When you take a moonlit stroll on the beach, how often do you think about the tiny grains of sand creeping in between your toes? From above, sand seems like a bunch of tiny brown rocks, perhaps peppered with occasional shells or cigarette butts. But sand has a far more fascinating story to tell.
Composed of the remnants of volcanic explosions, eroded mountains, dead organisms, and even degraded man-made structures, sand can reveal the history--both biological and geologic--of a local environment. And examined closely enough, as the scientist and artist Gary Greenberg has, sand can reveal spectacular colors, shapes, and textures.
These images of sand from around the world were taken by Greenberg using an Edge 3D Microscope and can be found in his book, A Grain of Sand, which was published earlier this year by Voyageur Press.
Bright green olivine is a significant mineral in Hawaii's slow-flowing basaltic lava and is rich in iron. Its density allows it to separate from other sand grains in the rolling and depositing action of waves, which results in the accumulation that tints this beach a yellowish green. Dense sands like olivine are also resistant to weathering, allowing it to endure millennia of constant waves. (Magnification 110x)
The pitted and frosted surface of these grains is typical of desert sand, where grains constantly collide with one another. Many desert sands have a faint red color caused by a thin layer of iron that precipitates from the atmosphere and coats the grains. (Magnification 85x)
This sand, red from iron oxide, was found at Makena Point, Maui. It eroded from igneous rock, which was produced by the solidification of molten magma. (Magnification 125x)
Not all sand is made of tiny bits of rock. Biogenic sand, which forms from the remains of marine life, is the major ingredient of many tropical beaches. The grains here are tiny fragments of a baby sea urchin shell.
The raised bumps on the white grain represent the sites of insertion for the sea urchin's spines. The blue grain has eroded to the point that the raised bumps have been completely rubbed off. (Magnification 100x)
Looking like a puffy white star studded with little pearls, this is the shell of an amoeboid protist called a foraminifera, or foram. An estimated four thousand types of forams live in the world's oceans.
The shells, called tests, are made mainly of calcium carbonate, which the animals derive from carbon atoms in the air and water. Forams thus play a significant role in the carbon cycle. (Magnification 75x)
The glasslike needles are sponge spicules, which form the internal skeletons of sponges. They are made of silica, can be found in a variety of bizarre shapes (including spiders and fishhooks), and are hard and sharp enough to cut through human flesh.
They surround the tip of a spiral shell, composed primarily of calcium carbonate, that has broken off and eroded. (Magnification 70x)
Man-made objects can also become sand. This grain was found on the Greek island of Delos, one of the most important mythological, historical, and archaeological sites in Greece.
Delos had no indigenous marble, and an enormous amount of marble had to be quarried and brought to the island to erect the temples. Over the years, the marble blocks have eroded and the local beaches are now peppered with different types of marble. (Magnification 130x)
Some sand comes from decidedly less artistic human activity. Here, a small grain of copper is impacted into a larger nugget, also of copper. These grains precipitated downwind of an unregulated, smoke-belching copper smelter. (Magnification 110x)
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