{"id":37092,"date":"2022-10-20T00:00:00","date_gmt":"2022-10-20T00:00:00","guid":{"rendered":"https:\/\/c01.purpledshub.com\/bbcskyatnight\/?post_type=purple_issue&p=37092"},"modified":"2023-03-30T09:03:21","modified_gmt":"2023-03-30T09:03:21","slug":"a-history-of-the-moon-in-eight-features","status":"publish","type":"post","link":"https:\/\/c01.purpledshub.com\/bbcskyatnight\/2022\/10\/20\/a-history-of-the-moon-in-eight-features\/","title":{"rendered":"A history of the Moon in eight features"},"content":{"rendered":"\n

The Moon bears the scars of its long and violent past. Astronomer Will Gater <\/strong>looks at eight features that reflect its extraordinary history that you can see for yourself <\/p>\n\n

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Few objects in the Solar System record the remarkable history of our planetary neighbourhood more starkly than the Moon. Not only does it bear the scars of eons of impacts by asteroids and comets, but its very existence is testament to a cataclysmic collision that\u2019s thought to have forged the Earth we stand on today. When we gaze at the airless lunar surface, a barren landscape of deep shadows, shining mountain peaks and grey basalt plains, we can also reflect on our own small imprint, quite literally, on the cosmos. The footprints of humanity\u2019s first Solar System explorers remain there even to this day, and likely will do for millennia yet. In this feature, we highlight eight areas for you to examine with a telescope that tell the story of the past, present and future of our nearest neighbour. Let\u2019s start by rolling the clock back to the Moon\u2019s early days. <\/p>\n\n

<\/div>
\n

Where to find our eight lunar features <\/strong><\/h4>\n\n\n\n

An at-a-glance observing guide <\/p>\n\n\n\n

\"\"<\/figure><\/div>\n<\/div><\/section>\n\n

1. The seas of the lunar nearside <\/strong><\/h4>\n\n

Eons of heavy bombardment formed the Moon\u2019s basins <\/strong><\/p>\n\n

KIT: Naked eye\/Small telescope<\/strong><\/p>\n\n

\"\"
Mare Nectaris, an easy spot with its bright stripe, is an impact basin that flooded with lava <\/figcaption><\/figure><\/div>\n\n

About 4.5 billion years ago, the Moon was formed in a violent impact when an object about the size of Mars smashed into the early Earth. This cataclysm left a cloud of superheated material circling Earth that, so our current understanding goes, eventually coalesced into the Moon. After around 500 million years, our companion in space had cooled to form a solid body, rather than a seething ball of molten rock. But it was around this time that another series of massive impacts are thought to have occurred. These punched into the lunar globe, leaving enormous scars across its surface, known as basins. <\/p>\n\n

Over time these are believed to have been filled in by immense flows of molten rock from within the Moon, becoming the lunar \u2018seas\u2019 we observe on the Moon today. Known to astronomers as \u2018maria\u2019, these dark regions create the \u2018face\u2019 in the Moon and are visible to even the naked eye. They are made of dark, basaltic rock and extend in vast, vaguely circular plains across much of the lunar nearside. One of the most interesting to observe with a small telescope is the Mare Nectaris, in the southeast quadrant of the Moon\u2019s disc. Thought to be just under four billion years old, when the lighting conditions are right \u2013 as they will be on the nights of 12 and 29 November \u2013 you can still see hints of concentric ring shapes thought to be left over from its formation. <\/p>\n\n

2. Mare Serenitatis wrinkle ridges <\/strong><\/h4>\n\n

A shrinking skin lined the Moon\u2019s face with wrinkles <\/strong><\/p>\n\n

KIT: Small telescope<\/strong><\/p>\n\n

\"\"
The Sea of Serenity looks smooth but is riddled with tectonic ridges <\/figcaption><\/figure><\/div>\n\n

As you cast your eye over some of the lunar seas at the telescope eyepiece, you may notice that these ostensibly smooth basalt plains actually show subtle textures. Not only are there clear variations in their colour \u2013 or rather shade of grey \u2013 but they also contain features where the land rises and falls in distinct narrow ridges, winding across the surface. These are known as \u2018wrinkle ridges\u2019 and for a while there was a debate about how exactly they formed. Were they volcanic in origin or a product of the seas deforming as these landscapes contracted after their formation? Scientists now think that in most cases it was likely the latter: the ridges emerged when the lunar seas experienced underground movements that wrinkled up the expansive basalt plains above. <\/p>\n\n

With a small telescope of around 4\u20136 inches in aperture, the best time to look for wrinkle ridges is when they are illuminated obliquely, that is when they are positioned near to the terminator. We\u2019ve chosen to highlight Mare Serenitatis, pretty much the entirety of which is criss-crossed by wrinkle ridges, and which recent research suggests formed around 3.4 billion years ago. They will be well-lit on 12 and 13 November. There are also some other wonderful examples in the northern Mare Imbrium, close to the Bay of Rainbows, so you may want to note when the terminator passes through the region.<\/p>\n\n

