14/06/2016 Forces and Motion. 14/06/2016Moments A moment is a “turning force”, e.g. trying to open or close a door or using a spanner. The size of the.

Slides:



Advertisements
Similar presentations
Preview Section 1 Inside the Earth Section 2 Restless Continents
Advertisements

The restless earth. The earth as it appeared 65 million years ago Early Geologists missed the most obvious observation that Africa’s coast line closely.
Plate Tectonics.
Plate Tectonics Review
Shake, Rattle, and Roll the Earth
STRUCTURE OF THE EARTH Noadswood Science, 2011.
Plate Tectonic Test Review Answers!
PLATE TECTONICS HOW THE EARTH MOVES. STRUCTURE OF THE EARTH The Earth is made up of 3 main layers:  Core (inner and outer)  Mantle  Crust Inner core.
Why does Earth have mountains?
Chapter One Section 1 Plate Tectonics
Earth’s Interior Section1.
Plate Tectonics: Continental Drift. a relatively new scientific concept introduced some 40 years ago. revolutionized our understanding of the dynamic planet.
AMY SHANTA BABOOLAL PHYSICS PROJECT: MECHANICS. ARISTOTLE’S ARGUMENTS One of his well known arguments is: to understand change, a distinction must be.
What type of boundary is represented here?
Earth Shaping Chapter 16. Earth Shaping Theory   It was a gradual change over time.   In early 1900’s Alfred Wegener proposed the theory of continental.
Earth Materials – Geology Plate tectonics Why have all the mountains not worn away by now?
The Earth’s Interior & Plate Tectonics. The Earth’s Interior The Earth’s Interior can be broken up into 4 major zones Crust Mantle Outer core Inner core.
Chapter 8 Lesson 1 What are Earth’s layers made of?
Earth Materials – Geology Plate tectonics Why have all the mountains not worn away by now? 100’s of free ppt’s from library
Notes 11 – Plate Tectonics Earth Science Mrs. Gordon Saturday, October 10, 2015Saturday, October 10, 2015Saturday, October 10, 2015Saturday, October 10,
 Composition: Silicon, Oxygen, and Aluminum  Types: › Continental Crust: solid & rocky outer layer › Oceanic Crust: thin & dense material.
Our Amazing Planet. Planet Earth Earth’s Layers Crust Earth’s thin outermost layer. – Continental Crust (land) - thick low density rock (granite). –
Our Amazing Planet.
Plate Tectonics L.O: To understand how tectonic plates move and the theory of continental drift.
Plate Tectonics. The Structure of the Earth A thin crust km thick A mantle – has the properties of a solid but it can also flow A core – made.
1 Hi Guys This term we have 2 more units: Changing Earth Working world For the next 6 weeks it is ‘Changing Earth’
1 2 pt 3 pt 4 pt 5pt 1 pt 2 pt 3 pt 4 pt 5 pt 1 pt 2pt 3 pt 4pt 5 pt 1pt 2pt 3 pt 4 pt 5 pt 1 pt 2 pt 3 pt 4pt 5 pt 1pt Pulling me apart Pulling me apart.
The Earth’s Interior & Plate Tectonics Physical Science Chapter 17 Section 1.
The Earth and it’s layers
Theory of Continental Drift (pg ) The Theory of Continental Drift states that all continents on Earth were once joined together as Pangaea, but.
Our Amazing Planet. Engage Assignment Make a 3 slide power point on each of the three types of plate boundaries – Convergent boundaries – Divergent boundaries.
Forces that act on the Earth. The Inner Core The deepest layer in Earth is the inner core. It is located at the center of Earth because it contains.
Plate Tectonics Unit:. Composition of the Earth: Layers of the Earth: 1.Crust: 5-100km thick. a.Oceanic crust: thin and more dense, mostly basalt b.Continental.
Dynamic Planet Module Review. Bending of a wave due to changes in its velocity 1.Convection 2.Reflection 3.Subduction 4.Refraction.
Africa The Red Sea between Africa and the Arabian peninsula in Asia marks a region where two pieces of the lithosphere are slowly moving apart. Over the.
Just as the theory of Evolution underpins Biology The theory of Plate tectonics is the basis of Earth Science So how did the theory of Plate tectonics.
CHAPTER TEN PLATE TECTONICS. Background Information  The Earth is made up of several layers that have different properties and compositions.  There.
List 1 fact about Earth. Agenda for Monday Nov 22 nd 1.Finish Movie 2.Layers of the Earth notes.
Science 7: Unit E: Planet Earth Topic 4 – The Moving Crust.
 In 1912, German scientist Alfred Wegener proposed the idea of continental drift.  Based on evidence he saw, he believed that the continents must have.
The Structure of The Earth Convection currents Tectonic Plates Plate Movements.
Earth’s Layers The three main layers of Earth are the crust, mantle, and the core. These layers vary greatly in size, composition (what they are made of),
Plate Tectonics 8 th Grade Science. Earth’s Composition.
Structure of the earth. Inner Core – This is in the centre of the earth where it is hottest. It is solid and consists of Iron and Nickel with temperatures.
P5 Space 4 Reflection Revision Seminar.
Plate Tectonics.
LAYERS OF THE EARTH PLATE BOUNDARIES PLATE TECTONICS CONTINENTAL DRIFT
What is the Earth made of?
Plate Tectonics.
Earth Materials – Geology Plate tectonics
Unit 1B Natural hazards.
Momentum.
21/09/2018 Plate Tectonics The idea of continental drift is now referred to as plate tectonics. How can the continents move?
Earth’s Layers The three main layers of Earth are the crust, mantle, and the core. These layers vary greatly in size, composition (what they are made of),
Plate Tectonics Earth’s Interior Convection Currents
Plate Tectonics Theory that the outer rigid layer of the earth (the lithosphere) is divided into a couple of dozen "plates" that move around across the.
Plate Tectonics 8th Grade Science.
Momentum 27/11/2018 Any object that has both mass and velocity has MOMENTUM. Momentum (symbol “p”) is simply given by the formula: P V M Momentum = Mass.
Outer Core Liquid layer of Earth’s core Surrounds inner core.
Momentum 28/12/2018 Any object that has both mass and velocity has MOMENTUM. Momentum (symbol “p”) is simply given by the formula: P V M Momentum = Mass.
Continental Drift 1912 – German Scientist Alfred Wegener
Earth’s Dynamic Crust & Interior
Earth Layers Physical Layers Continental Drift Seafloor Spreading Plate Boundaries
QUICK REVIEW… Layers of the Earth
Plate Tectonics.
Unit 2.2 – Plate Tectonics EQ1: How was scientific evidence used to come up with the Theory of Plate Tectonics, and has the theory become widely accepted.
Presentation transcript:

