Otrobonita/noicy-space-talks huggingface dataset:
CMP: Yes. I was, too. I just happened to look out, and there it was.
CC: Just talked to E1 Lago a few minutes ago, Ron, and all the neighbors are out - are at your home around _he squawk box, listening. And Jan said to tell you that Jaime and Jon will be out here at - with us tomorrow. We're going to all - They're going to watch the burn from here - the LOPC and the trim burn.
CMP: Oh, hey, good deall Yes, I've got some real fine neighbors down there, I'11 tell you that.
CMP: You know, I look at that D-Caldera from a distance - I can still see it in the binocs - and I keep trying to look for some hint of a topographic expression, a topographic rise surrounding D-Caldera. And I can't see a hint of a shadow, difference in the color, or anything. It's Just flat out in the middle of a flat plain, and it's a D-shaped de- pression that's slumped down. There's no rise around the rims - or anything.
CC: Roger. Got you. Must be frustrating, because it's supposed to have some type of topographical ex- pression, huh?
CMP: Yes; right. You know, it's supposed to have some- thing. But it looks like it Just fell right out of the flat plain, you know. It took part of the - took part of the plain with it, because there are these bubble-looking things down in D-Caldera.
CMP: How many frames in the next Nikon mag do I have to diddle with?
CC: Okay, we're running that one through FAO here. Stand by a moment, Ron, on that.
CMP: For the ejecta pattern of Eratosthenes, you can just see it looking back into the Sun now, and the terminator is right - right in the middle of Eratosthenes now. And you can sure see the classic impact eJecta pattern around it. It goes out for - you know, _]most two crater diameters as we can see the topographic expression. You can see the scalloping or scouring as it's gone back across there, due to the shadows that are crea_ed in the low Sun angle. ll0B/11 Tape
CC: Ron, at your convenience, we would like H TANKS l, 2 2, and 3 FANs, OFF. H 2 TANKB l, 2, and 3 FANS to OFF.
CMP: Okay. I'm going to turn off all the H 2 FANS. There's B, 2, and l, are all OFF.
CMP: I took a bath last night. I think I'11 try to shave tonight. Starting to itch underneath this helmet.
CC: You mean you're not going to come home with a beard, huh?
CMP: Well, Jon wanted me to, but I can't seem to get past the itching stage.
CC: Just be comfortable. Just be comfortable. You got another week to go.
CMP: (Laughter) I know it. I've already shaved once. And when you - when you start to shave, you can only - you can only put that brushless shaving cream on - oh, maybe a third - a third of your face and start hacking on it there because it dried out real quick. So you put on a little bit, then scrape it off with a razor, then get some more on and then scrape it off.
CC: Okay, Ron, FAO's data says that on magazine Yankee Yankee, we have 20 unscheduled frames that you can use prior to the scheduled photography. After the scheduled photography, anything that's left will also be yours.
CMP: Oh, okay. Yankee Yankee must be the next one up then. I can change - put that in, huh?
CC: That's affirm, Ron. You can go ahead and put it for the scheduled photography.
CC: I can see your thoughts there, Ron. You're going to get those 20 shot up before Jack ever gets up there, huh?
CMP: (Laughter) Oh, that is a good thought. No, it's just that every once in awhile at these termina- tors, you kn ow, you - you have some real good shots, and we Just can't schedule them, you know, all the time, because sometimes you can't do it. But you take one or two shQts of each terminator when it comes by, you get some real good pictures.
CMP: (N_....lng)
CMP: Okay, magazine Yankee Yankee is in the Nikon - finally.
CMP: I think I mentioned here the other night, didn't I, putting that magazine in there - you know, it's a real critical tight fit. And you get it pushed in there Just right, and then in zero g, the thing bounces back out of the way, you know - before you can get the back on there.
CC: Roger. You don't think - -
CMP: Good camera, though.
CC: - - Nikon was designed for zero gravity, huh?
CMP: (Laughter) No, it works great. Sure something to be said about a removable magazine cassette though.
CMP: But then again, you can focus the Nikon.
CMP: Hey, Houston; America. Tape ll0B/13
CC: Okay, Ron. We're here.
CMP: Okay. I was looking over this transfer list - about 184:00, and I don't remember Gene and Jack leaving their helmet stowage bags back to me. So I think they must have them in the LM - in Challenger.
CC: Okay, we'11 make a note of that and check it out tonight. Okay.
UNKNOWN: let's see, probably about time to P20 here. Plus-X forward, SIM bay attitude; 2 ENTER ENTER, plus 5 ENTER .... - okay, PROCEED. Noun 78 - Well, that's already loaded. 52.25; plus X is 180; okay? Except we're going to do - half degree dead band 2 ENTER - 2-1/2 degree dead band, I mean. Plus 2.50 .... number 50 is the Moon. And right now, we'd like to orbrate around the Moon .... - 2 _ ,.°
CC: Hey, Ron, do you have your volume 3 handy?
CMP: Yes, as a matter Of fact.
CC: Your last call about the helmet stowage bags. Where - whereabouts in volume 3 is that?
CMP: At 184 - about 19.
CMP: Took -
CC: Okay, we got it. Thank you.
CMP: They got suited and took their helmets and gloves with them over in the LM - took their helmets and gloves with them over to LM, and they said they were going to send the back. But I don't think they ever did. We all got busy, and so they've still got them over there somewhere.
CC: Ron, we're going to lose you in about i minute, and you're looking great. No problems at all.
CMP: Okay, we'11 see you on the other side there, Bob. Thank you.
CC: Roger, Ron. And at 169:51 or thereabouts, we'11 _ see you.
CC: And you'11 be eating, wo we won't call you. But we'11 be standing by.
CMP: (Laughter) Okay. Tape lllA/1 APOLLO 17 AIR-TO-GROUND VOICE TRANSCRIPTION
CC: Okay. And, Jack - -
CC: - - When you're not holding on with two hands, we'd like the frame count from you.
LMP-EVA: Wait a minute. Yes.
CDR-EVA: Is that Van Serg over there?
LMP-EVA: Ahhhh -
CC: You have a bearing of 234 - -
LMP-EVA: I think it's - -
CC: - - and a range of 2.1.
LMP-LM: I don't know - no - it's - Okay.
LMP-EVA: We got to get around SWP here and then - -
CDR-EVA: Well, let's - yes.
CC: Copy 80.
LMP-EVA: SWP or Bowen, I mean - Bowen, I guess it is.
CDR-EVA: Well, yes.
LMP-EVA: That's SWP over there. Bowen is out here ahead of us.
