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Received — 2 August 2026 ⏭

EAGLE

✇NASA Science
By: Stephen Carney
31 July 2026 at 23:02

EAGLE

Explorer for Artemis Geology, Lunar, and Earth — a NASA satellite program to study surface biology and geology on Earth, with technologies that could support future missions to the Moon and Mars.

Future Mission

NASA’s EAGLE program — Explorer for Artemis Geology, Lunar, and Earth — will be a series of satellite missions studying surface properties using technologies for Earth observation that will also benefit future missions to the Moon and Mars, where they could identify critical resources and safe landing sites.

The satellites making up the first two EAGLE missions will study biology and geology on Earth’s surface to support agriculture, disaster response, and other needs. Each mission will carry a different instrument with capabilities that complement each other. The first mission (EAGLE-VSWIR) is scheduled to take flight in 2028.

Mission Type

Orbiter

Target

Earth, Moon, Mars

Launch

No earlier than 2028

Objective

Study surface composition and changes

  • EAGLE-VSWIR

    EAGLE-VSWIR (Visible to Shortwave Infrared) will observe the Earth’s surface every 16 days with a high-resolution imaging spectrometer, which measures light reflected from the planet’s surface, separating wavelengths across the visual and into the infrared spectrum. The patterns created by light being reflected or absorbed across this spectral range act like fingerprints, letting scientists identify the composition of the surface. 

    A similar instrument, NASA’s EMIT (Earth Surface Mineral Dust Source Investigation), has been monitoring Earth from the International Space Station since July 2022, characterizing the surface mineral composition of Earth’s arid lands, monitoring ecosystem status, and tracking health and safety hazards — such as methane leaks and acid mine drainage — among other applications.

    EAGLE-VSWIR will have 25 times more capability than EMIT has today. This technological leap will allow scientists to map surface deposits of critical and rare-earth minerals, strengthen food security, and aid wildfire prevention and recovery. It can also highlight environmental hazards such as oil spills or landslide risks, and monitor water quality and availability.

    Region of Nevada as observed by NASA's EMIT with spectrum on right edge
    The front of this image cube shows a region in Nevada observed by NASA’s EMIT imaging spectrometer; the cube’s sides show the spectral fingerprint for every point in the image and can be used to discover mineral resources. EAGLE-VSWIR will have 25 times greater performance beyond NASA’s current state-of-the-art EMIT.
    NASA/JPL-Caltech

  • EAGLE-TIR

    The EAGLE-TIR mission will provide Thermal InfraRed (TIR) imagery when it launches two to three years after EAGLE-VSWIR, measuring energy emitted from the surface and producing data that scientists can use to map temperature, composition, and critical mineral deposits. On Earth that would let researchers monitor wildfires and volcanic activity, track drought and water use by crops, study urban heat islands, observe the rates that snow or ice accumulates or melts, and better understand Earth’s resilient ecosystems.

    EAGLE-TIR follows on from ECOSTRESS (ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station), which has been observing Earth from the International Space Station since 2018. ECOSTRESS was designed to study how different ecosystems respond to drought and water stress, and the data has provided a vital understanding of how plants’ water use changes throughout the day. Since ECOSTRESS also measures emitted energy in the thermal infrared, its surface-temperature products have also been used for urban planning and wildfire monitoring. 

    Further innovation and lessons learned from ECOSTRESS has led to EAGLE-TIR, which will carry a multi-band thermal radiometer. EAGLE-TIR’s great strength compared to existing missions is that it provides detailed imagery of the entire globe every two days, day and night, at multiple wavelengths not available from other instruments.

    Aerial view of Namib desert in Infrared captured by ECOSTRESS
    This image shows the minerals contained in Namibian dunes using ECOSTRESS data. EAGLE-TIR will have more spectral channels to enable even better mineral discrimination.
    NASA/JPL-Caltech

  • EAGLE Program

    By advancing vital techniques for measuring our planet’s surface composition, resources, and hazards, the EAGLE program addresses critical needs in Earth observation, with technologies that can also transfer to planetary exploration, where they’ll serve as pathfinders for future missions to the Moon and Mars.

    015B0489.NEF
    As the Artemis II crew came close to passing behind the Moon and experiencing a planned loss of signal, they captured this image of a crescent Earth setting on the Moon’s limb on April 6, 2026.
    NASA
Featured Video

EAGLE

NASA unveiled the EAGLE program as one part of its “Ignition” event on March 24, 2026, when it announced a wide-ranging series of transformative agencywide initiatives. With EAGLE (the Explorer for Artemis Geology, Lunar, and Earth missions), NASA will deploy breakthrough hyperspectral images across Earth with later missions anticipated for the Moon and Mars in rapid succession. On Earth they’ll identify critical minerals for national security, enable precision agriculture, and support disaster response. On Earth and at Mars they will locate critical minerals and resources such as ice for propellants, rare-earth elements for technology, and construction materials for habitats.

