A year-end-straddling collection of science-related blog carnivals await your reading attentions:
Grand Rounds Vol 8:No 15 – The Twitter Edition
A year-end-straddling collection of science-related blog carnivals await your reading attentions:
Grand Rounds Vol 8:No 15 – The Twitter Edition
SOS is taking a year-end holiday break — Happy Holidays to all, see you in the new year!
The past week’s crop of (mostly) science-related blog carnivals:
December Scientiae — Ultimate Goals
Fantastic video from NASA’s Solar Dynamics Observatory — Comet Lovejoy traveled behind the Sun (through its upper atmosphere!), and survived the passage (direct link):
H/T: Gizmodo
A svelte but satisfying batch of science-related blog carnivals for your reading today:
This week’s image comes to you from a display of minerals at the University of Denver’s Olin Hall — it’s a sample of Pyrite:
Also known (if not loved) as “fool’s gold,” it’s an iron sulfide — actually, the most common of the sulfide minerals. And surprisingly enough, it’s been both a blessing and a curse.
On the bad side of things (aside from the confusion factor for would-be gold hunters), pyrite oxidizes fairly rapidly when exposed to humidity. This is a prime cause of acid mine drainage (a big problem in areas with old, inactive mines), and can cause spontaneous combustion in coal mines with high-sulfur coal seams. Meanwhile, pyrite’s oxidized products take up greater volume than its unoxidized form, helping cause mine collapses.
On the positive side of the ledger, pyrite has many potential uses. It’s been a commercial feed stock for production of a number of useful chemicals, is still used in hobbyists’ “crystal radios,” and can be used to make low-cost photovoltaic solar panels.
The past week’s crop of science-related blog carnivals for your reading fun:
Circus of the Spineless #68 – gifts galore!
Grand Rounds, Vol. 8 No. 11: The Tumblr’d Edition
This week’s photo comes to you from Swiftcurrent lake — a beautiful little lake in the Many Glacier region of Glacier National Park in Montana:
The mountains in the background get their shape from the same force that lent its name to this part of the park — the mountains are what’s left after the glaciers of the last ice age retreated. Swiftcurrent lake was created from the combination of glacial-driven erosion (carving its basin), retreat deposition (leaving a moraine to impound water), and melting (to fill the lake).
Sadly, though, only 25 active glaciers remain of the 150 or so that were here 150 years ago — and they’ll be gone in another decade, if current warming trends continue.
I normally try to avoid repeating myself on posts here — but this week’s video is just too good to put off until later. In case you missed last Saturday’s launch of NASA’s / JPL’s Mars Science Laboratory (MSL) “Curiosity” rover to Mars, here’s the first five minutes of flight — up until the separation of the 1st and 2nd stages (direct link):
And even better, here’s video of the separation of MSL from the upper stage (direct link):
And if that isn’t enough for you, did you hear that some astronomers in Australia were able to make a quick video clip out of some images they took of MSL and the Atlas launch vehicle’s Centaur upper stage on their way toward Mars (direct link)?
By the way, what looks like a comet is the Centaur venting its left-over propellants; MSL is the tiny dot to its left.
H/T: Tom’s Astronomy Blog, Universe Today