Otrobonita/noicy-space-talks huggingface dataset:
CC: Roger, Jim. And you might want to start the DAC.
LMP-EVA: Bearing 345; range - Yes, I'm glad you reminded me.
UNKNOWN: Remind me to stop it when we get there. Boy, you know, looking upslope, look how much more huw_ocky it is. It's Just a different - different terrain.
CDR-EVA: It sure is. It sure is. Pretty h,,mmoeky and driving is much sportier.
CDR-EVA: Oh - Hang on. Hang on, there we go. This Rover is super.
CC: A little mercy there.
CDR-EVA: Best tractor I ever drove.
UNKNOWN: Do we stay above it?
CDR-EVA: Yes. (Laughter) Oh, yes.
LMP-EVA: I hope you stay above it.
CDR-EVA: Yes, wait a minute. (Laughter) What do you think we ought to do here, Jim?
CDR-EVA: Whoa, that a boy. 94/19 Tape
LMP-EVA: I wish I could lean up, too.
CDR-EVA: Okay; Rover's stopped.
UNKNOWN: Okay; it looks like - from this position - I'd say that's probably Spur down there, the large one, Dave.
CDR-EVA: Oh, yes. Definitely.
LMP-EVA: Where you got blocks in - -
CC: Beautiful, Jim. Try to get a lock on that beauty - -
LMP-EVA: There's a real fresh one Just down-Sun from here.
CC: - - and maybe some other landmarks around it so we can drive down to it.
LMP-EVA: 0h, no problem there - -
CDR-EVA: No problem there. We - -
CDR-EVA: - - We'11 get to Spur for you, no problem.
LMP-EVA: Get the read-outs.
CDR-EVA: Yes. Be careful you don't fall down getting out.
LMP-EVA: - - 100, 80, 90, and motor temps are lower limit.
CC: Okay, Jim. Copied. And proceed carefully now.
CDR-EVA: *** you ought to take that tool off of there. It's Just hanging you up everytime you turn around.
LMP-EVA: I haven't had it on at all this morning, Dave.
CDR-EVA: Really? You haven't hung up on it?
LMP-EVA: I haven't had it on.
CDR-EVA: No, the tool on the side of the Rover.
LMP-EVA: Oh, I see.
CDR-EVA: Your feet keep hanging up.
LMP-EVA: Man, is this a steep slope.
CDR-EVA: It sure is, isn't it? Joe, for lack of good antenna pointing, I'm going to bypass the TV this time.
CC: Okay, Dave. Whatever you say.
CDR-EVA: Going back PM1/W- Yes, PM1/WB.
CC: And, Dave, we're assuming that you can't get around to the right position - -
CDR-EVA: The slope is - -
CC: - - beside the Rover to point that antenna adequately.
CDR-EVA: Yes, that's right, Joe. And the slope is real steep. And - like I'd mentioned before, the sight- ing device doesn't transmit eno-gh light to really make it very easy to find the Earth. It could take me a couple of minutes there to be - Just to find you, and I think you've seen the same thing. But if you would like, I'11 give it a try.
CC: Negative, Dave. We agree with you exactly. We're in good shape. Just proceed carefully on the - the - --_ the soft powder.
CDR-EVA: Yes, we're going to do that because it really is. But you can't say that we didn't sample the Apennine Front.
CC: Jim, did you turn the DAC off yet?
CC: Okay; good thinking.
LMP-EVA: It's off, and I'm reading a half a MAG.
CDR-EVA: Okay; let's attack that boulder. You got your h_m_er?
LMP-EVA: Put it back on, I do. Got to be a bear to get back up there, you know.
CC: Hey, troops, I'm not sure you should go downslope very far, if at all, from the Rover.
CDR-EVA: No, it's not Car. Let me try it, Jim, you Just stay there.
LMP-EVA: I think we can sidestep back up.
CDR-EVA: It's not that hard.
CC: Well, but make sure you check it now; Just proceed carefully.
CDR-EVA: Okay; I'm halfway, and I'11 go back first. Why don't you stay there, Jim?
LMP-EVA: Okay. Come back up.
CDR-EVA: The Rover makes it feel so easy.
LMP-EVA: I know it. Should have parked right beside it.
CDR-EVA: Think I will.
LMP-EVA: If you will, I'11 - I'11 walk down, Dave. Want me to carry some of those tools?
CDR-EVA: I can carry them easier.
CC: Okay, Dave. How's the footing?
CDR-EVA: I think I'11 - The footing is _ll right, except that you have to work pretty hard - to get back up, so - I think what I'm going to do - -
CC: Jim, are still up near the Rover?
CDR-EVA: - - as Jim walks down - Wait a minute until I get there, Jim.
CC: Jim, let's - -
CDR-EVA: Hold on, Jim. Wait a minute, Jim. Don't go yet. Let me drive the Rover down there.
CC: - - Ask you to walk around to the front there, and Just take a general rough guess as to where the Earth is. You don't even have to use the sighting device. Point it about correctly, and we're going to give the TV a try.
CDR-EVA: Oh, Joe. I can see where the Earth is in general. We're going to make a change here. I'm going to drive down. If I get Successfully down there, then Jim can w,lw down. So we don't have to expend all the energy.
LMP-EVA: And there's a beautiful little rock track here in - it went in a circular arc.
CDR-EVA: Really_
LMP-EVA: Yes. It rolled into the hill. It's amazing.
CDR-EVA: Well, photograph it.
LMP-EVA: Yes, I am. Instead of going straight down the hill, it curved into the hill.
CDR-EVA: That right?
LMP-EVA: Yes. A little angular fragment, Joe, about 2 inches long.
LMP-EVA: Came down slope - -
CC: Fantastic. -
LMP-EVA: - - curved into the hill and stopped. 94/23 Tape
CC: And, Dave, are you driving now?
LMP-EVA: Meantime, I'11 be taking a pan from here, Dave.
CDR-EVA: Yes, good idea.
CC: Good idea, Jim.
LMP-EVA: Looks like it's going to be our high point.
CDR-EVA: It's the high point.
CDR-EVA: Hey, Jim. Could you watch me as I back up here?
LMP-EVA: Sure can.
CDR-EVA: Got your eye on me?
LMP-EVA: I have my eye on you.
CDR-EVA: Okay. I'm going to back up gently here.
LMP-EVA: I think I'm going to - move downslope a little bit.
CDR-EVA: ... you watching me?
CDR-EVA: ... you know?
LMP-EVA: ... - is that right?
LMP-EVA: I wouldn't know, but I would think you'd be better off with that ... uphill.
CDR-EVA: Yes, I am - until I back it up.
