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#32
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Tycho was mentioned too, but never flew for obvious safety reasons...
.. .. End the dangerous wasteful shuttle now before it kills any more astronauts.... |
#33
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In article , Matt Wiser wrote:
Since the sites considered for 17 have been mentioned, what about 16? They went to Descartes, and Alphonsus was on the short list for both 16 and 17, where else? The short list was Descartes, Alphonsus, Copernicus, and Kant Plateau. Marius Hills was a late discard, dropped when the decision to concentrate on highland sites was made firm. Alphonsus was rejected as probably contaminated by Imbrium ejecta. Copernicus was particularly notable because its central peak probably contains ancient highland material from down below. However, Apollo 12 had provided a tentative date for Copernicus, it was close to several previous landing sites and thus didn't provide geographical diversity or long baselines for the surface experiments, and what were thought to be post-impact volcanic features were then thought well-understood. Kant Plateau, east of Descartes, shared many of Descartes's virtues and had better photographic coverage, and some thought it offered hope of primitive highland material. But majority opinion was that any primitive material there probably had random impact debris on top, and Descartes seemed to offer a clearer geological context (ironically, debris problems turned out to be very serious at Descartes...). And there was a strong, but incorrect, belief that major features at Descartes were volcanic. Schroter's Valley was a candidate for 18 or 19, as (and I may be wrong on this) TLP have been sighted there and the scientists wanted to see if there was active volcanic activity... The Aristarchus / Cobra Head / Schroeter's Valley area attracted mission planners early on -- lots of strange features, persistent reports of transient events -- but even after later capability improvements, it was really outside the area Apollo could reach. -- "Think outside the box -- the box isn't our friend." | Henry Spencer -- George Herbert | |
#34
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In message , bob haller
writes Tycho was mentioned too, but never flew for obvious safety reasons... "A day late and a dollar short". We've been through this. |
#35
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(Henry Spencer) wrote: In article , Matt Wiser wrote: Since the sites considered for 17 have been mentioned, what about 16? They went to Descartes, and Alphonsus was on the short list for both 16 and 17, where else? The short list was Descartes, Alphonsus, Copernicus, and Kant Plateau. Marius Hills was a late discard, dropped when the decision to concentrate on highland sites was made firm. Alphonsus was rejected as probably contaminated by Imbrium ejecta. Copernicus was particularly notable because its central peak probably contains ancient highland material from down below. However, Apollo 12 had provided a tentative date for Copernicus, it was close to several previous landing sites and thus didn't provide geographical diversity or long baselines for the surface experiments, and what were thought to be post-impact volcanic features were then thought well-understood. Kant Plateau, east of Descartes, shared many of Descartes's virtues and had better photographic coverage, and some thought it offered hope of primitive highland material. But majority opinion was that any primitive material there probably had random impact debris on top, and Descartes seemed to offer a clearer geological context (ironically, debris problems turned out to be very serious at Descartes...). And there was a strong, but incorrect, belief that major features at Descartes were volcanic. Schroter's Valley was a candidate for 18 or 19, as (and I may be wrong on this) TLP have been sighted there and the scientists wanted to see if there was active volcanic activity... The Aristarchus / Cobra Head / Schroeter's Valley area attracted mission planners early on -- lots of strange features, persistent reports of transient events -- but even after later capability improvements, it was really outside the area Apollo could reach. -- "Think outside the box -- the box isn't our friend." | Henry Spencer -- George Herbert | Thanks for the info on 17 and 16. FETM mentioned Marius Hills and Hadley Appenine as sites for 15, with Hadley winning out, were there any others considered? And where was 14 supposed to go originally if 13 hadn't had the...difficulties Lovell and his crew experienced? ----== Posted via Newsfeed.Com - Unlimited-Uncensored-Secure Usenet News==---- http://www.newsfeed.com The #1 Newsgroup Service in the World! 100,000 Newsgroups ---= 19 East/West-Coast Specialized Servers - Total Privacy via Encryption =--- |
