Thermal Emission Imaging System

Additionally, it helps scientists to understand how the mineralogy of Mars relates to its landforms, and it can be used to search for thermal hotspots in the Martian subsurface.

THEMIS is managed from the Mars Space Flight Facility at Arizona State University and was built by the Santa Barbara Remote Sensing division of Raytheon Technologies Corporation, an American multinational conglomerate headquartered in Waltham, Massachusetts.

Eight of these have wavelengths between 6 and 13 micrometers, an ideal region of the infrared spectrum to determine thermal energy patterns characteristic of silicate minerals.

In a THEMIS image taken at night, however, thermophysical properties of the surface can be inferred, such as temperature differences due to the materials' grain size (thermal inertia).

The presence of minerals such as carbonates, silicates, hydroxides, sulfates, amorphous silica, oxides, and phosphates can be determined from THEMIS measurements.

The THEMIS infrared camera was designed to be used in conjunction with data from the Thermal Emission Spectrometer (TES), a similar instrument on Mars Global Surveyor.

The instrument's approach provides data on localized deposits associated with volcanoes, hydrothermal processes, and the alteration of minerals by surface and/or subsurface water.

The THEMIS instrument, before being mounted onto Mars Odyssey.
Two false-color maps of the same area of Mars. The left one is very pixelated, while fine details are visible in the right one.
Spatial resolution comparison between MGS's TES instrument and Odyssey's THEMIS instrument. (The spectral resolutions are inversely related.)
Two maps of the same area on Earth. The left one is grayscale, while the right one is false-color and shows the distributions of quartz (red), carbonate minerals (green), and iron-rich minerals (purple).
Sample map from Terra's ASTER instrument: Saline Valley , California
A grayscale map of an area on Mars (from 5° N to 6° S and from 10° W to 358° W (or 2° E), crossing 0° in both axes), with a false-color overlay (cyan, green, yellow, red) showing hematite abundance on the surface.
Map showing distribution of hematite in Sinus Meridiani . This data was used to target the landing of the Opportunity rover . Hematite is usually formed in the presence of water. Opportunity landed in this area and did find much evidence for water.
Mars - horizon views (video; 1:24; Odyssey orbiter ; THEMIS camera; 9 May 2023)