C1.7 EARTH AND ITS ATMOSPHERE MarkScheme

Similar documents
C1.7 EARTH AND ITS ATMOSPHERE

Q1. Scientists study the atmosphere on planets and moons in the Solar System to understand how the Earth s atmosphere has changed.

The bar chart shows the composition of a sample of dry air from the Earth s atmosphere. Name the three gases shown in the bar chart.

Carbon Cycling Internal

EARTH TAKES SHAPE 1. Define all vocabulary words. Crust: The thin and solid outermost layer of the Earth above the mantle. Mantle: The layer of rock

Astro 1010 Planetary Astronomy Sample Questions for Exam 4

2 Complete the following sentences to describe the properties of the different layers of the Earth s structure. Use the words given below.

Plate Tectonics. Chapter 8

Plate Tectonics Practice Test

Earth s Early History. Lesson Overview. Lesson Overview Earth s Early History

Unit 2 Lesson 1 Geologic Change over Time. Copyright Houghton Mifflin Harcourt Publishing Company

Climate Regulation. - What stabilizes the climate - Greenhouse effect

Terrestrial Planets: The Earth as a Planet

Chapter 7 Earth and the Terrestrial Worlds

Earth as Planet. Earth s s Magnetic Field. The Earth s s Crust. Earth s s Interior

klm Mark Scheme Science B 4462 / Chemistry 4421 General Certificate of Secondary Education CHY1H Unit Chemistry Examination June Series

Table of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement

Lesson 3.1 Matter and the Environment. Water s abundance is a primary reason there is life on Earth.

Section 1: How Did Life Begin? Chapter 19: History of Life on Earth. Section 2: The Age of Earth

Plate Tectonics. Continental Drift Sea Floor Spreading Plate Boundaries

Unit 4 Lesson 6 Plate Tectonics

Year 9 Geography end of Year Examination

Plate Tectonics. These icons indicate that teacher s notes or useful web addresses are available in the Notes Page.

Ch 9.1 Notes. Objective: Be able to explain the theory of plate tectonics and be able to explain evidence that supports it.

The Cycling of Matter. Day 1

Activity 1-2: Origin of the Earth

Carbon Cycle Activity

Section 1: Earth s Interior and Plate Tectonics Section 2: Earthquakes and Volcanoes Section 3: Minerals and Rocks Section 4: Weathering and Erosion

Lecture 20. Origin of the atmosphere (Chap. 10) The carbon cycle and long-term climate (Chap. 8 of the textbook: p )

Lithosphere: (Rocky Sphere) Solid, rocky, outer layer of the Earth. Includes the crust and part of the upper mantle. Lithosphere

Astronomy. physics.wm.edu/~hancock/171/ A. Dayle Hancock. Small 239. Office hours: MTWR 10-11am

10/11/2010. Acceleration due to gravity, a. Bulk Properties Mass = 6 x kg Diameter = 12,756 km Density = 5515 kg/m 3 (mix of rock and iron)

Earth s Atmosphere. Atmospheric Composition 78% Nitrogen 21% Oxygen 1 % Argon, 0.03% Carbon dioxide, Water. Recall the Electro-Magnetic (EM) Spectrum

Formation of the Earth and Solar System

Discusssion / Activity 1 Suggested Answers. INSPECTION COPY for schools only

The Essential Cosmic Perspective Chapter 7.5: Earth as Living Planet. Dr. Regina Jorgenson

Directed Reading. Section: The Theory of Plate Tectonics. to the development of plate tectonics, developed? HOW CONTINENTS MOVE

Core Idea ESS2 Vocab. Earth s Systems. How and why is Earth constantly changing?