#36
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In article , Matt Wiser wrote:
...FETM mentioned Marius Hills and Hadley Appenine as sites for 15, with Hadley winning out, were there any others considered? Pre-13, when 15 was still an H-series (non-rover) mission, it was penciled in for Davy -- a crater chain, thought volcanic, thought to have brought up deep interior material. Early crew training emphasized possible Davy equivalents on Earth. Then Apollo lost two missions, and the original H-series 15 was one of the ones killed. Now 15 was a J mission and probably had a rover (there was some small question whether the rover would be ready in time for 15), and moreover it was one of only three remaining landings. J missions could do a proper job on more complex sites, they could land at somewhat higher latitudes, they had a more flexible descent path that could clear higher uprange obstacles... and Davy wasn't good enough to be worth 1/3 of what was left of Apollo. Descartes would have been a candidate but better landing-planning photos were needed before putting a landing there; 13 hadn't had a chance to do it and 14 would be a bit late. People had been eying the western foot of the Apennines -- part of the Imbrium basin rim -- as a place where deep rocks might be exposed, plus it offered Hadley Rille -- the origin of the rilles still being rather a mystery -- and some mare surface as well. It had originally been seen as hard to reach because of the need to clear the Apennines, but the J-series improvements made it accessible. And the northern position would complete a triangle of surface-instrument sites, and the inclined orbit would carry the CSM over areas not yet seen. So Hadley-Apennine was on the shortlist. The Marius Hills area was the only other major candidate. Thought to be volcanic, thought likely to be a deep volcanic system, and it has its own rilles. Many geologists thought more highly of Hadley, but overall it was pretty much a tie, and Dave Scott broke it in favor of Hadley. And where was 14 supposed to go originally if 13 hadn't had the...difficulties Lovell and his crew experienced? 14 had been tentatively assigned Littrow -- a site somewhat to the west of the Apollo 17 site -- with Rima Bode II being the other short-list site. The objective for either one was to investigate a dark layer interpreted as a pyroclastic deposit from late volcanic activity. After 13's failure, dating of the Imbrium impact (i.e., Fra Mauro) was still a high science priority. Moreover, post-13 program cutbacks meant that 14 was going to be the last H mission. Fra Mauro was unusual in being a site that would *not* benefit much from greater surface mobility, meaning that it was not a good choice for a J mission but was a good fit for the last H. The icing on the cake was that a Fra Mauro mission could get landing-planning photos of Descartes -- already being eyed for one of the J missions -- and a Littrow mission couldn't. (Source for most of this, by the way, is Don Wilhelms's "To a Rocky Moon", an excellent book.) -- "Think outside the box -- the box isn't our friend." | Henry Spencer -- George Herbert | |
#37
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Henry Spencer wrote:
In article , Matt Wiser wrote: ...FETM mentioned Marius Hills and Hadley Appenine as sites for 15, with Hadley winning out, were there any others considered? Pre-13, when 15 was still an H-series (non-rover) mission, it was penciled in for Davy -- a crater chain, thought volcanic, thought to have brought up deep interior material. Early crew training emphasized possible Davy equivalents on Earth. ....snip... People had been eying the western foot of the Apennines -- part of the Imbrium basin rim -- as a place where deep rocks might be exposed, plus it offered Hadley Rille -- the origin of the rilles still being rather a mystery -- and some mare surface as well. It had originally been seen as hard to reach because of the need to clear the Apennines, but the J-series improvements made it accessible. And the northern position would complete a triangle of surface-instrument sites, and the inclined orbit would carry the CSM over areas not yet seen. So Hadley-Apennine was on the shortlist. The Marius Hills area was the only other major candidate. Thought to be volcanic, thought likely to be a deep volcanic system, and it has its own rilles. This bit of history has me somewhat reassured about site selection. The bits and pieces I'd run into suggested a bizarre fixation with recent vulcanism to the detriment of other issues (like dating major events and understanding impacts in the lunar context), so it's good to have that set straight. Gotta put Wilhelms on the holiday reading list... Bill Keel |
