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Mystery drones emerging from the ocean and they are not from USA or any other country
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By USH
For over 80 years, covert research into exotic propulsion, anti-gravity systems, and spacetime manipulation has been housed within deep black programs, classified efforts shielded from both public and congressional oversight.
Now, on April 14, 2025, Michael Katzios, the new White House science chief, made a bold claim: “Our technologies permit us to manipulate time and space...” Shortly after, he doubled down, promising innovations that would let us “bend time and space” and “drive us further into the endless frontier.” These weren’t offhand remarks, they were published on the official White House site, signaling intent.
What does "Manipulating Spacetime" really mean? Spacetime is the four-dimensional framework of our universe. Per Einstein’s theory, mass and energy warp this fabric, creating gravity and affecting time. To manipulate it would mean bending reality itself, shortening distances, warping time, or enabling faster-than-light travel.
Just days before Katzios’ remarks, President Trump said: “We have a weapon that no one has a clue what it is... more powerful than anything even close.” Was he referencing to a spacetime weapon?
Trump isn’t the first high-level figure to hint at such capabilities. Back in 2019, Lt. Gen. Steve Kwast publicly discussed technology capable of transporting a person anywhere on Earth in under an hour, suggesting real-world applications of physics far beyond current norms. He also touched on wireless, space-based energy transmission.
Rumors have long circulated about transatmospheric vehicles, craft capable of seamless operation both within Earth’s atmosphere and in space. Though unconfirmed, these platforms may represent a technological bridge between known aerospace systems and genuine spacetime engineering. (Consider Gary McKinnon’s 2002 discovery during his hack of U.S. military systems: references to a secret space fleet and "non-terrestrial officers.")
But it is not only about manipulating time and space.
What might they also have: Anti-Gravity Propulsion: Altering inertia with plasma or exotic materials, referenced in Navy patents. Warp Drives: Bending space around a craft to move without motion. Zero-Point Energy: Tapping the quantum vacuum for limitless energy, a paradigm-shifting source of power.
But why some groups want to keep it secret? There are compelling reasons for secrecy, none of them rooted in public interest:
Control of Power – Whoever controls this tech controls the future. Economic Impact – It would collapse the fossil fuel, aviation, and defense sectors. Weaponization Risk – These tools could be catastrophic in the wrong hands. Psychological Shock – It would rewrite everything we know about science and our place in the cosmos.
Despite growing testimony and a trove of leaked documents, officials continue to dismiss these claims. The Deep State line remains unchanged: “No empirical evidence exists for reverse-engineering extraterrestrial technology.” But the evidence says otherwise.
Supporting evidence: 1. Exotic materials reportedly recovered in 1950s, held by Lockheed. 2. The 1953 Robertson Panel even set the tone for decades of deliberate obfuscation, publicly debunking UFOs while secretly studying their implications. The CIA used Project Blue Book to publicly debunk UFOs. 3. As early as 1966, the U.S. Air Force reportedly managed over 30 classified anti-gravity projects. 4. A 1971 Australian Defense report referenced America’s "Advanced Saucer Aircraft" and a Cold War “UFO crash program” into anti-gravity propulsion. 5. The US government, through its CIA's Office of Global Access (OGA), is reported to have a secret program to retrieve and reverse-engineer crashed UFOs. This program, which began in 2003, is said to have recovered at least nine non-human aircraft, some of which were intact. The OGA works with special operations forces like SEAL teams to conduct these retrievals, keeping the operations highly secret. 6. CIA allegedly blocked a 2024 transfer of exotic materials from Lockheed to Bigelow Aerospace.
Ben Rich, former head of Lockheed Skunk Works, reportedly stated: “We now have the technology to take ET home.”
Don Phillips, also from Lockheed, confirmed reverse-engineering efforts related to recovered UFO craft, allegedly including materials from the infamous 1947 Roswell incident.
Dr. Salvatore Pais, a Navy scientist, filed patents (2016–2019) for highly unconventional devices, including a Space-Time Modification Weapon. These patents describe the use of electromagnetic fields, plasma, and rotational force fields. Theoretically, this device could create a spacetime modification weapon more powerful than hydrogen bombs. The Navy invested USD 508,000 testing the concept between 2016-2019.
But what could be the reason they are starting to reveal it now? The sudden shift toward public statements about advanced capabilities seems deliberate.
Consider the possible motives: 1. Strategic Signaling: A subtle warning to adversaries: “We possess technology beyond your reach.” 2.Controlled Disclosure: Shaping the narrative gradually to maintain public trust and institutional control. 3. Leaks Are Coming: Private-sector breakthroughs or whistleblowers may soon expose the truth. 4. Justifying Black Budgets: Revealing exotic tech lends credibility to decades of hidden spending under national security.
