OK, some more from my scribblenotes:
First Anthony Colaprete, the PI, has a big supressed smile on his face.
The plume was about 10-12 km across, perfectly fitting into the 1 degree FOV of the LCROSS sheparding craft.
The crater created (which was imaged in the NIR (Near Infrared) showed a crater between 20 and 30 meters in diameter with ejecta up to 100 meters away as it fell back to the lunar surface.
The measured temp before impact was -220 to -230 degrees C, the impact created temps +400-500 C.
The Infrared Spectrum showed clear indications of water and/or water ice, along with other absoptions which were not discussed. They were able to create a model spectrum that fit the full spectrum very well, but since that didn't involve water (and is under continuing analysis) that wasn't discussed. Certainly his team, as well as the LRO and Ground Based obs has some ideas, but those results will come out in a few months (spring?) when the nalysis and peer review is completed. Sodium was one clear detection from ground based obs.
OH (hydroxyl) was detected in the emission spectrum in UV as the plume was photolysized by sunlight after the impact.
Ground based observations suffered by the last minute change of impact locataion from the Cabeus A crater to Cabeus proper, which made the plume less visible from earth, but increased the value of the obs made by the LCROSS spacecraft.
The earth based astronomers concurred with that decision, since the goal was really to hit the best location.
They came with 100 meters of their targeted impact site (Goal was 3.5 km)
About 2 weeks ago they knew that they had a robust water detection, had team meeting and agreed to go public...after that it was all creating slides
If you have any other questions, ask away and I'll see if the answer is in my scribblenotes, or watch the replays!!
Wayne