Blue Moon Rayed-Crater Blowout

Like "catching some rays"? This weekend's Blue Moon invites us to explore the beauty and dazzle of crater rays, the tracks left by powerful impacts in the not-so-distant past.

You may need sunglasses for these rays

Full frontal lighting by the Sun at full Moon nixes shadow detail, but highlights crater rays large and small.
Frank Barrett / celestialwonders.com

Your calendar has a special surprise this month — two Full Moons. The first occurred on July 1st across the Americas and the second, a "Blue Moon," happens early Friday morning July 31st. What are we to do with such an abundance of moonlight? Let's use the opportunity to explore rays and what I like to call "beacon craters."

Every lunar phase brings a unique set of lighting circumstances that highlights a particular class of features. Crescent Moons focus our attention on rarely noticed seas and craters along the lunar limb; a half Moon bowls us over with the richness and diversity of craters and rills. A full Moon usually means "time to relax" and catch up on sleep, but let's go rogue this weekend. After all, there won't be another Blue Moon till January 31, 2018.

At full Moon, the Sun shines over the Earth’s “shoulder,” hitting the Moon’s face square on and lighting up one whole side of the lunar globe. Just as a light shining directly in your face hides the shadows cast by your nose, cheekbones and wrinkles, so the Sun shining in the Moon’s face hides all shadow detail. The result: a flat, pasty, two-dimensional moon. Not much to look at, right? I beg to differ.

Rayed craters come into their own then, as do a plethora of smaller craters, both with and without rays, that light up like stars or tiny explosions in the shadowless full Moon afternoon.

Old rock sprinkled atop new

The impact that excavated the crater Copernicus (top) about 800 million years ago ejected boulders and pulverized highland material across hundreds of miles to create one of the Moon's most striking ray systems. Some of the boulders unearthed brighter, unweathered material upon impact. The crater Pytheas, northeast of Copernicus, is visible below and left of center. A prominent ray, perforated with secondary impact craters, lies to its east (left) and is easy to see in a small scope.
NASA / Apollo 17

Rayed craters are craters surrounded by halos of impact debris that were excavated when meteorites and asteroids struck the Moon long ago. Pulverized rocks from those impacts fled the scene of the crime as great plumes of ejecta that moments later crashed back down to the surface tens to hundreds to even a thousand miles or more from ground zero.

Frozen splashes in time

The full Moon displays more than a dozen easily visible rayed craters in a small telescope. Besides the obvious Tycho–Copernicus–Kepler–Aristarchus quartet, don't miss the smaller but brilliant Byrgius, the twin "Headlights" (Stevinus R and Furnerius C), Proclus, and the side-by-side Menelaus and Manilius.
Frank Barrett

Some of the falling rocks were large enough to create secondary impact craters that exposed fresh crustal materials untainted by space weathering. That’s why ray systems are bright compared to much of the lunar surface — the impacts that created them happened relatively recently. In other cases, such as the magnificent Copernicus system, the impact dug through the darker mare lavas into the original bright, highland crust and mixed this deeper, lighter-toned rock with that excavated by secondary impacts.

The brightest, most extensive system of rays emanates from 53-mile-wide Tycho, which formed an estimated 108 million years ago. Perhaps an observant Deinonychus caught site of the flash of impact. Rays fade over time; they're sand blasted by micrometeorite impacts and bombarded at the atomic level by the solar wind and cosmic rays until they darken and blend into the surrounding landscape.

Lunar glare bomb

The interior of Aristarchus (left) is one of the brightest locales on the Moon. Through a telescope around full Moon it looks like a 100-watt bulb aimed in your face. Rocks exposed inside the crater may be bright highland material or possibly even granites. That, combined with its relative youth, makes the crater highly reflective.
NASA / Apollo 15

After Tycho, craters Copernicus, Kepler, and Aristarchus are the obvious standouts in the rayed crowd. While Aristarchus's rays aren't as broad or contrasty as those of Copernicus, the crater's relatively youthful age of 450 million years makes it the brightest large formation on the Moon. Nothing compares to its dazzle.

Volcanic imposter

Proclus, 17 miles wide, looks like it's blowing its top. The optical illusion is caused by missing rays along its southwestern side due to the oblique impact that formed the crater.
NASA / Apollo11

Located near the opposite limb of the Moon, Proclus is second behind Aristarchus in brilliance and proof that not all rays form neat radial patterns. Streamers shoot off to the east, north, and south, but are missing to the southwest, hinting that Proclus formed in an oblique, low-angle impact. To my eye, the asymmetry makes the crater look like a caldera atop a volcano spewing fire and ash. What do you see?

