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Uses Of Hydrocarbons

The hydrocarbons are the most broadly used organic compounds known, and are quite literally the driving force of western civilization. The greatest amounts of hydrocarbons are used as fuel for combustion, particularly in heating and motor fuel applications. The primary components of natural gas are methane and ethane. We are all familiar with the ...

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UsesOfHydrocarbons
Biology

Neurons

Until recently, most neuroscientists thought we were born with all the neurons we were ever going to have. As children we might produce some new neurons to help build the pathways - called neural ... Continue reading

Neurons
Biology

St. John's Wort

St. John's wort is an herb that has been used for centuries for medicinal purposes, including to treat depression. The composition of St. John's wort and how it might work are not well understood. ... Continue reading

StJohnsWort
Biology

Proteins Function Through Their Conformation

To produce proteins, cellular structures called ribosomes join together long chains of subunits. A set of 20 different subunits, called amino acids, can be arranged in any order to form a polypeptide ... Continue reading

ProteinConformation
Biology

How Does The Turtle Get Its Shell?

Many invertebrates, such as beetles and lobsters, have shells, but the turtle is the only living vertebrate with a shell (except for the armadillo or course). A turtle's top shell is called the ... Continue reading

HowDoesTheTurtleGetItsShell

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.