What are some ways to represent Earth s

Size: px
Start display at page:

Download "What are some ways to represent Earth s"

Transcription

1 Topographic Maps 8.9C Interpret topographical maps and satellite views to identify land and erosional features and predict how these shapes may be reshaped by weathering

2 What are some ways to represent Earth s surface? Maps are models that represent Earth s surface. They are helpful because they can show large areas of the three dimensional surface on small, flat surfaces. Different types of maps show different types of information. Latitude and longitude are used to find places on Earth All flat maps distort Earth s surface

3 Globe: A round map! Here is the same information flat! Not very readable is it? Because the Earth is round and maps are flat, it is impossible to create a map with a perfect scale. Some parts of the map will be too large, while others will be too small. The larger a territory represented by a map, the greater that the distortions in scale will be.

4 Aerial and Satellite Images Aerial means taken from airplanes and satellite means from satellites that orbit Earth Some look like photographs and some are a collection of data that may not be visible (such as infrared that looks at temperatures on earth)

5 More on Satellite Views Satellite views can be used to learn about erosion and how the land has changed images taken over time can be used for comparison and interpretation of erosional features (ex. after a flood)

6 Geological Maps Geologic maps shows rock types and ages They also show geological features and fault lines Colors and letters give information about the rocks, while lines show elevation

7 Key Features on Maps: Map title Compass rose/orientation Map key or legend Map scale Location markers (latitude and longitude)

8 What s the difference?

9 What are the uses of topography in the real world? Topography has a number of uses including: Agriculture - Topography is often used in agriculture to determine how soil can be conserved and how water will flow over the land. Environment - Data from topography can help to conserve the environment. By understanding the contour of the land, scientists can determine how water and wind may cause erosion. They can help to establish conservation areas such as watersheds and wind blocks. Weather - The topography of the land can have an impact on weather patterns. Meteorologists use information on mountains, valleys, oceans, and lakes to help predict the weather. Military - Topography is also important to the military. Armies throughout history have used information on elevation, hills, water, and other landforms when planning their military strategy.

10 Texas Historically, mapmakers used a variety of methods to indicate elevation. To get a quick sense of elevation, we can use color, as in this map.

11 Contours and Profiles You can generate a profile of a landform from the contour lines on a topographic map. But you probably don t have access to this technology so what do you do on a trip? Simple contour map

12 Imagine you are on vacation with your family in a national park. You have a simple trail map that shows you where to hike. But the map does not tell you anything about what the land looks like. Will you have to cross any rivers or valleys? How far uphill or downhill will you have to hike?

13 So on your vacation you need - Topographic Maps! Topography is the shape, or features, of the land. These features can be natural such as mountains, plateaus, and plains or human-made such as dams and roads. To show the topography of an area, mapmakers draw a topographic map.

14 On vacation you would need a topographic map! People use topographic maps to locate interesting landforms, to find their way through an area, and to determine the direction water flows in an area. The wiggly lines are called contour lines. They show elevation, slope and relief

15 Elevation, slope and relief: Elevation how high above sea level a place is Slope how steep it is. The more gradual a slope, the further apart the contour lines are, the steeper, the closer the lines Relief the difference between its high and low points. For example, subtracting the lowest elevation on a map from the highest, gives you the measure of the area s relief

16 Elevation, slope and relief on a map:

17 A closer look at Contour Lines Equal elevation Follow any given line from one side to the other. This continuous line indicates equal elevation.

18 Rules of Contour Lines Never cross each other Connect with themselves The contour interval is the same on a map Get closer together as land gets steeper Get further apart as land gets flatter Circles show highest and lowest points (tops of mountains and bottom of depressions)

19 Contour Interval The change in elevation from contour line to contour line is called the contour interval The distance that separates contour intervals

20

21 How do they make topo maps? There are a number of ways that information is gathered to make topographical maps. They can be divided into two primary methods: direct survey and indirect survey. Direct survey - A direct survey is when a person on the ground uses surveying equipment, such as levels and clinometers, to directly measure the location and elevation of the land. Indirect survey - Remote areas may be mapped using indirect methods. These methods include satellite pictures, images taken from planes, radar, and sonar (underwater).

