Tuesday, March 12, 2013

Plate Tectonics Essay



Plate Tectonics
Throughout the history, the earth’s geography has changed a lot. Scientists had started focusing on the changes made on earth’s surface between 1900s. The theory which states that Pangaea existed, and it separated through the time of 200 million years is called Theory of Plate Tectonics. This theory is agreeable, because as the Pangaea is mapped, there are some landforms such as deserts, mountains etc., which can be connected. Not only landforms, but fossils of dinosaurs are found in the neighbors surfaces as shown by Pangaea.
The waves of energy travelling through earth’s layers are known as seismic waves. Breaking of rocks inside the earth cause these waves to act, mostly resulting in earth quakes. This is an evidence to prove the theory of plate tectonics true, because earth quakes must have played a vital role in spreading of surface into pieces. There are three main types of seismic waves. Firstly, P-waves are the primary waves, which travel back and forth horizontally. These waves are the first one to come. Then S-waves approach, which travel up and down, and can travel through rocks only. After those two waves, Love-waves reach which travel up, down, back and forth. Seismic waves have a great effect on the earth’s geography change over long periods of time throughout history.
On the surface of earth, there are huge chunks of rocks known as plates, producing different natural landforms when they move. There are two types of plate, continental plate, which is found under the solid land surface. Secondly the oceanic plate comes, which is found under the ocean water surface. Plate boundaries are the huge deformation zones, which are divided into three main types. Convergent boundaries are formed when boundaries move together, in contrast Divergent boundaries are formed when boundaries movie a part from each other. Transform boundaries are formed when two boundaries slide past each other.  Large chunks of rocks form landforms such as volcanoes, trench and ridge.
Fracture in earth’s crust is known as faults. Fault can cause a movement on the point inside the earth known as focus. This movement travels to surface of the earth by seismic waves and the point where the movement begins on the surface of the earth is known as epicenter. There are mainly three types of faults. Normal faults are caused when one side of surface moves downwards. In contrast, Reverse fault is caused when one side of surface moves upwards. Strike-slip fault is caused when both surfaces slide past each other. Faults have contributed evidently in changing the earth’s geography throughout the history.
Earth’s geography has changed throughout the long period of time. The theory of Tectonic Plates is agreeable, because there is a lot of evidence proving it. Beliefs as simple as Global warming support this theory too. Earth wasn’t the same when it was created, because there are signs and historical figures still existing as an evidence of it today. Main topics, such as Seismic waves, Plate boundaries and faults are scientifically tested proofs of the existence of the theory of Plate Tectonics.



Reflection

  • What did you enjoy most about this project and why?
I enjoyed making quizzes, because it was in my control. I felt like a teacher, and I knew that it is a big responsibility as well as hard work to make the students the topic that is being taught.

  • What was the most challenging for you during this project and why?
      The most challenging thing for me to do in this project was deciding what activities to choose. Another        thing that was hard for me was to manage time, and set a certain time for each activity.                                         

  •          What new skills did you learn from doing this project?

I learned that finishing work on time should be our first priority, and I learned that if pictures are involved in a presentation, it attracts the audience more.
  • Is there anything you could have done to improve any of your work? Explain.
I could have been more detailed, and focused on the little mistakes I made. Little mistakes took my score from my desirable score to a lower score. I also think I would have proofread my work, or get checked from someone else, to make it better.
  • What would you change about this project?
I would change the lab to be more fun and entertaining so it can attract student, not because they would be working with each other, but they would learn something useful and use it in their lives too.




Tuesday, November 6, 2012

Crystals & Minerals

Crystals- First we poured the beaker with distilled water, and heated it on an electric burner. We had 3 choices of minerals which were Halite, Sugar and Epsomite. And to identify we added different food color in beakers. We kept stiring the solution and kept adding the mineral, untill the solution was fully saturated. After that we turned the burner off, and placed a tag on the beaker for identification. Then they were placed in the window, and we observed them every day, and took readings. We used 2 processes for crystallizing. First evaporation takes place, and later it solidifies.

Mineral Properties-

Color  Color when a person looks at the mineral.

Streak   Color which is produced when mineral is scratched.


Luster

Metallic Luster                                         Non-Metallic Luster














Cleavage   Minerals which cut evenly

Fracture  Minerals which cut unevenly

Composition   Chemical properties.

Other Properties:

Magnetism  Minerals that consist magnetic energy


Mineral Identification

Graphite:

Color-Silver
Luster-Metallic
Opaque
Fracture





Quartz:


Color-Transparent, White
Luster-Non Metallic
Clear, blurry image
Cleavage

Saturday, October 27, 2012

Rock Types

Rock Cycle
Rocks change constantly from one type to another. First the magma uplifts by the force of gases through a mountain, which is mostly referred as Volcano. When these molten rocks travel outside, they are named as lava. Because of the different temperature of inside and outside of earth, the lava solidifies and become solid, known as Igneous Rock. By weathering and erosion, the rocks break down in small sediments. Later, these sediments are pushed together and become a new rock, known as Sedimentary Rock. As the rocks travel downwards by the layers of the earth, they heat up and pressure acts on them, making layers and producing another kind of Metamorphic Rock. The rocks keep travelling downwards, and finally meet up with magma, which is located at the most bottom of the layers. And so on, the rock forming cycle keeps working.

Rocks

Metamorphic Rock: Rocks formed by heat and pressure.

Magma: Molted rocks inside the earth.

Lava: Molted rocks outside the earth.

Solidification: The process by which lava cools down and becomes solid.

Igneous Rock: Rocks formed when lava is cooled down and solidifying.

Weathering: When rocks are broken down by storms etc.

Erosion: When rocks are moved from the surface by winds etc.

Sediment: Small rocks broke down by weathering and erosion.

Compaction: Process by which sediments come together.

Cementation: Process by which sediments are glued together.

Sedimentary Rock: Rocks formed when compaction and cementation takes place with sediments.

Rock Types

Igneous Intrusive Rock: Igneous Rocks that are formed inside of the earth.

Igneous Extrusive Rock: Igneous Rocks that are formed outside of the earth.

Sedimentary Clastic Rock: Sedimentary rocks formed when little fragments are glued together.

Sedimentary Crystalline Rock: Sedimentary Rocks formed when minerals and evaporation.

Sedimentary Bioclastic Rock: Sedimentary Rocks formed when left over of dead organisms are glued together.

Metamorphic Foliated Rock: Metamorphic Rocks formed as layers.

Metamorphic Non-Foliated Rock: Metamorphic Rocks formed without layers.