Friday, January 30, 2009

This week we took a break from rocks and we learned about heating and everything like that. then we started a lab about lab where we brought rocks in and investigated

Monday, January 26, 2009

This week

This week we had a test on the unit of rock formation. Finley was out for that. After that we headed on studying rocks. We did an experement with looking at rocks that were the same types. We had to disquinguish the rocks and describe it. rocks cryatalize larger when they take longer to cool rather than when it cools quickly the cryatlas are really small that was basically our week

Monday, January 19, 2009

The Week

This week we leared about crystals and rocks. We did an experement wit cryatalization to see if our class hypothisis of crystals form biger when a rock cools slower than faster. In our experement we had moth balls and we melted them... We put them in different cups in diffrent cooling places. One in a cool area where that would resmeble where the rock would cool faster. Another in a room temp. area to see a mix of cool and warm and lastly a hot area to show the rock cooling faster. the next day we saw that the cooler area had tiny crystals the area of room temp. had a decient sixe crystals lastly the warmer area had the biggest cryatals. So we proved our hypothisis correct.. Lastly in the week we began a lab on rocks and trying t distinguish one type from the other. Some trays had the same types. Some rocks wrer very light some crystaly, some layerly. We've yet to finish it.

Friday, January 9, 2009

Week after X-mas

This week we started to talk about heat and 3 types of heating sourses. Conduction Convexion and Radiation. Monday we started to review review heating because we were off for holiday break. Tuesday we learned about convexion and that oven mitts are only ventelators to protect your extremities from the potentual dangers from the heat. We also learned about how when you put a spoon up to a burner that the paritcles heat up and warm up the spoon and you feel the heat.



Wendsday we learned about lava lamps and that when they get lifted by the particles It falls down. On thursday mr.finley was out and we reviewed this. Friday we took a quis and chilled out
-I HATE THE GATORS

Friday, December 19, 2008

This week

This week we mainly studyied tetonic plates and how the planet evolved over billions of years. The reason why we have a core full of magma was because a world like mars crashed into the Earth and mixed the land ind inner fratures together. Plates came together gorming mountains, or volcanos. As the volcanos erupted new land developed. We learned about the 3 different types of bounderies, Divergent, Convergent, and Transform Bounderies. Divergent bounderies is when plates move apart, Convergent ones are when the plates push together,this causes mountains and higher elevations/land to form, lastly their are Transform Bounderies this is when plates scrape past eachother


This picture is showing all the bounderies
These are the earths major plates


The World's Lithospheric Plate sizes
Plate
Area (km2)
Plate
Area (km2)
Pacific
103,300,000
Scotia
1,600,000
North American
75,900,000
Burma microplate
1,100,000
Eurasian
67,800,000
Fiji microplates
1,100,000
African
61,300,000
Tonga microplate
960,000
Antarctic
60,900,000
Mariana microplate
360,000
Australian
47,000,000
Bismark microplate
300,000
South American
43,600,000
Juan de Fuca
250,000
Somali
16,700,000
Solomon microplate
250,000
Nazca
15,600,000
South Sandwich microplate
170,000
Indian
11,900,000
Easter microplate
130,000
Philippine
5,500,000
Juan Fernandez microplate
96,000
Arabian
5,000,000
Rivera microplate
73,000
Caribbean
3,300,000
Gorda microplate
70,000
Cocos
2,900,000
Explorer microplate
18,000
Caroline microplate
1,700,000
Galapagos microplate
12,000

Saturday, December 13, 2008

This week we stared to look at gelogical phenomineons. We discovered that once in New Jersey two plates spepperated and now it is a valley. We have discovered the different types of rocks. Metomorphic, Ignious, and lastly Sedmemntary. Ignious is formed from lova/magma that has been cooled and hardens, Sedementary forms sedement mud or clay that has been pressed together by pressure Metomorphic is formed by rock that undergoes through both pressure and heat. We also did a test about if citric acid made a difference in erosion compared to water. We emidiatly saw acid bubbling in the container and the chalk got smaller sat to the water the only real difference was the color. That was my week.
-Go Sooners

Saturday, December 6, 2008

This week we learned about maps and contour lines indexes and more. We put to gether a map of new jersey and we saw that we saw that their was a valley or something inbetween mountains. We think this accures by earthquakes and that the plates shifted and thats why this valley is running throught NJ