EMIT

EMIT (Earth Surface Mineral Dust Source Investigation) measures the mineral composition of Earth’s dust source regions, to help scientists understand how they heat or cool our planet.

Learn More About EMIT

ECOSTRESS

ECOSTRESS (ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station) is accurately measuring the temperature of plants on Earth.

Learn More About ECOSTRESS

The post EAGLE appeared first on NASA Science.

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It Appears the Reports of Venus’s Death Were Greatly Exaggerated—New Models Suggest the Planet is Still Geologically Active

✇The Debrief
By: Christopher Plain
26 July 2026 at 12:07

New computer models of Venus’s surface features, including ridges likely caused by volcanic activity, have determined that the second rock from the Sun remains geologically active to this day.

The ETH Zurich research team behind the new Venusian models, which suggest that Venus may still have active volcanoes, said their findings could help planned NASA and ESA missions select the most promising targets. The new models could also help in the search for rocky planets outside of our Solar System, including those that may support life.

Venus Previously Considered Geologically Dormant for Over 100 Million Years

Venus has long fascinated planetary scientists due to its similarities. For example, the planet’s mass and circumference make it roughly 95% the same size as Earth overall. However, although Venus’ elliptical orbit brings it closer to Earth than any other planet in the Solar System, its extreme surface temperatures and toxic atmosphere make it inhospitable to life as we know it.

Ground and space observations have detected rift valleys on Venus’s surface, which the research team notes indicate tectonic activity. Some can measure up to 10,000 kilometers and resemble the longest ridges on Earth. Although the timing of Venus’ rift formations remains uncertain, the team said most scientists have typically considered the planet to be geologically dormant. Some estimates have put their formation more than 100 million years ago.

Curious if data captured by space and ground-based observatories could provide enough information to answer the timing question, a research team from ETH led by Taras Gerya, a Professor of Geodynamics at the Department of Earth and Planetary Sciences, decided to plug that data into computer models. According to their results, the reports of Venus’ demise may have been greatly exaggerated. 

Models Reveal Planet Likely Supports Active Volcanoes

Working under Professor Gerya’s supervision, Master’s candidate and lead author of the paper detailing the team’s work, Xi Yang, and colleagues employed computer models to simulate the planet’s rifts in high-resolution and 3D. The team said these models allowed them to “accurately replicate these rift structures” in a level of detail never achieved. The data also allowed them to perform simulations to best determine how they originally formed.

Critically, the team notes that earlier attempts to model Venus’ tectonic history and potential ongoing activity had been mostly two-dimensional. Yang’s team also said those earlier models had relied on “simplified material assumptions” that his team was able to expand upon.

After completion, the models yielded several compelling results. First, they indicated that the broad ridges geologists call ‘rift flanks’ form along the edges of rift valleys at a time when the rifts are still “geologically young.” Specifically, the team’s models suggested that these flanks formed when Venus was still either actively moving or had only recently stopped moving.

A closer look at the simulations also suggested that these geological rifts open over a much shorter time scale than previously assumed, with an estimated rate between 3 and 10 centimeters per year. The models also indicated that rift flanks tend to flatten very quickly once the movement ends.

“The older the rift system, the less steep and narrow its flanks,” they explained.

A comparison to erosion patterns on Earth also supported a more recent time frame for the rift flank formations spotted on the Venusian surface from the Magellan probe during its 1990s mission. The team said that these formations and their models suggest that “Venus remains an active planet with a more dynamic interior than had been previously believed.”

“Venus remains geologically “alive” and even hosts active volcanoes,” they explained.

Planned NASA & ESA Missions Could Confirm Models

When discussing the implications of their work, Professor Gerya said the findings “help us to better assess the tectonic activity on Venus.” The team noted that their models could also guide future missions by pinpointing potentially active regions worthy of closer examination.

The ETH team said their study also has planetary formation implications, particularly for rocky planets like Venus and Earth. Such data could prove valuable in the search for rocky exoplanets, including the type that may host life.

Moving forward, the study authors noted that NASA and the European Space Agency (ESA) are actively preparing “multiple missions” to explore Venus in further detail. ETH geophysics professors Paul Tackley and Gerya, and their team of collaborators, are already participating in ESA’s EnVision mission.

The work includes developing instruments for the orbiter to analyze the surface in greater detail. Scheduled for launch in the early 2030s, the team said that EnVision will explore the planet more thoroughly than previous efforts “from its core to its upper atmosphere.”

The study “Recent active rifting on Venus revealed by wide rift flank uplifts” was published in Nature Geoscience.

Christopher Plain is a Science Fiction and Fantasy novelist and has spent the last six years as Associate News Editor and Head Science Writer at The Debrief. Follow and connect with him on X, learn about his books at plainfiction.com, or email him at christopher@thedebrief.org.

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