To Log This Cache:
1. According to the colors of the sand, what mineral(s) do you think is in the sand?
2. Are you seeing any display of shells or rocks in the sand?
3. On your walk here, was the sand the same or different color?
4. Post a picture anywhere around ground zero. If you do NOT want to be in the picture, take an original picture such as your GPS in the pic or an original item.
What creates different colors of sand? Why is some sand soft and fine, but other types feel rough? Where does beach sand come from, anyway? The sand found on a specific beach is created by its surroundings. It’s unique to that beach—like a fingerprint.
Most beaches get their sand from rocks on land. Over time, rain, ice, wind, heat, cold, and even plants and animals break rock into smaller pieces. This weathering may begin with large boulders that break into smaller rocks. Water running through cracks erodes the rock. In areas where it’s cold enough to freeze, water expands as it turns to ice. This forces the cracks open wider. The freeze-thaw cycle happens over and over again. Each time, gaps widen. Pieces break off. Over thousands of years they break down into smaller and smaller rocks, pebbles, and grains of sand.
Pounding waves and the ebb and flow of tides also make sand. These motions knock rocks, pebbles, and sand grains against each other. This action wears them down. It also smooths the rough edges. The smaller and rounder the grains become, the softer the sand feels.
Different minerals in rock weather differently. Some don’t hold up well. Others, such as quartz and feldspar, are much tougher. These two minerals last longer than others and make up a typical sandy beach. Quartz tinted with iron oxide appears light brown. Feldspar is tan. Together, they create the sand-colored hue of many beaches.
In areas with volcanoes, sand comes from volcanic rock. This explains the colored beaches of the Hawaiian Islands. Red beaches come from volcanic rock that’s rich in iron. Green beaches have lots of the mineral olivine. And black beaches are created from obsidian, or volcanic glass. When lava flows into water, it hardens so quickly it shatters, creating shards of obsidian. Over time, waves smooth the shards, turning them into sand.
Beach sand is more than just minerals from land, however. Some sand also comes from the ocean. Shells and other hard pieces from marine organisms wash up on shore. Pounding waves break them into smaller, sand-sized pieces. In tropical areas with coral reefs, this is the main source of beach sand.
Such reefs are home to animals, like parrotfish, that graze on coral. Parrotfish eat the algae that live on and in the corals. But they’re not delicate eaters. They chow down on big bites of coral, including the skeleton. Chunks of skeleton get ground up and pooped out as sand. A single parrotfish can create hundreds of pounds of sand each year!
Sand also comes from the remains of tiny creatures called foraminifera (forams for short). Forams are single-celled, amoeba-like protists. They form protective shells out of calcium carbonate. That’s the same stuff found in most shells and coral skeletons. When forams die, their shells are left behind as sand. In Bermuda, forams build pink shells, giving beaches there a unique hue.