Tuesday, October 13, 2009

 

New Videos!

I finally downloaded my camera. Sorry, the videos are a bit large (too big to email) and they may take a while to download.


So, that sweet boy kitty that stole my heart and then disappeared... here he is:






Just listen to that little meow! See, I'm a sucker.







Also, it rained a bit today. Supposedly there was more rain in this storm than predicted, and it was predicted to be the largest in 46 years.


Brandi wasn't too excited about the rain. (For some reason, I have to slide the play bar over a bit to get it to start actually playing the video.)






But once the rain was over, at least for a while, she was very very happy. (sorry, this is a really big file)







And then everyone slept.



Thursday, April 05, 2007

 

Giant crystals enjoyed perfection

from the BBC

Giant crystals enjoyed perfection
The cave was discovered in 2000


With lengths over 11m, the giant gypsum crystals found in Mexico's Cueva de los Cristales are a great natural wonder.

Now, a Spanish-Mexican team thinks it can explain how these marvels acquired their immense form.

The scientists studied tiny pockets of fluid trapped in the crystals and conducted back-up lab experiments.

They report in the journal Geology that the solution from which the crystals grew must have been kept in a very narrow, stable temperature range.

The researchers' analysis leads them to believe there are other dramatic caves waiting to be discovered in the Naica mine complex south-east of Chihuahua city.

"If the theory we propose for the 'genetic' mechanisms of the crystals is right, then I would not be surprised if miners find more of these caves in the next few years," Juan Manuel Garcia-Ruiz, from the University of Granada, Spain, told BBC News.

Bigger than 'swords'

Already two remarkable caves are known at Naica, which has yielded some of the world's most significant deposits of silver and lead.

The 120m-deep Cueva de las Espadas (Cave of Swords), discovered in 1912, is named for its metre-long shafts of gypsum (a calcium sulphate mineral that incorporates water molecules into its chemical formula).

And although individually there are fewer crystals in the 290m-deep Cueva de los Cristales, its beams are considerably bigger.

Professor Garcia-Ruiz and colleagues believe they can now show how these differences emerged.

The team studied tiny fluid samples embedded inside the crystals themselves.

These watery inclusions record tell-tale chemical details of the saline and temperature conditions of the saturated solution from which the mammoth structures developed.

'Perfect conditions'

Both caves owe their origin to the volcanism which laid down the metal sulphides - the ores - that have proved so valuable.

Copious amounts of calcium sulphate would also have been created towards the end of this mineralisation process more than 20 million years ago - but in the hot fluids that infused the cracks and cavities in the rock, this calcium sulphate would have taken the form of anhydrite.

Anhydrite has the same chemical formula as gypsum, except that it excludes water. Only as the magma chamber deep under the Naica mountain cooled did the hot fluids above start to fall to a temperature at which anhydrite could switch to gypsum.

Professor Garcia-Ruiz and colleagues say their studies indicate that the deeper of the two caves - Cueva de los Cristales - must have been kept just below the transition temperature for many hundreds of thousands of years.

"The conditions were perfect. By maintaining the temperature just below 58 degrees for a very long time you get a few, very big crystals," said Professor Garcia-Ruiz.

"You can see that many areas on the cave's walls are empty; they have no crystals. The walls are red because of the iron oxide. The reason we know this happened for many years is because we studied the fluid inclusions inside the crystals."

It is likely the upper cave - Cueva de las Espadas - fell below the transition temperature much more rapidly and consequently grew many, smaller crystals.

Heritage future?

The particular crystalline form taken by the gypsum is selenite which is known for its translucency.

Their future will be dependent on the fate of the mine.

At the moment, access is restricted to prevent damage to the soft crystals.

And the only reason humans can get in the caves at all is because of the ongoing pumping operations that keep them clear of water.

If, when Naica's ores are no longer viable, the mine is closed and the pumping is stopped, then the caves will be submerged - and the crystals will start growing again.

"I've recommended to the mining company that they try to preserve them and I would like to see Unesco get involved," explained Professor Garcia-Ruiz.

"Later on we should decide whether to keep them available for people to visit and enjoy, or let the natural scenario return."


 

Excuse Me?


Thursday, February 01, 2007

 

Yikes


 

He Hee


 

Rachel sings itsy bitsy spider in spanish!


Tuesday, October 24, 2006

 

Cat Update

Well, Flower is a monster - just like in Monsters, Inc. - she is cute and loveable but makes you want to scream.

Here she is looking guilty because she is on the dining table. Notice that her healing leg doesn't seem to be any issue for her.


She and Carrie are starting to get along slightly better - Flower still drives Carrie nuts, but Carrie runs away from her a little less. Here they are playing with this little bird that chirps and moves when its motion sensor is triggered.



They look like happy cats. :)

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