3. Vallis Schr\u00f6teri <\/strong><\/h4>\n\n

An immense eruption made the longest valley on the Moon\u2019s near side <\/strong><\/p>\n\n

KIT: Small telescope<\/strong><\/p>\n\n

\"\"
The snake-like 160km valley sits close to prominent crater Aristarchus, terminating in a wide feature called the Cobra\u2019s Head <\/figcaption><\/figure><\/div>\n\n

Lunar volcanism has sculpted and shaped many of the surface features we see through a telescope today. The next two stop-offs in our history of the Moon demonstrate this perfectly. <\/p>\n\n

Within the great expanse of the lunar sea known as Oceanus Procellarum, on the western side of the Moon, lies the striking crater Aristarchus. You can\u2019t miss it. Even in binoculars its bright walls stand out prominently from the darker plains surrounding it. Yet, look at it with a telescope and you\u2019ll notice there\u2019s an even more intriguing feature than Aristarchus lying close by. Extending away from the crater to the northwest is a wiggling line, known as the Vallis Schr\u00f6teri or Schr\u00f6ter\u2019s Valley. This is what lunar geologists refer to as a \u2018sinuous rille\u2019 and it is thought to have been formed about 2.5 billion years ago when an immense eruption of lava carved a long, valley-like path through the landscape. In total Vallis Schr\u00f6teri wanders over 160km across the lunar surface and is around 500 metres deep. Its large extent means that the valley is pretty easy to see in a small scope \u2013 though as we\u2019ve seen with other features, the right illumination is key. To really see it well this month, aim to observe it on the nights of 6 and 7 November, as well as 18 November.<\/p>\n\n

4. The Marius Hills <\/strong><\/h4>\n\n

A landscape littered with enigmatic volcanic lunar domes <\/strong><\/p>\n\n

KIT: Small\/Large telescope<\/strong><\/p>\n\n

\"\"
The lighting has to be just right to see these rough, pimply volcanic mounds<\/figcaption><\/figure><\/div>\n\n

Heading south across the Oceanus Procellarum we reach another volcanic landscape thought to have emerged two to three billion years ago, but which may be as young as 800 million years in places. The surface here, west of the bright crater Kepler, is dominated by huge areas of flat lunar sea and a scattering of moderately-sized craters. Yet when the terminator sits close to the crater Marius, it is possible to see that there are numerous small peaks in this region rising up from the smooth basalt surroundings of Procellarum. <\/p>\n\n

These raised \u2018bumps\u2019 are known as the Marius Hills. Referred to as lunar domes, they are similar to shield volcanoes on Earth, which form when lava oozes onto the surface creating rounded volcanic peaks. Magma coming up from deep below the surface may then have caused further eruptions that formed the valley-like rilles in this area. These can also be photographed with modest imaging equipment on large telescopes. To see the Marius Hills well visually, though, you\u2019ll need a telescope of 150\u2013200mm and a night of good seeing. <\/p>\n\n

5. Copernicus crater <\/strong><\/h4>\n\n

Apollo 12 and 14 explored south of the crater and returned samples of ejecta from its formation <\/strong><\/p>\n\n

KIT: Naked eye\/Binoculars\/Small telescope<\/strong><\/p>\n\n

\"\"
Copernicus with its stunning stair-like terraced walls <\/figcaption><\/figure><\/div>\n\n

There is perhaps no better reminder of the Moon\u2019s dramatic history than the myriad craters that pepper its globe \u2013 from the centimetre-sized ones visible in Apollo surface images, all the way up to those large enough to see from Earth with the naked eye. The rate of asteroid and comet impacts has dropped off over time, but even today small meteoroids still slam into the surface. <\/p>\n\n

The craters of the Moon have been central to piecing together its history. When linked to the samples returned home by the US Apollo missions, the density of craters on any given surface and how they overlap can be used as proxies for the age of that landscape. Detective work like this leads planetary scientists to believe that the crater Copernicus is 800 million years old. Its formation marks the start of the \u2018Copernican\u2019 era that extends to the present. Copernicus is one of the Moon\u2019s most visually stunning craters. As well as having rippling terraced walls that change appearance over the lunar day, it is surrounded by an impressive ray system. These were made when ejecta was thrown over 600km away during the violent impact that created Copernicus. To see this extraordinary feature for yourself, seek it out on the nights around 4 November and 15 November using binoculars or a small telescope.<\/p>\n\n

6. The Apollo 11 landing site <\/strong><\/h4>\n\n

A small moment in the Moon\u2019s lifetime, but a giant leap for mankind <\/strong><\/p>\n\n