CDR-EVA: Yes .... he said two- -
CC: 234/2.1- -
LMP-EVA: 234--
CC: Reading ought to be about 240; 240 for a heading for there.
CC: 234 - -
CC: - - 2.1.
CC: Okay. And we think you're even farther north than I was saying. Maybe it's about 215 would be your heading for there. 234/2.1.
CDR-EVA: Okay, Bob. I'11 find it.
LMP-EVA: And all the big blocks still look like subfloor from the Rover. But big blocks in here are only about a - a third of a meter in diameter. And they're subrounded to subangular. Okay. We're up on the plains again now, Just off the brink and slope.
LMP-EVA: That sure looks like - looks llke outcrop ... down in the East Massif on the lower slopes, if it's here the high albedo is. Doesn't it? See it over there?
CDR-EVA: Yes - Yes. Yes. It does - ... was one of my guidelines for the geophone deployment - ... points.
UNKNOWN: There's some more of the blue-gray rock here in the east end of the South Massif down low, Tape lllA/3
LMP-EVA: Yes. It looks like it might have been a slump block or something.
CDR-EVA: Yes. You can see it's blue-gray because of it's contrast with the light mantle.
LMP-EVA: Yes. It might be a sluJnp block, or something - like that.
CDR-EVA: Jack, I'm going to go to the left.
LMP-EVA: You going to go soon? (Laughter) Need 234 - -
CDR-EVA: No, No. I'm going over here. This is closer. That's a shorter cut.
LMP-EVA: Okay, that - that's probably Bowen there, don't you think?
LMP-EVA: Oh, well - -
CDR-EVA: Well, see, we never got too far - -
CC: How about a - how about a range and bearing, guys. 228/3.4.
CDR-EVA: Maybe we got too far east. Okay. It's And we're moving along at 10 to 12 clicks. That's all it'11 hack.
CC: Copy that. How about an amps reading? We haven't had one of those for a couple of ...
LMP-EVA: Starting to rain again. Got a crater ahead of yOU.
CDR-EVA: 0ooh, boy. up-Sun.
LMP-EVA: Down-Sun isn't much easier than
CDR-EVA: It's just easier on the eyes. You Just can't see any more, that's all. You don't have that static, huh?
LMP-EVA: No. Hope you've still got an antenna; I haven't looked recently.
CDR-EVA: Hope there's no holes in the high gain.
LMP-EVA: Might have hit it on a rock.
CDR-EVA: Oh, boy. Okay. The - we're back into the mantle area population of fragments is still I percent or so. The crater off to our left, which is at 227 and 3. - What is that?
LMP-EVA: 3.1.
CDR-EVA: 37
LMP-EVA: 3.3; 227/3.3.
CDR-EVA: - is a fairly good-sized depression, but it's completely mantled. There's no blocks showing in the wall at all. How do you read, Bob?
CC: Loud and clear. We're listening. in
LMP-EVA: Now there's that crater the wall of that de- And one pression or hollow near it. it has big block in the side as if it penetrated the mantle exposed and some of the wall of the depression. Just about a 30-meter crater. Valley of Taurus- Littrow is not planar.
CDR-EVA: No, it isn't.
LMP-EVA: I'm glad we changed it to a subfloor instead of a plains unit.
LMP-EVA: Okay. We're in the inner wall of the depression here, and the rocks still look like subfloor gabbro. Boy, there's certainly not much variety.
LMP-EVA: Okay. Generally, there are few exotics.
CDR-EVA: Ooh, now that's got to be Cochise.
LMP-EVA: Ah, look at Cochise. Tape lllA/5
CDR-EVA: That's Cochise.
CC: Roger. We think you're coming up on Cochise.
CDR-EVA: Get your self a couple pictures while you're look- ing right at it.
CDR-LM: Bob, we are on the south - or northeastern rim of Cochise. I'm going to work my way around the other side. And Bob - -
CDR-EVA: - - looking at the western wall of Cochise, I can see a contact within the subfloor between albedo units, one of which is a light tan-gray and the other is a light blue-gray. May reflect the two kinds of subfloor gabbro we've already sampled. and Vesicular nonvesicular. And that contact that looked like it was dipping - apparent dip in the wall - was to the north. And the west wall dipping to the north about 20 degrees.
CC: Okay. Copy that. What - which one's on top? Can you tell?
CDR-EVA: Yes. The blue-gray's on top. I'm sorry.
CC: Thank you. And you got a bearing and range there at the rim of Cochise?
CDR-EVA: I took a picture of it and - Okay. We're at 228/B.0, and we're not - we're headed south and not quite on the - on the east rim.
CDR-EVA: I'11 give you a hack at the east rim. I was -
LMP-EVA: I took some pictures right into Cochise, too, when we were coming up.
CDR-EVA: Good. It'11 show on yours, too, probably - I hope.
LMP-EVA: Quick; give them a mark. 230/2.9.
CDR-EVA: MARK. We're on the east rim.
CDR-EVA: Well, we're sort of inside the east rim a little bit.
CDR-EVA: We're halfway between the rim and where the blocky wall starts.
CC: All right. Copy that.
CC: Yes. We got that.
LMP-EVA: Cochise is much like Horatio and - actually, more like Camelot, although not as blocky in the walls, in general, in that it - it has blocky walls but a mantled rim. Again, all the blocks I see in here are big ones. And blocks down to about 20 centi- meters are subaugular, in general, and appear to be the - have the appearance of the subfloor gabbro, although most of the smaller rocks are not - do not appear to be highly vesicular.
CC: All right. We're copying that all.
CDR-EVA: We're at 232 and 2.7.
LMP-EVA: Watch it.
CDR-EVA: You know why - what happened there?
CDR-EVA: I was just about to take a picture, and the min- ute you take your eye off anything - Tape lllA/7
CDR-EVA: Yes. I got another view of that contact, and let's put that - let's put that on the northwest wall of Cochise and dipping to the southeast.
LMP-EVA: All right. South and east is to our left.
CDR-EVA: No, no, no, no, no. Put it on the northwest wall dipping to the northeast.
LMP-EVA: Yes, that's right. See that, Geno, can you see that over there?
CDR-EVA: 0h, yes. I can see it now between the gray and blue-gray?
CDR-EVA: Oh, yes. Yes, I sure do.
LMP-EVA: Can you swing in there, and let me get another shot of it?
CDR-EVA: You betcha.
LMP-EVA: Oh, this is a good view right here. Okay now, I need to have you go left.
