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Engineering

Teeny Tiny Technology

What's the smallest thing you can imagine? Can you think of something extremely tiny that is also extremely strong--many times stronger than steel--and very flexible? Give up? The answer is carbon ... Continue reading

TinyTechnology
Mathematics

Eratosthenes Measured Earth’s Circumference—Centuries Before Columbus Sailed

Eratosthenes (c. 276 – 194 BC) was born more than 2200 years ago in the Greek city of Cyrene, now a city in the North African country of Libya. (The Greek Empire surrounded much of the Mediterranean ... Continue reading

EratosthenesEarthCircumference
Biology

Will That Be One Hump or Two?

Camels are highly adaptive to their environments. Often called the ships of the desert, they have been domesticated by humans for thousands of years, as beasts of burden and as transportation. What ... Continue reading

Humps
Astronomy

What Is Microgravity?

Gravity is a force that governs motion throughout the universe. It holds us to the ground and keeps the Earth in orbit around the Sun. Microgravity describes the environment in orbital space flight, ... Continue reading

Microgravity

Sedimentary Rock

SedimentaryRockSedimentary rock is one of three rock types on earth. Rock types are classified according to how the rock is formed. Igneous rock forms as it cools to a solid from molten rock. Metamorphic rock forms when rock is altered by intense heat, pressure, or both. Sedimentary rock is formed from particles derived from other rock through the processes of weathering, erosion, and deposition.

Sediments are eroded by flowing water in streams, by waves or ocean currents, by wind, ice, or gravity. Most erosion is done by flowing water. As eroded sediments move along, they grind against other rocks. This adds to the erosive power of the water, wind, or ice and further erodes the moving sediment. The grains become rounder, smoother, and smaller. The size and shape of the grains in a sedimentary rock give clues to its history. Coarse, angular grains could not have moved far from their source rock. Small, rounded grains must have been rolled along for hundreds of miles. Streams deposit tons of sediment into the oceans every day. In the oceans, sediment may be moved by currents and waves and later be dropped in layers upon the seafloor. Remains of organisms can be preserved as fossils as they drop and are quickly buried in accumulating sediments. Sedimentary rock is the only rock type containing fossils.

As layers of sediment build up, overburden pressure begins to squeeze the grains together. Water between the grains can leave once dissolved minerals behind after it is squeezed out or driven off by heat. These minerals cement the grains together into rock. Heat and pressure at burial depth can also fuse grains together into solid rock. As earth's forces cause the solid crust to move, sedimentary rock formed from sediments on the ocean floor or in valleys can be uplifted to the surface, perhaps reaching mountaintops. Some may become metamorphosed. Once at the surface, the rock is again exposed to weathering and erosion. New sediment forms, and the rock cycle continues. Because all rock at the surface is eroded and eventually forms new deposits, sedimentary rock is the most abundant rock type on earth.