Humanity Sees the Other Side of the Moon
1959 — Luna 3 Photographs the Far Side of the Moon
First photograph: 03:30 UTC
On October 7, 1959, humanity saw a landscape that had
remained hidden throughout all previous human history. It was the other side of
the Moon. At 03:30 UTC, the Soviet spacecraft Luna 3 began
photographing the lunar far side. The accomplishment was remarkable not simply
because of the distance involved, but because of a fundamental characteristic
of the Moon's motion. The Moon rotates on its axis. But it takes approximately
the same amount of time to rotate once as it takes to orbit Earth once. This
condition, called synchronous rotation, causes nearly the same lunar
hemisphere always to face Earth. Small oscillations known as libration allow
observers to see somewhat more than half of the lunar surface over time. But a
large portion of the Moon remained permanently hidden from direct observation
on Earth. Generations of astronomers could map craters, mountains, and dark
volcanic plains on the familiar lunar face. No telescope, regardless of its
power, could look around the Moon and show what lay beyond its edge. To see the
far side, humanity would have to send a camera there. Luna 3 did exactly that. The
spacecraft had launched on October 4 and swept past the Moon's southern polar
region on October 6. Its trajectory then carried it behind the Moon and
outward, placing its cameras in position to look back at the illuminated far
hemisphere. At 03:30 UTC on October 7, from a distance of roughly 63,500
kilometers from the lunar surface, the photographic sequence began. Over
approximately 40 minutes, Luna 3 exposed 29 photographs. Together
they covered about 70 percent of the Moon's far side. Taking the
pictures was only the first challenge. There were no digital cameras. Luna 3
used photographic film. The spacecraft therefore contained an automated
miniature photographic laboratory. After exposure, the film was chemically
developed, fixed, dried, and then scanned electronically. The resulting image
information could be transmitted toward Earth by radio. It was, in effect, a
photographic laboratory and long-distance image transmitter traveling through
deep space. Seventeen usable photographs were eventually received on Earth. By
modern standards, they were poor. They were grainy. Contrast was limited. Fine
surface details were difficult to distinguish. But their scientific importance
did not depend upon photographic beauty. For the first time, human beings could
see enough of the hidden hemisphere to recognize its large-scale geography. And
the far side contained a surprise. It looked different. The familiar
Earth-facing hemisphere contains enormous dark regions known as maria—ancient
impact basins later flooded by basaltic lava. These broad plains create many of
the patterns people have imagined as a “Man in the Moon.” The far side showed
far fewer large maria. Instead, much of it appeared bright, rugged,
mountainous, and densely cratered. Among the features visible in Luna 3's
photographs was a dark region later named Mare Moscoviense—the Sea of Moscow.
Other features received names as astronomers began constructing the first maps
of the newly revealed hemisphere. Later lunar spacecraft would greatly improve
upon Luna 3. Zond probes photographed additional territory. American Lunar
Orbiter spacecraft mapped potential Apollo landing regions and other portions
of the Moon. Apollo astronauts saw the far side directly as they traveled
around the Moon. Modern spacecraft such as the Lunar Reconnaissance Orbiter
have mapped the entire lunar surface at resolutions Luna 3's engineers could
scarcely have imagined. Those later observations revealed one of the solar
system's largest impact structures—the enormous South Pole-Aitken basin—spanning
much of the lunar far side. Scientists also came to understand why the two
hemispheres differ so strongly. The Moon's crust is generally thicker on the
far side. On the near side, enormous ancient impacts penetrated more deeply and
were followed by extensive volcanic flooding, producing the dark maria visible
from Earth. The far side experienced a different geological history. But before
scientists could explain that difference, they first had to discover it. Luna 3
provided the first glimpse. The achievement becomes even more remarkable when
placed in chronological perspective. Only two years and three days earlier,
Sputnik 1 had become the world's first artificial satellite. Now a spacecraft
had traveled to the Moon, passed behind it, automatically photographed an
unseen world, developed the pictures onboard, and begun the process of
returning those images across hundreds of thousands of kilometers of space. The
Space Age was barely two years old. Already, humanity had seen beyond the
horizon of another world. Why It Matters: Luna 3's photographs gave
humanity its first view of the Moon's far side and revealed that the two lunar
hemispheres are strikingly different. The mission transformed an entire
hemisphere from an unknowable region into a place that could be photographed,
mapped, named, and scientifically investigated. It also demonstrated
sophisticated deep-space navigation, automatic photography, onboard film
processing, and long-distance image transmission at the very beginning of the
Space Age.