CDR-EVA: Okay. I got two of them in there, too.
CDR-EVA: Look at that rock right in front of us. It looks like a contact between a blue and a gray.
LMP-EVA: Oh, yes, there it is. Yes, you're right.
CDR-EVA: We can't get down to it, but take a picture.
LMP-EVA: Well, I think we've done - I think we've got that relationship. I think we got it at station l, as a matter of fact.
CDR-EVA: Inner rim - -
LMP-EVA: Well, now, that might be glass covered. That might be a glass coating; the way it sort of hangs on the outside there. Hard to say.
CDR-EVA: Okay, we're at 234/2.5.
LMP-EVA: Starting to sling dust. I wonder if we've lost our fender.
CDR-EVA: No, they're on there tight .... - -
LMP-EVA: You think that's Van Serg? Right over there.
LMP-EVA: There it is. Bet you.
CDR-EVA: Yes. I think you're right, because that's Just about the right place. Let's see, 234 - okay, is where - and 2.1 is where we want to go, and I'm 230/2.5. at
LMP-EVA: Okay, our - -
CDR-EVA: Pretty close.
LMP-EVA: - - 0ur block population in - here now on the south rim of Cochise and it's - and up ahead of us looks like it's up to 5 percent. And it's - all looks like subfloor - light to tan subfloor gabbro - or tan-gray. You don't see much blue-gray; not out on here. lllA/9 Tape
LMP-EVA: There's a recent hit.
CDR-EVA: This Rover is getting tested for what it was built for now.
CDR-EVA: I tell you it handles Just the way as advertised, maybe even better.
CC: Okay. We think you guys are getting to the point we ought to swing a little bit west to make that 234/2.1.
CDR-EVA: Yes, I am, Bob.
LMP-EVA: I think we - We've got it. Tallyho.
CDR-EVA: Bob - Bob. That's my fix. I'm Just navigating to it.
CDR-EVA: I know where. I'11 get there.
LMP-EVA: We have a Tallyho on Shorty - I mean of Van Serg. How about through there, Geno. Thanks.
CC: Let's not prejudge the crater too much.
CDR-EVA: You want 234/2.1. Okay.
CC: And remember we talked about parking on the south- east rim.
CDR-EVA: It wanders like our wander factor in here has got to be 50 percent.
LMP-EVA: Bob, you're cut -you're being cut out. I can't tell what you're saying. Isn't that where we want to go, over there?
CDR-EVA: 23 - Well, -
LMP-EVA: Well, - look, ... way to get - -
CDR-EVA: ..... found the crater.
CC: 234 or 232 - -
LMP-EVA: No, we didn't ... there on the right.
CC: - - It doesn't make much difference, 17. If you see Van Serg, that's what we want.
CDR-EVA: Well, you're - Let me wander over that way. That's where I want to get, but I couldn't go there because of that -
LMP-EVA: There's a different looking rock there.
LMP-EVA: Yes, I think you're going to have to bear right.
LMP-EVA: Yes, I know (laughter).
CDR-EVA: Okay, Bob. We're still primarily in an extreme block field here now. It's up to a 20 percent cover, aud - of fragments mostly the subfloor. Some of it looks quite highly shattered. There's - I Just saw one piece that looked like a white anorthositic rock.
CDR-EVA: How's this look to you? We can go farther up there, I guess. Let me go farther up.
LMP-EVA: Well, okay, if you can get up.
CDR-EVA: Get a little farther on the southeast.
LMP-EVA: A little higher is apt to overdo it.
LMP-EVA: There are - there is some - some grayish rocks that are-- Tape lllA/11
CDR-EVA: Oops! I centered. Right, coming up here. I turn to the right and park right here.
LMP-EVA: - - That have a - somewhat of a swirl texture. 230/2,2.
CDR-EVA: Okay, Bob, we're at
CC: Copy that. Copy you parked.
CDR-EVA: Yes. What did I say? 230 on that? Yes, bearing is 230/2.2, and I'm parked on a heading of 320, which gives you a better view.
CC: Copy 320 for the parking.
CDR-EVA: Yes, 3 - 330.
LMP-EVA: Oh, boy. This is getting harder and harder. Got it ... also. Don't know what's wrong with it, now. I might have got it twisted.
CDR-EVA: Here, let me look at it.
CDR-EVA: Here let me look at it. I'd say stay put, but I don't think you have any choice.
LMP-EVA: That fender Just curled under, that's where we're getting the dust - starting to warp.
CDR-EVA: Look at those other fenders, talk about warping.
LMP-EVA: Did I get it twisted or something?
CDR-EVA: Yes, you did twist it when you put it on. Okay, squanch down.
LMP-EVA: I'm squanched.
CDR-EVA: Okay. Had one twist in it.
LMP-EVA: Boy, that makes a difference.
CDR-EVA: Sure does. Here. Your footpan's down, too.
LMP-EVA: I'11 get it. It's lost it's stiffness in there. Okay - okay, I guess now I'11 plan for Shorty, huh? ... Van Serg.
CDR-EVA: Okay, 2 POWER 's ON - crater right now.
CC: And, Gene, before you go away, we'd like the rest of the Rover readouts, like batteries. And how about a SEP temp readout before one of you guys leave there?
CDR-EVA: Get - Can you get that on that side, Jack?
CDR-EVA: Well, there's so much- -
CDR-EVA: - - Just over the gage. It's about 12 - 125 on the SEP.
LMP-EVA: Boy, everything is really bad now. The fender warped.
CDR-EVA: Yes, the fender cut - dug under. See if you can straighten it out.
CC: Okay, and leave the covers - - lllA/13 Tape
CDR-EVA: Okay. Amp hours, 82 and 80. Battery, 122 and off scale low. Forwards are 210, 240; Rears are 225 and 2 - 220.
CDR-EVA: That's Just a sample of the kind of - kind of dust we would have got, Jack, if we hadn't of had that fender yesterday. Fender's almost worn out.
LMP-EVA: Can you get a dustbrush, and let's check our camera.
CDR-EVA: Stay where you are, and I'11 give you a zappareno wherever you are.
LMP-EVA: That it?
LMP-EVA: Okay, how mauy bags do I have.
CDR-EVA: I don't know, but I've got a lot of dusting to do here.
LMP-EVA: Do you have a lot of bags?
CDR-EVA: Yes. I must have - I've got four of them is all.
LMP-EVA: I'd better change my bag.
CDR-EVA: Can't even read the Rover.
LMP-EVA: Yes. I have an empty bag on me now, right, a collection bag?
