Cassini image of the moon Mimas in the shadow of Saturn’s rings. Enlarge to see Mimas. Via Lights in the Dark
Ukulele Consultant and Ego Kabuki Critic.
Tapwater Jackson has been performing lobotomies with a broken ketchup bottle since 1953.
Occasionally, I am tapwaterj at gmail dot com. But, really, so what?
Cassini image of the moon Mimas in the shadow of Saturn’s rings. Enlarge to see Mimas. Via Lights in the Dark
Crescent Enceladus with Saturn’s rings. Taken in visible light with the Cassini spacecraft narrow-angle camera on Jan. 4, 2012.
Archive of High-Res Photos From NASA’s Gemini Missions. NASA via Wired Science.
M3-class solar flare. Via Lights in the Dark Click image for animation.
Loving the Chambered Nautilus to Death
From the New York Times: It is a living fossil whose ancestors go back a half billion years — to the early days of complex life on the planet, when the land was barren and the seas were warm.
Intrinsic Fluorescence in Lepidozia Reptans
Nikon Small World Photomicrography CompetitionBig Sisters — Saturn’s two largest moons, Rhea and Titan
Via J. Major, Lights in the Dark
Raw images taken in red, green and blue visible-light channels were combined to make this color version. The spacecraft was 1,828,949 km (1,136,456 miles) from Rhea when the images were taken.
Credit: NASA / JPL / Space Science Institute. Edited by Jason Major.
This up to 1000 years old snow has metamorphosed into highly pressurized glacier ice that contains almost no air bubbles. Thus it absorbs the visible light despite the scattered shortest blue fraction, giving it its distinct deep blue waved appearance. This cavity in the glacier ice formed as a result of a glacial mill, or moulin.
Rain and meltwater on the glacier surface is channelled into streams that enter the glacier at crevices. The waterfall melts a hole into the glacier while the ponded water drains towards lower elevations by forming long ice caves with an outlet at the terminus of the glacier. The fine grained sediments in the water along with wind blown sediments cause the frozen meltwater stream to appear in a muddy colour while the top of the cave exhibits the deep blue colour.
Due to the fast movement of the glacier of about 1 m per day over uneven terrain this ice cave cracked up at its end into a deep vertical crevice, called cerrac. This causes the indirect daylight to enter the ice cave from both ends resulting in homogeneous lighting of the ice tunnel.
Overfished ecosystem held together by a single species. Ars Technica
Diatoms are a Girl’s Best Friend. Mary Ann Tiffany, San Diego State University. Via Presurfer