14/06/2016 Forces and Motion

14/06/2016Moments A moment is a “turning force”, e.g. trying to open or close a door or using a spanner. The size of the moment is given by: Moment (in Nm) = force (in N) x distance from pivot (in m) Calculate the following turning moments: 100 Newtons 5 metres 200 Newtons 2 metres

14/06/2016 Balancing moments 100 Newtons200 Newtons 2 metres Total ANTI-CLOCKWISE turning moment = 200x2 = 400Nm Total CLOCKWISE turning moment = 100x2 = 200Nm The anti-clockwise moment is bigger so the seesaw will turn anti-clockwise

14/06/2016 Balanced or unbalanced?

14/06/2016Stability 1. Centre of mass is within the wheelbase – no problem! 2. Centre of mass is directly above the edge of the wheelbase –car is on the point of toppling 3. Car falls over

14/06/2016 Centripetal force Consider a ball of Pleistocene attached to some string: The ball is kept in its path by the tension in the string – an example of a CENTRIPETAL FORCE. This force also produces the change in velocity due to the direction constantly changing. This force is INCREASED if you increase the mass of the object, its speed or decrease the radius of the circle. Other examples of centripetal forces: Orbits Electrons

14/06/2016Momentum Any object that has both mass and velocity has MOMENTUM. Momentum (symbol “p”) is simply given by the formula: Momentum = Mass x Velocity (in kgm/s) (in kg) (in m/s) P VM What is the momentum of the following? 1)A 1kg football travelling at 10m/s 2)A 1000kg Ford Capri travelling at 30m/s 3)A 20g pen being thrown across the room at 5m/s 4)A 70kg bungi-jumper falling at 40m/s

14/06/2016 Conservation of Momentum In any collision or explosion momentum is conserved (provided that there are no external forces have an effect). Example question: Two cars are racing around Teville Gate. Car A collides with the back of car B and the cars stick together. What speed do they move at after the collision? Mass = 1000kgMass = 800kg Speed = 50m/sSpeed = 20m/s Momentum before = momentum after… …so 1000 x x 20 = 1800 x V… …V = 36.7m/s Mass = 1800kg Speed = ??m/s

14/06/2016 More questions… 1)A white snooker ball moving at 5m/s strikes a red ball and pots it. Both balls have the same mass. If the white ball continued in the same direction at 2m/s what was the velocity of the red ball? 2)A car of mass 1000kg heading up the M1 at 50m/s collides with a stationary truck of mass 8000kg and sticks to it. What velocity does the wreckage move forward at? 3)A defender running away from a goalkeeper at 5m/s is hit in the back of his head by the goal kick. The ball stops dead and the player’s speed increases to 5.5m/s. If the ball had a mass of 500g and the player had a mass of 70kg how fast was the ball moving? 4)A gun has a recoil speed of 2m/s when firing. If the gun has a mass of 2kg and the bullet has a mass of 10g what speed does the bullet come out at? (Hint: total momentum before is zero and the gun has a negative velocity afterwards)

