May 4, 2009
What happened to that mountain?
Posted by adventuresinscience under EC project, at home scienceNo Comments

Prepare to get dirty and have some fun learning about Weathering and Erosion.

What Happens To A Mountain?
Question: What changes will happen to the mountain of soil over the course of a month
Hypothesis: I think …
Procedure
- Build a “mountain” of soil 50 cm (about 20 inches) high in an undisturbed location in your backyard yard.
- Observe the mountain once a week for the next 1.5 month. Measure its height and width and note any changes in its surface.
RECORDING DATA: This chart will be a log of your experiment. Make a chart that includes
- the date and time,
- the height & width,
- observations (description),
- daily drawings of your mountain.
Analysis and Conclusions..After observing the mountain for an extended period of time, answer the following questions
- What was the initial height of your mountain
- What was the final height?
- How much soil did your mountain loose (subtract #2-#1) ?
- Prediction: How long do you think it would take for your pile to weather away
- HINT: A. Divide the answer from question # 3 by the number of days you observed.
- B. Take the amount of final soil height ( question #2) and divide it by the number you got in step A )
- What forces do you think might have caused changes in your mountain?
- Why do you think your soil weathering away so quickly?
- What naturally protects soil from erosion?
- What could you do to your mountain to conserve soil or make it more erosion proof?



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


Seismometers are delicate scientific tools used to detect tremors from earthquakes. Seismometers are the forward sentinels in those locations there earthquakes and volcanoes are active. When a volcano comes to life, scientists will place many seismometers in remote areas all around the volcano in order to monitor its activity. An increase in tremors is one sign hat a volcano is closer to erupting. The readings from many seismometers become the first line of safety for the people living near a volcano. Because of the dangers involved, most seismometers are designed to transmit by radio or satellite their data to a central spot where scientists can interpret it. With enough data and the proper calculations, scientists can warn people in time of possible danger. This project will give you an idea of how a seismometer works. Don’t forget to share your results at Zoom kids, click 