CDR-EVA: Empty.
CC: Okay, 17--
LMP-EVA: Don't know how much time do we have here?
CC: Okay, 17. We're looking at a nominal station 9 here. You've got about 25 minutes remaining.
CC: This may be the first and only one of the traverse.
LMP-EVA: The geology won't let it be nominal. Hey, I've got some new bags, Bob.
CC: Okay. We copy that, Jack.
LMP-EVA: And I guess I 'm pretty good on film.
CC: Okay. And you're going to get a radial sample here, and so you might check your Rover sample bag supply.
LMP-EVA: That's right. I want to take that.
CC: And you might - and you might give me frame count or check it to make sure you're okay.
LMP-EVA: I Just did, and it's 123.
CDR-EVA: How do you want the SEP blankets?
CC: Leave them closed, please, Gene - -
CDR-EVA: Open or closed?
CC: - - as closed as they'11 get.
CDR-EVA: We been riding with this thing off?
LMP-EVA: What ?
CDR-EVA: SEP?
LMP-EVA: Yes, it should be off.
CDR-EVA: Yes, it is. Doesn't seem like it'd get much data that way. Even if it's hot.
CC: Yes, but it's - it's automatic - - lllA/15 Tape
CDR-EVA: I guess they're worried about getting it so hot it - -
CC: It shuts itself off when it gets above 108, so it's no good anyway.
CC: We've been hoping all day - it's been off all day. We've been hoping that it would - since station 6 - We've been hoping that it would cool down so that we could get some more data, but it's not, obviously.
CDR-EVA: That's a - that's a shame.
LMP-EVA: This is starting to look like a geological survey expedition. The vehicle's are all covered with dust.
LMP-EVA: Oh, look what's in there.
CDR-EVA: I don't think I can read that unless I dust it with a lens brush - Okay. Get my - Okay, can I get by you here?
LMP-EVA: My - my bag look all right to you.
LMP-EVA: Okay. Okay. What are we going to do here? We're going to go up there and sample on the rim, look at the walls, and the floor, and miscellaneous, and - -
CDR-EVA: Well, we are on the rim ...
LMP-EVA: - -then you're going to take 500 millimeters when you get back to the Rover while I do a radial sample.
CDR-EVA: Okay. the crater. Bob, I think the mantle objective here really is imaterial and - because the - there's - the blocky eJecta around the crater covers - oh, boy - Well, it looks like it - it extends several hundred meters out from the rim- say a couple of hundred meters.
CC: Ail right. Copy that, Jack.
LMP-EVA: We're quite a ways - we're pretty close to the rim.
CC: Yes, we can see that.
LMP-EVA: We're pretty close. I'11 go up on the rim, Gene, and see what we've got.
LMP-EVA: Tiptoe through the tulips (singing) - - Okay. Let's get grabs before you guys leave.
LMP-EVA: (Singing) I'm getting it right now. Let me see; anything else you want me to do while I 'm here?
LMP-EVA: Sure look like shocked rocks to me.
CDR-EVA: Lot of glass splattered on some of these, Jack.
CDR-EVA: We might even find some shatter cones. But don't tell anybody. blocky. Whoo l
CDR-EVA: _I_K. Gravimeter. Copy that.
LMP-EVA: Bob. This is about - I think this is the only clearly - well, I won't even say that. This is at least a blocky - a large blocky rim crater. But even it has the mantle dust ma - arterial Tape lllA/17 covering the rim, partially buried rocks. And it's down on the floor, as near as I can tell, and on the walls. The crater itself has a central mound of - of blocks that's probably 50 meters in diameter - that's a little high - BO meters in diaw_ter. It - Many of the blocks are - -
CDR-EVA: Holy Smoley!
LMP-EVA: - - intensely shattered in that area, as the ones that are on the walls. I don't see any sign of organization of the blocks in the walls right now. There's a possibility that on the west wall, there's an indication that there's slightly darker gray rocks starting about halfway down the crater. And that's - that level is coincident with what appears to be a bench on the northwest wall. And that bench - hints of that bench - it's not continuous, but hints of it are around on the north wall and, I think, right below us - yes, on the southeast wall. The - We'11 start - The rocks are pretty badly broken in many cases. And - well, I haven't seen any real glass yet. Yes. We'11 start looking at them a little more carefully.
CDR-EVA: Some of them - That looks like a breccia right there in front of us.
LMP-EVA: Yes. There's some interesting patterns on the surface. Geno, but -
CDR-EVA: Okay? on locators, occasionally.
LMP-EVA: Do that?
LMP-EVA: Okay, Gene's tearing apart one of the - -
CDR-EVA: Here. There you go.
LMP-EVA: - - very intensely fractured rocks. And it comes off in small flakes. Let's get this one, because this will he the best oriented one for documenta- tion, plus why don't you get that one you've got inside there?
LMP-EVA: Got a bag?
UNKNOWN: Bag 568 is a fragment from the surface. That's a corner, I think, off the block that Gene documented here.
CDR-EVA: Yes; it is.
LMP-EVA: We'11 get - we'11 get another sample - that'11 be from inside the block.
CDR-EVA: Get it with this real easy. Here's a whole big - we ought to take that just as is.
LMP-EVA: Well, put it - put it in your - put a bag around if we - around one end if we can. Here the other end is smaller.
CDR-EVA: Yes. Hold this - -
LMP-EVA: Let me hold this end. Let me hold it, and you put the bag on.
CDR-EVA: That's breccia, too. That's - -
LMP-EVA: Well, it's - -
CDR-EVA: Well, see that? See the white fragments in there?
LMP-EVA: Yes. It certainly--
CDR-EVA: It's got a lot of very small - -
LMP-EVA: It - it looks like this big one over here. You know, it might be that the - these are - might be pieces of the projectile. I don't know. Be- cause it doesn't look like - it's not subfloor.
CDR-EVA: Okay. Pin it down. lllA/19 Tape
LMP-EVA: Well, that's wrapped in - if you can put it - if you put it end down, it may stay in the bag.
CDR-EVA: I doubt it.
CDR-EVA: It's a 480, and it's a - a relatively tabular [sic] shape, and it's about - -
LMP-EVA: And it's highly friable. It breaks apart.
LMP-EVA: In small chips. Well, you can - you did it with your hands there. I call that being friable, compared to what we 'ye seen ar4vway.
CDR-EVA: Okay, and let me get in after of that. The soil next to the boulder down about 3 centi- meters, is in bag 569.
LMP-EVA: Okay. And the soil and chips - about two-thirds of a meter from the boulder - -
CDR-EVA: Get another one?