Planet Earth. Our Home APOD

Grades 9-12: Earth Sciences

Continental Drift. & Plate Tectonics

Outline 9: Origin of the Earth: solids, liquids, and gases. The Early Archean Earth

9.1- Earth Forms and Life Begins

Outline 9: Origin of the Earth: solids, liquids, and gases

Nebular Hypothesis (Kant, Laplace 1796) - Earth and the other bodies of our solar system (Sun, moons, etc.) formed from a vast cloud of dust and

Plate Tectonic Vocabulary Chapter 10 Pages

ESS2.A: EARTH MATERIALS AND SYSTEMS

Yanbu University College. General Studies Department. PHSC001 Course. Chapter9 (Basic Geology: Earthquakes and volcanoes ) Worksheet Solutions

EARTH S HISTORY. Geological Evolution

Earth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes.

25-Nov-14. The Structure of Earth s Interior. What unique features of Earth are important for life as we know it?

Follows the scientific method (O,Q,H,E,C,R)

The History of the Earth

Geosphere Final Exam Study Guide

22.4 Plate Tectonics. Africa

Earth s Interior HW Packet HW #1 Plate Tectonics (pages )

HOW GEOGRAPHY AND GEOLOGY AFFECT BIOLOGICAL DIVERSITY

TEST NAME:Geology part 1 TEST ID: GRADE:06 - Sixth Grade SUBJECT:Life and Physical Sciences TEST CATEGORY: My Classroom

sonar seismic wave basalt granite

PTYS 214 Spring Announcements. Next midterm 3/1!

MCAS QUESTIONS: THE EARTH S INTERIOR, CONTINENTAL DRIFT, PLATE TECTONICS

Salt Water. Copyright 2012 LessonSnips

Outline. Origin and History of Life

ASTR-101 Section 004 Lecture 9 Rare Earth? John T. McGraw, Professor

Shape and Size of the Earth

TOPIC 1: RELATIVE DATING ESSENTIAL QUESTION: HOW DO WE DETERMINE A ROCK S AGE BY THE SURROUNDING ROCKS?

1. The process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle is known as

H Li. Mass Number. Number of Electrons Hydrogen He Draw diagrams to show the electronic structure of the elements above.

The structure of the Earth

S Illustrate and explain how carbon, nitrogen, and oxygen are cycled through an ecosystem.

Chapter 2: Physical Geography

The Terrestrial Planets

1 Earth s Oceans. TAKE A LOOK 2. Identify What are the five main oceans?

The Earth in the Universe

b. atomic mass H What is the density of an object with a volume of 15cm 3 and a mass of 45g?

The Earth Fast Facts. Outline. The Solar System is Ours! Astronomy 210. Section 1 MWF Astronomy Building

THE INTERNAL STRUCTURE OF THE EARTH

Structure of the Earth EARTH ( ) - need a solid, will not go through a liquid

Rocks and the Rock Cycle. Banded Iron Formation

1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation)

Social Studies. Chapter 2 Canada s Physical Landscape

Slow and Steady By ReadWorks

ammonia carbon dioxide hydrogen nitrogen electrical heat solar sound (a) In air, the two most common gases are oxygen and...

Theory of Continental Drift

Today. Events. Terrestrial Planet Geology - Earth. Terrestrial Planet Atmospheres. Homework DUE next time

I am getting absorbed by a leaf during photosynthesis to make sugar. Go to the Trees.

Phys 214. Planets and Life

The Earth s Structure

MAR110 Lecture #4 Fundamentals of Plate Tectonics

The Earth - Surface and Interior

water erosion lithosphere Describe the process of erosion and deposition. chemical weathering Dissolving limestone is an example of.

Earth. Properties of Earth. Earth's Interior. Earth is the planet that we know best

The performance expectation above was developed using the following elements from the NRC document A Framework for K-12 Science Education:

PLATE TECTONICS Chapter 4 Notes

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

abrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG)

Section 2: The Atmosphere

Chapter 20 Earth: The Standard of Comparative Planetology

2) Earthquakes and volcanoes are most alike because a) Both can occur at the midlines of tectonic plates b) Both can occur as a result of transform

Climate & Earth System Science. Introduction to Meteorology & Climate CHAPTER 1 LECTURE 1. Question: Introduction to the Atmosphere

Transcription:

C.7 EARTH AND ITS ATMOSPHERE MarkScheme M. (a) (i) it = water vapour condensed accept temperature went below 00 C / boiling point of water allow cooled to fm liquid / water / rain do not accept evapated fmed the oceans / seas igne rain accept (water vapour) cooled and fmed the ocean / sea f marks igne oxygen / nitrogen increased igne reference to volcanoes / respiration used by (green) plants / algae accept photosynthesis / plants give out oxygen changed into oxygen dissolved in oceans / seas accept (locked up) in shells / skeletons (of animals) (locked up) in carbonates / sedimentary rocks (locked up) in fossil fuels / named fossil fuel (b) (i) cannot get to / reach / drill to / see the ce accept the ce is (too) far down (into the Earth) / do not know what happens under the crust / Earth s surface accept it is (too) hot / radioactive igne lack of evidence unqualified any three from: heat / energy released from radioactive decay / processes accept radioactivity / nuclear reactions (causing) convection currents in the mantle 3 [8] Page

M.(a) (i) H O must be fmula CaO must be fmula carbon dioxide from the air / (Earth s early) atmosphere accept carbon dioxide from millions of years ago fmed (sedimentary) rocks fossil fuels igne trapped / sted (b) (i) decreases rapidly at first then slowly levels off allow both marks if the description is crect using either rapidly slowly allow crect use of figures f either marking point if no other mark awarded, allow CO decreased f mark accept photosynthesis used by plants dissolved in oceans locked up in fossil fuels fmed fossil fuels locked up in rocks fmed rocks (c) (yes) it = percentage of carbon (dioxide) igne yes no because the percentage of carbon dioxide is increasing which causes global warming (to increase) allow (carbon dioxide) causes greenhouse effect/climate change (no) Page

because the percentage of carbon dioxide is low () compared to millions of years ago () allow global warming can be caused by other facts (e.g. Sun / water vapour / methane) [0] M3.(a) (i) (Iceland is) on a boundary between (tectonic) plates allow where tectonic plates move apart / meet / collide any one from: igne trems (small earthquakes) are random / have no pattern igne difficult to predict / no evidence / no proof not all trems (small earthquakes) indicate that the volcano will erupt allow these trems (small earthquakes) may be false alarms scientists cannot monit what is happening below the Earth s crust in the Earth s mantle (b) water vapour / steam released by volcanic activity condensed to fm the oceans allow a description of condensing do not accept other gases condensing (c) earthquakes are caused by the sudden movement of the Earth's (tectonic) plates igne collision (of tectonic plates) caused by convection currents in the Earth's mantle caused (by the heat released) by radioactive processes (within the Earth) [7] Page 3

M4.(a) (i) Wegener / they could not explain how continents could move allow not enough no evidence no proof (of movement) igne status / technology because the (Earth s) crust (is divided into tectonic) plates the heat (released) from radioactive processes causes convection currents in the mantle (that move the tectonic plates) (b) (i) fms a solid freezes accept would block pipes (iii) neon argon because the boiling points are almost the same only 3 degrees different do not allow reference to melting points [0] M5. (a) carbon dioxide dissolves in water/oceans marine ganisms use (dissolved) carbon dioxide to fm their shells/skeletons limestone was fmed from the shells/skeleton of marine ganisms accept carbon dioxide became locked up in sedimentary rocks/carbonates/limestone precipitation fmation of insoluble carbonates plants / algae photosynthesise/ absb/use carbon dioxide accept remains of plants/algae/ marine ganisms contain locked up carbon dioxide/carbon in the fm of fossil fuels do not accept plants use carbon dioxide f respiration (b) (i) because these gases/molecules contain the elements / atoms in amino acids the gases / they contain carbon, hydrogen and nitrogen igne oxygen Page 4

igne small-scale / timescale igne references to water/oceans other theies nobody knows what was in the Earth s early atmosphere accept these gases / hydrogen / methane / ammonia may not have been in the Earth s early atmosphere accept carbon dioxide / nitrogen may have been in the Earth s early atmosphere accept reference to Venus present atmosphere igne concentration of gases there may not have been (continuous) lightning Miller and Urey selected only the gases needed to produce amino acids [5] Page 5