Wednesday, February 27, 2013

Radiometric Age Dating

Radiometric Age Dating

photo.JPG

1. Draw a 10x10 grid on paper
2. Use M&M's, skittles, pennies, etc. (has to have a heads and tails)
3. Put 100 items, heads up on the grid (100 left)
4. Take all off, shake and empty on grid
5. Take all heads up items off (47 left)
repeat #4 & #5
-as repeated-
(18 left) then,
(5 left) then,
(4 left) then,
(3 left) then,
(3 left) then,
(1 left) then,
(0 left)

As a class we averaged these numbers out to show that nearly every shake & empty, 50% of the items were removed.

The graph would look something like this:


Monday, February 25, 2013

Geologic Time: on Adding Machine Tape

Time on Earth is LONG.
Time that Life has been on Earth is SHORT.
Time that People have been on Earth is VERY SHORT!

This project is a great way to show students tangibly how long Earth's timeline is. The scale for the measurements on the adding machine tape is  1 cm = 10 million years ( 1 mm = 1 million years). 

[We only labeled up the the Pre-Cambrian period] 



What do we know? And more about fossils!

How are you coming along with learning the geologic time scale?

I am getting more familiar with the different eras and periods we need to know within the geologic time scale, but I do not have them memorized yet. I think that I will make use of the mnemonic device to remember the periods within the Paleozoic, Mesozoic, and Cenozoic Era's:
Come Over Some Day, Maybe Play Poker. Two Jacks Cover Two Queens.
Cambrian, Ordovician, Silurian, Devonian, Mississippian, Pennsylvanian, Permian, Triassic, Jurassic, Cretaceous, Tertiary, Quaternary.

What do you know about fossils?
ALL fossils show that something at some point was alive.

Often times fossils can be found inside and preserved in amber, which is fossilized tree resin.

Trace fossils: footprints, burros



Petrified wood

Mold and Cast



Carbonized leaf fossils



Whole animal fossils





Making Fossils Lab:
We made three different mixtures of plaster and sand, added a shell, and let the mixtures harden over two days. When we returned to class, we broke the shell out of the hardened mixtures. We were trying to see which mixture was the best; i.e. easiest to get the shell out, and left a defined imprint. 

Hypothesis:
We guessed that the more sand there was in the mixture the easier the it would be to get the shell out. 

Our mixtures were (manipulated variable): 
60% plaster to 20% sand- 60mL to 20mL
50% plaster to 50% sand- 40mL to 40mL
20% plaster to 60% sand- 20mL to 60mL (error: we had to add 5% more plaster so that the mixture would cover the shell and harden)

Our constant was:
30mL water

Our three mixtures:
photo.JPG

50/50:
image.jpeg
60/20 plaster/sand:
image.jpeg
25/60 plaster/sand:
image.jpeg

Result: 
As we worked on getting the shells and imprints out of the hardened mixtures we found that the 50/50% mixture was the best for removal and had clear and defined imprints. The 60/20 plaster/sand was very hard to break apart. The 25/65 plaster/sand mixture broke apart very easily. 

**After we finished the activity we decided that this activity was probably not applicable for the classroom, as getting the shell out of the hardened mixture required a hammer, which would not be safe. 




Friday, February 22, 2013

Sun Observations


"Measure the gnomon's height from the point where the shadow begins, to the top directly above that point. The shadow is measured from the stick where the shadow begins to the end of the shadow. If the shadow stick is thick, do not add the thickness of the stick to the length of the shadow.
Once you have the shadow length, you can calculate the angle of the Sun with trigonometry using the shadow length and gnomon height: Remember that you need to make a minimum of 3 measurements and find the angle values for each measurement. You will then average the three angles for your final value". -Mitchell Klett MSED 252
Pictured above is my project with my measurements of shadows. 

Wednesday, February 20, 2013

Geologic Time Scale

We are beginning to talk about Geologic Time in Earth Science class. One thing that we have to know is the order of the geologic time eras. The following video shows, what I assume to be, a GREAT high school science project talking about geologic time. This is such a fun way to present the knowledge and get some cross-curriculum enjoyment! Singing, dancing, all with the information makes for a stupendous project! I would definitely give them an 'A'!





Monday, February 4, 2013

If I Had One-Hundred Dollars


If our solar system represented $100 dollars, how would you break up that money to proportionally represent the mass inside of the solar system.

Sun- $80 correct answer $99.85
Mars- $.50 correct answer $0.00004
Venus- $.50 correct answer $0.0003
Earth- $2 correct answer $0.0003
Mercury- $2 correct answer $0.00002
Jupiter- $4 correct answer $0.106
Saturn- $4 correct answer $0.032
Uranus- $1 correct answer $0.006
Neptune- $1 correct answer $0.005
Satellites- $1 correct answer $ almost nothing
Minor Elements- $3 correct answer $ almost nothing
         (comets, asteroids, Trans-Neptunian Objects's, etc.)

Order of the Planets:
My Very Educated Mother Just Served Us Nachos.

The Solar System to Scale
http://www.scalesolarsystem.66ghz.com/