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By NASA
NASA, ESA/Matthias Maurer An astronaut aboard the International Space Station snapped this picture of the Moon as the station orbited 265 miles above the U.S. state of Minnesota on Dec. 17, 2021.
Astronauts aboard the orbital lab take images using handheld digital cameras, usually through windows in the station’s cupola, for Crew Earth Observations. Crew members have produced hundreds of thousands of images of the Moon and Earth’s land, oceans, and atmosphere.
On Saturday, Sept. 14, 2024, International Observe the Moon Night, everyone on Earth is invited to learn about lunar science, participate in celestial observations, and honor cultural and personal connection to the Moon. Find an event to join in the celebration.
Image credit: NASA, ESA/Matthias Maurer
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By NASA
The dome-shaped Brandburg Massif, near the Atlantic coast of central Namibia, containing Brandberg Mountain, the African nation’s highest peak and ancient rock paintings going back at least 2,000 years, is pictured from the International Space Station as it orbited 261 miles above.
Image Credit: NASA
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By NASA
2 min read
Preparations for Next Moonwalk Simulations Underway (and Underwater)
University of Florida researcher Rob Ferl (seated) and co-principal investigator Anna-Lisa Paul practice the experiment to study the effect of gravity transitions on the plants’ gene expression.University of Florida For the first time, a NASA-funded researcher will fly with their experiment on a commercial suborbital rocket. The technology is one of two NASA-supported experiments, also known as payloads, funded by the agency’s Flight Opportunities program that will launch aboard Blue Origin’s New Shepard suborbital rocket system on a flight test no earlier than Thursday, Aug. 29.
The researcher-tended payload, from the University of Florida in Gainesville, seeks to understand how changes in gravity during spaceflight affect plant biology. Researcher Rob Ferl will activate small, self-contained tubes pre-loaded with plants and preservative to biochemically freeze the samples at various stages of gravity. During the flight, co-principal investigator Anna-Lisa Paul will conduct four identical experiments as a control. After the flight, Ferl and Paul will examine the preserved plants to study the effect of gravity transitions on the plants’ gene expression. Studying how changes in gravity affect plant growth will support future missions to the Moon and Mars.
The university’s flight test was funded by a grant awarded through the Flight Opportunities program’s TechFlights solicitation with additional support from NASA’s Division of Biological and Physical Sciences. This experiment builds on NASA’s long history of supporting plant research and aims to accelerate the pace and productivity of space-based research.
The other Flight Opportunities supported payload is from HeetShield, a small business in Flagstaff, Arizona. Two new thermal protection system materials will be mounted to the outside of New Shepard’s propulsion module to assess their thermal performance in a relevant environment, since conditions will be similar to planetary entry. After the flight, HeetShield will analyze the structure of the materials to determine how they were affected by the flight.
Flight Opportunities, within NASA’s Space Technology Mission Directorate, facilitates demonstration of technologies for space exploration and the expansion of space commerce through suborbital testing with industry flight providers. Through various mechanisms, the program funds flight tests for internal and external technology payloads.
To learn more, visit: https://www.nasa.gov/space-technology-mission-directorate/
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Last Updated Aug 28, 2024 EditorLoura Hall Related Terms
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By NASA
4 Min Read Into The Field With NASA: Valley Of Ten Thousand Smokes
NASA scientists begin a day’s field research in Katmai National Park. Credits:
NASA/Patrick Whelley In June 2024, the Goddard Instrument Field Team (GIFT) hiked deep into the backcountry of Alaska’s Katmai National Park to study the Valley of Ten Thousand Smokes, site of the largest volcanic eruption of the twentieth century. The team’s task: traverse a vast volcanic debris field layered with glacier ice, gathering data and samples to help us better understand this place on Earth and similar terrain on other worlds.
Buried glaciers on Mars and Earth. Top: Orbital view of partially-exposed ice beneath an eroding deposit on Mars, from HiRISE. Bottom: Edge-on view of a partially buried glacier in Alaska with a LiDAR (Light Detection and Ranging) device in the foreground, from the Goddard Instrument Field Team. Novarupta, the volcano that erupted here in 1912, ejected more than three cubic miles of ash from Earth’s subsurface. The ice nearby is now insulated by, and mixed with, thick layers of geologically “young” volcanic debris. (For comparison, many of the eruption sites NASA teams study are tens of thousands to millions of years old.) Mars, too, has glaciers and ice sheets covered in layers of airfall materials, including dust and volcanic ash.
On Mars, as on Earth, some of the planet’s history is in disguise. Ancient volcanic materials are buried underneath newer deposits of ashy debris. Patterns in these layers (think thickness or thinness, color and texture, chemical and mineral signatures) hold a lot of information, but the message isn’t always clear. Erosion and other surface processes hide evidence of past eruptions, even enormous ones. Since relatively fresh volcanic material blankets the Valley of Ten Thousand Smokes, it’s an ideal place to observe the early stages of these changes.