LMP-EVA: I'm going to finish my pan.
CC: Roger, Jim and Dave. Proceed very carefully now, please.
CDR-EVA: Oh, we are. We're doing it really cool.
CC: Super cool.
CDR-EVA: Super cool.
CDR-EVA: How am I doing, Jim_
LMP-EVA: Doing okay. Want me to come over there and get on?
CDR-EVA: No - no. Stay there.
LMP-EVA: That pan's complete, Joe. -_
CC: Roger, Jim. Copy that. And, understand you're proceeding down towards that large block now.
CDR-EVA: Very gently. And I'11 even put - put the old girl downhill here, Jim.
LMP-EVA: ... be rough.
UNKNOWN: Oh, I wish I had the bigger camera to take a picture of the Rover moving along there.
CC: And, Dave and Jim. When you stop, we'd like for you to Just take a rough guess with that antenna. Give us the right switch setting, and we're going to give it a try with our big dish down here.
CDR-EVA: Okay. Stand by. Too far from the rocks.
UNKNOWN: Okay; let's try ...
CDR-EVA: Okay, Jim, you can come on down now.
LMP-EVA: Yes. I estimated a what - 20-degree slope?
LMP-EVA: 15 or 20? 94/25 Tape
CDR-EVA: Closer to 15, probably.
LMP-EVA: Don't - Here .... The Rover looks like - Although, see the back wheel's off the ground.
CDR-EVA: Yes. I think I'11 get back on.
CDR-EVA: Tell you what, Jim. We'd better abandon this one.
LMP-EVA: Afraid we might - -
CDR-EVA: Here, come on down.
LMP-EVA: - - ... Rover.
CDR-EVA: Here, you come down and get on.
LMP-EVA: Okay. Well, let me take a picture here anyway.
CDR-EVA: Yes, take a picture.
LMP-EVA: Are you really - let me hold that Rover and you come up and look at this, because this rock has got green in it, a light green - -
UNKNOWN: - - color. Come on.
CDR-EVA: Okay; I'11 Just stand here until you're through - -
CDR-EVA: - - and then I'11 go up and take a look at it.
LMP-EVA: The first green rock I've seen - light green.
CC: Roger. We're copying all of it.
LMP-EVA: Okay. Where do you want me to hold it?
CDR-EVA: I'11 Just come down and stand on your side.
UNKNOWN: On my side?
CDR-EVA: You stand there and take a break.
LMP-EVA: I'm taking one.
CDR-EVA: Okay. Are you firmly situated there?
CDR: Dave and Jim, use your best Judgment here, the block's not all that important, and we'd like you to spend most of the remaining time at Spur Crater. The remaining Front time, that is.
CDR-EVA: Roger, Joe. We sure will. -_
CC: And talk to us if we can give you any help here.
CDR-EVA: No, we're okay. It's Just that this slope's pretty steep, and I Just cannot take too much time - here.
CC: Yes, sir. We're hearing you.
CDR-EVA: It's a big breccia - that's all it is.
CDR-EVA: I - I don't see anything, Jim.
LMP-EVA: About halfway up, maybe you have to look down-Sun to see it. It looks like a light green layer, not necessarily a thick layer. Light green.
CDR-EVA: You mean on the surface? _
LMP-EVA: Yes, on the surface.
CDR-EVA: Hey, you're right.
CC: Can you photograph it, Jim?
LMP-EVA: I took - I took a couple. Easy, Dave.
CDR-EVA: Yes. Okay. 94/27 Tape
CDR-EVA: Did you take it down-Sun?
LMP-EVA: Yes, I took two down-sun at 7 feet.
CDR-EVA: Okay. Take a couple of cross-Sun's here.
UNKNOWN: Be great if we'd get some of that - green - -
LMP-EVA: - - that green material.
CDR-EVA: I'11 get it. I think I can get it with my tongs all right.
LMP-EVA: Gee, that's great.
CDR-EVA: It seems to be a - surface material or else it's a very frangible clast in this big piece of breccia. Dig m_ tongs into it.
LMP-EVA: Sure it's green and not Just white albedo again?
CDR-EVA: No, it's green.
LMP-EVA: It looks green. And I - I noticed Just downslope from the rock, you kicked up the surface and there's some more green there.
CDR-EVA: Getting a little.
LMP-EVA: This rock is - about 3 meters long.
CDR-EVA: Why don't you describe the thing, Jim, while I'm down - -
LMP-EVA: Subangular - very rough-textured surface. And the surface that's facing northwest - is the dark, typical breccia. And it looks like - what appeared to me - like there's a layer - there that might be a foot and a half, 2 feet thick, appears the - a light greenish color. Dave's sampling right now.
CC: Roger, Jim. Copy you loud and clear. Superb.
LMP-EVA: And on the side to the southeast is again the breccia. Isn't that right, Dave?
CDR-EVA: Yes. And I got a little frag. Don't drop it. There. And I got some green, and I got a frag out of the breccia.
CDR-EVA: It's fairly loose - breccia, as breccias go. Oh, and there's a great big white clast on the inside, but - man, like an inch or so.
LMP-EVA: If you want I'11 - -
CDR-EVA: No, no, I'11 get it.
CDR-EVA: Stand there, let me work.
CDR-EVA: *** does it.
CDR-EVA: 168, Joe. Got a little bit of the green, and I got a chunk about 3 inches of the rock itself.
CC: Roger, Davy. Copy.
CDR-EVA: And I think we'11 call it quits on that one.
CC: Sounds good, Dave. We're interested in moving towards Spur- -
LMP-EVA: It's going to take us awhile.
CC: - - but carefully.
CDR-EVA: Yes. But carefully. Okay, Jim. Just stand right there and let me ease on down.
LMP-EVA: Yes. It's going to take us a while to work down- slope.
LMP-EVA: I think it'11 probably be best for you to get on first.
CDR-EVA: Put this where I won't lose it.
LMP-EVA: Hand it to me, I'11 put it under my seat.
CDR-EVA: I can put it under mine. It won't go anywhere. Trouble is, if I get on first, I'm not sure you're going to have a seatbelt.
LMP-EVA: Well, I don't know that I want to - drop it. I can hold on. We're not going to go that fast here.
CDR-EVA: That's - that's for sure. Okay.
CDR-EVA: Okay, I'm on.
LMP-EVA: Did you get the other strap in? Here, let me strap you in. Dave?
CDR-EVA: Just a minute. Let me get settled down here first.
CDR-EVA: Tell you what might be better, Jim. Let me ease on down the hill here to a flatter spot for you to get on. Okay?
LMP-EVA: Okay; yes. No sweat.
