1. Model: A representation of a real object or event. Ex: Map Globe Graphs A. Models are useful because they allow an easier way to study objects or

Similar documents
OBJECTIVES. Identify the means by which latitude and longitude were created and the science upon which they are based.

6. The greatest atmospheric pressure occurs in the 1) troposphere 3) mesosphere 2) stratosphere 4) thermosphere

Earth In Space Chapter 3

Topographic Maps Practice Questions and Answers Revised October 2007

Solar System. 1. The diagram below represents a simple geocentric model. Which object is represented by the letter X?

Newton s Law of Gravity

The Earth Really is Flat! The Globe and Coordinate Systems. Long History of Mapping. The Earth is Flat. Long History of Mapping

Geography I Pre Test #1

Celestial Sphere. Celestial Coordinates. Lecture 3: Motions of the Sun and Moon. ecliptic (path of Sun) ecliptic (path of Sun)

Earth-Sun Relationships. The Reasons for the Seasons

Solar Angles and Latitude

The Basics of Navigation

World Map Lesson 4 - The Global Grid System - Grade 6+

Interaction of Energy and Matter Gravity Measurement: Using Doppler Shifts to Measure Mass Concentration TEACHER GUIDE

Pre and post-visit activities - Navigating by the stars

Which month has larger and smaller day time?

Stellarium a valuable resource for teaching astronomy in the classroom and beyond

Basic Coordinates & Seasons Student Guide

Review 1. Multiple Choice Identify the choice that best completes the statement or answers the question.

Motion & The Global Positioning System (GPS)

EDMONDS COMMUNITY COLLEGE ASTRONOMY 100 Winter Quarter 2007 Sample Test # 1

8.5 Comparing Canadian Climates (Lab)

2. Orbits. FER-Zagreb, Satellite communication systems 2011/12

UTM Zones for the US UTM UTM. Uniform strips Scalable coordinates

1. In the diagram below, the direct rays of the Sun are striking the Earth's surface at 23 º N. What is the date shown in the diagram?

1-2. What is the name given to the path of the Sun as seen from Earth? a.) Equinox b.) Celestial equator c.) Solstice d.

Stage 4. Geography. Blackline Masters. By Karen Devine

Seasonal & Daily Temperatures. Seasons & Sun's Distance. Solstice & Equinox. Seasons & Solar Intensity

CELESTIAL CLOCK - THE SUN, THE MOON, AND THE STARS

CELESTIAL MOTIONS. In Charlottesville we see Polaris 38 0 above the Northern horizon. Earth. Starry Vault

The Four Seasons. A Warm Up Exercise. A Warm Up Exercise. A Warm Up Exercise. The Moon s Phases

astronomy A planet was viewed from Earth for several hours. The diagrams below represent the appearance of the planet at four different times.

The Globe Latitudes and Longitudes

Earth Coordinates & Grid Coordinate Systems

Motions of Earth, Moon, and Sun

What causes Tides? If tidal forces were based only on mass, the Sun should have a tidegenerating

FOR TEACHERS ONLY. The University of the State of New York REGENTS HIGH SCHOOL EXAMINATION PHYSICAL SETTING/EARTH SCIENCE

Chapter 3: Weather Map. Weather Maps. The Station Model. Weather Map on 7/7/2005 4/29/2011

Coordinate Systems. Orbits and Rotation

Geometry and Measurement

Gravitational potential

EARTH'S MOTIONS. 2. The Coriolis effect is a result of Earth's A tilted axis B orbital shape C revolution D rotation

SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

Tropical Horticulture: Lecture 2

Geometry and Geography

Navigation: Latitude and Longitude

Answers for the Study Guide: Sun, Earth and Moon Relationship Test

Orientation to the Sky: Apparent Motions

Celestial Observations

Section 4: The Basics of Satellite Orbits

DETERMINING SOLAR ALTITUDE USING THE GNOMON. How does the altitude change during the day or from day to day?

