THIS MONTH AT THE DELAWARE COAST |
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| Please send in your suggestion for the question of the month. Questions and answers will be posted as the months unfold. For more information, contact Wendy Carey. | |
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Question of the Month - January, 2003
Topic: Heavy Minerals |
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A layer of black sand is often seen on the beach after
storms. Although it's surprising to see black sand beaches along Delaware's
coast, it's not too unusual. This black beach covering is an accumulation
of dark sand grains which are more difficult for winds and waves to move
than the lighter colored quartz sand. Along Delaware's shoreline, the
dark sands typically consist of heavy iron-rich minerals such as magnetite
and illmenite; garnet, tourmaline and hornblende are another minerals
commonly found in the dark sand mix.
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| These heavy minerals have a smaller grain size
or diameter, but a greater specific gravity or density when compared to
the white quartz sand. These characteristics result in a different hydraulic
behavior from quartz grains and therefore these heavy minerals are often
concentrated by waves and currents to form dark layers within the beach
sand. Black sand deposits are often "left behind" as a lag layer
during high wave conditions of winter, when the quartz-rich sand is preferentially
transported alongshore or offshore. |
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The next time you encounter a layer of black sand on the beach surface, take a small portion in your hand for closer examination. The sand grains are usually very small and are likely to stick to your hand and under your nails. Compare them to the typical white/tan sand from Delaware's beaches; observe differences in shape, grain size and color. Excavation of a small trench in the beach may reveal isolated layers of dark sand within the white layer-cake beach deposits, depicting a recent history of storm or high wave and wind events. |
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Please send in your suggestion for the question
of the month. Questions and answers will be posted as the months
unfold. For more information, contact Wendy
Carey.
|
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