. Page ll31
LMP-EVA: *#* break - grab the gnomon, John, and we - H °w about a set of tongs and a shovel? That ought to be good.
CDR-EVA: Think that ought to work?
CDR-EVA: Okay, that'11 probably save us some energy.
LMP-EVA: Yep; think we might need it. Guess what?
LMP-EVA: Look at that. #** the wheels.
LMP-EVA: Yeah. That's the gnomon stick. See the legs?
LMP-EVA: They're still in the bag.
CDR-EVA: Houston, you got any recommendations there?
CC: Yeah, I think you ought to just use - your scoop or something for a gnomon.
CDR-EVA: See what happened?
CC: No. We can't see it now - -
LMP-EVA: Pulled it right out of there.
CC: - - but I understand exactly what you mean.
CDR-EVA: You blew it.
LMP-EVA: Okay, I got the wand, and the legs stayed in the bag. Okay, give me a shovel, John. We can use the scoop.
CDR-EVA: Okay; well, we can use the shovel if - Where - where do you want to go?
LMP-EVA: I don't care. Anywhere is fine. This looks like a - Here's a nice little cracked one right there.
CDR-EVA: Yup.
LMP-EVA: These are angular - there's some angular and rounded rocks right there.
CC: Just pick anything in the picture for scale. - -
CC: All we'11 lose is the vertical.
LMP-EVA: Okay. You can stick the tongs in there, John.
LMP-EVA: It'11 go in the ground. I tried that a minute ago. It worked great. I don't see why I'm doing a down-Sun - hut I'11 do it.
LMP-EVA: Hey, Tony, can you get a locator from the TV on this sample?
CC: I sure can. We've got it now.
LMP-EVA: Just pan by it. Okay; thank you.
CDR-EVA: Excuse me.
CDR-EVA: Okay, that's going in bag 407. It was some soil and some dirt, a rounded rock - But wait a minute, Charlie, let me get a - of that.
CDR-EVA: Let'a grab this angular one next.
LMP-EVA: All right. 96/7 Tape
CDR-EVA: No, now- Wait. Charlie!
CDR-EVA: Let me get it with the tongs.
LMP-EVA: Leaning on that shovel is easy.
LMP-EVA: Might be the same kind, John, that you picked up on the way there.
LMP-EVA: #** won't - get the sack there.
CDR-EVA: Maybe you can.
LMP-EVA: This is - partially sacked. There we go. You got it.
CDR-EVA: Okay, that - Get the after. Got it. 408, Houston, is the bag number.
LMP-EVA: Now, I'11 swap you.
CDR-EVA: Why don't you get a soil sample? ... - -
LMP-EVA: Okay; that's a good idea.
CC: Okay, and you've got about 10 minutes left before we'11 have to leave.
LMP-EVA: Okay, maybe we could go to one more area. And so we won't salt it with it, this is just one broken- up block here.
CC: Good plan. Hey, you fellows are always thinking.
LMP-EVA: Well, we try to please. 338 is the soil sample.
LMP-EVA: That spinning up that bag really works great. See anything down under there, John?
CDR-EVA: No. This is the second - this is rim of it. It's very soft. I didn't have any trouble digging down with the shovel.
LMP-EVA: Solid gray all the way - -
CDR-EVA: Solid gray all the way down. I see no layering.
LMP-EVA: Let me put this in your bag.
LMP-EVA: John, how about on the upper rim there? This - -
CDR-EVA: Look at - -
LMP-EVA: This might have been a secondary.
CDR-EVA: Look at that right over there, Charlie.
LMP-EVA: It's a - It's a really a unique white-looking something-or-other.
CDR-EVA: Yeah. Let's see what that is.
LMP-EVA: I think it's soil.
CDR-EVA: Well, you want to get some of it? It's unusual soil, if it is.
LMP-EVA: It might have been Just a little - yeah, it looks like a little teeny impact, doesn't it?
LMP-EVA: Hey, let's get a quick one and then go on up here and get some of these blocks on the upper rim.
CDR-EVA: Okay. Okay, there's f/11 at - okay. It's a down- Sun. Turn around and get a locator.
CDR-EVA: Boy, this - this 1/6 gravity is so neat!