The Size & Shape of the Galaxy

Chapter 3: Weather Map. Station Model and Weather Maps Pressure as a Vertical Coordinate Constant Pressure Maps Cross Sections

Name Class Date. true

12-1 Representations of Three-Dimensional Figures

Produced by Billy Hix and Terry Sue Fanning. As part of the TeachSpace Program. For more ideas and an image of the current phase of the moon, visit:

Douglas Adams The Hitchhikers Guide to the Galaxy

6. Base your answer to the following question on the graph below, which shows the average monthly temperature of two cities A and B.

Shape Dictionary YR to Y6

Geometry Notes PERIMETER AND AREA

The following words and their definitions should be addressed before completion of the reading:

UTM: Universal Transverse Mercator Coordinate System

Shadows, Angles, and the Seasons

Layers of the Earth s Interior

compass Encyclopedic Entry

16 Circles and Cylinders

Map Patterns and Finding the Strike and Dip from a Mapped Outcrop of a Planar Surface

Name Period 4 th Six Weeks Notes 2015 Weather

The Celestial Sphere. Questions for Today. The Celestial Sphere 1/18/10

What Causes Climate? Use Target Reading Skills

Chapter 1 Problems. 1micron m = microns. = cm. 1micron m = microns. 1 ft

Use WITH Investigation 4, Part 2, Step 2

Essential Question. Enduring Understanding

Geography affects climate.

Unit 1 - Radian and Degree Measure Classwork

Lab Activity on the Causes of the Seasons

AS COMPETITION PAPER 2008

Reasons for Seasons. Question: TRUE OR FALSE. Question: TRUE OR FALSE? What causes the seasons? What causes the seasons?

Sun Earth Relationships

Earth in the Solar System

Exercise 5.0 LUNAR MOTION, ELONGATION, AND PHASES

Curriculum Map Earth Science - High School

NASA Explorer Schools Pre-Algebra Unit Lesson 2 Student Workbook. Solar System Math. Comparing Mass, Gravity, Composition, & Density

4 The Rhumb Line and the Great Circle in Navigation

Earth, Sun and Moon is a set of interactives designed to support the teaching of the QCA primary science scheme of work 5e - 'Earth, Sun and Moon'.

Area of Parallelograms, Triangles, and Trapezoids (pages )

An Introduction to Coordinate Systems in South Africa

Measuring the Diameter of the Sun

Scales of the Universe

Today. Solstices & Equinoxes Precession Phases of the Moon Eclipses. Ancient Astronomy. Lunar, Solar FIRST HOMEWORK DUE NEXT TIME

Map Skills. Before Coming to Lab: Read Appendix III (pages ) in Trujillo & Thurman, 11 th ed.

The GED math test gives you a page of math formulas that

How do you find a place on a globe? How do you look up a place based on latitude and longitude?

Physics Kinematics Model

Quick Reference ebook

EARTH SCIENCES - TYPES OF MAPS TEACHER GUIDE

Exploring Solar Energy Variations on Earth: Changes in the Length of Day and Solar Insolation Through the Year

Angular Velocity vs. Linear Velocity

Measuring the Earth Using a GPS M. Scott Wilkerson & M. Beth Wilkerson, DePauw University, May 10, 2007

FIRST GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

Transcription:

1. Model: A representation of a real object or event. Ex: Map Globe Graphs A. Models are useful because they allow an easier way to study objects or events. 2. The shape of the Earth A. The earth is round. B. Evidence: 1) A ship sailing away a) Observation: A ship gradually disappears below the horizon. b) Inference: The earth s surface is curved.

2) Lunar Eclipse The shape of the earth s shadow is seen on the moon s surface as the moon enters and exits the eclipse. View from Outer space SUN

Earth s Shadow Earth s shadow is curved!!!

