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February 13, 2002 - Prior to September 11, 2001, the General
Slocum was the worst peacetime disaster in the history
of New York City. The National Underwater & Marine
Agency team led by marine surveyor, Ralph Wilbanks discovered
the remains of the GENERAL SLOCUM in November 2000.
The General Slocum burned in the East River, New York
June 15, 1904, when it became engulfed in flames during
an excursion past Manhattan. Before it had grounded
on North Brother Island, 1021 passengers, most of them
women and children, were either burned to death or drowned.
Rod Hatt with Commercial Testing & Engineering
Company confirmed the authenticity of the find.
It was reported that the sample of material Ralph Wilbanks
found was coke. These images were taken using polarized
reflected light of a polished surface.
Several features are readily observed that confirm
that the material is coal-derived coke:
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| Figure 1. Anisotropic
behavior is exhibited. This is a
partial organization of the carbon in a graphite
lattice. The
result is optically active grains. These are visible
as a
yellowish dust in the microphotographs. These grains
are
small, typically in the micron range. Photography
by Dr.
James Hower, University of Kentucky. |
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Figure 2. Inertinite
is plainly visible as dark irregular
material. This represents plant material that was
oxidized
at some point in the coals history. Most likely
during a wild fire in the environment of the
original coal plant material. This oxidized
plant material does not react in the coking
process, hence its name of Inertinite. In
some areas it can be seen that the Inertinite
minimized the formation of the anisotropic
material. This is seen as a lack of the yellow
dust material, or a shadow surrounding the
Inertinite. Photography by Dr. James Hower,
University of Kentucky. |
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| Figure 3. Devolatization
bubbles are plainly visible. These form during the coking process as the hot coal material
becomes plastic and flowable and the material
continues to produce gaseous vapors. Photography
by Dr. James
Hower, University of Kentucky. |
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