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Mapping Silicate Minerals From Space

New infrared surveys of silicates and related minerals provide insights for geological research, renewable energy, and rare Earth mineral exploration.
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This new map shows silica deposits across Earth's arid and semi-arid regions. The deposits were detected using data from the ECOSTRESS sensor aboard the International Space Station. Researchers looked for silica because it is often found in the same spots as valuable lithium-bearing and other minerals. Credit: Rabuffi, et al.

 

NASA-funded scientists have created new worldwide mineral maps that could help mark the location of precious resources. These high-value data are now within the easy and inexpensive reach of a computer. 

The developers of the maps used NASA thermal infrared (TIR) spectroscopy data to create maps of silicate, sulfate, and carbonate minerals in the planet’s arid and semi-arid regions. The maps, which complement other Earth sensor data, can provide scientists with important surface composition details for geological studies and resource prospecting.

Scientists developed the one-kilometer resolution maps using data gathered by two of NASA’s orbiting sensors: the ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) aboard the Terra satellite. The maps, now available through NASA’s Earthdata Search and the Land Processes Distributed Active Archive Center (LP DAAC), could be powerful tools for resource exploration and for understanding Earth’s geology.

“This achievement not only demonstrates how NASA Earth observation data can be used to identify regions for geological study and exploration, but also the power of cross-mission data synergy,” said Cole Krehbiel, project scientist for LP DAAC.

Identifying Minerals With TIR

Thermal infrared spectroscopy is a technique used to analyze the infrared energy emitted by materials. Each mineral on Earth's surface emits thermal radiation in its own way, producing unique spectral signatures that can be used for their identification. Scientists used TIR data from the ECOSTRESS and ASTER sensors to identify minerals, such as silica, spread across Earth’s arid regions—and it is the only known way to detect silica from space.

One big reason to study silicate deposits is to locate important resources. For example, lithium-bearing minerals, used in batteries and electronics, are often found in silicate-rich rocks such as quartz and feldspar. By mapping these rocks and minerals from space, researchers can identify areas that may contain other valuable deposits. 

Maps of silicates have another benefit: signs of their alteration on the surface can indicate the presence of underground geothermal activity, which could point the way toward sites for renewable, geothermal energy production.

Searching for Silicates

The new mineral maps are the product of a recent study led by Federico Rabuffi from NASA’s Jet Propulsion Laboratory in California, and a follow-on to an earlier experiment.

“We were exploring the possibility of mapping gypsum with ECOSTRESS data as part of work related to understanding landslides in the Western United States,” said Rabuffi. “Once we knew we were able to identify gypsum, we decided to try using ECOSTRESS data to detect main rock-forming minerals, knowing it would be good for future exploration and missions.” 

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Researchers tested their ability to map silicates with ECOSTRESS and ASTER data by comparing remote sensing observations of sites in California, New Mexico, and Morocco and comparing them with measurements made on the ground at those locations. The researchers found strong agreement between the satellite and field data, proving that the sensors are good tools for mapping minerals for space. Credit: Rabuffi, et al. 

To see if they could find silicates and other main rock-forming minerals in TIR data, the study team examined ECOSTRESS and ASTER observations of quartz in Algodones Dunes, California, gypsum in White Sands, New Mexico, and calcite in Mehdi Ridge, Morocco. Then they compared the TIR measurements with actual field data. The researchers found that the data matched, which meant the technology could be used to identify and map minerals from space.

Complementing EMIT and Others

While TIR data can be used to map silicates and other minerals, it does have its limitations. Mainly, it can only be used to detect some—not all—kinds of minerals. To truly characterize the composition of an area, TIR data need to be paired with complementary measurements from sensors detecting other kinds of minerals as well. 

For example, the Earth Mineral Dust Source Investigation (EMIT) sensor on the International Space Station (ISS) collects visible to shortwave infrared (VSWIR) observations that can detect oxides, sulfides, and clays, which can also be present around precious minerals.

“TIR data will help you find the silica geological formations that are part of the environment where you might find gold and lithium,” said Kerry Cawse-Nicholson, science lead for ECOSTRESS and member of the TIR mapping team. “EMIT and VSWIR are then needed for finding the clays and more specific markers of where these important minerals can be found.”

TIR silicates data could be used to support additional mineral mapping projects as well, including the joint NASA-USGS Geological Earth Mapping Experiment (GEMx). In that multi-year campaign, researchers are taking airborne imaging flights across the Western United States to search for unknown mineral deposits. Rabuffi’s TIR silicates data could provide clues for where to look.

In essence, the maps are a trove of easily accessed geological information and a potentially enormous time and effort saver. The data mineral researchers and experts can easily glean from them likely replace the need for many long hours sifting through other data. Or they may negate the need for expensive and difficult ground surveys in remote places. And in some cases, the digital data might provide virtual access to places we might not be able to reach at all.

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Last Updated

Sept. 11, 2026

Published

Sept. 11, 2026

Data Center/Project

Land Processes DAAC (LP DAAC)