LMP-EVA: Yes - are in bag 570.
CDR-EVA: Let me get over here. You're going to step on your gnomon there.
LMP-EVA: I wouldn't step on my gnomon. I'm going to get this one - crimped. Okay. There, very clearly, is a central mound. And now that we've looked at this one, the mound looks like it's composed of gray fragment breccias much like what we've Just sampled - -
LMP-EVA: Related to the projectile. Now, we've got to see if there is subfloor up here, or whether we're dealing with another unit somewhere.
CDR-EVA: got your after. Okay. I don't see any - -
LMP-EVA: Well, the more coherent rocks - this looks like subfloor.
CDR-EVA: I don't see any orange material either.
CDR-EVA: This particular rock we've sampled has tabular fractures, and in one-half of the rock, they are definitely oriented.
LMP-EVA: Boy, I'11 tell you, I don't - There's more dust on these rocks. It's harder to see a fresh sur- face. They're not as clean. That's subfloor.
CDR-EVA: Hey, and even the floor of the crater is mantled down there. what you got? A piece of glass?
CDR-EVA: Yes, I think it is glass. At least it's glass covered - Just glass covered. Houston, I've got an undocum-nted sample. It's about 2 meters left of where we Just sampled. It's a glass-covered - oh, baseball-size rock in 571.
CC: Copy that. lllA/21 Tape
LMP-EVA: A lot of these blocks up here, Houston, are - particularly the more fractured ones, but even some that aren't - are a gray matrix fragment breccia. And it looks like - really, the fragments are quite fine. There are no - On the rim anyway, we haven't seen any large fragments. The largest I've seen is about 2 centimeters. But down in the mound you can see some fragments that are probably half a meter in diameter.
CDR-EVA: Jack, are you going around that rim of the crater up there?
LMP-EVA: I was Just looking at rocks.
LMP-EVA: We - we - -
CDR-EVA: I want to get a pan before we leave back there.
LMP-EVA: Oh, yes. We need to see if - we can get some of the subfloor. I'm not sure I understand what's hap- pened here, yet. This should have brought up subfloor according to the theory, and it hasn't.
CDR-EVA: That looks like some of the - look at some of the breccias - the blue breccias with the white - big old slabby white - with the fracture face with the white inclusions.
LMP-EVA: Yes, it has that appearance all right, ttey, Gene. Do you see that rock - -
LMP-EVA: It 's sort of pointing west.
LMP-EVA: It's really neat. That's a unique fracture, isn't it?
CC: Roger, 17-- in a ... - -
CC: - - And we'd like to be moving from here in about 10 minutes, so we probably better be trending back toward the Rover, unless you're seeing something really great out there.
CDR-EVA: Jack, do you want me to put this in your bag and start - I'm sorry.
CC: Roger. You got - you got 10 minutes. I'm just telling you to start thinking about getting back.
LMP-EVA: Yes. We're always thinking that way.
CDR-EVA: Okay, Bob. One thing I noticed we do uncover. There's a lot of - oh, 2- 3, 4-millimeter-size fragments of glass we're kicking up all over the place.
CDR-EVA: Little glass balls.
LMP-EVA: Hey, Gene?
CDR-EVA: Almost like Pele's -
LMP-EVA: Gene ?
CDR-EVA: Yes. subfloor here. We ought to - -
CDR-EVA: Okay. Tape lllA/23
LMP-EVA: We ought to try to document it. But I tell you, most of the rocks are the - are the fine-fragment breccias. Let me see if I can't get one of those little - -
CDR-EVA: There's some glass.
LMP-EVA: Hey.
CDR-EVA: You see if they're like Pele's - -
CDR-EVA: - - ... eyeballs or whatever they are.
LMP-EVA: I think we can get some over here. If you're - if you're careful coming over here, we can get glass that looks like it may have crystallized in place there.
CDR-EVA: Okay. I'm talking about those little - little balls, too. See that - -
LMP-EVA: Whoo, take it easy - Take it easy.
CDR-EVA: Where are you? Right there?
CDR-EVA: Okay. Let me -
LMP-EVA: But I'm not sure that is. I Just - It may be breccia there - Everything is covered with dust here, and it's hard to tell the types. Most of the rocks we're seeing are breccias. Make sure that glass is in your stereo.
LMP-EVA: Okay, be careful with it.
CDR-EVA: Oh, shoot!
CDR-EVA: I don't have any bags so -
LMP-EVA: Okay, the glass - looks like a glass agglutinate. Oh, no!
LMP-EVA: Didn't break ?. Good. I think that will survive going back now.
LMP-EVA: Okay. It's a frothy - glass agglutinate is going to be in bag 481.
CC: Copy that. pile-type of bomb, Bob, if you'11 pardon the expression.
LMP-EVA: Although it's not flattened. It's - it's - it's a - it's an aggregate of glass in - or it's a pile of about four fragments, much like the one we're sampling.
CDR-EVA: Jack, we want to get a good scoop sample here. Maybe can we get some of those little fine pieces of glass around.
LMP-EVA: And it looks like it's - it's in place from the day it was born.
CDR-EVA: Oh, gol dig da! I'm having a hard time with this one.
LMP-EVA: A piece of that rock right behind it.
CDR-EVA: If I can -
LMP-EVA: Want a bag?
CDR-EVA: Yes. I'm going to turn around. Just not going to be able to get that one in the bag, I don't think.
LMP-EVA: Okay, Houston. My sample's in - 482 is a rock, but it doesn't look like subfloor. It looks like the blue-gray material we've been seeing - the breccia-type material.
CDR-EVA: Yes. 111A/25 Tape
LMP-EVA: I don't think there's difference.
CDR-EVA: Got it in!
LMP-EVA: Might Just as well throw them in m_ bag.
CC: Okay, and--
CDR-EVA: I want a scoop out of here, though, Jack.
CC: 17, why don't we get that scoop sample as the first sample of Jack's radial sample, 177
CDR-EVA: Okay. That's right. You're getting a radial sample. That's fine. I forgot you were doing that.
LMP-EVA: 0h, man.
CDR-EVA: That's all right, Jack. That won't come out. Just put it in there.
CDR-EVA: Okay. Let's let that one be the last -
LMP-EVA: Here's one.
CDR-EVA: Well, okay. Those are the last ones that you can take. Got a lock?
LMP-EVA: No, I don't see in my ... on that.
CDR-EVA: Okay. Okay, before you go back - I got to go down after a picture here. And I want to get a pan of this thing. We can get a stereo pan - as you start your radial sample.
