Observations of Hydrogen at Room Temperature (25{degrees}C) and High Pressure (to 500 Kilobars)

Hydrogen becomes a solid at 25 degrees C when subjected to a pressure of 57 kilobars. The high-pressure phase appears as a transparent crystalline mass. The refractive index of the high-pressure phase increases sharply with pressure, indicating a density increase of similar magnitude. At 360 kilobars the calculated density of the high-pressure phase is 0.6 to 0.7 grams per cubic centimeter.     

Spatial Variability of Turbulent Mixing in the Abyssal Ocean

Ocean microstructure data show that turbulent mixing in the deep Brazil Basin of the South Atlantic Ocean is weak at all depths above smooth abyssal plains and the South American Continental Rise. The diapycnal diffusivity there was estimated to be less than or approximately equal to 0.1 x 10(-4) meters squared per second. In contrast, mixing rates are large throughout the water column above the rough Mid-Atlantic Ridge, and the diffusivity deduced for the bottom-most 150 meters exceeds 5 x 10(-4) meters squared per second. Such patterns in vertical mixing imply that abyssal circulations have complex spatial structures that are linked to the underlying bathymetry.     

Aluminum Silicate System: Experimental Determination of the Triple Point

The kyanite-sillimanite-andalusite triple point exists in the pressure-temperature plane at 8 +/- 0.5 kb and 300 +/- 50 degrees C. Reactions are accomplished experimentally with a Bridgman opposed-anvil press (with an external furnace), modified to provide shearing of the sample charges. All three equilibrium boundaries are proved by reversed reactions.     

Archeological excavations in jalisco, Mexico

Recent archeological work in northeastern West Mexico has provided information about a previously unknown area and some evidence regarding its relationship with other parts of Mexico. An occupation as early as A.D. 100 is suggested.