mercoledì 25 luglio 2012

Many of the oddities are concentrated in Oceanus Procellarum, including Rümker, the Aristarchus Plateau, Schröter's Valley, and the Marius Hills. Across the Moon most familar small volcanic cones are standard domes like those near Kies, Hortensius and Cauchy. These were constructed by eruptions of lava flows from a central vent. Because the lavas were fluid they didn't build steep hills - normal 
domes have slopes of only a few degrees. But something makes the steeper-sided cones in the Marius Hills. If you look closely at 
Raf's image you may notice that the cones are quite irregular in shape. For some, the bottom has a gentle slope and the top is steeper. 
Others have an associated hilly flow. These observations suggest that the Marius Hills had different origins than the generic dome. There is spectroscopic evidence for ash at many of the cones so it is likely that explosive eruptions may have built 
lunar equivalents to terrestrial cinder cones. The hilly material surrounding some of the cones is probably viscous lava flows. The gentle slopes at the base of other hills may be due to normal dome lavas that are more fluid. So there are two unique features of the Marius Hills - there is a great concentration of volcanoes, and they have more pyroclastics than volcanoes elsewhere on the Moon. Asking why to both of these questions is reasonable, answering is hard.

Chuck Wood

Technical Details
Nov. 25, 2012, 23:28 UT. Mak-Cass 18 cm + Lumenera LU 075M.


Lunar Pioneer

Tuesday, August 13, 2013


An unexpected transit

Rafaello Lena, of the GLR Group in Rome passes along this serendipitous interruption of his efforts to record Earth atmosphere-grazing Perseid meteors and perhaps another lunar impact, captured at 1945 UT, Monday, August 12 . An aircraft, and easily "identified flying object," transits the evening Moon. Still 40 hours shy of its Quarter phase, the Moon was 377,200 km away as the terminator swung over central Mare Serenitatis and the Southern Highlands, sunrise over the 1972 landing site of Apollo 16.


  April 11, 2012

REBIRTH

LPOD-Apr11-12.jpg
image by Raf Lena, Rome, Italy

Kipuka is a lovely word that hardly anyone has heard of unless they've been to Hawaii. A kipuka is a high standing remnant of an earlier terrain now surrounded by lava flows. Raf has documented a classic example of a lunar kipuka, this slight rise (rising about 500 m over a radius of roughly 25 km) cut by the Opelt Rille at the boundary of maria Cognitum and Nubium. With lower resolution there isn't much difference between the rise and the surrounding, so it could be a large dome. But it is clear in Raf's image and the LRO excerpt at left that the rise is more fractured and more pitted with small craters. It isn't the same material - its older. The fact that the rise is cut by fractures suggests that its elevation may have resulted from it being domed upward when it was young. Its a kipuka now, but maybe it was a dome (or swell) before.


Chuck Wood


Related Links

Rükl plate 42

Later Addition

After posting this I came across an image released by NASA's Earth Observatory of young lava flows in Ethiopia. Part of it looked very similar to the kipuka described in today's LPOD.

LPOD-Apr11b-12.jpg
See the EO posting for details.


Wednesday, March 4, 2009


Raffaello Lena - GLRP & Selenology Today #13

From left to right, South to North. A very highly scaled section of a much larger 12.6 cm comparative polarity image of the Near Side portion of the Lunar South Pole, just above the rim of abyssal 19 kilometer wide Shackleton (lower left), future notional site of Armstrong Station, the American portion of the semi-permanently manned lunar outpost presently in the federal budget. Malapert Mountain, on the Right, has been the notional site of every possible multi-purpose lunar outpost imaginable, and for good reason. As on Earth, so it is on the Moon. Real Estate is "location, location, location."


Wow! It's not every day a person in the lunar community receives high praise from two highly respected forums, each of whom are Websites of Record. Nevertheless, there you have it.

That was enough for Lunar Pioneer Research Group to wave our hand and "give it up" for Raffaello Lena of the Geologic Lunar Research (GLR) group, truly dedicated publishers of Selenology Today.

Issue #13 was released on the web today, and this Number is dedicated to LCROSS.

First the LCROSS Observation Group, a primary contact point for amateur Plus Ultra observers preparing to record that impactor in action later this year, express high praise and gratitude to Raffaello Lena for featuring some really fine articles, written by senior members of the group explaining the importance of earth-bound "amateur" observers of the final stage of the LCROSS mission, in this latest issue of Selenology Today #13.

Now, if that were not enough, Raffaello Lena also received some very high praise tonight/this morning from, guess who... Chuck Wood, who put his Moon-powered LPOD spotlight on Mr. Lena, to illustrate "the P in LPOD doesn't just stand for Photograph, it also stands for "People."