3) Altitude of Polaris (The North Star) a) Polaris appears at different altitudes at different places at the same time. To Polaris (very, very far away) Reason: The Earth is round!! 90 o North Pole 60 o 20 o

90o 90o 90o

3. How Round Is The Earth?? A. The earth is not perfectly round (but very close). B. The shape of the earth is called an oblate spheroid. a) slightly bulged at the equator. b) slightly flattened at the poles. *********(Not Enough to See However!!!!)********

P.D.= Polar Diameter P.D. E.D.= Equatorial Diameter Earth E.D. > P.D. E.D.

C. Diameter / Circumference Measurements Diameter Circumference Polar Equatorial 12,714 km 12,756 km 40,008 km 40,076 km

4. How Smooth is the Earth??? A. Surface features such as mountains are very minor irregularities on a planetary scale. Ex: This line is too thick to show the true ocean depth. EARTH This point is too big to show the true height of the tallest mountains.

5. The Outer Spheres of the Earth A. Lithosphere 1) The solid outer shell of the earth. (Rocks) B. Hydrosphere 1) All of the water (H 2 O) on the earth s surface. C. Atmosphere 1) The shell of gasses (air) that surrounds the earth.

6. Locating Positions on the Earth A. Coordinate system 1) A system of intersecting lines on a surface used to pinpoint locations. Ex: latitude and longitude 7. Latitude A. The angular distance north or south of the equator. B. Lines of latitude are called parallels. C. Latitude starts at 0 o. D. The most latitude can be is 90 o.

North Pole 60 o N 30 o N North Latitude 0 o 30 o S 60 o S South Latitude Equator South Pole

Therefore, where the dashed line intersects the surface of the earth is the 45 o latitude line. What is this angle? 45 o What is the South Pole s Angle??? 90 o

E. In the northern hemisphere, latitude is found by measuring the altitude of Polaris (North Star). 1) Astrolabe: the instrument that measures the altitude of stars. To Polaris

Ex: Location X Altitude of Polaris = 34 o 34 o Latitude of X = Polaris Location X 34 o Angle is determined by reading where string crosses the protractor.

8. Longitude A. The angular distance east or west of the Prime Meridian (0 o Longitude). B. Longitude lines are called meridians. They all meet at the poles.

North Pole 90 o W 60 o W 30 o W 90 o E 60 o E 30 o E South Pole West Longitude East Longitude

C. The Prime Meridian passes through Greenwhich, England. D. Every 15 degrees of longitude is = 1 hour of time. Reason: Earth rotates (spins) 360 o in 24 hours. A circle has 360 o therefore: E. To Calculate Longitude: 360 o 24 hours = 15 o / hour 1) Find the number of hours between local time (your time) and the time on the Prime Meridian (Greenwich Time). 2) Multiply x 15 o / hour 3) a) If local time is earlier than Greenwhich time, your longitude is west. b) If local time is later than Greenwhich time, your longitude is east. Reason: Earth rotates from west to east.

F. Everyone on the same meridian of longitude has the same solar time. G. Ex: Local time: 4:00 am But what Greenwhich time: 1:00 am direction is it?? Your longitude: 45 o West Time Difference = 3 hours Time difference x 15 o = 45 o Ex: Your longitude: 90 o W Local time: 3:00 pm Greenwhich time: 9 pm But is it later or earlier in Greenwhich?? Time Difference x 15 o = 90 o W Time Difference = 90o 15 o = 6 hours Try this one on your own Ex: Local time: 10:00 am Friday Greenwhich time: 1:00 pm Friday Your longitude: 45 o W

And this one. Ex: Your longitude: 30 o E Local time: 5:00 pm Greenwhich time: 3:00 pm 9. One degree of latitude = 68 miles (110 km) A. Slightly less at the poles and slightly more at the equator due to the earth s imperfect shape. 10. One degree of longitude = at equator = 70 miles at the poles = 0 miles Reason: Longitude lines meet at the poles.