But perhaps the most compelling reason: a major event, whether real, staged, or cosmic in nature or eventually an alien contact scenario is on the horizon. This may be phase one of psychological preparation.
Finally; the evidence suggests that these exotic advanced technologies already exist, whether reverse-engineered or the result of disruptive physics breakthroughs. But what’s happening now isn’t full disclosure. It’s a carefully managed narrative operation, an information war cloaked in the language of advanced science.
References and must watch: Alex Jones and Top Deep State / COG Researcher Daniel Liszt: https://x.com/RealAlexJones/status/1913354709106098659 Richard Dolan: https://www.youtube.com/watch?v=qd7CIe5wnwQ View the full article
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By NASA
3 min read
Preparations for Next Moonwalk Simulations Underway (and Underwater)
NASA’s Curiosity Mars rover sees its tracks receding into the distance at a site nicknamed “Ubajara” on April 30, 2023. This site is where Curiosity made the discovery of siderite, a mineral that may help explain the fate of the planet’s thicker ancient atmosphere.Credit: NASA/JPL-Caltech/MSSS New findings from NASA’s Curiosity Mars rover could provide an answer to the mystery of what happened to the planet’s ancient atmosphere and how Mars has evolved over time.
Researchers have long believed that Mars once had a thick, carbon dioxide-rich atmosphere and liquid water on the planet’s surface. That carbon dioxide and water should have reacted with Martian rocks to create carbonate minerals. Until now, though, rover missions and near-infrared spectroscopy analysis from Mars-orbiting satellites haven’t found the amounts of carbonate on the planet’s surface predicted by this theory.
Reported in an April paper in Science, data from three of Curiosity’s drill sites revealed the presence of siderite, an iron carbonate mineral, within the sulfate-rich rocky layers of Mount Sharp in Mars’ Gale Crater.
“The discovery of abundant siderite in Gale Crater represents both a surprising and important breakthrough in our understanding of the geologic and atmospheric evolution of Mars,” said Benjamin Tutolo, associate professor at the University of Calgary, Canada, and lead author of the paper.
To study the Red Planet’s chemical and mineral makeup, Curiosity drills three to four centimeters down into the subsurface, then drops the powdered rock samples into its CheMin instrument. The instrument, led by NASA’s Ames Research Center in California’s Silicon Valley, uses X-ray diffraction to analyze rocks and soil. CheMin’s data was processed and analyzed by scientists at the Astromaterials Research and Exploration Science (ARES) Division at NASA’s Johnson Space Center in Houston.
“Drilling through the layered Martian surface is like going through a history book,” said Thomas Bristow, research scientist at NASA Ames and coauthor of the paper. “Just a few centimeters down gives us a good idea of the minerals that formed at or close to the surface around 3.5 billion years ago.”
The discovery of this carbonate mineral in rocks beneath the surface suggests that carbonate may be masked by other minerals in near-infrared satellite analysis. If other sulfate-rich layers across Mars also contain carbonates, the amount of stored carbon dioxide would be a fraction of that needed in the ancient atmosphere to create conditions warm enough to support liquid water. The rest could be hidden in other deposits or have been lost to space over time.
In the future, missions or analyses of other sulfate-rich areas on Mars could confirm these findings and help us better understand the planet’s early history and how it transformed as its atmosphere was lost.
Curiosity, part of NASA’s Mars Exploration Program (MEP) portfolio, was built by NASA’s Jet Propulsion Laboratory, which is managed by Caltech in Pasadena, California. JPL leads the mission on behalf of NASA’s Science Mission Directorate in Washington.
For more information on Curiosity, visit:
https://science.nasa.gov/mission/msl-curiosity
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Karen Fox / Molly Wasser
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Andrew Good
Jet Propulsion Laboratory, Pasadena, Calif.
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Last Updated Apr 17, 2025 Related Terms
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By NASA
3 min read
Preparations for Next Moonwalk Simulations Underway (and Underwater)
This team from University High School in Irvine, California, won the 2025 regional Oceans Science Bowl, hosted by NASA’s Jet Propulsion Laboratory. From left: Nethra Iyer, Joanne Chen, Matthew Feng, Avery Hexun, Angelina Yan, and coach David Knight.NASA/JPL-Caltech The annual regional event puts students’ knowledge of ocean-related science to the test in a fast-paced academic competition.