22 Learning to read topo maps Learning to use a topographic map is a difficult skill, because it requires you to visualize a three-dimensional surface from a flat piece of paper. Land Features and other objects are also indicated on a topo map More examples and links are posted on my website: Unit 4

23 Land Features you may see on a Topo Map:

24 Land Feature - Hill A small area of high ground. When you are on a hill, the ground slopes down in all directions.

25 Land Features - Depression Depression-a low point or hole in the ground, surrounded on all sides by higher ground.

26 Land Feature - Saddle Saddle-a dip or low point along the crest of a ridge. A saddle is not necessarily the lower ground between two hilltops; it may be a break along an otherwise level ridge crest.

27 Land Feature - Cliff Cliff-a vertical or near-vertical slope. A cliff may be shown on a map by contour lines being close together, touching, or by a ticked "carrying" contour line. The ticks always point toward lower ground.

28 Grand Canyon Isis Temple Can you find the cliffs?

29 Land Feature - Valley Valley-reasonably level ground bordered on the sides by higher ground. A valley may or may not contain a stream course. A valley generally has maneuver room within its confines. Contour lines indicating a valley are U- shaped.

30 Land feature - Ridge Ridge-a line of high ground with height variations along its crest. The ridge is not simply a line of hills; all points of the ridge crest are higher than the ground on both sides of the ridge.

31 Tracking Flowing Water How does water always flow? DOWNHILL How can we tell what direction (ex. N,S,NW,ESE) is downhill? PSC 121 Prince George's Community

32 Tracking Flowing Water (streams) You can look for elevation changes since water will flow from higher to lower elevations. Water will always flow down hill so the elevation of the contour lines will decrease in the direction water is flowing ft 2100 ft Here the stream flows toward the northwest.

33 Second way to read a stream: Downstream Upstream The second way to tell is to look at the pattern of the contour lines. Because streams will sit in a valley, the land on either side of them will be higher. As a result the contour lines form a "V" pattern like the one in the red on the map The point of the "V" points up stream. The open end of the "V" faces downstream. It is the presence of this "V" pattern that was used to recognize stream valleys PSC 121 PRINCE GEORGE'S COMMUNITY COLLEGE

34 Where erosion may occur A stream would run down the middle or side of the V s this is the most likely place where erosion would occur. Over time, this could change the landscape, erosion causes steep grades to soften. This is shown by the spaces in between contour lines getting wider.

35 Reminder of key terms! Weathering is the breaking down of rocks, soil and minerals Erosion a process (such as water flow or wind) which removes soil and rock from one location on the Earth's crust, then moves it Deposition the location where freshly eroded material gets placed

36 How can flowing water shape land? By weathering and eroding material Land gets weathered and eroded by flowing water. These, over time, form features such as valleys, cliff and canyons. Streams carry small pieces of sediment, while larger rivers carry larger particles and major storms can carry even larger pieces, like boulders. Groundwater below the Earth s surface form caves and this dissolved material is then eroded and the groundwater flows to new locations. Deposition by flowing water makes alluvial fans and deltas which help make flatter landscapes. Heavy rainfall and floods can cause rivers to rise and bring sediment to higher places Glaciers are also factor and can carve away entire mountains, or they may form lakes when they recede or melt.

37 Let s see what you have learned. E C D A B 1200m 1000m F 600m 800m

38 1. Could the elevation at the peak (B) be 1410 meters? No :The elevation must be under 1400 meters, but over 1300 meters. E C D A B 1200m 1000m F 600m 800m

39 2. What is the elevation at (E)? About 400 meters E C D A B 1200m 1000m F 600m 800m

40 3. If you walked a straight line from (D) to (C) would you walk over a ridge or down a valley? Down a valley: If the contour lines point up the slope it s a valley, if they point down the slope it s a ridge. E C D A B 1200m 1000m F 600m 800m

41 S 4. Just looking at the map, would it be easier to head down from the peak going East, or going North? East: When contour lines are close together that means there is a steep slope, the further apart the lines, the more gentle the slope and therefore an easier walk! Go N east! E C W D A B 1200m 1000m F E 600m 800m

42 Contour Practice 1.What is the contour interval of the map at left? How do you figure this out? 80 m 1.What is the elevation of point A? 320 m 2.What is the elevation of point B? 880 m 3.What is the elevation change between A and B? 560 m

43 Map Reading Activity: Topography Practice

44 Map your hand!

45 Supplies: 1. Your hand 2. Marker

46 Close to Home Local maps &s=50&name=Enchanted%20Rock Topo Map -

WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST. Which graph best shows the relative stream velocities across the stream from A to B?

WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST. Which graph best shows the relative stream velocities across the stream from A to B? NAME DATE WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST 1. The diagram below shows a meandering stream. Measurements of stream velocity were taken along straight line AB. Which graph best shows the

More information

Earth Science Landforms, Weathering, and Erosion Reading Comprehension. Landforms, Weathering, and Erosion

Earth Science Landforms, Weathering, and Erosion Reading Comprehension. Landforms, Weathering, and Erosion Reading Comprehension Name 1 How many people have been to the Rocky Mountains or the Grand Canyon? When people go to visit these natural wonders, they may not realize that it took millions of years for

More information

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

Map Patterns and Finding the Strike and Dip from a Mapped Outcrop of a Planar Surface Map Patterns and Finding the Strike and Dip from a Mapped Outcrop of a Planar Surface Topographic maps represent the complex curves of earth s surface with contour lines that represent the intersection

More information

Watershed Delineation

Watershed Delineation ooooo Appendix D: Watershed Delineation Department of Environmental Protection Stream Survey Manual 113 Appendix D: Watershed Delineation Imagine a watershed as an enormous bowl. As water falls onto the

More information

Topographic Survey. Topographic Survey. Topographic Survey. Topographic Survey. CIVL 1101 Surveying - Introduction to Topographic Modeling 1/8

Topographic Survey. Topographic Survey. Topographic Survey. Topographic Survey. CIVL 1101 Surveying - Introduction to Topographic Modeling 1/8 IVL 1 Surveying - Introduction to Topographic Modeling 1/8 Introduction Topography - defined as the shape or configuration or relief or three dimensional quality of a surface Topography maps are very useful

More information

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

OBJECTIVES. Identify the means by which latitude and longitude were created and the science upon which they are based. Name: Key OBJECTIVES Correctly define: isolines, gradient, topographic map, contour interval, hachured lines, profile, latitude, longitude, hydrosphere, lithosphere, atmosphere, elevation, model EARTH

More information

BASIC LESSON Objective(s)

BASIC LESSON Objective(s) [Geology - Landforms] [K-1: Basic] [Grades 2-3: Advanced] BACKGROUND Landforms are natural features of the Earth's surface. They are created by the movement of ice or water, earthquakes, lava flows, volcanoes,

More information

Igneous rocks formed when hot molten material (magma) cools and hardens (crystallizes).

Igneous rocks formed when hot molten material (magma) cools and hardens (crystallizes). Objectives You will learn about how the land of North Dakota was formed. Introduction North Dakota is a wonderful place to live. Have you ever though about how it was formed? To answer that question, you

More information

5-Minute Refresher: WEATHERING AND EROSION

5-Minute Refresher: WEATHERING AND EROSION 5-Minute Refresher: WEATHERING AND EROSION Weathering and Erosion Key Ideas Weathering is the wearing away of the surface of rock, soil, and minerals into smaller pieces. Example of weathering: Wind and

More information

WEATHERING, EROSION, and DEPOSITION REVIEW

WEATHERING, EROSION, and DEPOSITION REVIEW WEATHERING, EROSION, and DEPOSITION REVIEW Weathering: The breaking up of rock from large particles to smaller particles. a) This Increases surface area of the rock which speeds the rate of chemical weathering.

