In the shadows of secrecy, the National Aeronautics and Space Administration has
embarked on daring expeditions hidden from public knowledge. But they're not venturing into the
unknown alone. Enter Elon Musk, the enigmatic tech genius and billionaire extraordinaire,
partnering with NASA in a mission that promises to shatter our perceptions. Together,
this dynamic duo has pooled their resources and unleashed their insatiable curiosity to
plumb the mysterious depths of our vast ocean. Beneath the waves, during their audacious joint
endeavor, Elon Musk and NASA stumble upon an unforeseen marvel. Its implications are
so far reach that concealing it becomes an impossible feat. A revelation of such
magnitude demands a bold voice, and Elon Musk steps forward to share this unnerving
discovery with the world. But why does he take the lead, instead of the renowned space
agency that initiated the venture? Join us as in today’s video as we uncover the
truth behind Elon Musk's stunning revelation of NASA's terrifying underwater revelation.
Elon Musk, in covert collaboration with NASA, has been orchestrating a series of strategic maneuvers
that promise to be the most groundbreaking scientific partnership of our time. However, their
joint expedition took an unforeseen turn when recent revelations shed light on the extensive
ventures NASA and Musk embarked upon, some of which unfolded in the Arctic. The chain of events
commenced with the deployment of an underwater robot by a team of researchers, unveiling
a spectacle that defied all expectations. This remotely operated underwater vehicle,
known as Ice Fin, delved into the depths of a seawater-filled crevasse within
Antarctica's colossal ice shelf. As the vehicle's cameras relayed their findings,
a mesmerizing transformation unfolded before the astonished eyes of the scientific community. The
once cloudy and smooth meteoric ice walls morphed into a green and rugged texture, signifying
a remarkable shift towards salty marine ice. Simultaneously, NASA, Elon Musk, and New Zealand
researchers observed this astounding phenomenon from a vantage point 1,900 feet above, immediately
recognizing it as a groundbreaking demonstration of ice pumping—an occurrence never before directly
witnessed in an ice shelf crevasse. Justin Lawrence, a visiting scholar
at the Cornell Center for Astrophysics and Planetary Science, vividly described the
awe-inspiring atmosphere within the room as this unexpected sequence of events unfolded. "We beheld
the mesmerizing sight of ice melting below us, flowing into the crevasse, and then refreezing.
And as we ascended further, the inexplicable continued to captivate us," Lawrence shared.
The unparalleled insights gleaned from Ice Fin's unprecedented exploration of the crevasse unveiled
over a century's worth of hidden geological processes beneath the ice shelf. This momentous
discovery profoundly impacted the entire research team, prompting them to document their findings in
a published paper. The comprehensive reports were derived from the Kamb Ice Stream field campaign,
backed by Antarctica New Zealand and other research organizations from New Zealand. Led by
Professor Christina Hulbe from the University of Otago, the team received invaluable support from
Elon Musk, as well as NASA's astrobiology program. Working in conjunction with Brittany Schmidt,
an associate professor leading the Planetary Habitability and Technology Lab at Cornell,
they successfully joined forces and deployed the remarkable Ice Fin. Schmidt's team had
dedicated nearly a decade to developing Ice Fin, and the astonishing results it yielded served as
a testament to their unwavering commitment. By complementing the recent investigations
of the rapidly changing Thwaites Glacier, also facilitated by an Ice Fin vehicle,
this analysis promises to refine sea-level rise models by providing unprecedented high-resolution
views of the ocean. The exploration encompasses not only the sea floor but also the intricate
interactions between ice and contrasting glacial systems within the West Antarctic Ice Sheet.
The Thwaites Glacier, vulnerable to warm ocean currents, stands as one of the most precarious
ice masses on the continent. Meanwhile, the mostly ice-covered Kamb Ice Stream has remained dormant
since the late 1800s. However, if activated, Kamb has the potential to contribute significantly to
rising sea levels, amplifying the region's overall impact by 12 percent. Antarctica,
a complex and dynamic system, demands our attention on both fronts: the swiftly
transforming systems and the more serene ones that hold future risks, remarked Schmidt. By
studying both Kamb and Thwaites in tandem, we gain invaluable knowledge about this enigmatic realm.
NASA and Elon Musk joined forces to provide financial backing for the development of Ice
Fin and the exploration of Kamb, expanding the boundaries of oceanic exploration beyond Earth.
The discovery of marine ice within the crevasse holds significance as it could serve as a parallel
for conditions on Jupiter's icy moon, Europa, which is the primary focus of NASA's upcoming
Europa Clipper mission set to launch next year. In the future, subsequent lander missions might
directly search for microbial life within the ice. Equipped with a comprehensive range of
oceanographic tools on a modular frame, Ice Fin boasts a diameter of less than 10 inches and a
length exceeding 12 feet. It was carefully lowered through a borehole, created by New
Zealand researchers using hot water, into the ice shelf, connected by a tether. Over the course of
three dives, spanning a distance of three miles near the grounding zone where Kamb transitions to
the floating Ross shelf, Ice Fin diligently mapped five crevasses while simultaneously
recording vital water conditions such as pressure, salinity, and temperature. The team also conducted
a thorough analysis of various ice attributes, capturing details on water mixing and melt rates.