LMP-EVA: Yes. Are you going to - You - you take the after from there, and I'11 go over here and -
CDR-EVA: Okay. You - -
LMP-EVA: Well, wait a minute.
CDR-EVA: - - you need the gnomon?
CDR-EVA: From - from behind me, where we were. Well, I think I'11 just take my radial right from here to the Rover.
CDR-EVA: That's great. That's great. Just do that, and then you'11 be right back at the Rover.
LMP-EVA: And I'11 take my pan from here, so you -
CDR-EVA: Man, there's about four or five different modes of travel out here.
CDR-EVA: I don't believe it.
CDR-EVA: I think I'm out of film.
LMP-EVA: You're out of film?
CDR-EVA: 150. And it stopped clicking. Jack, I - I - I didn't get the rest of that crater down there.
LMP-EVA: I can get it.
CDR-EVA: Well, here's where I -
LMP-EVA: Well, I'm going to be out of film, too, here before long.
CDR-EVA: Okay. Just don't worry about it then. Just press on with your radials.
LMP-EVA: I've got - I got a good pan over here. Did you get the crater at all? Tape lllA/27
CDR-EVA: I got the right half of it and probably two-thirds of it, so we're going to - I'm Just going to have to let that do. Okay. I'm going to see if I can get some 500s while you're doing that.
LMP-EVA: Hey, this isn't going to be an ideal - radial sample - but it will have to do. Giddyapping over hill and dale (singing).
CDR-EVA: Bob, would you tell me what your primary desires are again on the 500, based upon what we have?
CC: Okay. The primary desire will be the North Massif, the blocks, and the trail.
CC: And while you're at the Rover, they want you to take the gravimeter off again, and we'11 get another Rover and a - well another surface measure- ment here, as well - to check against the Rover.
CDR-EVA: Okay. Here's a reading. I think I owe you one of those, don't I?
CDR-EVA: 670, 037, 801; 670, 037, 801.
CDR-EVA: I didn't know we were going to do both of these things. I thought we were going to do one or the other. But - if we're going to do it, we might as well do it right.
CDR-EVA: MARK it. It's flashing.
LMP-EVA: Okay, bag - stand by - 52 Yankee is at the rim crest.
CDR-EVA: Well, I'11 tell you what I'm going to do. I'm going to use the Rover to steady the 500, and see what happens. Oh, no. Oh, me. Well, shoot! This isn't working out too well, Dr. Parker.
LMP-EVA: This isn't working out too well. I've got to get rid of this scoop.
CDR-EVA: Just set it there and take your sample. We'11 get it.
LMP-EVA: I'11 take the samples going back.
LMP-EVA: Just like in training, the scoop doesn't stay locked to the ...
CC: Okay, 17. We'd like you to press on. We'11 abort the radial sample. We'd like to leave here in_ne- diately, if not sooner, to head for station 10. Enough of the 500 millimeters, Gene. And we'11 give you some information here on mags. We need the gravimeter put back on the Rover, if you haven't already. If it's on the ground, we didn't get the mark, but it's probably done by now. And we're going to take the DSEA out of the tape recorder here, and we'd like to get that all done pronto.
CDR-EVA: Okay. 85 is the mag count on the 500.
CC: Copy 85 on the 500.
LMP-EVA: I think that's a smart move, Bob. I don't think - I don't think the radial sample's going to tell you much here.
CC: Okay. Let's take a -
LMP-EVA: I don't under - I - I -
CC: Ca ahead.
CDR-EVA: We don't have a scoop of it, do we? Tape lllA/29
LMP-EVA: Look what's underneath it.
CDR-EVA: Well, I don 't know what 's underneath it.
CDR-EVA: Well, I wanted to make sure we got some of those small glass balls.
LMP-EVA: Yes, we'11 get a scoop of it. Upon the top.
CDR-EVA: Okay. Here's your gravimeter reading from the surface; 670, 057, 101; 670, 057, lO1.
CDR-EVA: You want me to change my mag at the next station?
LMP-EVA: Come here, Gene, quickly. We can't - we can't leave this. This may be the youngest mantle over - whatever was - -
CDR-EVA: Take pictures of it. I don't have any film.
LMP-EVA: - - was thrown out of the craters.
CDR-EVA: Take pictures of it. Bob, we've got to take 5 more minutes. We'11 be right with you.
CDR-EVA: What Jack's done is he dug a - a trench in a - the southwest-northeast direction, and he discovered about 3 inches below - _ inches below the surface - a very light-gray material.
LMP-EVA: Possibility here - Careful, Geno.
CDR-EVA: Take that crust.
LMP-EVA: Well, I'm trying - I'm trying to get the - the upper portion there. There we go.
LMP-EVA: The first 2 centimeters, bag _83. The next 5 - Ahhh - in 48_. AughI
CDR-EVA: Get some?
LMP-EVA: I got quite a bit.
CDR-EVA: That 's enough.
LMP-EVA: I got quite a bit. Here, you got to put that away, don 't you?
CDR-EVA: Yes. material, be in - probably in 486, if we're lucky - get it off.
LMP-EVA: I think it is 486, right?
CDR-EVA: Yes. 485 i
LMP-EVA: 485. Okay. What did I say 483, 484? Okay.
CDR-EVA: You with us, Bob?
LMP-EVA: He's mad at us now.
CC: How'd you guess?
LMP-EVA: Okay. The third sample is in 485.
LMP-EVA: Okay. Whoops, sorry. Bob, a possibility here is that the - this upper 6 inches of gray material in here is the latest mantling in the area and the light-colored debris may be what's left over from the impact. understand.
CC: Okay, I copy. I But we'd like to get you going. In case you didn't get the clue.
CDR-EVA: I know. We 're going. Okay.
LMP-EVA: All right. What else? Magazines. Tape lllA/31
CDR-EVA: No, we'11 change them at the next station. Isn't
LMP-EVA: No, I've got to have some. I got to get some, or I can't take -
CDR-EVA: Okay, I need a magazine too, Bob. I don't have any film at all.
LMP-EVA: Okay. You want Bravo, huh?
CDR-EVA: Bravo. And I'11 get the tape - I'11 get the DSEA. Bravo was outside there, I thought.
LMP-EVA: There you go. Let me get this - hold it one - long enough for me to get this. Then I can get rid of this all at one time.
LMP-EVA: Well, that's all right.
CDR-EVA: I can't put that back in.
CDR-EVA: I got - I got Bravo.