CDR-EVA: You see right at i o'clock there, it levels out in that little depressions.
LMP-EVA: Right down here? Okay.
CDR-EVA: Okay. Look, why don't you - move back there and let me ease the thing down. Move away from it, so I won't hit you.
LMP-EVA: Yes, let me back off.
CDR-EVA: Okay. Back off good.
LMP-EVA: Yes. In fact, I'd Just as soon meet you down where it 's level.
LMP-EVA: If you want, I'11 meet you at Spur. for you to get on.
LMP-EVA: Just so you - you stay uphill.
CDR-EVA: The uphill side.
CDR-EVA: There. That's a nice spot, right there.
CDR-EVA: Why don't you - grab your seatbelt and let me hold it for you, and maybe you can give it a try.
UNKNOWN: No, I'11 - I'11 Just toss this thing on, Dave.
CDR-EVA: Easy, easy. Okay. Okay?
LMP-EVA: All righty.
CDR-EVA: Okay. Okay, Joe. We're mov - moving now.
CC: Okay, Dave. And, Jim, if you can easily turn the camera on, might be a good place.
LMP-EVA: No chance right now, Joe.
CDR-EVA: Not now, Joe, let us ease our way down.
CDR-EVA: Okay, Jim?
CDR-EVA: I'11 take a little right turn here. Okay. Came up all right; should be able to go down all right.
LMP-EVA: Going down's a little more tricky.
CDR-EVA: Yes, we can - get a little a - couple of Christie's here and there.
LMP-EVA: Over Christie's, heading right for Spur, Joe.
CDR-EVA: Not bad, is it? Jog here.
CC: And, Dave, give us a call as you come up toward Spur - -
CDR-EVA: We're -.]most to Split now.
CC: - - we've got some parking instructions.
CDR-EVA: Parking instructions. Okay. Let's see, do we want to hit the upper rim or the lower rim of Spur?
LMP-EVA: You see that large block on the - -
LMP-EVA: - - the northern rim.
CDR-EVA: Yes, I think we should work down to the northern rim, right?
LMP-EVA: Yes, if we're going to sam - sample any blocks there on the rim, that'd be the place to do it.
CC: Sounds good to us. And, Dave, we'd like for you to - to park east of the area you're going to be working in, so - so we can look down-Sun. And park facing west, and we'11 give you a NAV update later.
CDR-EVA: Okay. We're in good shape, Joe. That one wall there has quite a bit of debris, doesn't it?
LMP-EVA: Yes, and it looks like it's - again has a linear pattern running north and south.
CDR-EVA: A]most does. exposed
LMP-EVA: We're talking about the debris that's on the - the north wall - of Spur. And the slope here at Spur is - oh, 8 to lO degrees.
CDR-EVA: Okay; I'm parking east on a level slope here ....
CDR-EVA: RiF_ht down by all the (laughter) ... crater. Be a nice place to park.
LMP-EVA: Yes, it looks good - good place. Take a - take a break here.
CDR-EVA: Yes. Yes, I think we're Just about level, right there.
CDR-EVA: Okay. Okay, Joe.
LMP-EVA: I'11 - I'11 give them a reading if you want, Dave.
CDR-EVA: Yes, Till get the TV on.
CDR-EVA: We're at Spur Crater, Joe.
UNKNOWN: I'11 give them the shadow device, too. Okay; the heading is 290, 349, 7.3, 4.7, 095, 100, 82, 90; motor temps are both lower limit.
CC: Copy, and standing by for the shadow.
LMP-EVA: And, the shadow is - it's 4 degrees left.
CDR-EVA: Let's get the other two.
LMP-EVA: You mean roll and pitch?
CDR-EVA: Yes, the pitch is about 3 degrees down, and the roll - -
LMP-EVA: You have to hold it in the damp position, I guess.
CDR-EVA: If I can get the - there, it's damping. The roll's 5 degrees, right.
CC: Roger; we copy. And it was at - -
CDR-EVA: And, Jim, why don't you get off here, first - -
LMP-EVA: Okay. - - first heading
CC: - - glance that that is still a good heading. We'11 be back with you.
CC: And, Dave and Jim- -
LMP-EVA: I'm off and I'm going to take a pan.
CC: - - Okay; sounds good.
LMP-EVA: Okay, I'm with the TV.
CC: And we - we're looking at about 30 minutes working time here at this station.
CDR-EVA: Oh, good. Okay, Joe. We're going to FM TV now.
CDR-EVA: And I'11 give you general pointing, and you can try your - your big dish.
CC: Okay, Dave. Try -t?y to use the sight on this one and Just make sure that the filter is flipped up sun out of the way, please. The filter.
CDR-EVA: Oh!
CC: Dave, we had the picture momentarily. We've lost Are it now. you still fighting the antenna?
CDR-EVA: Yes. You got it now?
LMP-EVA: We picked up some more green material here, Dave.
CDR-EVA: Sure it isn't that light gray albedo stuff?
LMP-EVA: No, it looks green.
LMP-EVA: The contrast.
LMP-EVA: No, I see white; I see a light green; and I see a brown.
CDR-EVA: Stand where you are and give me alinement on the antenna, and see if I can get pointed at the Earth. You can turn to your right there - take about three steps right, and if you look up - don't fall back - Just look up - you'11 be able to aline the antenna in your position relative to the Earth. You'11 have to take your visor up probably. Do you see the Earth up there?
LMP-EVA: Can't get mY back ... fall over. - -
CC: - - Dave and Jim, you could look at the meter on the LCRU and peak up AGC while you move the antenna. Make sure, also, that the sun filter is up off the sighting device.
CDR-EVA: Joe, it has been ever since we started the shade down and everything else. And there's Just not that much - -
CDR-EVA: - - light ... really·
CC: Just checking.
CDR-EVA: Okay; try the AGC, then .... radar.
CC: Okay; that's good. Beautiful, beautiful. Right on the money.
UNKNOWN: can use that sound to lock in, Dave.
CDR-EVA: You know I did that, I didn't even look at that I Just used your AGC. All right.
UNKNOWN: also get the sound when you're locked on, too.
CDR-EVA: Okay, Jimmy. Let's go to work·
LMP-EVA: Roger. You don't think there's green here, huh?
CDR-EVA: No, Jim, I - I don't know. I think it's a gray. ·.. gray in the albedo. At least, that would be my guess.
LMP-EVA: Oh, it might be the EV visor that makes it look green. But, it's worth sampling. Notice that large rock on the northwest side, Just on the inner edge there·
LMP-EVA: Clearly a breccia. Look - look at the clasts; you can see the clasts from here.