KIT: Large telescope<\/strong><\/p>\n\n

\"\"
In the southern Sea of Tranquility, track down from crater duo Ritter and Sabine towards Moltke to find Apollo 11\u2019s landing site <\/figcaption><\/figure><\/div>\n\n
\"\"
A Lunar Reconnaissance Orbiter photo taken from just 24km up shows the tracks from Aldrin and Armstrong\u2019s 2.5-hour moonwalk <\/figcaption><\/figure><\/div>\n\n

Our next stop brings us to where the timeline of our own species and that of our nearest neighbour intersect. More than 50 years ago, humanity made its first steps onto another world during the Apollo 11 mission. The landing site where US astronauts Neil Armstrong and Edwin \u2018Buzz\u2019 Aldrin completed that historic exploration lies in the southern half of the Mare Tranquillitatis, the Sea of Tranquility. While it is not possible to see any of the mission hardware that the crew left there with a telescope from Earth, NASA\u2019s Lunar Reconnaissance Orbiter in orbit around the Moon has been able to photograph the lunar module descent stage and trails left by the astronauts. It can still be fun to track down the landing area at the eyepiece, though. This month, 11 and 12 November are good nights to go looking for it. First locate the pair of craters Ritter and Sabine on the edge of the Mare Tranquillitatis. Then track your eye towards the promontory that pokes out into the sea close to the crater Moltke. About halfway along this line is the area where Apollo 11 landed. <\/p>\n\n

7. Chang\u2019e 5 landing region <\/strong><\/h4>\n\n

The vast Ocean of Storms, where the Chinese led the vanguard of modern missions <\/strong><\/p>\n\n

KIT: Small telescope<\/strong><\/p>\n\n

\"\"
The solidified magma surface of Oceanus Procellarum where Chang\u2019e 5 landed <\/figcaption><\/figure><\/div>\n\n
\"\"
The spacecraft drilled and scooped rock and soil from the region in late 2020 <\/figcaption><\/figure><\/div>\n\n

We may not have walked on the Moon for decades, but uncrewed missions have continued to explore it in our place. Today, the US Lunar Reconnaissance Orbiter circles the Moon capturing exquisitely detailed images, while recent Chinese missions have heralded a new era of robotic lunar surface exploration. <\/p>\n\n

Among these is the Chang\u2019e 3 mission, whose lander and rover touched down in 2013, and the Chang\u2019e 4 mission that made the first landing on the lunar far side, in Von K\u00e1rm\u00e1n crater, in 2019. It was able to return high-resolution images of the area and deploy a rover to explore features up-close. Another success for the Chinese came in 2020, with the landing of Chang\u2019e 5. It was deployed to a landing site in the northern Oceanus Procellarum or Ocean of Storms, where it gathered almost 2kg of samples that were returned to Earth by a spacecraft waiting in lunar orbit. Chang\u2019e 4\u2019s landing site is hidden from view on the far side, but with a small telescope it is possible to see the wide region that Chang\u2019e 5 studied. The landing site is a little way northeast of the fascinating volcanic feature Mons R\u00fcmker, which will be wellpositioned for observation on 7, 8 and 9 November.<\/p>\n\n

8. The lunar south pole <\/strong><\/h4>\n\n

The first woman on the Moon will probably walk at its southern pole <\/strong><\/p>\n\n

KIT: Large telescope<\/strong><\/p>\n\n

\"\"
NASA has identified 13 potential landing sites for Artemis III\u2019s crew around the southern pole\u2019s craters <\/figcaption><\/figure><\/div>\n\n

We finish our observing tour with a look to the future. While the Moon will be largely unchanged for eons, it may once again become a destination that humans visit and explore. Certainly that\u2019s the hope of many space agencies and commercial entities around the world. <\/p>\n\n

But such plans have been mooted for decades and deadlines all too often slip further beyond the horizon. Will the current push to return there, perhaps for longer periods, be the one that finally happens? If it is, there is one place that will be high on the list of possible landing sites: the lunar south pole region, near Shackleton crater. In fact, NASA has already picked out several potential landing spots in the region for its planned human landing mission, Artemis III. There, permanently shadowed craters offer the promise of water-ice, which could be used for making rocket fuel, while sunlit peaks and crater rims provide sites for bases with solar panels. For us amateur astronomers, the south pole region is also a fascinating area to take in at the eyepiece, with huge craters, mountains and undulating terrain creating a rich and captivating view in medium- to large-aperture telescopes using high magnification. Cast your eye over it when conditions are favourable on the nights of 11 and 12 November, because it could be a place where the next chapter in the Moon\u2019s history is about to be written\u2026 <\/p>\n\n

\n\n
\"\"<\/figure><\/div>\n\n

Will Gater <\/strong>is an astronomy journalist, author and presenter. <\/p>\n\n

<\/p>\n\n

<\/div>\n\n

PHOTOS: WILL GATER, PETE LAWRENCE, NASA GODDARD\/ARIZONA STATE UNIVERSITY, CNSA\/CLEP<\/p>\n","protected":false},"excerpt":{"rendered":"

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