CDR-EVA: We lost the dark slide out of Bravo, and it's in the dirt. I'm not going to pick it up.
CC: All right. Copy that. There's no point in putting it back in. It probably wouldn't go in anyway.
CDR-EVA: Well, that's dirty. Okay. I'm changed. And I don't know what the mag count is, but let me get the D6EA. If this thing is true to form, I'm going to have to get in there - I got to - ... tripped. Well, now what's - Hey, we got some rocks in that big bag. Okay. We're done with the SEP. DSEA is coming out. I hope there's something on it.
CDR-EVA: Oh - Jiminy Christmas - I can't even pick up that big bag to close the gate.
CDR-EVA: I've got to - I've got to trip that latch with - with tongs or something to lock it.
CC: Okay. And, Jack; Houston. Over.
CC: Okay, we've - -
CC: - - had a change of heart here again, as usual. And we're going to drop station 10 now that we've heard you so much, and we're going to get a double core here. And we'd like to get the - some football-size rocks while you're doing that. But double core here, and then we're going to leave here and go back to the LM. want a double core here. I don't think we can do it, Bob. It's too rocky.
CDR-EVA: You don't think we'11 get through that stuff you Just trenched?
LMP-EVA: Well, I'm afraid there are rocks all through it, Gene. We can try, but -
CDR-EVA: Let's try it.
LMP-EVA: Well, I don't like to try things that there is a probability of failure on - if you can - You're Just going to lose some time. Okay, mag Nancy in on the LMP's camera.
CC: Copy that. here, Houston. But we can try it.
CDR-EVA: Sure. If we get a single, we get a single out of it.
LMP-EVA: Oh, you're doing it, huh?
CDR-EVA: I've got it started. debate the issue.
CDR-EVA: No, it takes too much time debating it.
LMP-EVA: Well, let's see how much time it takes. I hope you're right.
CC: Okay. And -
CDR-EVA: Okay, andwe need a - we need a lower out of my bag.
LMP-EVA: Let me get the core.
CDR-EVA: A lower out of mybag is all we need.
CDR-EVA: Yes. I want to get ... for you.
CC: Okay. We have to have you guys moving in 10 min- utes. And we'd like to also deploy EP number 5 here.
CDR-EVA: Okay. I'11 start on the ... - -
LMP-EVA: - - ... the lower 5?
LMP-EVA: This is a lower, right?
LMP-EVA: ... And I'11 put it - I'11 put that right there.
CDR-EVA: Okay. The lower is 50; the upper is 37.
LMP-EVA: Why don't you put it up - well - You put the gnomon away. Put it fairly near that trench. At least there is some documentation there. I'11 try to have the pan going while you're doing it. Okay, Houston. Which way you going to drive out of here?
CDR-EVA: I'm driving out of here -
CDR-EVA: I - I've got to go right. I got to go right. pulled
UNKNOWN: Okay. Pin i is and safe. Pin 2 is pulled - safe. Pin 3 is pulled and safe.
CC: Okay, Jack. And we'11 document it back to the Rover, I guess is the best way. That doesn't look too hard, Gene. Until Just now.
CDR-EVA: Thank you. Oops, looks like you proved me wrong.
LMP-EVA: The first core was easy; the second one a little tougher; and then it got tough down at the end. There, I'm getting a picture of you. Okay?
CDR-EVA: Okay. 111A/35 Tape
CDR-EVA: You got it from here? Okay.
CDR-EVA: Core but it wants to slide out. It's full. No rocks in it. It looks like Just the same stuff we've been traveling through.
CC: Okay, Jack. I think you better help Gene with that - recovering that core there where the ... going to fall out.
LMP-EVA: You know, I think you're right. And if you'11 Just wait until I finish the pan, that's exactly what I'm going to do.
CC: Okay. I didn't know what you were doing.
CDR-EVA: Bob, it's capped.
CC: Got you. Okay.
CDR-EVA: You hold - Just hold the handle.
LMP-EVA: Okay? I can take this one.
CDR-EVA: It's very - very loose soil, Jack. And it's - Just any little movement and you'11 lose some of it.
CDR-EVA: Let me cap that end. Don't move it.
LMP-EVA: Uh-oh, you're - you almost knocked some out. Get your - you know where your thing is.
CDR-EVA: Yes, but I need you - that - that cap's on you. The last one's gone off the Rover.
LMP-EVA: That's all right. I'11 stay here. Go put yours out there. I won't move it.
CDR-EVA: Any little movement and that stuff starts - - Yes. Okay.
CDR-EVA: Go - turn around. I'11 get the r,mmer.
CDR-EVA: Oh, man! Even these pins are getting stiff. Okay, Bob. The top rammed down - oh, almost half way without any effort.
LMP-EVA: The ... back on.
CDR-EVA: The bottom rammed down about an inch.
CDR-EVA: Okay, Robert. Let's see. Turn around and I'11 get this. What was the last thing - let's see - we had to do?
LMP-EVA: A couple of football-size rocks.
CDR-EVA: You got the DSEA? core. I got the double core. And I got one sample sample of a radial (laughter).
CC: We got a - that's a unique one.
LMP-EVA: In nV pocket (laughter).
CC: And have we got the gravimeter back on the Rover?
LMP-EVA: Yes; it's on.
LMP-EVA: And we want to get a large block. Why don't we - Why don't we - -
CC: Okay, and there's a- -
CC: - - ... here for a SESC from the shallow trench. We'd also like to have you moving in 4 minutes. That's with wheels rolling in 4 minutes.
LMP-EVA: SESC, huh?
CC: Roger; but we have to have the wheels rolling - -
LMP-EVA: I don't know if we can do that. We can try it.
CC: We want the wheels rolling in 4 minutes, so I don't think it's practical at this time.
CDR-EVA: Bob, we cannot get an SESC in 4 minutes - -
CDR-EVA: - - and roll - -
CC: - - Copy that.
CDR-EVA: - - at the same time.
CDR-EVA: Now, I've got to push this latch on the - on the gate to get it locked - on the pallet to get it locked.
CDR-EVA: Push the pallet while I trip the latch, will you? Because I got to trip the latch. There's so much dust in that core.
CDR-EVA: No. No. Wait a minute. Open it up. Wait a minute.
CDR-EVA: Now - now that's where - now let me trip it.
LMP-EVA: Okay. Try it.
CDR-EVA: Locked?
LMP-EVA: That got it. That got it.
LMP-EVA: Got a big rock there, too? amazes
LMP-EVA: It's a - well, you know, the thing that me is that there's no subfloor around here.
