Columbia River Sand, US-Canada Boundary
Two blast furnace slag particles are present in this
sample. They are evident by the lack of reflection
in the opaque particles. The black blast furnace slag particles are glass with
inclusions. They are not
conductive and have low refractive indices relative to the black metal oxides. The
black metal oxides are
much better reflectors because they tend to be semi-conductors and have real
refractive indices far from
1.680, the mounting medium used in this case.
Transmitted Circular Polarized Light and Reflected Darkfield Illumination
Definition/Function:
This deposit sample was part of a study for the distribution of slag particles introduce
into the Columbia River from a
smelter upstream. A strandline deposit forms at a special boundary or interface. That
boundary can be the site of wave action, current,
or subsurface characteristics. Strandline deposits form on beaches and at the leading or
trailing edge of air classified
sand deposits.
Significance in the Environment:
Characteristic Features:
Associated Particles:
References: