Today we got pizza in class to represent the Earth's layers! They represent:
Crust - Earth's Mantle
Sauce - Asthenosphere
Cheese - Oceanic Crust
Toppings - Continental Crust
MSED252 Blogs
Friday, April 19, 2013
Friday, April 5, 2013
Importance of Water!
US populations mid 1800's:
Most all of these cities are on the east coast. The only city I haven't heard of on this list is Spring Garden, PA. I believe all these cities are on the water. This was important in 1800's because they traded and traveled by water.
•New
York, NY
•Baltimore,
MD
•Boston,
MA
•Philadelphia,
PA
•New
Orleans, LA
•Cincinnati,
OH
•Brooklyn,
NY
•St.
Louis, MO
•Spring
Garden, PA
•Albany,
NY
Most all of these cities are on the east coast. The only city I haven't heard of on this list is Spring Garden, PA. I believe all these cities are on the water. This was important in 1800's because they traded and traveled by water.
Distribution of the Water "If I had 100 Dollars":
My Guess
Oceans: 90
Clouds:
.5
Rivers:
1
Lakes: 2
Seas: 1
Ground
Water: 2
Soil
Moisture: .5
Glaciers: 3
Actual
Oceans 97.2
Glaciers
2.15
Ground
Water 0.62
Fresh
Water Lakes 0.09
Salt
Water Lakes and Seas 0.08
Variable
0.07
Soil
moisture 0.05
Atmosphere
0.01
Streams 0.0001
Monday, March 25, 2013
Story of a rock
I am Sandstone which means I am a sedimentary rock. Sedimentary rocks form from weathered sediments, when they are compacted
and squeezed to make a rock. We are pushed down into the earths crust after layer after layer of rock
covers us. Then as we are pushed down, heat and pressure increase. The continued pressure transforms the rock. We are now a metamorphic rock.
Friday, March 22, 2013
Siumulations, Models, and Analogues
A simulation is an imitation of something
A model is a larger or smaller representation of something else.
An analogue is comparable to something else
Lesson plan examples of models:
Sedimentary rock layer lesson: http://library.thinkquest.org/J002289/act.html
-- Sedimentary rocks are made in layers. The layers of mud,sand, or even seashells are built up over a long period of time. The layers get squeezed and stuck together to make new rocks. This cookie is made in layers and you can still see the layers even after it is pressed and cooked.
Making fossils: http://www.canteach.ca/elementary/life19.html
-- Students make impressions of leaves, shells, flowers, etc.
Metamorphic rock: Butterfingers, crayons melted together.
Igneous: crystallization, fudge,
A model is a larger or smaller representation of something else.
An analogue is comparable to something else
Lesson plan examples of models:
Sedimentary rock layer lesson: http://library.thinkquest.org/J002289/act.html
-- Sedimentary rocks are made in layers. The layers of mud,sand, or even seashells are built up over a long period of time. The layers get squeezed and stuck together to make new rocks. This cookie is made in layers and you can still see the layers even after it is pressed and cooked.
Making fossils: http://www.canteach.ca/elementary/life19.html
-- Students make impressions of leaves, shells, flowers, etc.
Metamorphic rock: Butterfingers, crayons melted together.
Igneous: crystallization, fudge,
Monday, March 18, 2013
A Mineral is...
A Mineral is...
1. Naturally occurring
2. Solid
3. Inorganic
4. Has an orderly internal structure of atoms
5. Has a definite chemical composition
Most Common Earth Elements:
1. Naturally occurring
2. Solid
3. Inorganic
4. Has an orderly internal structure of atoms
5. Has a definite chemical composition
Most Common Earth Elements:
Oxygen | 46.6% | |||
Silicon | 27.7% | |||
Aluminum | 8.1% | |||
Iron | 5% | |||
Calcium | 3.6% | |||
Sodium | 2.8% | |||
Potassium | 2.6% | |||
Magnesium | 2.1% | |||
Other | 1.5% |
Wednesday, March 13, 2013
Elements, bonding, form
What do I know about...
Mrs. Stewart's crystal garden: http://mrsstewart.com/magic-salt-crystal-garden/
Recipe:
This is a classic crystal-growing project. You use charcoal briquettes (or other porous materials), ammonia, salt, bluing, and food coloring to grow a sort of crystal garden.
- elements
- bonding
- form/crystals
Mrs. Stewart's crystal garden: http://mrsstewart.com/magic-salt-crystal-garden/
Recipe:
This is a classic crystal-growing project. You use charcoal briquettes (or other porous materials), ammonia, salt, bluing, and food coloring to grow a sort of crystal garden.
- Place chunks of your substrate (i.e., charcoal briquette, sponge, cork, brick, porous rock) in an even layer in the non-metal pan. You want pieces that are roughly 1-inch in diameter, so you may need to (carefully) use a hammer to break the material up.
- Sprinkle water, preferably distilled, onto the substrate until is has been thoroughly dampened. Pour off any excess water.
- In an empty jar, mix 3 tablespoons (45 ml) uniodized salt, 3 tablespoons (45 ml) ammonia, and 6 tablespoons (90 ml) bluing. Stir until the salt is dissolved.
- Pour the mixture over the prepared substrate.
- Add and swirl a bit of water around in the empty jar to pick up the remaining chemicals and pour this liquid onto the substrate, too.
- Add a drop of food coloring here and there across the surface of the 'garden'. Areas with no food coloring will be white.
- Sprinkle more salt (about 2 T or about 30 ml) across the surface of the 'garden'.
- Set the 'garden' in an area where it will not be disturbed.
- On days 2 and 3, pour a mixture of ammonia, water, and bluing (2 tablespoons or 30 ml each) in the bottom of the pan, being careful not to disturb the delicate growing crystals.
- Keep the pan in an undisturbed place, but check on it periodically to watch your very cool garden grow!
Monday, February 25, 2013
What do I know?
What do I know?
1. The geologic time scale: I know the mnemonic device come over some day maybe play poker two jacks cover two queens, but I can not remember any of the periods they stand for besides Cambrian Mississippian and Pennsylvanian
---When I looked it up - Cambrian, Ordovician, Silurian, Devonian, Mississippian, Pennsylvanian, Permian, Triassic, Jurassic, Cretaceous, Tertiary, Quaternary. This is the order from oldest to present.
2. About fossils: I really don't know much about fossils at all. I know bones are considered fossils, that there can be imprints of old living things, and amber holds a lot, but that's about it.
---When I looked it up - Fossils are preserved remains or traces of animals, plants, and other organisms from the remote past. Amber is tree sap that is fossilized. Trace fossils are things that indicate life was there such as footprints and burrows. Petrified wood is wood that has been replaced by minerals. Other fossil types include, mold and cast, carbonized leaf fossils, and the whole animal caught itself.
(http://www.google.com/url?sa=i&rct=j&q=&esrc=s&source=images&cd=&cad=rja&docid=EoiVb503YFJ7gM&tbnid=gLMEeNWwuc3ptM:&ved=0CAUQjRw&url=http%3A%2F%2Fdefendingjehovahswitnesses.blogspot.com%2F2011%2F12%2Ffossils-links-to-information.html&ei=Go4rUd-XN-TB2wX1zYHgCQ&bvm=bv.42768644,d.b2I&psig=AFQjCNE-5WCp1bEgdwkpX0eUdYt1jUY6GA&ust=1361895311068258)
On Monday in class we did an experiment with making fossils. My group decided to have 3 different mixtures. One cup was a 50/50 ratio: 40mL of sand and 40mL of plaster. Another was 60mL of sand and 20mL of plaster. The last cup started out with 60mL of plaster and 20mL of sand, but we had to add 5 more mL of sand to cover the whole shell, making it 25mL of sand. Today, Wednesday, we broke apart these cast and molds. We found out our 50/50 mixture was the easiest to break and was the only one that came out whole. However, this was a flat shell compared to our other two swirly shells, so this could have had an impact. The one that had 60mL of plaster was extremely hard to break and the fossil came out in bits and pieces, but the pieces did have good imprints on them.
1. The geologic time scale: I know the mnemonic device come over some day maybe play poker two jacks cover two queens, but I can not remember any of the periods they stand for besides Cambrian Mississippian and Pennsylvanian
---When I looked it up - Cambrian, Ordovician, Silurian, Devonian, Mississippian, Pennsylvanian, Permian, Triassic, Jurassic, Cretaceous, Tertiary, Quaternary. This is the order from oldest to present.
2. About fossils: I really don't know much about fossils at all. I know bones are considered fossils, that there can be imprints of old living things, and amber holds a lot, but that's about it.
---When I looked it up - Fossils are preserved remains or traces of animals, plants, and other organisms from the remote past. Amber is tree sap that is fossilized. Trace fossils are things that indicate life was there such as footprints and burrows. Petrified wood is wood that has been replaced by minerals. Other fossil types include, mold and cast, carbonized leaf fossils, and the whole animal caught itself.
(http://www.google.com/url?sa=i&rct=j&q=&esrc=s&source=images&cd=&cad=rja&docid=EoiVb503YFJ7gM&tbnid=gLMEeNWwuc3ptM:&ved=0CAUQjRw&url=http%3A%2F%2Fdefendingjehovahswitnesses.blogspot.com%2F2011%2F12%2Ffossils-links-to-information.html&ei=Go4rUd-XN-TB2wX1zYHgCQ&bvm=bv.42768644,d.b2I&psig=AFQjCNE-5WCp1bEgdwkpX0eUdYt1jUY6GA&ust=1361895311068258)
On Monday in class we did an experiment with making fossils. My group decided to have 3 different mixtures. One cup was a 50/50 ratio: 40mL of sand and 40mL of plaster. Another was 60mL of sand and 20mL of plaster. The last cup started out with 60mL of plaster and 20mL of sand, but we had to add 5 more mL of sand to cover the whole shell, making it 25mL of sand. Today, Wednesday, we broke apart these cast and molds. We found out our 50/50 mixture was the easiest to break and was the only one that came out whole. However, this was a flat shell compared to our other two swirly shells, so this could have had an impact. The one that had 60mL of plaster was extremely hard to break and the fossil came out in bits and pieces, but the pieces did have good imprints on them.
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