A team of students from University High School in Irvine earned first place at a fast-paced regional academic competition focused on ocean science disciplines and hosted by NASA’S Jet Propulsion Laboratory in Southern California.
Eight teams from Los Angeles and Orange counties competed at the March 29 event, dubbed the Los Angeles Surf Bowl. It was the last of about 20 regional competitions held across the U.S. this year in the lead-up to the virtual National Ocean Sciences Bowl finals event in mid-May.
Santa Monica High School earned second place; Francisco Bravo Medical Magnet High School in Los Angeles came in third. With its victory, University repeated its winning performance from last year. The school also won the JPL-hosted regional Science Bowl earlier this month.
Teams from all eight schools that participated in the JPL-hosted 2025 regional Ocean Sciences Bowl pose alongside volunteers and coaches.NASA/JPL-Caltech For the Ocean Sciences Bowl, teams are composed of four to five students and a coach. To prepare for the event, team members spend months answering multiple-choice questions with a “Jeopardy!”-style buzzer in just five seconds. Questions come in several categories, including biology, chemistry, geology, and physics along with related geography, technology, history, policy, and current events topics.
A question in the chemistry category might be “What chemical is the principal source of energy at many of Earth’s hydrothermal vent systems?” (It’s hydrogen sulfide.) Other questions can be considerably more challenging.
When a team member buzzes in and gives the correct answer to a multiple-choice question, the team earns a bonus question, which allows teammates to consult with one another to come up with an answer. More complicated “team challenge questions” prompt students to work together for a longer period. The theme of this year’s competition is “Sounding the Depths: Understanding Ocean Acoustics.”
University High junior Matthew Feng, a return competitor, said the team’s success felt like a payoff for hours of studying together, including on weekends. He keeps coming back to the competition partly for the sense of community and also for the personal challenge, he said. “It’s nice to compete and meet people, see people who were here last year,” Matthew added. “Pushing yourself mentally — the first year I was shaking so hard because I wasn’t used to that much adrenaline.”
Since 2000, JPL’s Public Services Office has coordinated the Los Angeles regional contest with the help of volunteers from laboratory staff and former Ocean Sciences Bowl participants in the local community. JPL is managed for NASA by Caltech.
The National Ocean Sciences Bowl is a program of the Center for Ocean Leadership at the University Corporation for Atmospheric Research, a nonprofit consortium of colleges and universities focused in part on Earth science-related education.
News Media Contact
Melissa Pamer
Jet Propulsion Laboratory, Pasadena, Calif.
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melissa.pamer@jpl.nasa.gov
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Last Updated Mar 31, 2025 Related Terms
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By NASA
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An Ocean in Motion: NASA’s Mesmerizing View of Earth’s Underwater Highways
Earth (ESD) Earth Explore Explore Earth Science Climate Change Science in Action Multimedia Image Collections Videos Data For Researchers About Us This data visualization showing ocean currents around the world uses data from NASA’s ECCO model, or Estimating the Circulation and Climate of the Ocean. The model pulls data from spacecraft, buoys, and other measurements.
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Earth (ESD) Earth Explore Explore Earth Science Climate Change Science in Action Multimedia Image Collections Videos Data For Researchers About Us 8 Min Read Going With the Flow: Visualizing Ocean Currents with ECCO
The North American Gulf Stream as illustrated with the ECCO model. Credits:
Greg Shirah/NASA’s Scientific Visualization Studio Historically, the ocean has been difficult to model. Scientists struggled in years past to simulate ocean currents or accurately predict fluctuations in temperature, salinity, and other properties. As a result, models of ocean dynamics rapidly diverged from reality, which meant they could only provide useful information for brief periods.
In 1999, a project called Estimating the Circulation and Climate of the Ocean (ECCO) changed all that. By applying the laws of physics to data from multiple satellites and thousands of floating sensors, NASA scientists and their collaborators built ECCO to be a realistic, detailed, and continuous ocean model that spans decades. ECCO enabled thousands of scientific discoveries, and was featured during the announcement of the Nobel Prize for Physics in 2021.
NASA ECCO is a powerful integrator of decades of ocean data, narrating the story of Earth’s changing ocean as it drives our weather, and sustains marine life.
The ECCO project includes hundreds of millions of real-world measurements of temperature, salinity, sea ice concentration, pressure, water height, and flow in the world’s oceans. Researchers rely on the model output to study ocean dynamics and to keep tabs on conditions that are crucial for ecosystems and weather patterns. The modeling effort is supported by NASA’s Earth science programs and by the international ECCO consortium, which includes researchers from NASA’s Jet Propulsion Laboratory in Southern California and eight research institutions and universities.