CDR-EVA: You sure can .
UNKNOWN: And, it looks like it's a different color rock. Well, it's a dark -
CDR-EVA: Okay, let's go sample the rim over here.
CDR-EVA: Down-Sun - to your handy-dandy camera movement.
LMP-EVA: Houston, you should be pointing right at the LM.
CC: Roger, Jim. We're looking.
CDR-EVA: Okay, Jim. There's a good pile of rocks right here.
LMP-EVA: Hey, look at that light colored rock with - -
LMP-EVA: - - it almost looks like a white vein on top of the other rock.
CDR-EVA: Yes, look at that. How about that, We'11 get that one.
CC: Get it now.
LMP-EVA: It's a- -
CDR-EVA: Yes. It's a breccia. It's a dark - it's a dark gray rock that looks like a - actually it looks like a big pinnacle with a small gray and white breccia on top of it. The pinnacle is about 6 inches across and 4 or 5 inches high. On top of it is about a 2- to 3-inch subangular frag with a light gray,- or medium gray matrix, and about 20 percent white clast in it. Really unique. It stands out - (laughter) it's amazing. Okay, Jimmv. Let's gather some data. sample
LMP-EVA: You've got a there, right?
LMP-EVA: Okay. Oh, there are sparklies and all kinds of breccia .... the soil.
CDR-EVA: It's sort of caked on the top, though. Yes. Another black matrix%fine-grained with white clast - millimeter size - and there are some very fine grained little sparkles in there, though..
LMP-EVA: Okay. I even see some vesicles in it.
CDR-EVA: Yes. Look underneath there, Jim.
LMP-EVA: Yes. _--
CC: Just standing by for the nl_m]ner,Dave.
CDR-EVA: 194.
LMP-EVA: Yes. Let me get the other one that is sitting right next to it. Look how (cough) the upper layer of the soil here is caked.
CC: Standing by for the n,,mher, Jim. 94/37 Tape
CDR-EVA: No_ better yet, why don't you gather some soil? We gave it
LMP-EVA: 194 - -
CDR-EVA: - - Joe, we gave it to you but you blocked us.
CDR-EVA: We'11 get it to you. Yes. Let's get soil in this bag.
CDR-EVA: Right there by the rock.
CDR-EVA: Leave the rock whole.
CDR-EVA: Is that a glass - glass one, sitting right below it?
LMP-EVA: It sure looks like it. It was under itMwasn't it?
CDR-EVA: Yes. Yes. Let me take a picture. Just a minute, let me take a picture, and why don't you pick up that little piece of glass and put it in the bag, too.
CDR-EVA: That must have been under the rock.
CDR-EVA: Okay, I got the picture.
CDR-EVA: Pick up that little rock.
CDR-EVA: That a boy. Okay, let me get a picture. I think the next order of business is that neat one there.
LMP-EVA: Okay, well, there, too - Just to the west of you, Dave, is some of that - what we've been calling __-_... green material - clearly visible._ See what I mean?
CDR-EVA: Yes. That's Just a light - -
LMP-EVA: Okay. I'd call it light gray but, we'11 check it when we get home.
CDR-EVA: Well, it's definitely different from the next rock, or the one we Just picked up.
LMP-EVA: Yes. you mean - -
CDR-EVA: Well, look at this one right here.
LMP-EVA: That's what I'm talking about.
CDR-EVA: Okay. Sure is. That's awful big, but I think we ought to sample here anyway, all those little frags.
CDR-EVA: I've got to admlt it really looks green to me, too, Jim, but I can't believe it's green.
LMP-EVA: Oh, it's a good story - something about green cheese? (Laughter) Who would ever believe it.2
LMP-EVA: I hope it is green when we get it home.
LMP-EVA: Oh, my, it is green.
CDR-EVA: It is green.
LMP-EVA: I told you it was green.
CDR-EVA: You're right, ooh, fantastic - hey hold this! Wait a minute, I can't put this into the bag yet - -
LMP-EVA: Look at this. This has got be something ....
CDR-EVA: Man, that looks almost - now it's gray. The visor makes it green, Jim. (Laughter)
LMP-EVA: It's green.
CDR-EVA: A different shade of gray.
LMP-EVA: Yes, I know. I put my visor up, too.
CDR-EVA: But it's a very light grain, very fine grain, sure looks like a basalt with some very - less than millimeter-size vesicles in it, maybe 5 percent or so. It's a subangular rock. It's friable - I can - maybe it's not a basalt. It's friable - I can scrape it off with my glove and I put some streaks in it, in case anybody wonders what that is when we get back. But, it's definitely different from anything we've seen before. 195 - let me get another one here.
CC: Roger, 195. And, it sounds green to me.
CDR-EVA: With the visor on, Joe, I was about ready to call it a dunite, but I opened up my visor, and I was wrong. I didn't get to call it what I wanted to. Here's another one of the same stuff, Jim.
UNKNOWN: Okay, why don't - why don't you get a sample - let me take a picture, and you get a sample of the soil, okay. Why don't you _ust scoop in between them.
CDR-EVA: Yes. I think this is a big frag here, but, it broke - -
CDR-EVA: - - when it hit. All these pieces are roughly the s_e.
LMP-EVA: Yes. Not much soil here, really.
CDR-EVA: No, it really isn't.
CC: Dave and Jim, is it your impression that you are sampling on the eJecta blanket of Spur Crater, now?
CDR-EVA: Yes, sir; probably from the deepest part, because we're right on the rim.
LMP-EVA: Okay, 195.
CDR-EVA: Wouldn't you agree with that, Jim?
CDR-EVA: Okay. Now let's go down and get that unusual one. - get that unusual - one. There's a dense - and there's another unusual one; look at the little crater here, and the one that's facing us. There is a little white corner to the thing.
CC: Okay, Dave. Get as many of those as you can, and you might be watching for a place where you think the rake might help you.
CDR-EVA: Yes. I think we can probably do a rake here, Joe.
CC: Okay, sounds like a good place. - -
CDR-EVA: - - Okay, there's a big boulder over there down-Sun of us, that I'm sure you cmn see - there is a boulder down in front of us I'm sure you can see, Joe, which is gray. And it has some very outstanding gray clasts and white clasts, and oh, boy - it's a beaut! We're going to get ahold of that one in a minute.
LMP-EVA: Okay, I have mY pictures, Dave.
CDR-EVA: Okay, let's see. What do you think the best way to sample it would be?
LMP-EVA: I think probably - could we break off a piece of the clod underneath it? Or - or I guess you could probably lift that top fragment right off.
CDR-EVA: Yes. Let's - let me try. Yes. Sure can. And it's a - a white elast, and it's about - oh, boy!
