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Bill Dunford profile thumbnail

Bill Dunford

Bill Dunford is just another desktop astronaut, following the adventures of the robotic spacecraft all across the Solar System. He blogs about his experiences at Riding with Robots on the High Frontier and as @ridingrobots.

Latest Blog Posts

Many More Colors than Red: Exploring Mars with Spectroscopy

Posted 2013/05/20 01:31 CDT | 0 comments

Mars gives up its secrets through the unseen colors of its rocks.

Dueling Desolations: Mercury vs. the Moon

Posted 2013/05/13 01:02 CDT | 7 comments

They look so similar they can be hard to tell apart, but each hides its own mysteries.

Dark No More: Exploring the Far Side of the Moon

Posted 2013/04/29 02:11 CDT | 3 comments

The first human beings to see the mysterious "dark" side of the moon were not astronauts.

Older blog posts »

Latest Processed Space Images

CRISM Reveals the Minerals of Lampland Crater - Mafic Minerals

CRISM Reveals the Minerals of Lampland Crater - Mafic Minerals

Posted 2013/05/20 | 0 comments

The north rim of Lampland Crater on Mars as seen by the CRISM instrument on board the Mars Reconnaissance Orbiter in infrared light that contains information related to the mineralogy of iron-containing minerals.

CRISM Reveals the Minerals of Lampland Crater - Visible Light

CRISM Reveals the Minerals of Lampland Crater - Visible Light

Posted 2013/05/20 | 0 comments

The north rim of Lampland Crater on Mars as seen by the CRISM instrument on board the Mars Reconnaissance Orbiter in enhanced visible color.

CRISM Reveals the Minerals of Lampland Crater

CRISM Reveals the Minerals of Lampland Crater

Posted 2013/05/19 | 0 comments

An animation showing several views of Lampland Crater on Mars. First, a wide context view, then a close-up on the north rim, both provided by the Mars Express orbiter. Next, two observations by the CRISM instrument on board the Mars Reconnaissance Orbiter: one in enhanced visible color and another showing wavelengths sensitive to mafic mineralogy. In that last view, red indicates the presence of olivine or iron phyllosilicates, green is low-calcium pyroxene, and blue is high-calcium pyroxene.

More pictures processed by Bill Dunford »

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