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Fossil Energy - The Basics

Contrary to what many people believe, fossil fuels are not the remains of dead dinosaurs. In fact, most of the fossil fuels we find today were formed millions of years before the first dinosaurs. Fossil fuels, however, were once alive! They were formed from prehistoric plants and animals that lived hundreds of millions of years ago. Think about ...

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FossilEnergyTheBasics
Geology

What Are The Key Ingredients For An Avalanche?

All that is necessary for an avalanche is a mass of snow and a slope for it to slide down. For example, have you ever noticed the snowpack on a car windshield after a snowfall? While the temperature ... Continue reading

Avalanche
Biology

Why is Red-Green Colorblindness a 'Guy Thing?'

Colorblind girls and women are rare, while men who can't match their socks are relatively common. The reason is a genetic phenomenon called sex-linked inheritance. Humans have 23 pairs of chromosomes. ... Continue reading

ColorBlindness
Physics

Galileo Thermometers

Every substance has the property of 'mass', which is the basic physical presence of matter. Matter occupies space. A physical mass contained within a physical space produces the physical property of ... Continue reading

GalileoThermometers
Astronomy

It's Dusty Out There

There is no lower limit to the size of the solid particles that move around the Sun. Small asteroids grade downward into large meteoroids and then into smaller pebbles and so on down to the tiniest ... Continue reading

ItsDustyOutThere

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.