More information

Chapter Overview. Bathymetry. Measuring Bathymetry. Echo Sounding Record. Measuring Bathymetry. CHAPTER 3 Marine Provinces

Chapter Overview. Bathymetry. Measuring Bathymetry. Echo Sounding Record. Measuring Bathymetry. CHAPTER 3 Marine Provinces Chapter Overview CHAPTER 3 Marine Provinces The study of bathymetry charts ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools. Most ocean floor features

More information

EARTH SCIENCES - TYPES OF MAPS TEACHER GUIDE

EARTH SCIENCES - TYPES OF MAPS TEACHER GUIDE EARTH SCIENCES - TYPES OF MAPS TEACHER GUIDE MATERIALS: Electronic Reader - Maps 5 different types of maps (see lab) inflatable globes local topographical map Objective: To understand the uses and importance

More information

(K-5) A scientist keeps a notebook to record his/her process (experiences, observations, and thinking).

(K-5) A scientist keeps a notebook to record his/her process (experiences, observations, and thinking). FIFTH GRADE Science Curriculum Framework 1 Investigations will be integrated with social studies and mathematics where appropriate. 2 Investigations will be integrated with language arts non-fiction reading,

More information

Basic Elements of Reading Plans

Basic Elements of Reading Plans Center for Land Use Education and Research at the University of Connecticut Basic Elements of Reading Plans University of Connecticut. The University of Connecticut supports all state and federal laws

More information

The Basics of Navigation

The Basics of Navigation The Basics of Navigation Knowledge of map reading and the use of the compass is an indispensable skill of bushcraft. Without this skill, a walker is a passenger and mere follower on a trip. To become a

More information

Rapid Changes in Earth s Surface

Rapid Changes in Earth s Surface TEKS investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes, and landslides Rapid Changes in Earth s Surface Constant Changes Earth s surface is constantly changing. Wind,

More information

Advice For the multiple-choice questions, completely fill in the circle alongside the appropriate answer(s).

Advice For the multiple-choice questions, completely fill in the circle alongside the appropriate answer(s). SPECIMEN ASSESSMENT MATERIAL GCSE GEOGRAPHY Paper 1 Living with the physical environment Specimen Materials For this paper you must have: a pencil a ruler. Time allowed: 1 hour 30 minutes Instructions

More information

Benchmark Identify physical & human characteristics of places, regions in North America. Grade Level Indicator Describe, compare landforms, climates, population, vegetation, economic characteristics of

More information

Glacier Erosion Notes

Glacier Erosion Notes Name Date ES per Mr. Landsman Glacier Erosion Notes Erosion: the of weathered material. Glacier: A large mass of ice and snow that exists year-round and moves under the influence of. Evidence for Glacier

More information

Missouri Regions Shaped by Land Forms and Geology

Missouri Regions Shaped by Land Forms and Geology Missouri Regions Shaped by Land Forms and Geology Lesson Abstract Summary: MO GLE: Subject Areas: The students will use various resources to compare and contrast the geology of each Missouri region to

More information

Map reading made easy

Map reading made easy Map reading made easy What is a map? A map is simply a plan of the ground on paper. The plan is usually drawn as the land would be seen from directly above. A map will normally have the following features:

More information

Grades 3-5. Benchmark A: Use map elements or coordinates to locate physical and human features of North America.

Grades 3-5. Benchmark A: Use map elements or coordinates to locate physical and human features of North America. Grades 3-5 Students use knowledge of geographic locations, patterns and processes to show the interrelationship between the physical environment and human activity, and to explain the interactions that

More information

2 Wind Erosion and Deposition

2 Wind Erosion and Deposition CHAPTER 3 2 Wind Erosion and Deposition SECTION Agents of Erosion and Deposition BEFORE YOU READ After you read this section, you should be able to answer these questions: How can wind erosion shape the

More information

Deserts, Wind Erosion and Deposition

Deserts, Wind Erosion and Deposition Deserts, Wind Erosion and Deposition By definition, a desert has less than 10 in (25 cm) of precipitation per year. Deserts occur at 30 o and 60 o in regions of descending air. Deserts can be hot or cold.