11. To pinpoint more specific locations>>>degrees are subdivided into minutes and seconds. A. One degree = 60 minutes B. One minute = 60 seconds Ex: Latitude of location X: 43 o 17 30 N Ex: What are the coordinates of Ithaca, NY? 42 o 29 N, 76 o 30 W 12. FIELDS A. Any region of space in which a quantity can be measured at any point. Ex: Temperature field magnetic field Gravitational field elevation field

12. Fields can be shown on a map. 1) Lines called isolines are drawn connecting points of equal value. Ex: Isotherms: lines of equal temperature. Isobars: lines of equal pressure Contour lines: lines of equal elevation. C. Field values change with time 1) Some change fast Ex: temperature air pressure. 2) Some change slowly Ex: elevation

D. Drawing Field Maps 1) Several field values (numbers) are plotted on a map. 2) Isolines are drawn connecting points of equal value.

160 170

E. Reading Isolines Maps 1) Distance on maps is shown by using a scale. Ex: 0 5 10 2) Every point on the same isoline has the same field value. 13. Gradient A. A measure of the rate of change across a field. (slope of field). B. General Rule: The closer the isolines, the greater the gradient (or steeper the slope) High or steep gradient Low or gentle gradient

C. Calculating Gradient Change in field value Gradient = Distance (RT front page) Ex: Calculate the gradient between points A and B on the map below: 100 120 140 160 180 200 220 240 meters A B 0 km 50 km 100 km Gradient = Change in field value Distance 80m 50km Distance between A and B = 50 km Change in field value between A and B = 180m-100m = 80m Plug the numbers into the above equation = 1.6 m/km

14. Topographic Maps A. Maps that show the elevation field of an area. B. Topographic maps show the shape of the land by using contour lines which are lines of equal elevation (isolines). C. Contour Interval: The number of feet between lines (contours) To figure out the contour interval, count the lines that are between the numbered lines. 5 lines = 100 feet therefore: 1 2 3 4 5 500 5 goes into 100, 20 times so the contour interval = 20 feet 400

D. Hills: Shown on a map by circular lines. E. Depressions (holes): Shown on a map with circular lines with hachures.

F. When contour lines cross a river, they bend upstream. Therefore, the river flows opposite of the way the contour lines bend.

15. On a topographic map, latitude and longitude are in the corners of the map. 43 o 15 43 o 15 72 o 30 72 o 15 N 43 o 00 43 o 00 72 o 30 72 o 15 Latitude covered: 43 o 15 43 o 00 = 15 minutes Longitude covered: 73 o 30 73 o 15 = 15 minutes Direction is indicated by which way the numbers increase. N S E W

?? What is the contour interval of this map????

16. Map Profile: The side view of a section of a topographic map. Procedure: 200 100 1) Draw a line x-y 2) Figure out contour interval 20 feet 3) Lay a strip of paper on the line and mark elevation on it. 4) Mark any features (swamp, streams hilltops etc..) on paper 5) Decide the max and min numbers needed for profile 6) Place strip of paper on bottom of graph. 7) Mark off the correct elevations and connect the dots. 240 220 200 180 160 140 120 100 80 60 x x x

17. USGS Topographic Maps A. Areas covered are called quadrangles (Quads). B. These come in 3 sizes according to Latitude and Longitude. 1) 7.5 minute 2) 15 minute 3) 30 minute C. Numerical Scale: Tells how many map units are covered by each ground unit. Ex: 1:24,000 (7.5 quad) This means that for every one map unit there are actually 24,000 ground units.

1:62,500 (15 quad) Ex: 1cm on map = 62,500 cm in real life. OR 1 inch on map = 62,500 inches in real life. 1:250,000 (30 quad)

18. Scientific Notation: A. Using powers of 10 to express very large or very small numbers. Ex: 1) 3.8 x 10 4 = 38,000 2) 28.9 x 10 8 = 2,890,000,000 3) 67 x 10-6 =.000067 4) 5,300,000 = 5.3 x 10 6 5) 400,000 = 4.0 x 10 5 6).00065 = 6.5 x 10-4