Evidence that Venus is volcanically active

Post contributed by Dr. Robert Herrick, Institute of Northern Engineering, University of Alaska Fairbanks – @robertrherrick

Venus is almost the same size as Earth, but it does not presently have plate tectonics. What it has instead, and whether the way it releases internal heat has changed with time, has been the source of debate for decades. A key point of contention has been how the level of current volcanism compares to Earth. Even if all plate-tectonics related volcanism is excluded, Earth still has numerous volcanic eruptions every year at places like the large basaltic shield volcanoes of Hawaii, the Galapagos Islands, and Iceland. The Magellan mission imaged more than 40% of Venus at least twice from 1990 to 1992 with synthetic aperture radar (SAR) at resolutions of 100-200 m, but it is only in the last decade that computer hardware and software have made it possible to systematically search that data for changes with time. Recently the first detection of a surface change of a volcano during the Magellan mission was made, indicating that Venus is presently volcanically active (Herrick and Hensley, 2023).

Image 1: A) and B) show the same area on Venus as imaged by the Magellan spacecraft eight months apart in 1991; North is up. For comparing SAR images to overhead photographs, image A) can be thought of as looking at the scene from a vantage point off to the right with the sun shining from the left; in B) the vantage point is from the left and the sun is to the right. The shape of the feature labeled “Expanded Vent” has changed over the interval between images, meaning that the volcano on which the vent is perched must have erupted.

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Ice Deposits Revealed by Radar Within Craters on Mercury

Post contributed by Dr. Edgard G. Rivera-Valentín, Lunar and Planetary Institute, Universities Space Research Association.

Although its surface can reach 800°F (427°C), some of Mercury’s craters conceal vast ice deposits that, in a sense, “sparkle” in the light of radar (Image 1). The so-called radar bright features were first identified in 1992 using ground-based observatories, in particular the Arecibo Observatory in Puerto Rico, which provided magnificent views down to craters tens-of-kilometers in diameter all the way from Earth. The ice lies within craters whose morphology and location results in areas that do not receive direct sunlight (i.e., permanently shadowed regions). This allows for the low temperatures needed to retain ice over millions of years.

Image 1: Radar image of Mercury’s north polar terrain (> 75°N) in polar stereographic projection. The five notable craters, Chesterton (88.5°N, 126.9°W), Tolkien (88.8°N, 211.1°W), Tryggvadóttir (89.6°N, 171.6°W), Kandinsky (87.9°N, 281.2°W), and Prokofiev (85.7°N, 297.1°W) are labeled. Radar backscatter is noted in grayscale from black (below noise levels) to white (high backscatter). All bright areas are radar bright features, which are located within craters that have permanently shadowed regions. These are the locations of ice deposits on Mercury. For scaling reference, Chesterton crater has a diameter of 37.2 km. Image credit: Figure 2 in Rivera-Valentín et al. (2022) PSJ 3,62.

The discovery of the radar bright features at Mercury’s poles was one of the motivators of NASA’s MESSENGER (Mercury Surface, Space Environment, Geochemistry, and Ranging) mission, which studied Mercury between 2011 – 2015. That is because although the radar scattering properties of the features were reminiscent of observations of the Martian polar layered ice deposits, as well as of the icy moons of Jupiter, they alone did not uniquely indicate the presence of water ice. The detailed studies by MESSENGER along with the earlier radar observations together now strongly suggest deposits of water ice. This is due to their location, evidence from high resolution and long exposure imaging, and measurements of epithermal and fast neutron fluxes.

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