14/06/2016 A past exam question… Two lorries are travelling in the same direction along a motorway. 1)Calculate the momentum of Lorry A as it travels along the motorway. 2)Calculate the momentum of Lorry B as it travels along the motorway. (3 marks) 3)Lorry B collides with Lorry A and they stick together. Calculate the common speed of the lorries immediately after the collision. (3 marks) June 2000 Lorry A Mass = 20,000kg Speed = 14m/s Lorry B Mass = 30,000kg Speed = 20m/s

14/06/2016 Newton’s Laws of Motion 1) If an unbalanced force acts on an object that object will either accelerate or change direction: 2) That force is given by F=ma 3) When a force acts on an object there is an equal force acting in the opposite direction (“Action and reaction are equal and opposite”) F A M These are my three laws of motion (summarised):

14/06/2016 Newton’s 2 nd Law Instead of F=ma Newton actually said that the force acting on an object is that object’s rate of change of momentum. In other words…  mv TF Force = Change in momentum Time (in N) (in kgm/s) (in s) For example, David Beckham takes a free kick by kicking a stationary football with a force of 40N. If the ball has a mass of 0.5kg and his foot is in contact with the ball for 0.1s calculate: 1)The change in momentum of the ball, 2)The speed the ball moves away with

14/06/2016 Example questions 1)A golfer strikes a golf ball with a force of 80N. If the ball has a mass of 200g and the club is in contact with it for 0.2s calculate a) the change in momentum of the golf ball, b) its speed. 2)A tennis player strikes a serve with a force of 30N. If the ball has a mass of 250g and the racket is in contact with it for 0.15s calculate the ball’s change in momentum and its speed. 3)A footballer takes a goal kick by kicking a 0.4kg football away at 10m/s. If his foot was in contact with the ball for 0.1 seconds calculate the force he applied to the ball. 4)A golfer strikes a 200g golf ball away at 50m/s. If he applied a force of 50N calculate how long his club was in contact with the ball for.

14/06/2016 Energy loss in collisions We’ve also said that in a collision momentum is conserved (unless an external force acts). The same cannot usually be said for kinetic energy… For example, consider the following collision. How much kinetic energy is lost? Mass = 1000kgMass = 800kg Speed = 50m/sSpeed = 20m/s Kinetic energy = ½ x mass x velocity squared in J in kg in m/s In the “Forces” module we looked at how to calculate an object’s kinetic energy: Mass = 1000kgMass = 800kg Speed = 20m/sSpeed = 30m/s Before After

14/06/2016 Energy loss in collisions Consider a head-on collision where the cars stick together. How much kinetic energy is lost in this example? Where does all the energy go? In this example more kinetic energy was lost. We say it was a “less elastic collision”. An “elastic collision” is one where the kinetic energy is conserved. Speed = 50m/sSpeed = 30m/s Speed = 10m/s Before After

14/06/2016 The Structure of the Earth A thin crust km thick A mantle – has the properties of a solid but it can also flow A core – made of molten nickel and iron. Outer part is liquid and inner part is solid The average density of the Earth is much higher than the crust, so the inner core must be very dense

14/06/2016 Tectonic theory People once thought that the oceans and the continents were formed by shrinkage from when the Earth cooled down after being formed. Alfred Wegener proposed something different. Consider Africa and South America: These continents look like they “fit” together. They also have similar rock patterns and fossil records. These two pieces of evidence led me to believe that there was once a single land mass. This is my TECTONIC THEORY.

14/06/2016 The Answer: 1)Scientists discovered 50 years later that the Earth generates massive amounts of heat through radioactive decay in the core. This heat generated convection currents in the mantle causing the crust to move 2)We also now know that the sea floor is spreading outwards from plate boundaries Tectonic theory The Evidence: 1)Some continents look like they used to “fit” together 2)Similar rock patterns and fossil records The Problems: Wegener couldn't explain how continental drift happened so nobody believed him Conclusion – scientists now believe Wegener’s Tectonic Theory

14/06/2016 Tectonic plates

14/06/2016 Movements of the crust When the lithosphere (“crust”) moves three things can happen: 1) Plates move past each other, causing earthquakes 2) Plates move away from each other – a “constructive plate margin”. The gap is filled with magma which cools to form basalt. This is called sea floor spreading. 3) Plates move towards each other – a “destructive plate margin”. The thinner one slides underneath (“subduction”) and partially melts. This causes volcanoes and earthquakes.

14/06/2016 Evidence for sea floor spreading Since the Earth was formed the north and south poles have periodically “________ ____”. When tectonic plates move apart and _____ fills the gap the iron particles in the magma orientate themselves in line with the Earth’s ________ field. This means that the rock formed on the sea floor contains a “magnetic __________” of the changing field: These magnetic patterns can be used to prove that sea floor spreading does happen, and at a rate of about 2cm per _____. Words: impression, magma, swapped over, magnetic, year