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Glass Structures
There has been so much controversy over the fusion crust of my rock and the questions that
revolve around its coming through the atmosphere and showing the proper amount of heating
that I have decided to include this section on glass particles I have found near the outer
surfaces of the rock. After taking a sample from near the surface of the rock, I began
looking at all of the sand and debris that came out of the place where the sample was
taken. Much to my surprise, I found a small piece of glass. It is flat on one side (the
side that would have been the top) and on the other side, the volcanic portion of the rock
has molded the glass to the exact shape of its container. This proves that the rock did
get very hot after the sand was deposited, since the melting point of sand is over 1000
degrees, if I remember correctly. Since the glass is flat on one side, it lends more
support to the hypothesis that this rock had a single orientation as it came through the
atmosphere, since it would have probably been cooled by the time it hit the ground. Also,
little pieces of rock and sand are melted in the glass, much like it was a tiny
paperweight.
This first picture was taken with a halogen bulb, so the color is not true. The next picture was taken with natural light and shows a little dark on my screen.
Here you can see that the glass is clear, except for the particles that are imbedded within it. You can see some of the ridges from this view. You are looking at the bottom of the glass with the flat side away from you.
To me this is more proof that the volcanic structure of this rock is able to withstand a lot of heat. If sand melts at over 1000 degrees, then the volcanic portion must have a higher melting point than sand. If the sand was able to melt to a liquid and stay in the vesicle, the temperature must have gone over 1000 at this part of the rock for at least long enough to make the sand liquid. Since not all of the particles melted and some are melted within the glass, this little paperweight should tell us almost exactly what temperatures were encountered as this fell through the atmosphere.
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Contents
Core Samples Fusion Crust Age Chemistry Martian Dust Mars Model Local Volcanoes Geology Report Glass Internal Structure Boundary Sites
Overview Home Write NASA
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