#38
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In article ,
William C. Keel wrote: This bit of history has me somewhat reassured about site selection. The bits and pieces I'd run into suggested a bizarre fixation with recent vulcanism to the detriment of other issues... Well, in hindsight there *was* an excessive fixation on recent vulcanism, partly because volcanic theories of lunar features were still fighting a rear-guard action against the rise of impact theories. It really took the Apollo results to hammer home the lesson that the lunar surface was overwhelmingly shaped by impacts and their immediate side effects, with independent vulcanism taking only quite a minor and early role. -- "Think outside the box -- the box isn't our friend." | Henry Spencer -- George Herbert | |
#39
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(Henry Spencer) wrote: In article , Matt Wiser wrote: ...FETM mentioned Marius Hills and Hadley Appenine as sites for 15, with Hadley winning out, were there any others considered? Pre-13, when 15 was still an H-series (non-rover) mission, it was penciled in for Davy -- a crater chain, thought volcanic, thought to have brought up deep interior material. Early crew training emphasized possible Davy equivalents on Earth. Then Apollo lost two missions, and the original H-series 15 was one of the ones killed. Now 15 was a J mission and probably had a rover (there was some small question whether the rover would be ready in time for 15), and moreover it was one of only three remaining landings. J missions could do a proper job on more complex sites, they could land at somewhat higher latitudes, they had a more flexible descent path that could clear higher uprange obstacles... and Davy wasn't good enough to be worth 1/3 of what was left of Apollo. Descartes would have been a candidate but better landing-planning photos were needed before putting a landing there; 13 hadn't had a chance to do it and 14 would be a bit late. People had been eying the western foot of the Apennines -- part of the Imbrium basin rim -- as a place where deep rocks might be exposed, plus it offered Hadley Rille -- the origin of the rilles still being rather a mystery -- and some mare surface as well. It had originally been seen as hard to reach because of the need to clear the Apennines, but the J-series improvements made it accessible. And the northern position would complete a triangle of surface-instrument sites, and the inclined orbit would carry the CSM over areas not yet seen. So Hadley-Apennine was on the shortlist. The Marius Hills area was the only other major candidate. Thought to be volcanic, thought likely to be a deep volcanic system, and it has its own rilles. Many geologists thought more highly of Hadley, but overall it was pretty much a tie, and Dave Scott broke it in favor of Hadley. And where was 14 supposed to go originally if 13 hadn't had the...difficulties Lovell and his crew experienced? 14 had been tentatively assigned Littrow -- a site somewhat to the west of the Apollo 17 site -- with Rima Bode II being the other short-list site. The objective for either one was to investigate a dark layer interpreted as a pyroclastic deposit from late volcanic activity. After 13's failure, dating of the Imbrium impact (i.e., Fra Mauro) was still a high science priority. Moreover, post-13 program cutbacks meant that 14 was going to be the last H mission. Fra Mauro was unusual in being a site that would *not* benefit much from greater surface mobility, meaning that it was not a good choice for a J mission but was a good fit for the last H. The icing on the cake was that a Fra Mauro mission could get landing-planning photos of Descartes -- already being eyed for one of the J missions -- and a Littrow mission couldn't. (Source for most of this, by the way, is Don Wilhelms's "To a Rocky Moon", an excellent book.) -- "Think outside the box -- the box isn't our friend." | Henry Spencer -- George Herbert | Thanks for the information and the source: looks like I'll be trying to find the book in either my county library or my old college library... ----== Posted via Newsfeed.Com - Unlimited-Uncensored-Secure Usenet News==---- http://www.newsfeed.com The #1 Newsgroup Service in the World! 100,000 Newsgroups ---= 19 East/West-Coast Specialized Servers - Total Privacy via Encryption =--- |
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