From the Field

Amazing Sands From Around the World

Photo © Siim Sepp (www.sandatlas.org), used with permission

Tourism boards from Australia to Tahiti like to boast about their beaches, many proclaiming to have the whitest sands in the world. But since when is white sand superior to all others? 

Sand comes in an absolute rainbow of colors — from teal to orange to black, white, blue, and even pink — but only if you know where to look. And the unique geology behind these sands is often as cool as the colors themselves. 

Here are seven weird and colorful sands from around the world that will put your average beach sand to shame. (And check out our story on the hobby of sand collecting. Yes, really.)

  • Olivine Sand

    Hawai’i, USA

    Olivine sands from Hawai’i. Width of view is 20 mm. Photo © Siim Sepp (www.sandatlas.org), used with permission

    My sand obsession started on Hawaii’s Papakōlea Beach, where I saw my first olivine sands. Olivine is an igneous mineral formed from the crystallization of magma. At Papakōlea, the olivine erodes out of an ancient volcanic cinder cone that encloses the semi-circular beach. Sand of almost exclusively olivine grains is very rare, and Papakōlea is one of only four green sand beaches in the world. The others are Hornindalsvatnet in Norway, Punta Cormorant in the Galapagos Islands, and Talofofo Beach in Guam.

  • Garnet Sand

    Australia

    Garnet sand from Australia. Width of view is 20 mm. Photo © Siim Sepp (www.sandatlas.org), used with permission

    Garnet is found in small quantities in many different types of sand. But in a few locations you can find sands dominated by garnet, which look red, purple or pink depending on the light and source rock. Some notable garnet sand locations include California’s Pfeiffer Beach, various beaches in New York and Rhode Island, Idaho, Alaska, coastal Namibia, and Australia.

  • Glauconite Sand

    France

    Glauconite beach sand from France. Width of view is 20 mm. Photo © Siim Sepp (www.sandatlas.org), used with permission

    Greensand — not to be confused with green sands formed from olivine— is a sand or sandstone that gets its blue-green color from mineral glauconite. These sands erode from glauconitic sandstones, which are typically formed from ancient marine sediments laid down in the Cambrian or Cretaceous Periods. Notable examples of glauconite sand are found in Estonia and France.

  • Star Sand

    Japan

    Japanese star sand. Photo © Siim Sepp (www.sandatlas.org), used with permission

    Star sand is the celebrity of rare sands. Found on Japan’s Ryukyu Islands, including Okinawa, it’s formed from the shells of microscopic, single-cell ocean organisms called foraminifera. Different species of foraminifera create different shell shapes, and the rare, star-shaped ones in Japan are formed by the species Baculogypsina sphaerulata. These tiny little sunbursts are just a few millimeters across, but you can still see them with the naked eye. The sand sample above also contains shells from the Calcarina foram genus, often called sun sand.

  • Ooid Sand

    Utah, USA

    Ooid sand from Stansbury Island, The Great Salt Lake. Width of view 5.5 mm. Photo © Siim Sepp (www.sandatlas.org), used with permission

    Ooid are small, rounded pellets that usually formed in warm, shallow, wave-agitated waters. In these conditions,  minerals suspended in the water — usually calcite or aragonite — gradually accumulate around a central grain. (Somewhat similar to how snow sticks to a snowball rolling downhill.) If you cut them in half, you would see concentric circles much like tree rings. Most ooids are round, but others are long, smooth cylinders.

    Famous ooid sand locations include the Persian Gulf, the Yucatán Peninsula, and the Bahamas. The sample above is a rare example of a non-marine ooid sand, from Stansbury Island in Utah’s Great Salt Lake.

  • Black Sand

    Hawai’i, USA

    Black beach sand from Punalu’u Beach in Hawai’i. Width of view 20 mm. Photo © Siim Sepp (www.sandatlas.org), used with permission

    Even non-arenophiles (or sand lovers) are familiar with black sand. Black beach sand is made up of volcanic glass, which forms when lava flows into the oceans and cools rapidly. Black sand can be found on dozens of volcanic beaches around the world, including Hawai’i, Iceland, New Zealand, and throughout the tropical South Pacific.

    But not all black sand is volcanic… sometimes it can be formed from other minerals. Often light-sand beaches will have streaks or patches of dark sand, commonly mistaken for oil or other pollution. These are actually patches of heavy mineral sand exposed by the waves.

  • Mica Sand

    France

    Mica sands from France. Width of view 20 mm. Photo © Siim Sepp (www.sandatlas.org), used with permission

    What do your kitchen countertops and eyeshadow have in common? Mica. Formed from the minerals biotite or muscovite, mica is common in igneous rocks, like granite, and is mined around the world for use in products as varied as cosmetics, electrical components, and construction.

    Small portions of mica lend a subtle sparkle to many different sands, particularly in riparian areas, but like garnet they can also occur in large quantities. The sample above, from Cap Coz, France, is particularly rich in muscovite and biotite flakes.

Justine E. Hausheer

Justine E. Hausheer is a science writer for The Nature Conservancy, covering the innovative fieldwork and research conducted by Conservancy’s scientists around the world. She has a degree from Princeton University and a master's in Science, Health, and Environmental Reporting from New York University. Justine has battled swarms of mosquitos, steep trails, and the wilds of the Papua New Guinea rainforest — all for a good story. When not writing about conservation science, she enjoys having far-flung adventures, long hikes, and waking up at dawn to bird. More from Justine E.

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1 comment

  1. thank you so much for this fantastic article! i’m collecting fun sands from around the world as a present for a friend, and this is just the reference i needed! thank you! 🙂