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Steller Sea Lion Biology

The Steller sea lion (Eumetopias jubatus) is the largest member of the Otariid (eared seal) family. Males may be up to 325 cm (10-11 ft) in length and can weigh up to 1,100 kg (2,400 lb). Females are smaller than males, 240-290 cm (7.5-9.5 ft) in length and up to 350 kg (770 lb) in mass. Males and females are light buff to reddish brown and ...

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StellerSeaLionBiology
Biology

Bacteria Sometimes Catch A Virus

Bacteria sometimes catch a virus. Bacteriophages--'bacteria-eaters'-- or phages, are viruses that use bacteria to multiply. The phage attaches to a bacterium, injects its own genetic material, either ... Continue reading

BacteriaSometimesCatchAVirus
Astronomy

Live Fast, Blow Hard, and Die Young

Massive stars lead short, yet spectacular lives. And, they usually do not go quietly, instead often blowing themselves apart in supernova explosions. Astronomers are curious about the details of the ... Continue reading

LiveFastBlowHardDieYoung
Biology

Why Aren't Mice More Like Us?

The sequence of the human genome was published two years ago, and recently, the sequence of the mouse genome was published. Amazingly, 99% of mouse genes have a counterpart in people. So why are they ... Continue reading

Mice
Geology

Lightning Striking Again

What's hotter than the surface of the sun, moves with incredible speed, lasts a few seconds and goes out with a bang? If you said lightning, you're right. Lightning strikes cause thousands of forest ... Continue reading

LightningStrike

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.