The project provides models that are the best possible reconstruction of the past 30 years of the global ocean. It allows us to understand the ocean’s physical processes at scales that are not normally observable.
ECCO and the Western Boundary Currents
Western boundary currents stand out in white in this visualization built with ECCO data. Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Greg Shirah/NASA’s Scientific Visualization Studio Large-scale wind patterns around the globe drag ocean surface waters with them, creating complex currents, including some that flow toward the western sides of the ocean basins. The currents hug the eastern coasts of continents as they head north or south from the equator: These are the western boundary currents. The three most prominent are the Gulf Stream, Agulhas, and Kuroshio. NASA Goddard’s Scientific Visualization Studio.
The North American Gulf Stream as illustrated with the ECCO model. Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Greg Shirah/NASA’s Scientific Visualization Studio Seafarers have known about the Gulf Stream — the Atlantic Ocean’s western boundary current — for more than 500 years. By the volume of water it moves, the Gulf Stream is the largest of the western boundary currents, transporting more water than all the planet’s rivers combined.
In 1785, Benjamin Franklin added it to maritime charts showing the current flowing up from the Gulf, along the eastern U.S. coast, and out across the North Atlantic. Franklin noted that riding the current could improve a ship’s travel time from the Americas to Europe, while avoiding the current could shorten travel times when sailing back.
A visualization built of ECCO data reveals a cold, deep countercurrent that flows in the opposite direction of the warm Gulf Stream above it. Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Greg Shirah/NASA’s Scientific Visualization Studio Franklin’s charts showed a smooth Gulf Stream rather than the twisted, swirling path revealed in ECCO data. And Franklin couldn’t have imagined the opposing flow of water below the Gulf Stream. The countercurrent runs at depths of about 2,000 feet (600 meters) in a cold river of water that is roughly the opposite of the warm Gulf Stream at the surface. The submarine countercurrent is clearly visible when the upper layers in the ECCO model are peeled away in visualizations.
The Gulf Stream is a part of the Atlantic Meridional Overturning Circulation (AMOC), which moderates climate worldwide by transporting warm surface waters north and cool underwater currents south. The Gulf Stream, in particular, stabilizes temperatures of the southeastern United States, keeping the region warmer in winter and cooler in summer than it would be without the current. After the Gulf Stream crosses the Atlantic, it tempers the climates of England and the European coast as well.
The Agulhas current originates along the equator in the Indian Ocean, travels down the western coast of Africa, and spawns swirling Agulhas rings that travel across the Atlantic toward South America. Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Greg Shirah/NASA’s Scientific Visualization Studio The Agulhas Current flows south along the western side of the Indian Ocean. When it reaches the southern tip of Africa, it sheds swirling vortices of water called Agulhas Rings. Sometimes persisting for years, the rings glide across the Atlantic toward South America, transporting small fish, larvae, and other microorganisms from the Indian Ocean.
Researchers using the ECCO model can study Agulhas Current flow as it sends warm, salty water from the tropics in the Indian Ocean toward the tip of South Africa. The model helps tease out the complicated dynamics that create the Agulhas rings and large loop of current called a supergyre that surrounds the Antarctic. The Southern Hemisphere supergyre links the southern portions of other, smaller current loops (gyres) that circulate in the southern Atlantic, Pacific, and Indian oceans. Together with gyres in the northern Atlantic and Pacific, the southern gyres and Southern Hemisphere supergyre influence climate while transporting carbon around the globe.
The Kuroshio Current flows on the western side of the Pacific Ocean, past the east coast of Japan, east across the Pacific, and north toward the Arctic. Along the way, it provides warm water to drive seasonal storms, while also creating ocean upwellings that carry nutrients that sustain fisheries off the coasts of Taiwan and northern Japan. Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Greg Shirah/NASA’s Scientific Visualization Studio In addition to affecting global weather patterns and temperatures, western boundary currents can drive vertical flows in the oceans known as upwellings. The flows bring nutrients up from the depths to the surface, where they act as fertilizer for phytoplankton, algae, and aquatic plants.
The Kuroshio Current that runs on the west side of the Pacific Ocean and along the east side of Japan has recently been associated with upwellings that enrich coastal fishing waters. The specific mechanisms that cause the vertical flows are not entirely clear. Ocean scientists are now turning to ECCO to tease out the connection between nutrient transport and currents like the Kuroshio that might be revealed in studies of the water temperature, density, pressure, and other factors included in the ECCO model.
