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NASA’s New Horizons spacecraft has captured images of frozen nitrogen glaciers on Pluto carrying numerous ‘floating’ hills that may be fragments of water ice, giving an insight into the dwarf planet’s fascinating and abundant geological activity.
These hills individually measure one to several kilometres across, according to images and data from New Horizons. The hills, which are in the vast ice plain informally named Sputnik Planum within Pluto’s ‘heart,’ are likely miniature versions of the larger, jumbled mountains on Sputnik Planum’s western border.
They are yet another example of Pluto’s fascinating and abundant geological activity, NASA said. Since water ice is less dense than nitrogen-dominated ice, scientists believe these water ice hills are floating in a sea of frozen nitrogen and move over time like icebergs in Earth’s Arctic Ocean.
The hills are likely fragments of the rugged uplands that have broken away and are being carried by the nitrogen glaciers into Sputnik Planum. ‘Chains’ of the



drifting hills are formed along the flow paths of the glaciers.
When the hills enter the cellular terrain of central Sputnik Planum, they become subject to the convective motions of the nitrogen ice, and are pushed to the edges of the cells, where the hills cluster in groups reaching up to 20 kilometres across.
At the northern end of the image, the feature informally named Challenger Colles — honouring the crew of the lost space shuttle Challenger — appears to be an especially large accumulation of these hills, measuring 60 by 35 kilometres.
This feature is located near the boundary with the uplands, away from the cellular terrain, and may represent a location where hills have been ‘beached’ due to the nitrogen ice being especially shallow.
The new image was captured using New Horizons’ Multispectral Visible Imaging Camera (MVIC) instrument.
The image resolution is about 320 metres per pixel. The image measures a little over almost 500 kilometres long and about 340 kilometres wide.

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