LMP-EVA: Oh, man! I got -
CDR-EVA: Look at that.
LMP-EVA: Look at the - glint.
CDR-EVA: Aaah.
LMP-EVA: Almost see twinning in there. found.
LMP-EVA: I think we found what we came for.
CDR-EVA: Crystal rock, huh? Yes, sir. You better believe it.
CDR-EVA: Look at the plage in there.
CDR-EVA: _lmost all plage .... As a matter of fact - (laughter) Oh, boy, I think we might - ourselves something close to anorthocite, because its crys- talline, and there's Just a bunch - it's Just _L]most all plage. What a beaut.
UNKNOWN: That is really a beauty. And, I - there is sa - there 's another one down there.
CDR-EVA: Yes. We'11 get some of these.
CC: Bag it up.
CDR-EVA: Ah, ah. Beautiful. Hey, let me get some of that clod there. No, let's don't mix them- let's make this a special - one. I'11 zip it up.
LMP-EVA: Okay. 196,
CDR-EVA: Make this bag a special bag.
CDR-EVA: Our first one. Don't lose your bag now, Jim. (Laughter) Oh, boy. Okay, let's get some of the other - maybe - Let me take a picture first in here. I got it. No sweat. Now, we got to think of how to get that other piece there. Maybe if you could put your scoop in it, and break off a chip - do you think? Don't you?
CDR-EVA: I don't know. Try it. Put your scoop there in the middle and break off a chip.
LMP-EVA: It's not a clod, is it?
CDR-EVA: Yes. It is a clod.
LMP-EVA: Want to take this piece here?
CDR-EVA: Yes. Let me get you a bag. Wait. Let me take a picture first, so you know which one we got. Okay. Go ahead. Number 170.
CC: Roger. 170.
CDR-EVA: Okay. (Laughter)
CDR-EVA: Boy, that's a beautiful rock - -
CC: - - Are you working on the outside of the crater or are you - -
CDR-EVA: - - that other one. Gosh! Look at - -
CC: - - over the - the lip right now?
CDR-EVA: Oh, Just a tad over the lip on a little bench, but it 's -
LMP-EVA: Dave, could you hold that one?
LMP-EVA: I don't know whether it'11 fit in the bag or not. Got it ?
CDR-EVA: No. It dropped. See if you can pick it up again. I think it'11 fit in the bag, Joe - Jim.
LMP-EVA: A little frangible.
CDR-EVA: Yes. It really is. I think I can get it with the tongs. Here.
CDR-EVA: There's a contact sort of - on there. We ought to try and get the contact if we can. Okay, babe. Open the bag.
UNKNOWN: Okay, I got.
CDR-EVA: That a boy. Good show. Post-pick-up picture. Okay; roll that beauty up. Let's goget some more of that.
LMP-EVA: I think we ought to get over that big rock.
CDR-EVA: Yes. We're getting there.
LMP-EVA: Before we run out of time.
LMP-EVA: Because I think that big rock is probably more important.
CDR-EVA: It's a big breccia, though .... - -
CC: Dave, we think you might be about to run out of film.
CDR-EVA: - - this in the bag. That's right.
CC: - - maybe you better check that now.
CDR-EVA: All right, Joe. Jim, this one we got to pick up, and then we'11 go to the big rock. And if you could - put that in my bag - and then check my film. Joe, this crater is a gold mine.
CC: And there might be diamonds in the next one.
CDR-EVA: Yes, babe.
LMP-EVA: Okay ... - -
CC: Jim, - -
LMP-EVA: - - Okay .... down here.
CC: - - Get a reading on Dave's camera for us, please.
LMP-EVA: Oh, he's got a lot left. He's only reading 145. Sounds
CC: Roger, good. good.
CDR-EVA: Got her, Jim?
CC: Dave and Jim. - -
CC: - - Did you fill a bag after 1707 If so, we missed the number, and we can probably sort it out later.
CDR-EVA: This one. No, we - I think that was the last one, Joe. We'11 rely on you to sort it out later.
CDR-EVA: Okay, I have - oh - look at this, Jim.
LMP-EVA: Ha, what a contact! _
CDR-EVA: Look, what a contactl
LMP-EVA: Yes, man!
CDR-EVA: I've got - Man, oh m_u. I got about a 4 incher, Joe. It's subrounded, and on one half of it, we have a very dark, black, fine-grained basalt with some - it looks like some very thin laths in it And, of plage - nothing else. in one region, there is some millimeter-type vesicles along a linear pattern very close to the contact. And, the other side of the contact, we have a pure, solid-white, fine-grained frag, which looks not unlike the white clasts in the 14 rock. But it's a beautiful contact in here. And, we'11 call this one bag number - -
LMP-EVA: 198.
CDR-EVA: 198.
CC: Roger. Copy 198. And, Jim, you may have dropped your sample bags.
LMP-EVA: Yes. I dropped one.
CDR-EVA: He dropped one, Joe, thank you.
LMP-EVA: (Laughter) I don't know what we would do without you, Joe.
CDR-EVA: Hey, isn't that super? Get the picture.
LMP-EVA: Yes, I got the picture.
CDR-EVA: Don't fall down. Okay. We'11 ease over to that big rock. Looking on the way for anything else unusual.
CDR-EVA: It's another clod that evidently hit. Let's sam- ple it Just to get the - distribution around the circumference of the rim here. Okay. You want to put that bag in my pocket?
LMP-EVA: Yes, I will as soon as I zip it.
LMP-EVA: Okay. It's in there.
CDR-EVA: Okay, got enough fingers left to get me another one?
LMP-EVA: Yes. What would you like? The -
CDR-EVA: Bag.
LMP-EVA: Oh, yes, the bag. I was going to - I was wonder- ing why you wanted to use the scoop.
CDR-EVA: Don't think we can get a scoop on this one. I think it's going to - Oh, look at this one (laughter).
LMP-EVA: Diamonds, huh?
CDR-EVA: Don't move out of that - your shadow. No. I got a big - is that glass, or is that basalt? Look at that frag there. Let me take a picture from where - it came from under that rock.
UNKNOWN: Think so?
CDR-EVA: Yes. It looks like a big piece of glass. It's got some bubbles in it. Oh, look at that. Isn't that pretty?
UNKNOWN: That's a glass-coated breccia.
CDR-EVA: Yes, but look at the glass.
CDR-EVA: It's shiny. 199.
CDR-EVA: Let me get some more of this, Jim.
CDR-EVA: Here's - Well - Okay. There's another piece of the frag that it went with.