Tracking Ocean Temperatures and Salinity
When viewed through the lens of ECCO’s temperature data, western boundary currents carry warm water away from the tropics and toward the poles. In the case of the Gulf Stream, as the current moves to far northern latitudes, some of the saltwater freezes into salt-free sea ice. The saltier water left behind sinks and then flows south all the way toward the Antarctic before rising and warming in other ocean basins.
Colors indicate temperature in this visualization of ECCO data. Warm water near the equator is bright yellow. Water cools when it flows toward the poles, indicated by the transition to orange and red shades farther from the equator. Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Greg Shirah/NASA’s Scientific Visualization Studio Currents also move nutrients and salt throughout Earth’s ocean basins. Swirling vortexes of the Agulhas rings stand out in ECCO temperature and salinity maps as they move warm, salty water from the Indian Ocean into the Atlantic.
The Mediterranean Sea has a dark red hue that indicates its high salt content. Other than the flow through the narrow Strait of Gibraltar, the Mediterranean is cut off from the rest of the world’s oceans. Because of this restricted flow, salinity increases in the Mediterranean as its waters warm and evaporate, making it one of the saltiest parts of the global ocean. Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Greg Shirah/NASA’s Scientific Visualization Studio Experimenting with ECCO
ECCO offers researchers a way to run virtual experiments that would be impractical or too costly to perform in real oceans. Some of the most important applications of the ECCO model are in ocean ecology, biology, and chemistry. Because the model shows where the water comes from and where it goes, researchers can see how currents transport heat, minerals, nutrients, and organisms around the planet.
In prior decades, for example, ocean scientists relied on extensive temperature and salinity measurements by floating sensors to deduce that the Gulf Stream is primarily made of water flowing past the Gulf rather than through it. The studies were time-consuming and expensive. With the ECCO model, data visualizers at NASA’s Goddard Space Flight Center in Greenbelt, Maryland, virtually replicated the research in a simulation that was far quicker and cheaper.
A simulation built with data from the ECCO model shows that very little of the water in the gulf contributes to the water flowing in the Gulf Stream.
Download this visualization from NASA Goddard’s Scientific Visualization Studio. Credits: Atousa Saberi/NASA’s Scientific Visualization Studio The example illustrated here relies on ECCO to track the flow of water by virtually filling the Gulf with 115,000 particles and letting them move for a year in the model. The demonstration showed that less than 1% of the particles escape the Gulf to join the Gulf Stream.
Running such particle-tracking experiments within the ocean circulation models helps scientists understand how and where environmental contaminants, such as oil spills, can spread.
Take an ECCO Deep Dive
Today, researchers turn to ECCO for a broad array of studies. They can choose ECCO modeling products that focus on one feature – such as global flows or the biology and chemistry of the ocean – or they can narrow the view to the poles or specific ocean regions. Every year, more than a hundred scientific papers include data and analyses from the ECCO model that delve into our oceans’ properties and dynamics.
Credits: Kathleen Gaeta Greer/ NASA’s Scientific Visualization Studio Composed by James Riordon / NASA’s Earth Science News Team
Information in this piece came from the resources below and interviews with the following sources: Nadya Vinogradova Shiffer, Dimitris Menemenlis, Ian Fenty, and Atousa Saberi.
References and Sources
Liao, F., Liang, X., Li, Y., & Spall, M. (2022). Hidden upwelling systems associated with major western boundary currents. Journal of Geophysical Research: Oceans, 127(3), e2021JC017649.
Richardson, P. L. (1980). The Benjamin Franklin and Timothy Folger charts of the Gulf Stream. In Oceanography: The Past: Proceedings of the Third International Congress on the History of Oceanography, held September 22–26, 1980 at the Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA on the occasion of the Fiftieth Anniversary of the founding of the Institution (pp. 703-717). New York, NY: Springer New York.
Biastoch, A., Rühs, S., Ivanciu, I., Schwarzkopf, F. U., Veitch, J., Reason, C., … & Soltau, F. (2024). The Agulhas Current System as an Important Driver for Oceanic and Terrestrial Climate. In Sustainability of Southern African Ecosystems under Global Change: Science for Management and Policy Interventions (pp. 191-220). Cham: Springer International Publishing.
Lee-Sánchez, E., Camacho-Ibar, V. F., Velásquez-Aristizábal, J. A., Valencia-Gasti, J. A., & Samperio-Ramos, G. (2022). Impacts of mesoscale eddies on the nitrate distribution in the deep-water region of the Gulf of Mexico. Journal of Marine Systems, 229, 103721.
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Last Updated Mar 03, 2025 Editor Michael Carlowicz Contact James Riordon Related Terms
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