Regolith - NASA
causes melting, and the reaction of H with FeO forms H 2 0 vapor and submicroscopic metallic Fe grains in the resulting agglutinate glass. This process continues until the surface layer is buried by fresh ejecta or is broken up by a large crater. Trenches and core tubes into the regolith reveal that it is stratified with many buried soil horizons.
Download Regolith - NASA
Information
Domain:
Source:
Link to this page:
Documents from same domain
ALH84001 - NASA
curator.jsc.nasa.govMartian Meteorite Compendium C Meyer 2012 Figure 2: Photograph of exterior surface of Martian meteorite ALH84001.Note the large cavity on this surface. The cube is 1 cm. (NASA # S85-39567) Figure 3: Close-up photograph of a small piece of Martian meteorite ALH84001 illustrating rounded carbonate inclusions with orange interiors and black-white-black rims.
Related documents
The Younger Dryas - National Climatic Data Center
www.ncei.noaa.govice sheet was rapidly melting and adding freshwater to the ocean. Scientists have hypothesized that, just prior to the Younger Dryas, meltwater fluxes were rerouted from the Mississippi River to the St. Lawrence River. Geochemical evidence from ocean sediment cores supports this idea (Carlson et al. 2007), although other possible
Safety Guideline for Steel Melting Shop
steel.gov.inSteel Melting Shop (SMS) receives Hot Metal (HM) from Iron-making units and converts it into various grades of Steel and casts them into Slabs, Blooms, Billets, Beam blanks, Rounds and thin slab- HR coils. Those are delivered as products to down-stream units (Long, Section & Flat Products). SMS is the first stage in the