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Tuesday, 12 November 2019

Marshmallow Catapult.

Everything on earth has potential energy. This means that it could move even if it isn't right now. When an object is moving it has kinetic energy

Say we stored energy in a spring. That spring will have the potential to move, however it wont move until we let it. Like a Catapult, a catapult has the potential to move at anytime we just need to set it off. The catapult is going to transfer energy from the spring to a marshmallow. The marshmallow will have potential energy until the catapult is released. As the marshmallow is flying through the air it will have kinetic energy meaning it is moving. 

The reason i'm using a catapult. The catapult experiment requires minimal equipment, is fun and shows how potential and kinetic energy works really well.

To make this catapult you will require.
  1. 10 Popsicle sticks.
  2. 4 rubber bands (Not crap)
  3. 1 bottle cap (Milk cap recommended)
  4. Ammo (Marshmallow in our case)
  5. Hot glue gun
1. The first thing you want to do is gather all your materials. 

2. Rubber band two pieces of Popsicle sticks together at the ends.












3. Stack the remaining eight sticks together and rubber band the ends together.











4. Slide the stack of eight in between the other two pieces.











5. Now use the fourth band to secure all the sticks together.











6. Use a hot glue gun to stick the milk cap to the end of the catapult (wait till dry).












7. Put your mini marshmallow in the milk cap and Enjoy!

Results: 














These are the numbers this experiment got.

How to calculate energy.
Potential energy - Due to position
Potential energy is Mgh. M (Mass), g (Gravitational acceleration) and h (Height).

Kinetic energy - Due to movement 
Potential energy is 1/2 mv^2. M (Mass), V (Velocity).

Example 
Let's say for example I climbed to the top of a ten-story building. To do this calculation we will need to know our mass (i weigh around 80kg). For this calculation we will also need to know the acceleration due to gravity or g (acceleration of gravity is 9.81m/s^2). Now we have to convert the ten-story building into meters (which is about 32m roughly).  Now multiply these together, I got 25 113.6 joules. If we do significant digits that is 2.5 x 10^4 joules of energy that my body has at the top of the building and as long as I stay at the top of that building I can use that on the way down. I don't want to jump of the building so for kinetic energy we will use a baseball instead. Remember kinetic = (1/2mv^2). If I pitch a baseball and there are two different pitches. When I throw, I probably throw it at around 20mph. Where a pro pitcher throws at about 100mph. Now to figure out how much kinetic energy would be in one of my throws and then a pro's. First, we need the weight of the baseball (lets say 0.145kg). Since we are doing kinetic the only other value we need is the speed (20mph = 13.0m/s). For these we always have to convert to m/s. A 100mph pitch then is roughly 45 m/s. Now let's figure out how much kinetic energy my pitch would have. We use the equation 1/2mv^2. M (0.145), V (9.0m/s). We then take that 1/2 and square the velocity and get 5.9 joules. Do the same with the Pro's and we should get 150 joules.

Not all potential energy will turn into kinetic energy. Some of the potential energy will turn into sound and heat energy.

That in a simpler way.
M        G        H
80 × 9.81 × 32 = 25113.6 joules of potential energy.
1/2m           v^2
0.145  x  9.0^2 = 5.8725 joules of kinetic energy.

Monday, 4 November 2019

Rock Cycle

Rock cycle


What is the rock cycle?
The rock cycle is a concept in geology that describes how rocks change through geologic time.
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Intrusive Igneous Rocks
Intrusive, or plutonic, igneous rocks form when magma cools slowly below the Earth's surface. Most intrusive rocks have large, well-formed crystals.

Image result for intrusive igneous rocks

Diorite is an intrusive igneous rock with a composition between that of granite and basalt. It usually occurs as large intrusions (---), dikes (---) and sills (---) within continental crust. These often form above a convergent plate boundary where an oceanic plate sub-ducts underneath a continental plate. Melting of the oceanic plate produces a basaltic magma (---) that rises and intrudes the granitic rock of the continental plate. There, the basaltic magma mixes with granitic magma's or melts granitic rock as it ascends through the continental plate. This produces a melt that is intermediate in composition between basalt and granite. Diorite forms if this type of melt crystallises below the surface.

Image result for diorite

Gabbro is an intrusive igneous rock, it is usually black or dark green in colour and composed mainly of the minerals plagioclase (---) and augite (---) . Could find out much more.

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Granite is a light coloured intrusive igneous rock with grains (---) large enough to be visible with no special equipment. It forms from the slow crystallisation of magma below Earth's surface. Granite is compose mainly of quartz (---) and feldspar (---) with little bits of mica (---), amphiboles (---), and other minerals. This mineral composition usually gives granite a red, pink, grey or white colour with dark mineral grains visible through out the rock.

Image result for granite rock

Pegmatite are  intrusive igneous rocks that form during the final stage of magma's crystallisation.
They contain large crystals and they sometimes contain minerals that are rarely found in other types of rocks (---). The name pegmatite has nothing to do with the mineral composition of the rock. Most pegmatite have a composition similar to that of granite.

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Peridotite is a dark coloured, ultramafic (---) igneous rock. Peridotite contain olivine (---) as its primary mineral, also with other mafic minerals like pyroxenes and amphiboles. Their silica (---) content is low compared to other igneous rocks. They also contain very little quartz and feldspar. Much of earths mantle is believed to be Peridotite. different types of Peridotite include dunite, lherzolite, harzburgite, wehrlite.

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Extrusive Igneous Rocks
Extrusive igneous rocks form when magma reaches the Earth's surface a volcano and cools quickly. Most extrusive (volcanic) rocks have small crystals.

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Andesite is an extrusive igneous rock that is usually light to dark grey in colour.

Basalt

Obsidian

Pumice

Rhyolite

Scoria

Clastic Sedimentary Rocks
Breccia
Conglomerate
Sandstone
Siltstone
Shale

Chemical Sedimentary Rocks
Iron ore
Chert
Flint
Dolomites
Limestones

Organic Sedimentary Rocks
Coal
Dolomites
Limestones

Friday, 1 November 2019

Line graph

What does the graph show us?
How the population of NZ changed over the years.

Why do you think the numbers of Māori change? Because they breeded with pakeha.


Why do you think numbers of Europeans changed? Because more came from foreign countries.