CDR-EVA: I got one here.
CC: Okay, 17. What's out there in the distance on a hillside in the field of view of the camera? The camera is pointing at it. Oh, I'11 bet that's the - %hat's the - -
CDR-EVA: What's out there in the distance. Which hill? Let me see the - -
CC: - - that's the flag, I bet, on the charge.
CDR-EVA: Yes, but it's only - you're looking right at it, but it's only 10 meters away.
CC: Okay. It's hanging in front of the hills. That's the problem.
CDR-EVA: You're looking right at the flag.
CC: Okay. It's hanging in front of the hills. We thought we had an artifact or something like that. Okay. Press on.
LMP-EVA: Bob, bag 486 is a light-colored rock taken about 3 meters to the right of the Rover. It should be - you should be able to pick it out in that last pan, unless the focus was bad. Tape lllA/39
CDR-EVA: Bob, you got all your TG readings?
CC: Roger. We've got that. We'd like to have you climb on.
CDR-EVA: You want the LCRU off ?.
CC: Roger. Let's go to LCRU power off.
CDR-EVA: Okay, Jack, let's - better get going.
LMP-EVA: Yes. You know, I don't think there is any sub- floor in here. The rocks are so dust covered that it's hard to be sure, but no rock I picked up looked like subfloor.
CDR-EVA: Get on there one time. Ready? I got three of them that time.
CC: 17, Houston. Do you read me through the - the LM?.
LMP-EVA: You're loud and clear.
CDR-EVA: I get that twisted this time, if I can get off.
LMP-EVA: Oh, let's see if old twinkletoes can do it.
CDR-EVA: Jack, there's a big - a big one right there in my floor pan. That's what I did last time.
LMP-EVA: Okay. I 'm on, strangely enough.
CDR-EVA: Okay. Let's see. Okay. The charge is off to the - right.
LMP-EVA: Yes, you're all - You can clear it this way or - -
CDR-EVA: Yes. I see it. I see it.
CDR-EVA: I bet you they thought there was some more orange soil over there on the hills.
CDR-EVA: Get out of this block field, we'11 be able to move it a little bit.
LMP-EVA: I wonder where we stand on time.
CDR-EVA: Well, we've been out about 5 hours and 20 minutes or So.
LMP-EVA: Where is it - where are we headed, now that we are moving?
CDR-EVA: Well, I'm trying to get around - trying to get out of the block field here, then I'11 head back to the southwest. We going to Sherlock at all, Bob?
CC: No, we're going ... follow the ... - -
LMP-EVA: That must be Gatsby over there.
CC: And a reminder, Jack. We can get lots of photos. We've got lots of film left right now.
CC: And, 17. Gene, I guess you're the one that took the SEP out. If you could give me - do you're- member the reading of the SEP temperature when you broke it down?
CDR-EVA: Didn't even look, Bob.
CDR-EVA: It was 125 - 125 when we started the station.
CC: Roger. Copy that. Tape lllA/41
CDR-EVA: That's Gatsby there, I guess, huh?
CDR-EVA: It's not - it's not unlike Van Serg, though. Hey, you know that looks like mantling.
LMP-EVA: Hopefully, we can get a - watch your rock - there you go - we can get a shot looking back to the northwest - -
CDR-EVA: Yes, I'11 get that when I - -
LMP-EVA: - - into Gatsby, because it looks like the mantle streAm_ over the - the side from the southwest. Can you swing to your right - get up a little closer to the rim, there?
CDR-EVA: Hey, here's a couple fragments in spots -
LMP-EVA: Look at that. See that?
LMP-EVA: - from the northwest. Can you get that?
LMP-EVA: And from the southwest.
LMP-EVA: Yes. Go ahead. Keep going. Good shape. Got it.
CDR-EVA: We're 236/2.1.
LMP-EVA: Bob, what I'm looking at is the - northwest portion of Gatsby, where there's a very very concentrated block field on the inner wall, except where there are, on the southwest, three stream_ and on the northwest and north a continuous stream, if you will, on band, radial band, of mantle that is bur - appears to be burying that field, overlying and mantling the field. We got some pretty pic- tures of it, I think.
LMP-EVA: Bob, I'm more and more convinced there's a mantle. One possibility, I guess, is that, if it's a pyroclastic mantle, that in the lunar vacuum environment and with whatever volatiles we're dealing with, the stuff becomes extremely fine upon vesiculation. We may have been on it all the time and not known it - as far as recognizing it.
CDR-EVA: As soon as we come through this draw, ... smooth or free of any debris or boulders it is on the other side of the upslope.
LMP-EVA: Yes. Watch it.
CC: No. We have two of them behind you. We're going to deploy - we're going to deploy one. I'11 give you a reading soon on that.
CDR-EVA: Okay. Well, one - one I deploy at the end I know. I thought we had an extra one here somewhere.
CC: Okay. Yes, that's what I - Okay, that's the one we were planning on deploying all along, and it's there. We'11 be deploying at a range of 0.1, which is Just before you get to the SEP.
LMP-EVA: I guess Sherlock's going to be right over the top over here. I saw it when we were on that other ridge. Tape lllA/43
CDR-EVA: Hey, you know, there's a lot of bad landing places around here. That old Sun angle, I think, shows most of them up. Bob, I - -
CC: And, Geno, we were looking - -
CDR-EVA: I don't under - -
CC: - - at the map here - -
CDR-EVA: - - I don't unders - -
CC: - - and if you keep going straight to the LM, you're probably going to run into this crater area around San Luis Rey. You probably ought to head somewhat south of directly back to the LM, so we can at least tip the - western edge of Sherlock and then pick it up and go from there back to the SEP. It looks like it might be rather rough there in that dotted-lined area, if you can look at the backside of your map, Jack. 244/1.7.
CDR-EVA: Bob, I've already been doing it. I'm at
CDR-EVA: Already been doing that.
LMP-EVA: And, Bob, about - about 200 meters back, we crossed back into our standard mantle surface of about 1-percent fragment cover - -
CC: Okay 200 meters back, you - Okay. Copy that.
CDR-EVA: - - out of this - the block field, which -
LMP-EVA: I can see the LM. where those blocks are.
LMP-EVA: Yes, that's the block field, the Sherlock block field; that's right. That is a block field.
CDR-EVA: Some big ones there.
CDR-EVA: Old station 10. I might even call it 10 Alpha in honor of the Apollo Progr8_ Office. The - -
CC: 10 Bravo, Apollo.
CDR-EVA: - - Apollo Spacecraft Program Office.