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Carbon Dating

As isotopes break down, or decay they give off radiation. Materials that decompose in this way are said to have a 'half-life'. As the quantity of material present decreases, so does the actual rate at which the material decays. The process of dating artifacts by radioactive C-14 measurement depends strictly upon this condition. Using C-14 ...

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CarbonDating
Geology

A Undersea View of Our Earth's Geography

The ocean bottom is divided into three major areas: the continental shelf, the continental slope, and the deep ocean basin. The continental shelf extends underwater from each of the major land masses ... Continue reading

UnderseaEarthsGeography
Medicine

Resistance is NOT Futile!

Maybe if you are a Star Trek heroine up against the Borg, 'resistance is futile.' But if you are a germ that makes people sick, resistance - to antibiotics - is not futile at all. ... Continue reading

ResistanceisNOTFutile
Medicine

What Is a Bruise?

A bruise is a deposit of blood under the skin. It flows from tiny capillaries that break when you bump your shin on the furniture or take the batter's pop fly in the eye. The injury starts out looking ... Continue reading

WhatIsaBruise
Physics

Can Wint-O-Green Lifesavers® Light up Your Life?

Next time you're bored, grab a pack of Wint-O-Green Lifesavers® and lock yourself in the bathroom. Shut the blinds and make sure the room is pitch black. Allow your eyes to adjust and open the pack ... Continue reading

WintOGreenLifesavers

Rock, Mineral, Crystal, or Gemstone?

RockMineralCrystalGemstoneRocks and minerals are all around us and used every day, perhaps without us even being aware of them. Besides making up the solid, supporting surface of the earth we live and move upon daily, rocks and minerals are used in surfacing roads, in the concrete foundations of our homes, in the brick and mortar of buildings, in clocks, and for scientific and industrial purposes. Soil consists primarily of small pieces of rocks and minerals. Metals used in our automobiles, buildings, and tin cans come from rocks. People’s interest in and use of these natural materials has led to a need to better understand, classify, and locate certain rocks and minerals.

Rocks are solid, naturally occurring mixtures of substances, primarily minerals. Occasionally a rock may consist of a single mineral such as quartzite (pure quartz) or marble (pure calcite). A mineral is generally defined as a naturally occurring, inorganic (not from a living organism) solid with a definable chemical composition. A mineral may consist of a single element (such as sulfur or gold), though most are chemical compounds. Only eight elements make up nearly 99 percent of the minerals of earth’s crust. Oxygen makes up 46.8% of the crust, silicon 27.8%, aluminum 8.2%, iron 5.0%, calcium 3.6%, sodium 2.8%, potassium 2.6%, and magnesium 2.1%. Silicate minerals - those formed of silicon-oxygen compounds - are found in most common rocks.

It is the chemical make-up of a mineral which gives it its distinct properties. The types of atoms and how they are arranged and chemically bonded determine the color, shape, strength, hardness, or other properties of a mineral. The cleavage - the way a mineral breaks along planes - helps us identify it, as do its optical properties, its specific gravity, or special properties such as magnetism. Almost all minerals form crystals, generally as they cool and solidify from a melt or precipitate from solution. A crystal is a mineral with a regular, repeating geometric arrangement of atoms that gives the crystal flat faces formed at certain angles to each other. No two crystals are alike since their development depends upon available space as well as the temperature and pressure during their formation. A crystal can be distorted if not enough space is available as it forms. Gems are cut from gemstones, which are nicely formed crystals that are valued for their beauty and rarity.