The earth’s crust 3 layers: Crust, mantle and core. The mantle is mostly solid, but can move slowly The crust is cracked into tectonic plates How do tectonic.

Slides:



Advertisements
Similar presentations
AQA Chemistry Unit 1 This PowerPoint supports section C1.4, C1.5, C1.6 and C1.7 sections of the AQA Chemistry Unit 1 module.
Advertisements

VEGETABLE OILS A guide for GCSE students 2010 SPECIFICATIONS KNOCKHARDY PUBLISHING.
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.
STRUCTURE OF THE EARTH Noadswood Science, 2011.
FCAT Review Week 1 Earth Science
Earth’s Atmosphere Noadswood Science, Earth’s Atmosphere To know how the Earth’s atmosphere has changed over time Tuesday, May 05, 2015.
1 Elements and their atoms Each element of the Periodic table is built from one type of atom Atoms have a nucleus containing protons and neutrons, surrounded.
E.
The Structure of the Earth
Changes in the Earth Continental drift and processes at plate boundaries.
Noadswood Science,  To know how plant oils are useful in cooking Friday, August 07, 2015.
Crude Oil Noadswood Science, 2011.
Quiz 1.When we extract oil what must we do to the seeds first? 2.Once the oil is dissolved in a solvent what process happens next? 3.With lavender oil.
Section 5. Early Earth pg. 330 November 12th, 2014.
Changes to the earth and atmosphere. The Earths Structure All resources come from the Earth, its atmosphere and the oceans. The Earth is a sphere. It.
Finishing off from last time
Definitions Atom – Element – Compound – Mixture – Particles that make up all substances. A substance made up of only one kind of atom. A substance made.
End Show Slide 1 of 36 Copyright Pearson Prentice Hall 17-2 Earth's Early History.
Chapter 8 Lesson 1 What are Earth’s layers made of?
Prior learning –There are 3 kinds of rock – sedimentary, metamorphic and Igneous –Igneous rocks form crystals depending on the length of time it takes.
AQA GCSE Science & Additional Science Chemistry 1 Topic 6 Hodder Education Revision Lessons Plant oils and their uses Click to continue.
AQA GCSE Science & Additional Science Chemistry 1 Topic 7 Hodder Education Revision Lessons Changes in the Earth and its atmosphere Click to continue.
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.
GCSE Core Keywords: Suggest, Use information, Explain, Conclude, Calculate, Describe, Evaluate.
Oils from plants C1.6. What do I need to know? Recall that oils can be obtained from plants Describe the properties of oils and formation of emulsions.
Earth’s Layers TheoriesBoundariesEarthquakesVolcanoesOther
Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Bellringer The Earth is approximately 4.6 billion years old. The.
HOW DID WE GET HERE?? EARTH AND THE ORIGIN OF LIFE.
Extracting Vegetable Oils L.O: To understand where different oils come from and which are saturated and unsaturated Starter: Make a list of as many different.
C1b Oils, Earth and Atmosphere
GCSE Core Keywords: Suggest, Use information, Explain, Conclude, Calculate, Describe, Evaluate.
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.
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.
SOIL FORMATION. Weathering and Erosion Soil Layers  Soil is composed of 4 layers typically:  O horizon Top layer of organic matter  A horizon Weathered.
Study Hall Sitting in assigned seats. Not wondering around the room Sharpened pencil out, ready to begin 9 days until our 1 st EOG Test!
Polymerisation Alkenes can be used to make polymers such as poly(ethene) and poly(propene). In these reactions many small molecules (monomers) join together.
29/02/2016 Oils, Earth and Atmosphere The New Bridge Academy (AQA)
Alkali metals Group 1 Lithium reactive Alkane Hydrocarbon Methane Single bond Alkene Hydrocarbon Methene Double bond Alloy Mixture Metal steel Aluminium.
Advantages of using vegetable oils: Explain how plant oils are made: What are emulsions? What can plant oils be made from? Outline uses, benefits, drawbacks.
Plate Tectonics. Exploring Inside the Earth Geologists have used evidence from rock samples and evidence from seismic waves to learn about Earth’s interior.
C1 Choice and Challenge activities 1.The atom and the periodic table 2.Limestone and building materials 3.Extracting metals 4.Products from oil 5.Useful.
Air Chapter 31 Page 186.
The Early Atmosphere. Where did our atmosphere come from? Earth was formed around 4600 million years ago. We don’t know exactly, but the atmosphere was.
C1 Earth Chemistry. Limestone Limestone is a rock made mainly of calcium carbonate (CaCO 3 ) It was formed from the remains of animals millions of years.
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),
Plant Oils Where do the following come from?
Task Think of some different types of ‘oil’ used for cooking. What is meant by ‘poly-unsaturated’?
Chemistry 2 Acids and alkalis Learning outcomes
1) What is the approximate percentage of oxygen in Earth’s modern day atmosphere? . Answer 21 %
Unit 8 C: Plate Tectonics
Chemistry 1 summary sheet
The Evolution of the Atmosphere
21/09/2018 Plate Tectonics The idea of continental drift is now referred to as plate tectonics. How can the continents move?
The earth takes shape.
Elements, compounds and mixtures
Composition and evolution of the atmosphere
Outer Core Liquid layer of Earth’s core Surrounds inner core.
A guide for GCSE students KNOCKHARDY PUBLISHING
Chemistry of the atmosphere
Chapter 20 Section 3 The Earth Takes Shape Bellringer
Blessed William Howard Catholic High School
Energy in Chemistry W Richards The Weald School OCR Module 5
QUICK REVIEW… Layers of the Earth
The changing World Earth structure
Presentation transcript:

The earth’s crust 3 layers: Crust, mantle and core. The mantle is mostly solid, but can move slowly The crust is cracked into tectonic plates How do tectonic plates move? 1. Radioactive processes occur in the core which release heat. 2. The heat travels through the mantle by convention currents. These convection currents cause the plates to move a few cm per year If the movements are sudden, earthquakes and/or volcanoes can occur at the plate boundary When plates crash into each other, it causes mountain ranges Wegeners theory of crustal movement/ continental drift The continents were once joined by gradually moved apart. He thought this as there were similar fossils on continents that were very far apart (s america and africa) The shapes of the continents fitted He thought that the mountain ranges on the earth’s surface were caused by continents colliding. Scientists did not believe him as he could not explain how they moved What did they believe? They believed that mountain ranges were caused by the earth’s crust cooling and shrinking after it was first formed They also thought there was a land bridge (which had now sunk) between s America and Africa, which explains the fossils. Formation of the atmosphere The atmosphere is a layer of gases surrounding the earth. It is held in place by gravity During the first billions years of the earth’s existence there was intense volcanic activity. This released the gases which made up the atmosphere. One theory about the atmosphere is that… It was mostly carbon dioxide and water vapour. There was also small amounts of ammonia or methane There was little or no oxygen Earth’s Atmosphere

Today’s atmosphere The atmosphere has been the way it is today for 200 million years It is made up of mostly nitrogen (78%). It also contains 21% oxygen It contains 0.04% carbon dioxide The remainder is made up of water vapour, methane and noble gases Uses of noble gases- Helium (balloons) Neon (advertising signs) Argon (light bulbs) The differences between the early and today’s atmosphere Water vapour: There is much less water vapour now It condensed to form the oceans Carbon dioxide: There is much less carbon dioxide now. It was taken in by plants The plants died and formed layers These eventually formed sedimentary rocks (fossil fuels) It also dissolved in the oceans to form carbonate rocks. Oxygen: Produced by plants (photosynthesis) How did life begin? The Miller Urey experiment Amino acids are needed to make a living organism Amino acids are made up of carbon, hydrogen, nitrogen and oxygen Miller and Urey did an experiment to see if they could make amino acids under conditions like the early atmosphere They used water, ammonia methane and hydrogen. These did not react under normal conditions They did react when Miller and Urey used a high voltage to produce a spark. This simulated lightening This provided energy for the reaction 11 amino acids were formed This provides some evidence that lightening may have provided the energy to create life. Primordial soup theory Organic molecules (found in the sea) form a ‘primordial soup’ These then reacted together to form the first primitive cells Fractional distillation of air Fractional distillation is used to separate liquids with different boiling points. 1.Air is cooled until it condenses to a liquid (-200 C) 2.Carbon dioxide and water are removed from the mixture as they are solid at this temperature. 3.Liquid is warmed. 4.Nitrogen is collected at the top and oxygen at the bottom Uses of Nitrogen and Oxygen Nitrogen: Very unreactive so stops food going off Used to make ammonia Oxygen: Helps people breathe (accident scene or in hospital)

Vegetable Oils These are important foods as they provide us with a lot of energy and nutrients This is found in fruits, nuts and seeds To extract the oil, you need to crush the plant material and press the oil out Water and other impurities are then removed Cooking with vegetable oils Vegetable oils have a higher b.p that water This means they can be used to cook foods at higher temperatures (where the water would just evaporate) This means food can be cooked faster, and can also be flavoured differently However, oils release more energy when eaten, which turns to fat if not burned. Emulsions Some substances do not mix. They are said to be immiscible (eg oil and water). We can use an emulsifier to force them to mix. The remaining mixture is called an emulsion. Emulsions are more viscous than oil and water Emulsions provide better texture, coating ability and appearance Unsaturated oils contain C=C double bonds which can be tested for using bromine water (goes colourless as with alkenes) We can harden unsaturated oils to increase the melting temperature. This makes them solid as room temperature, which makes them useful as spreads. Hardening vegetable oils React with hydrogen at 60 ̊ C Use a Nickel catalyst to speed up the process The saturated oil is called a hydrogenated oil Plant oils