CC: Dave and Jim - -
CC: - - we're very pleased with your documented samples here. We think you ought to give some thought pretty shortly now, to getting us a - a rake sam- ple, if you can find a good area. And then we' re going to go for some bulk collection - just a lot of soil filling sample or collection bag 6.
UNKNOWN: It seems a shame. We got to go over and sample that big one there.
CDR-EVA: Yes. We'11 do that. Throw it in.
CC: And, Dave, you're going to want to cinch up Jim's ___ collection bag - -
CC: - - probably before you go much longer. It's coming very loose there.
CDR-EVA: Okay. Let me do it right now, Joe, Just - don't - so we don't forget it. 94/4'? Tape
CC: Roger. We sure don't want to lose that one.
LMP-EVA: Hey, you got something pretty good in there, don't you?
CDR-EVA: You turn a little right, Jimmy. I mean left, I'm sorry. It sure has come off. I don't know why.
CDR-EVA: Oh, yes, that getting in that Rover bit.
CDR-EVA: I can fix you here, partner.
CC: Okay, Dave, while you're working there we're thinking that we'd prefer Just a very quick sam- pling - of - of the large rock, if at all. And perhaps Just a quick photographic documentation of that large rock and then some rake sample.
CDR-EVA: Okay, Joe. Let me get Jim's bag - wait Jim, don't go anywhere yet.
CC: Dave and Jim, the science input now is that we want to forget that large block entirely. We want a- as large a collection of smaller frags as you can get us, and you'11 probably be working near the Rover for those.
CDR-EVA: Understand, Joe.
CC: And, we're coming up on about 10 to 15 minutes remaining here.
CDR-EVA: Okay. Okay, hang on partner. I think I got you - better. Okay, let me get your - unknot your scoop, over. Turn around.
CDR-EVA: Okay, why don't you go get the rake on.
CDR-EVA: I'11 get the gnomon. And while your're putting the rake on I'11 photograph this thing, anyway.
CDR-EVA: I think it looks very much like the 14 rocks.
CC: That a boy, Davy.
CDR-EVA: Though, it looks ma_vbe a little darker gray.
UNKNOWN: Okay, Dave. I'm set up whenever you are.
CDR-EVA: Okay; be right there.
CDR-EVA: There's a convenient piece broken off, right here.
CDR-EVA: Here I come.
LMP-EVA: Dave, how about over here?
CDR-EVA: Yes. Find a good spot.
LMP-EVA: Yes, and while I'm raking, there's a rock over there that has some - a linear pattern in it, that you might want to look at while I'm raking.
CDR-EVA: Okay, let me get the pictures of the place.
CC: And, Jim, how's your raking going? Are you pulling off any small frags?
CDR-EVA: Level ground is great.
LMP-EVA: Haven't started yet, Joe.
CDR-EVA: Got to document the area first here, Joe.
CC: Roger. We couldn't miss that.
CDR-EVA: How about right about here, huh? Why don't you - - --_
LMP-EVA: Yes, that's what I was thinking. That's good. You see that rock over at your - Just a little south of you?
CDR-EVA: Oh, I Just ran out of film.
CDR-EVA: Oh, myl Well, we can get that later. Let me change film MAGs while you rake, Jim.
CDR-EVA: And you'd better take the - -
LMP-EVA: Let me - I'm surprised you're running out all - already, though you must have taken a lot of pictures over there.
CC: And, either Dave or Jim - -
CDR-EVA: Joe, there was a - -
CC: - - when convenient - -
CDR-EVA: - - frag - -
CC: - - our TV camera's starting to warm up consider- ably. We'd like for you to clean off the camera top and the LCRU when convenient, please.
CDR-EVA: All right, Joe. And, mark bag 171 for a frag off of that big boulder. I'm pretty sure it was exposed right on the surface, fairly clean - right next to the boulder and looked like the same material.
CC: Okay, Al, in case you don't have your Flight Plan handy, we need to start a P20 plus X forward in a couple of minutes, and that will be followed by deploy of the g,w_, ray boom.
CMP: Roger; Karl, I'm with it.
CC: Al, are we in time to get a mark from you to when g,_ma you start the ray boom out?
CMP: Roger. I'm ready now. Gamma ray boom going out.
CMP: Now.
CC: Hey, time for exercise, Al.
CMP: Yes, I guess that's right, Karl.
CMP: MARK on the gamma ray boom.
CC: Al, you may be interested to know that the Rover boys are up on the slopes of Hadley Delta now. They got themselves up to - to an area where there angle is a considerable on the hillside, I'd guess 20 maybe -1most 30 degrees. And it's still very fine soil, which acts a lot like snow. And you should have saw Dave about 5 minutes ago; took a beautiful spill in it.
CMP: Tell them to be careful.
CC: Al, as you go around the corner, all your systems are looking good.
CC: See you on the other side.
CMP: Hello, Houston; Endeavour. Reading you loud and clear.
CC: Same here. How goes it up there?
CMP: Fine, Karl. And I got a couple of comments on Tsiolkovsky, in addition to what I said last rev. 9_/51 Tape
CC: Go ahead, we're ready to copy.
CMP: Okay, talk - discussing the - the flow in Crater Waterm_-n, south of Tsiolkovsky, I guess what I said before still applies. The - what looks like and on a map is the channel between Waterman Tsiolkovsky is, in fact, too high for anything to flow between the two. There's - there' s definitely some elevation there. However, looking at it this time, it's pretty plain that that channel - or gully, or whatever you call the breach in - in Tsiolkovsky's wall there between Waterman and Tsiolkovsky is caused by a graben-like fault system. There are two faults that run through there, and they run almost north and south right towards the central peaks, diverging - the one - the one on the west side, is slightly - is angled slightly to the northwest, but the other one goes flow in Waterman appears to be high in the - in the wall of Waterman, on the north edge, right where the fault zone crosses the - the rim of Waterman.
CMP: Okay, now there are a couple of other small - small craters around Tsiolkovsky. Particularly, one on the north side, on the northeast corner, the first large crater that you see there, has a very dis- tinctive lava flow or some kind of flow down - down in the crater. And that flow also originates up in the corner or up in the - in the high towards the rim of that particular crater, where there's some contact between the - the Tsiolkovsky rim and the rim of that small crater.
CMP: Now again, I saw no evidence of - of any kind of a rock slide to the south of Tsiolkovsky, but the one on the west there is, looks - you know every- time I go over it - it certainly confirms my opinion that that's a rock slide. The lineaments, the way the - the thing ended, the lobate - the and lobate tongues on it everything. It's inter- side there, is - different from - across that fault zone - is quite different from it is around the rest of the crater, maybe suggesting that that's -_ the source of the flow. The rim seems to be not as sharply defined; it's lower and appears to be out from the edge of the basin more than the rest of the - of the boundary or the rest of the eJecta pattern around Tsiolkovsky, and there where that very steep, almost smooth scarp is, on the west of Tsiolkovsky, seems to be the - the point at which it starts.