Among the intriguing formations observed were ripples, vertical runnels, golf ball-like dimples,
and peculiar features around the top of the crevasses resembling brinicles, consisting of
ice globs and finger-like protrusions. The researchers postulate that the ice
pumping phenomenon within the crevasse could potentially contribute to the relative stability
of the Ross Ice Shelf, which happens to be the world's largest ice shelf by area,
approximately the size of France, in comparison to the vulnerable Thwaites Glacier. Peter Washam,
a polar oceanographer and the second author of the paper, highlighted the protective and self-healing
qualities of large ice shelves, stating, "A lot of the melting that occurred near the grounding
line results in the re-freezing of water, forming marine ice that adheres to the bottom of the ice."
Ice Fin's mapping efforts on the sea floor revealed parallel sets of ridges believed to
be remnants left behind by ice shelf crevasses. This discovery provides a historical record
of 150 years of activity since the stagnation of the Kamb Ice Stream. As the grounding line
retreated and the ice shell thinned, the crevasses gradually lifted away. Lawrence, the lead author
of the paper, emphasized the ability to establish a direct link between the sea floor features and
the observations within the ice, enabling a unique opportunity to "rewind the process" in a sense.
The research undertaken received support from various programs, including the Planetary Science
and Technology from Analog Research Programs, Project Rise Up, and Future Investigators in
NASA Earth and Space Science and Technology Program, which were backed by NASA and Elon
Musk. New Zealand's Antarctic Science Platform and the United States Antarctic Program also played
pivotal roles in providing assistance, along with the involvement of the Hot Water Drilling
Initiative from Victoria University of Wellington. However, this wasn't the only joint creation of
Elon Musk and NASA. Scientists and astronomers have long known that exploring the oceans beneath
the icy surfaces of distant moons requires more than just basic tools. With his vision of
colonizing Mars, Musk joined forces with NASA once again. Their collaboration led to the development
of an underwater rover called BRUIE, designed to navigate the challenges of ocean worlds like
Enceladus and Europa. The ice shells on these moons serve as windows into the hidden oceans
below, where understanding the chemistry of the ice is crucial for uncovering potential
life. At Australia's Casey research station, BRUIE will embark on a month-long expedition,
exploring both inland lakes and the ocean to study the interface between water and ice.
Unlike traditional submersibles, BRUIE overcomes the obstacles posed by ocean currents and power
consumption through its unique buoyancy-based design. This one-meter-long rover crawls along
the underside of the ice, propelled by the denser water below, with large wheels
on each end facilitating its movement. NASA's robot also possesses the ability
to autonomously power on and off while collecting data, with a particular focus on prolonging its
operation beneath the ice without recharging. Beyond its mobility, this rover is programmed
to carry various instruments, including cameras and probes to measure factors like oxygen levels,
water temperature, pressure, and salinity. As data from BRUIE's initial missions returns,
scientists eagerly anticipate incorporating additional instruments into the tests. However,
even with extensive testing, the rover faces a significant challenge in extraterrestrial
exploration: identifying potential life forms that may appear dissimilar to those on Earth.
Dan Berisford, a mechanical engineer involved in the project, highlighted this in a NASA statement,
stating that detecting life forms divergent from what we know on Earth could prove challenging.
Elon Musk's team of scientists, intrigued by the statement and the deep-sea expedition,
confirmed another discovery previously speculated by NASA. A decade ago, during a NASA-sponsored
ocean expedition, scientists stumbled upon thriving populations of phytoplankton beneath
the Arctic Ocean's Sea ice. Now, in collaboration with Elon Musk, researchers are utilizing
underwater instruments and a NASA satellite to gain further insights into this peculiar
finding. Evidence of significant blooms beneath the sea ice has been uncovered, shedding light
on phytoplankton, which are plant-like organisms that absorb sunlight, absorb mineral nutrients,
and generate energy through photosynthesis. Phytoplankton can thrive in sunlit areas of
the ocean, sometimes becoming visible when conditions are favorable. They
play a crucial role as a food source and carbon recycler for the planet. However,
it was commonly believed that phytoplankton growth in the Antarctic Ocean was limited by the
ice cover, which hindered sunlight penetration. Nevertheless, new evidence reveals cracks, thin
spots, and gaps in the compact sea ice that allow sufficient daylight to reach the water below.
While the ice cover may appear impenetrable from satellite views, NASA's ICESat-2 laser technology
has unveiled fractures and openings within the Antarctic Sea ice. Sunlight filtering through
these cracks' fuels significant under-ice blooms in the Southern Ocean, a phenomenon previously
documented in the Arctic but now confirmed in the Southern Ocean. The expansive suitable conditions
for under-ice blooms in Antarctica surpass those in the Arctic, potentially leading to substantial
plankton masses when considering the overall area. This groundbreaking expedition conducted by
NASA and Elon Musk has brought forth remarkable findings. However, the discovery of phytoplankton
and its implications leaves us with mixed emotions and uncertain expectations. What do you anticipate
for the outcomes of these discoveries? Share your thoughts in the comments section below.