Also on This Day
2008 — Asteroid 2008 TC3 Strikes Earth Exactly Where
Astronomers Predicted
Atmospheric entry approximately 02:46 UTC
Before dawn on October 7, 2008, a small asteroid entered
Earth's atmosphere over northern Sudan. Such events are not unusual. Small
objects from space enter the atmosphere regularly, most burning up harmlessly
before reaching the ground. This event was different. Astronomers knew it
was coming. For the first time, an asteroid had been discovered in space
before an Earth impact and its arrival time and location successfully
predicted. The story began only about 20 hours earlier. At 06:39 UTC on
October 6, astronomer Richard Kowalski, working with the Catalina
Sky Survey's 1.5-meter telescope on Mount Lemmon in Arizona, detected a rapidly
moving object. The observations were sent to the Minor Planet Center. Orbital
calculations quickly produced an extraordinary conclusion. The object was on a
collision course with Earth. It received the designation 2008 TC3. The
asteroid was tiny by planetary-defense standards—only a few meters across. It
posed no serious threat to people on the ground. But scientifically, it
presented an unprecedented opportunity. Observatories around the world began
tracking it. During the hours before impact, professional and amateur
astronomers supplied hundreds of positional measurements, allowing scientists
to refine the asteroid's trajectory. NASA's Jet Propulsion Laboratory
calculated that it would enter Earth's atmosphere above northern Sudan at
approximately 02:46 UTC on October 7. And it did. The asteroid struck
the atmosphere at roughly 12.8 kilometers per second. At high altitude
above the Nubian Desert, it exploded in a brilliant fireball. For a time,
scientists thought the object might have been completely destroyed. Then came
another remarkable development. Meteor astronomer Peter Jenniskens
joined Muawia Shaddad of the University of Khartoum and Sudanese
students and researchers to search the predicted fall area. They found
meteorites. Eventually, hundreds of fragments were recovered from the Nubian
Desert. The meteorites became known collectively as Almahata Sitta,
Arabic for “Station Six,” after a nearby railway stop. Scientists could now do
something unprecedented. They had astronomical observations of an asteroid while
it was still in space. They also possessed physical pieces of that same
asteroid in laboratories on Earth. The connection between asteroid astronomy
and meteorite science had become direct. Analysis revealed that 2008 TC3 was
compositionally unusual, containing a diverse mixture of materials associated
with a rare meteorite type known as ureilites. The event also
demonstrated the rapidly improving capabilities of near-Earth-object surveys. A
small asteroid had been found only hours before impact, yet the international
astronomical community had been able to determine where and when it would
arrive. Larger hazardous asteroids are generally detectable at much greater
distances, potentially providing far more warning. Why It Matters: 2008
TC3 was the first asteroid discovered and tracked in space before its impact
with Earth was successfully predicted. The subsequent recovery of meteorites
linked telescopic observations of a specific asteroid directly with laboratory
samples, while the accurate impact forecast demonstrated an important
capability for modern planetary defense.
The Bigger Picture
October 7 brings together two events separated by nearly
half a century. At first they seem unrelated. Luna 3 looked outward toward the
Moon. Astronomers tracking 2008 TC3 looked for something coming toward Earth. But
both events depended upon the same fundamental ability: predict where an
object in space is going to be. Luna 3 could photograph the far side only
because engineers understood its trajectory well enough to send it around the
Moon and place it in the correct position at the correct time. 2008 TC3 could
be predicted to strike northern Sudan because astronomers measured its position
repeatedly and calculated its future path. This is celestial mechanics
transformed into practical capability. For centuries, astronomers used
mathematics to predict where planets would appear in the sky. During the Space
Age, those same principles acquired new purposes. They allowed us to send
spacecraft toward other worlds. And increasingly, they allow us to identify
objects that might come toward ours. The two events also represent different
forms of discovery. Luna 3 discovered by seeing something for the first time.
2008 TC3 demonstrated discovery through prediction. Scientists did not
merely watch the asteroid appear as a fireball and then reconstruct what had
happened. They saw it coming. That distinction is fundamental to planetary
defense. Finding an asteroid after it passes Earth tells us about the
population of near-Earth objects. Finding one before an encounter gives us
options. For an object only a few meters across, as 2008 TC3 was, the
appropriate response is observation. For a substantially larger asteroid
discovered sufficiently far in advance, the possibilities could eventually
include deflection. That is the same planetary-defense story we encountered on
September 26 with DART. DART demonstrated that humanity can deliberately
change the motion of an asteroid. 2008 TC3 demonstrated another essential part
of the equation: first, we must find it and determine where it is going. October
7 therefore spans two very different frontiers. In 1959, an entire hemisphere
of the Moon lay beyond human sight. In 2008, astronomers detected a tiny object
in the darkness of space and predicted where it would meet Earth. One expanded
the world we could see. The other expanded our ability to anticipate what might
reach us. Both began by looking carefully into the sky.
At a Glance
1959 — 03:30 UTC — Luna 3 begins photographing the
Moon's far side from roughly 63,500 kilometers above the lunar surface, giving
humanity its first views of a hemisphere that had never before been seen.
2008 — Approximately 02:46 UTC — Asteroid 2008 TC3
enters Earth's atmosphere over northern Sudan at the location and time
astronomers had predicted, becoming the first asteroid discovered before impact
whose collision with Earth was successfully forecast.