CC: Al, Vance here. You have any comments on the rim of the north, northwest side, where you, (cough) it appears the rim might have slipped or - or you have a - a fault which shows the displacement?
CMP: Oh, yes, Vance, very definitely. There are a couple of fault zones, through there, and you can - you can see the displacement quite clearly from the air. The one, the fault zone between Waterman and Tsiolkovsky, is a - is a lot more subtle, but I - but I'm quite sure that that's what's going on there. But the one on the west side is - is very clear. That 's - that 's true.
CC: Al, we'd like to have HIGH GAIN, AUTO.
CMP: And, Vance, another comment about that. You got HIGH GAIN, AUTO, by the way. Another comment about that, where that fault zone appears on the west side, there's much less mass wasting into the interbasin of Tsiolkovsky, than there is around the rest of the - of the crater. Most of that mass wasting seems to have taken place outside the crater.
CC: That's an interesting observation.
CC: Al, Vance and I called up to your apartment a little while ago. Your folks are there. And I guess, as you know, they've got a squawk box look - listening in. - -
CMP: - - oh, great.
CC: - - listening in on our loop with great interest. Except when you go behind the Moon, then they - then they watch the other show that's taking place on the surface. They said to say "Hello." And, they sound like they're having a good time up there.
CMP: Very good. Very good. Hello, folks.
CC: Al, in 30 seconds we're coming up to a pan camera operation MODE, STANDBY, POWER on.
CC: Al, while we're waiting for that pan camera off cue, I've got a couple of photo pads - a couple of Flight Plan updates here for you, if you can copy them.
CC: Okay. At 148 hours and 0 minutes, they would like to have you get some good shots on those lava flows you saw over in Imbrium. And the recom- mendations that we have are as follows: CM3, EL, 250-millimeter lens, CEX f5.6, 1/125th, infinity, five frames at 10-second intervals. Recommend convergent photos starting at TCA minus 30 seconds. The aim point is up to you. Magazine Q, and record frame number. And then on the same page, 148 hours and 18 minutes, we don't need to do that P52 there, because the platform looks very good.
CMP: Okay, Karl. Understand photos of the lava flows in Imbrium that we noticed on last rev. That'd be CM3/EL/250, CEX f5.6, 1125, infinity, five frames at 10 seconds, use magazine Q, and try and get convergent stereo starting at TCA minus 30.
CMP: And, also, delete the P52.
CMP: Karl, while we're going over Crisium here. Looking down at Picard at Peirce, and at Lick, I that's Lick Delta by the way, Lick Delta, Picard, and Peirce, all look like - they're - they're all about the same. They all have the same ring structure, all have the same low rims. The rims are - are - are what look like very shallow com- pared to the rims on the other craters I've seen around. And, also, they all have a slightly darker halo effect around the - the entire crater. But the - the color difference is very subtle.
CC: Roger, Al. As I look on the map here, they look like they might have been old craters flooded by the mare. Is that - does that seem feasible to you as you look at them?
CMP: No, it doesn't to me, Karl. They're a quite dif- ferent texture inside, and you can see the ring structure clear down to the bottom of the crater. So I would say that they were - they were - they were not flooded craters.
CC: Roger. Okay. _
CC: Hey, Al. Relevant to your observations coming up on Littrow here, Farouk has asked whether the comments that you made previously about Littrow, seeing a - a mauteling of dark material everywhere with a few puddles in the valleys, whether that same comment would - pertain to Sulpic, Sulpicia - yes - -
MCC: Sulpicius Gallus?
CC: - - Sulpicius Gallus. Or do you - -
CMP: - - yes, Okay. Sulpicius Gallus. Certainly, Karl.
CC: Right. Do they - do they look like very similar areas, or are there some contrasts there?
CMP: Okay. I'11 let you know when I get there. Unfor- tunately, I think I'm not - I think I'm going to be out of attitude to take a look at Sulpicius Gallus.
CC: Okay. That's for future reference then.
CMP: Yes, okay. But I'11 - if - if I can see across Serenitatis there, I'11 - I'11 give you a hack on that.
CC: Okay. I guess I should keep quiet awhile and let you look at Littrow coming up in about a minute.
CC: Al, we can have PAN CAMERA POWER, off, now.
CMP: Okay. PAN CAMERA POWER, off.
CMP: Okay. Karl, I can give you at least a partial answer on that question. The - the coloration that seems to be continuous from Littrow all the way around through Sulpicius Callus is the middle color. It's slightly darker than the rest of the mare basin itself and not quite as dark as some isolated or localized areas within the Littrow area. Now, those - those localized areas in the Littrow area were the areas in which I saw what ap- peared to be some ver - rather prominant distinc- tive cinder cones, with their own respective dark halo. And it seemed to be the same darkness as the rest of the material in local areas within the Lit- trow area. In other words, there are - there are three variations of color. There are three tones of color in the Littrow area. The darker tones are associated with - the - with the lowland areas, like the valleys and like - down on just at the edge of the mare surface. Then there's a lighter tone, which seems to be associated all the way around the - the - the ring or the rim of Serenitatis from Littrow all the way around through Sulpicius Callus. And I don't see any other colors around Sulpicius Callus, except that one. And they seem to encompass the area between the first wrinkle ridge and - and the contact between the mare basin and the front there. Sort of like between the Archuan Rilles and the first set of wrinkle ridges in the - in the Serenitatis Basin. And then -
CC: Roger. Wouldn't be at all surprised.
CDR-EVA: And I think I'11 brush off the camera for you, and I can brush off my camera before I change the film.
LMP-EVA: And, Joe, this looks like a pretty good place to rake. I've raked one swath here about 2 feet long and I've collected - oh, about 15 rocks.
CC: That's a Jackpot.
CDR-EVA: Put them in a big pile; I'11 be right over.
LMP-EVA: Oh, I don't know whether I want to do that, Dave.
CDR-EVA: Okay. Well, then, I'11 be right over.
CDR-EVA: I'11 Just do my film --
LMP-EVA: Though I think we can fill up the bag pretty fast, here.
CDR-EVA: Okay, then, you take the pictures and I'11 just change my film later.
LMP-EVA: Okay. I'11 --
CDR-EVA: Save - save the film changing here. Let me get you a bag.
CDR-EVA: Oh, yes. You did get a bunch. 172.