Cherie Achilles raises a rock hammer as Alexandra Matiella Novak stands by with a hand-held spectrometer and Alice Baldridge holds a container of rock samples. The hand-held spectrometer gives on-the-spot information about what its targets are made of, helping the team decide which samples to collect and bring back to the lab. In three days of violent eruption, Novarupta blasted an uncommonly wide variety of clays, minerals, and volcanic rocks throughout the surrounding valley. Since then, hot, sulfurous gases have filtered up through underground channels and escaped into the air via countless fumaroles (a.k.a. the “ten thousand smokes”). Fumaroles, together with erosion and other alteration processes, affect how minerals near Novarupta move and change. Research here can help us understand mineral movement and alteration on Mars and other worlds, too. The range of starting materials and alteration patterns in this valley, all from a single eruption, is difficult to match anywhere else.
Heather Graham studies a fumarole – a place where volcanic gases escape from underground – using a hydrogen sulfide collector and sampling equipment. Their goal: check the fumarole for encrusted evidence that microscopic organisms once lived here, consuming energy and changing the rocks’ composition. Research on these kinds of biosignatures helps us understand what the search for life could look like on other worlds. It’s a tough field site to access, especially with heavy science instruments. GIFT worked closely with local collaborators including Katmai National Park to coordinate the expedition. After years of planning and months of training, twelve field team members gathered and geared up in Anchorage, Alaska. Two tiny airplane flights, one all-terrain bus ride, and sixteen hiking miles later, they set up a base camp. From there, small groups hiked out and back each day, gathering data and sample material from throughout the valley.
Left to right: Tabb Prissel, Emileigh Shoemaker, Heather Graham, Andrew Johnson, Justin Hayles, Aditi Pandey, and Patrick Whelley hike out of the Valley of Ten Thousand Smokes. Scientists teamed up to carry large equipment from place to place and bring each other data from far-flung targets. Some results were predictable, like a new library of samples collected from several different “packages” of differently-composed volcanic debris. Some were surprising–like a core sample that came up containing a pocket of empty space instead of buried glacial ice.
Emileigh Shoemaker and her team use Ground Penetrating Radar (the red box shown here is the GPR antenna) to gather information about long stretches of Earth’s subsurface before physically breaking ground. Here, Shoemaker stands on a huge pile of volcanic ash; hidden beneath the debris is a glacier. GPR data, combined with core samples, soil moisture measurements, and pits dug at strategic locations, can reveal how the glacier is preserved. Analyzing the samples, processing the data, and putting it all together will take time. This is the beginning of GIFT’s Novarupta research, but it’s a chapter of a science story long in the making. Previous studies of the 1912 eruption and its aftermath influenced this expedition’s science plan. The 2024 data and samples, and the new questions arising from the team’s time in the field, are already shaping ideas about future work. NASA has visited before, too. Apollo astronauts and their geology trainers spent time in the Valley in 1965, finding it an unusually Moon-like place to study.
Fieldwork still plays a role in astronaut training–and in advancing lunar science. For example: Novarupta’s chemistry is partly a result of Earth’s plate tectonics. The Moon has volcanic landscapes with similar chemistry, but no tectonic plates. So, what else could explain the parallel? To help address this question, the 2024 team collected samples and ground-truth data from a range of rock formations comparable to the Moon’s Gruithuisen Domes.
Tabb Prissel, Aditi Pandey, and Justin Hayles at Novarupta. The dome of dark rubble behind the scientists is what’s left of the volcano itself: in 1912, material erupted from this spot buried miles of glaciated valley. On Earth, the Moon, Mars, and beyond, geologic processes encode pieces of our solar system’s history. Volcanic deposits store details about a world’s insides at the time of an eruption and evidence of what’s happened at the surface since. Rippling fields of sand dunes, gravel, and ash record the influence of wind where atmospheres exist, like on Venus, Mars, and Titan. Glaciers can tell us about climate history and future–and on Mars, ice research also helps to lay the groundwork for human exploration. It’s much easier to take a close look at these features and processes here on Earth than anywhere else. So, to understand planets (including our own), NASA field scientists start close to home.
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Last Updated Aug 22, 2024 Related Terms
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By European Space Agency
On 8 September 2024, the first of four satellites that make up ESA’s Cluster mission will reenter Earth’s atmosphere over the South Pacific Ocean Uninhabited Area.
This marks the end of the historic mission, over 24 years after it was sent into space to measure Earth’s magnetic environment. Though the remaining three satellites will also stop making scientific observations, discoveries using existing mission data are expected for years to come.
This ‘targeted reentry’ is the first of its kind. ESA’s efforts to ensure a clean end to the Cluster mission go beyond international standards, making the agency a world-leader in sustainable space exploration.
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