May 3, 2009
Be A Dirtmeister’s Science Reporters
Posted by adventuresinscience under EC Labs, extra creditNo Comments
How do the forces of erosion change the world in which we live? Join us and find out
Greetings Science Snoopers! You might say we’re going to really get “down and dirty” because our topic is erosion and one of the key things that erosion controls is DIRT! Most people don’t realize it, but every minute of every day, our earth is being changed by the forces of erosion. Wind, water, ice, insects, and even people help to move soil and wear away the surface of the planet. Your mission is to investigate one way that shapes your neighborhood and then write about it. Let’s begin by investigating the facts! Have fun being a Dirtmeister by doing these fun science experiments at home!
Did you do your lab report..If not click here
SAFETY ALERT: ALWAYS REMEMBER even the simplest activities with the most basic of materials can be harmful or dangerous, so parental supervision and guidance is critical at all times
At Home Science Experiments
- Neighborhood Erosion Experiment
- Soil Erosion Demonstration
- Soil Organic Matter (Aggregate Stability)
- Soil Air
- Particle Size Demonstration

In class this week we have learned what a minerals is using the mnemonic device: CRINS which stands for Crystal (repeating pattern), Recipe (definite chemical composition), Inorganic (non-living) Naturally formed, and Solid. Next, students learned the 8 ways that geologist can identify minerals: C3DFHLS- Color, Cleavage, Crystal structure, Density, Fracture, Hardness, Luster, and Streak. Students had quite an enjoyable time applying these properties to figure out the identity of mystery minerals. Lastly, students learned the 2 ways minerals can form-from evaporating solutions and from the cooling of magma and lava. Students learned that when they drink Kool Aid they are essentially drinking a solution because sugar is dissolved in water. They also learned that through the process of crystallization crystals are able to grow. Students were quite BEDAZZLED of the large size of crystals from a geode and the size of crystals from obsidian. I posed the questions as to why do you think the crystals were different sizes and their was always that ONE shining star in each class who correctly guess it had to do something with the temperature of the magma and lava. The quicker the molten rock cooled, the SMALLER the crystal. SLOW = BIG CRYSTALS FAST=small crystals