LMP-EVA: Okay. Got a little more swath.
CDR-EVA: Yes. It's about i meter long and one rake-width wide.
CDR-EVA: Yes. Good.
CDR-EVA: Glass on some. Most of them are rounded; right size.
CDR-EVA: Okay, do another one.
CDR-EVA: Oh, you're stepping on my tongs. That's all right. I'11 get them.
LMP-EVA: I can get them with the scoop here in a little bit.
CDR-EVA: Yes. Sure miss that yo-yo. Oh, good! That's three swaths 1 meter long apiece.
CDR-EVA: Damn bag isn't full yet. Let's shoot for a full bag. What do you say? Take it just a second to go one more sweep there.
LMP-EVA: Oh, my poor tong. Oh, I don't weigh that much up here, Dave, to break your tongs.
CDR-EVA: I don't know what I'd do without them.
LMP-EVA: So don't bury them.
CDR-EVA: Good, good, good. Shake anymore in the - Yes. That's too bad; we didn't get many out of that one. Why don't you take one over - Let me move the gnomon about B inches here, and take one on this side, Jim. Okay? Move the Gnomon back about a foot. Why don't you take a swath here and I'11 --
LMP-EVA: Yes, you know, because we're moving farther - a little farther from the rim --
LMP-EVA: -- You get less and less each swath.
LMP-EVA: This one ought to be a more fruitful one. Either that or my arm's getting tired. That's probably true, too.
CDR-EVA: How about a double core here, Joe? Got any ideas on that one?
CC: Dave, we're coming up on the departure time about 95/3 Tape 10 minutes from now. All we really need is soil from this same area. And we're making money hand over fist. Maybe a few walnut-sized rock% if there's some around.
CDR-EVA: We got - Okay, Joe.
LMP-EVA: A bagful.
UNKNOWN: We got a whole bagful of those in the comps. And that's in 172.
CC: Roger; copy 172. I guess all we need is a soil sample from this area and perhaps even larger rocks, if there's some grapefruit to football-size rocks there.
CDR-EVA: Yes. Yes, we'11 Just finish off Jim's collection hag here. I want to stow it anyway. Oh, look at that glass spherel - spherule down there. See that big one? I got to - Listen --
LMP-EVA: Oh, yes. I see it.
CDR-EVA: Why don't you back off and document the area. Let me get my tongs and pick that up.
CDR-EVA: Perfectly round, about - -
LMP-EVA: Yes. Here, let me help you.
CDR-EVA: Yes. Get the tongs.
CDR-EVA: Okay. Good, good.
LMP-EVA: Keep an eye on the spherule.
CDR-EVA: My toes are right on it. I got the tongs.
CDR-EVA: My little paw. So I'11 get you a bag; let you take a picture of that. I'11 get a bag; then you can get the soil.
LMP-EVA: Where you going to put that little spherule?
CDR-EVA: In the bag.
LMP-EVA: Not with the soil, though, are you?
CDR-EVA: Came out of the soil. I Just didn't want to miss it. We'11 remember that. That goes in bag num- ber 173, and, well, our friends in the back room are writing that down right now.
CC: How right you are. And we want to leave in about
CDR-EVA: Little fat ball.
CC: - - 5 minutes, and we still need the soil.
CDR-EVA: It's coming right now.
CC: Roger. We see it coming in.
CDR-EVA: Yes. Let's fill the bag.
UNKNOWN: Is that a full bag there?
CDR-EVA: Yes, sir. That's a full bag. That's a full bag.
LMP-EVA: I want to see you shake that one down.
CDR-EVA: All right. (Chuckle) Don't guess I will.
CDR-EVA: Okay. Better have a - 90-percent bag for sure. The - -
LMP-EVA: Don't pour your spherule out.
CDR-EVA: Okay; I think you need to reconfigure, and we'11 get ready to leave here.
LMP-EVA: Okay. I'11 go over and take this off, then.
CDR-EVA: Yes. Here, let me put this in your backpack. Stand there; that's good. I'11 get it.
CDR-EVA: I'm going to get a couple of big rocks, Jim. Then we'11 Just fill your bag and - call it a day - here.
CC: Sounds good, Dave. And we want to move in about 3 minutes. We're coming up against a hard stop here.
CDR-EVA: Okay; 3 minutes. Okay; that doesn't give us time to really do much then.
CC: Maybe one big rock wouldn't hurt.
CDR-EVA: Yes. Jim?
CDR-EVA: Why don't you come over here and get your scoop and scoop me up one big rock?
CC: And -
CDR-EVA: Now - and get your camera on it, because I don't - I don't have it - any film. How about this one right here that looks like it has some layering in it? Maybe.
LMP-EVA: Yes, that's the one I was talking about.
CDR-EVA: Right there?
CDR-EVA: Why don't you - -?
LMP-EVA: You want to point to it with the - -
CDR-EVA: Yes, I've got my foot right there. Why don't you take a couple of cross-Suns real quick?
CDR-EVA: Seven feet, cross-Sun? A little too far away, old
CDR-EVA: Okay. Now come grab your scoop and we'11 take it.
LMP-EVA: It's a pretty big one to try and get with a scoop.
CDR-EVA: Yes; you're right. I don't see anything else.
LMP-EVA: This little fracture.
CDR-EVA: Too big. Get another one.
LMP-EVA: Oh' Here, Dave.
CDR-EVA: Oh, sure.
LMP-EVA: Good boy.
CDR-EVA: Get that - that one on the - on your side.
CDR-EVA: Getting it. That a boy. There.
UNKNOWN: Should have left the rake on.
CDR-EVA: Yes. Can you get it? Good show.
LMP-EVA: Easy does it. Easy does it. That's it.
CDR-EVA: Up a little more. KeepY_ balance. Can you get it up higher?
CDR-EVA: Whup.' Don't fall backwards.
LMP-EVA: Yes. Man' I got it.
CDR-EVA: Good. Okay; fill that square. Okay, Jim. Let's get on the Rover and head back.
LMP-EVA: Okay, I haven't secured the rake there, yet.
CDR-EVA: Okay. You secure the rake, and I'11 secure the TV, and we '11 get moving. Page 847
CC: Sounds good, Dave and Jim. And we want to leave t
CDR-EVA: I wonder how I'm going to do this. camera
CC: - - the TV where it is right now. It's stowed in the proper position.
CDR-EVA: Okay. Oh, shoot.
LMP-EVA: Hardly room there, is there?
CDR-EVA: Don't have any room there is right. Any place we can put your bag on it? Isn't your -
LMP-EVA: Why don't you put that in one of those bags, Dave?