A rock is made of grains of one or more minerals that fit together.
1.

Go to Bitesize from the BBC to find out how rocks change due to weathering.
After you finish reading the information, take their on-line test to see how much you learned!

2. Visit Exploring Earth to view an interactive rock cycle animation.
3. Can you finish this rock cycle diagram from The Learning Zone?
4. Fill in the Rock Chart by visiting the web sites listed below.

Find information for your chart

Igneous
These rocks began as hot, fluid material.
It may have been lava or magma.

Sedimentary
These rocks are born cool at the Earth's surface, mostly under water.
They usually are made of layers.

Metamorphic
These rocks are made when sedimentary and igneous rocks beecome changed by conditions underground.

Did you know...

Up to 100,000 tons of rock a year fall to earth from space. That's why the earth gains weight each year! The largest meterorite in the world lies in the ground in Africa and weighs more than 60 tons!

Igneous means made from fire or heat. When volcanoes erupt and the liquid rock comes up to the earth's surface, then new igneous rock is made. When the rock is liquid & inside the earth, it is called magma. When the magma gets hard inside the crust, it turns into granite. Most mountains are made of granite. It cools very slowly and is very hard.

Obsidian is nature’s glass. It forms when lava cools quickly on the surface. It is glassy and smooth.

Pumice is full of air pockets that were trapped when the lava cooled when it frothed out onto the surface. It is the only rock that floats.

When mountains are first formed, they are tall and jagged like the Rocky Mountains on the west coast of North America. Over time (millions of years) mountains become old mountains like the Appalachian Mountains on the east coast of the United States. When they are old, they are rounded and much lower.

When large amounts of plants are deposited in sedimentary rocks, they turn into carbon, which gives us our coal, oil, natural gas and petroleum.

Metamorphic rocks were originally igneous or sedimentary, but due to movement of the earth's crust, were changed. Metamorphic rocks are the least common of the 3 kinds of rocks.


Mohs Scale of Hardness
Another way to identify rocks and minerals is by their hardness.
Rocks and minerals vary in hardness from talc, the softest, to diamonds, the hardest.
Hardness is also important because it may determine how a rock or mineral can be used.

Friedrich Mohs devised a hardness scale in 1812.
It has ten classifications, 1 being the softest and 10 being the hardest.
There is only one exception. That's mercury, which is a liquid.
Each classification will scratch the one before it.
Some people think the only stone that scratches glass is a diamond.
Today other man-made minerals with a hardness of 6 or higher can scratch glass.

Talc
Used for talcum powder, paint, rubber and plastics, your fingernail can easily scratch it, feels greasy and has a translucent, soapy look
Gypsum
Used for plaster of Paris and household wallboard, can be found in beautiful crystal rose shapes
Calcite

Typically found in the sedimentary rock called limestone, is also in marble, a metamorphic rock, which forms when limestone is put under strong heat and pressure, forms stalactites and stalagmites, makes shells

A great way to identify it is to drop a weak acid, like vinegar on it. Calcite will bubble. It also produces a double refraction of light, look though it at an image and you will see double!

Fluorite
Comes in many pretty colors, best known for purple, often fluorescent, transparent to translucent, Fluorine in fluorite prevents tooth decay, glass making, enamels, used to make high quality lenses for telescopes and cameras instead of glass
Apatite
Found in igneous, metamorphic and sedimentary rocks, usually in small amounts, usually green to blue, source of phosphorous used in fertilizer, its the mineral that makes up the teeth in all vertebrate animals, as well as their bones
Feldspar
Also known as orthoclase, milky variety called moonstone, used in ceramics and glazes, some show a milky translucence and occasionally used as gems
Quartz
The most common mineral on Earth, comes in many colors and shapes, but always has a glassy look, usually forms sedimentary rocks like sandstone, is also in igneous rocks like granite, and can be found in metamorphic rocks, too
Topaz
November's birthstone, Emerald and aquamarine are varieties of beryl, found in granites, can be found as pebbles in streams, used as a gemstone, to make a pink topaz, it must be heated, most blue topaz that is used for jewelry has been irradiated
Corundum
Sapphire and ruby are varieties of corundum, twice as hard as topaz, the second hardest natural mineral, used as gems, also in making watches and as an abrasive
Diamond

Simply a form of carbon, just like charcoal or graphite, used in jewelry and cutting tools, four times as hard as corundum

Today there are new materials harder than diamonds but they are man-made.

Other examples:
A fingernail is about 2 1/2
A penny is about 3.5
Glass is about 5 1/2


Web site created by
Jill Dembsky

Updated April 2008