Field of beacons

Dozens of youthful craters looking like a field of stars are visible around the time of full Moon north and east of Tycho. The dazzling "Cassini's Bright Spot" may or may not be related to Tycho's ejecta. Click for hi-resolution view.
Frank Barrett, with labels by the author

While you're in the neighborhood, be sure to stop by the crater Langrenus to nuzzle its fuzzy corona of fainter rays. On your way there, you just might get caught in the striking pair of "headlights" on either side of Stevinus.

I've saved the best for last. A motherlode of rayed and otherwise brilliant craters lies in a large region of ancient highlands bounded by Tycho to the south and the Menelaus–Manilius pair to the north. At full Moon, hundreds of freshly-punched craters so carpet the landscape, it resembles a glimmering field of stars. Use a magnification of 100x or higher to experience the full effect.

You'll find many of these tiny, barely-resolved bright spots on the full Moon, but nowhere are they more concentrated than here. My personal favorite is Hipparchus C, a 10-mile-wide perfectly circular divot. Many are undoubted tiny rayed craters, but some may get a boost from either the opposition effect, coherent backscatter, or both. For sure, the entire full Moon gets a kick from both processes, the reason it's brighter than can be accounted for compared to partial phases just before and after full.

Direct light vs. side lighting

From our perspective on Earth, the full Moon (left) is squarely lit by the Sun. With all shadows removed, the moon experiences an extra surge in brightness. At other lunar phases (right), sunlight shines from the side, creating shadows that add a third dimension to the landscape and tone down the Moon's brightness compared to full.
Bob King

The opposition effect is basically shadow-hiding. At full Moon, sunlight streams past Earth and strikes the Moon straight in the face, not off to one side as it does during other phases. Shadows cast by rocks and other irregularities "hide" behind those objects. Without shadows to "darken" the scene, the view directly in front of us peaks in light intensity.

Astronauts wear halos

Left photo: Apollo 17 astronaut Gene Cernan photographs his shadow on the moon surrounded by a bright halo caused by a local "opposition effect" as well as backscatter from fine lunar dust. Right photo: The  Apollo 16 astronaut taking the picture on the left side of the frame has the Sun directly behind his back with a bright "opposition" halo around his head. His companion's shadow has no halo — from the perspective of the first astronaut — because that astronaut stands off to the side at an angle to the Sun. Grains of lunar soil are especially bright directly opposite the sun because their shadows are hidden and coherent backscatter is at work.
NASA

Coherent backscatter also plays an important role in lighting up rays, craters, and the landscape in general. When a light source shines at a very direct angle at material made of a multitude of tiny, dust-like particles, multiple reflections combine to produce a single brighter reflection directly back at the observer. Retro-reflection of sunlight by the crystalline minerals making up the lunar regolith may also play a part. Rays and "fresh" craters are already brighter than the surrounding landscape, but only become more so at special times like full Moon.

So don't stay inside and hide like a shadow behind a rock this Friday and Saturday. Grab your scope and a lunar filter and I guarantee you'll walk away with a sparkle in your eye.


Taking your telescope out to look at the full Moon? Be sure and bring along a Sky & Telescope Moon map!

6 thoughts on “Blue Moon Rayed-Crater Blowout

  1. Anthony BarreiroAnthony Barreiro

    Thanks Bob. I look at the Moon through mounted binoculars or a small refractor pretty much every clear evening or morning. At my club’s monthly public star party this past Saturday night July 25 I was showing the Moon through mounted 15×70 binoculars — this was overkill, as the visitors lost their dark adaptation! One fellow was quite taken by Copernicus, and pleased that he was able to identify it from a map. This led to an interesting discussion of the relative ages of different craters, and then he noticed the ejecta ring and rays around Copernicus.

    From my back yard on Monday night July 27, once I looked away from the terminator, I noticed that the full Moon albedo features were really starting to stand out.

    I was a little confused by the pictures from the Apollo spacecraft in this article. They’re taken from different directions, and it took some neck gymnastics to figure out which way we’re looking in each picture.

    1. Bob KingBob King Post author

      Thanks Tony. The picture on the left has the Sun at the astronaut’s back and he’s facing into his haloed shadow. The right hand photo shows the same thing (another halo around the left astronaut’s head) and also the LACK of a halo around the second astronaut. That astronaut lacks a halo because his companion sees him from the side. You only get the opposition effect if the Sun, your head and a small patch of ground below are in alignment just like Sun, Earth and Moon during Full Moon. Does that help to explain it better?

      1. Anthony BarreiroAnthony Barreiro

        Thanks Bob. I get the halo effect. I was referring to the pictures of Pythias, Aristarchus, and Proclus that seem to have been taken from the LEM flying above the Moon’s surface, although perhaps they were taken from the command module in lunar orbit.

        Anthony

        1. Bob KingBob King Post author

          Tony,
          Sorry, I misunderstood your reference. Yes, the directions are kittywampus from orbit, so I tried to make sense of them, for instance, in the Pytheas-Copernicus caption, for the sake of observers.

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