More information

8/18/2014. Chapter 9: Erosion and Deposition. Section 1 (Changing Earth s Surface) 8 th Grade. Weathering

8/18/2014. Chapter 9: Erosion and Deposition. Section 1 (Changing Earth s Surface) 8 th Grade. Weathering Section 1 (Changing Earth s Surface) Weathering the chemical and physical processes that break down rock at Earth s surface Chapter 9: Erosion and Deposition 8 th Grade Mechanical weathering when rock

More information

Maps A Primer for Content & Production of Topographic Base Maps For Design Presented by SurvBase, LLC

Maps A Primer for Content & Production of Topographic Base Maps For Design Presented by SurvBase, LLC Maps A Primer for Content & Production of Topographic Base Maps For Design Presented by Definition and Purpose of, Map: a representation of the whole or a part of an area. Maps serve a wide range of purposes.

More information

Plate Tectonics: Ridges, Transform Faults and Subduction Zones

Plate Tectonics: Ridges, Transform Faults and Subduction Zones Plate Tectonics: Ridges, Transform Faults and Subduction Zones Goals of this exercise: 1. review the major physiographic features of the ocean basins 2. investigate the creation of oceanic crust at mid-ocean

More information

Climate, Vegetation, and Landforms

Climate, Vegetation, and Landforms Climate, Vegetation, and Landforms Definitions Climate is the average weather of a place over many years Geographers discuss five broad types of climates Moderate, dry, tropical, continental, polar Vegetation:

More information

Flood Zone Investigation by using Satellite and Aerial Imagery

Flood Zone Investigation by using Satellite and Aerial Imagery Flood Zone Investigation by using Satellite and Aerial Imagery Younes Daneshbod Islamic Azad University-Arsanjan branch Daneshgah Boulevard, Islamid Azad University, Arsnjan, Iran Email: daneshbod@gmail.com

More information

Weathering, Erosion, and Soils. Weathering and Erosion. Weathering and Erosion

Weathering, Erosion, and Soils. Weathering and Erosion. Weathering and Erosion Weathering, Erosion, and Soils 1 The Grand Canyon, a landscape shaped by weathering and erosion 2 Weathering vs. erosion Types of weathering Physical Chemical Rates of weathering and erosion Climate Rock

More information

Allows teachers to print reports for individual students or an entire class.

Allows teachers to print reports for individual students or an entire class. Map and Globe Skills Developed by teachers and geography specialists, Map and Globe Skills provides the strategies, skills and practice your students need to develop a strong understanding of basic mapping

More information

Earth Science. River Systems and Landforms GEOGRAPHY 1710. The Hydrologic Cycle. Introduction. Running Water. Chapter 14.

Earth Science. River Systems and Landforms GEOGRAPHY 1710. The Hydrologic Cycle. Introduction. Running Water. Chapter 14. Earth Science GEOGRAPHY 1710 River Systems and Landforms DAVID R. SALLEE Robert W. Christopherson Charlie Thomsen Chapter 14 Introduction Rivers and streams are dynamic systems that continually adjust

More information

GEOLOGIC MAPS. PURPOSE: To be able to understand, visualize, and analyze geologic maps

GEOLOGIC MAPS. PURPOSE: To be able to understand, visualize, and analyze geologic maps GEOLOGIC MAPS PURPOSE: To be able to understand, visualize, and analyze geologic maps Geologic maps show the distribution of the various igneous, sedimentary, and metamorphic rocks at Earth s surface in

More information

PREFACE. The many TRADOC service schools and DOD agencies that produce the ACCP materials administered by the AIPD develop them to the DETC standards.

PREFACE. The many TRADOC service schools and DOD agencies that produce the ACCP materials administered by the AIPD develop them to the DETC standards. PREFACE The Army Institute for Professional Development (AIPD) administers the consolidated Army Correspondence Course Program (ACCP), which provides highquality, economical training to its users. The

More information

EcoInformatics International Inc.

EcoInformatics International Inc. 1 von 10 03.08.2010 14:25 EcoInformatics International Inc. Home Services - solutions Projects Concepts Tools Links Contact EXPLORING BEAVER HABITAT AND DISTRIBUTION WITH GOOGLE EARTH: THE LONGEST BEAVER

More information

LABORATORY TWO GEOLOGIC STRUCTURES

LABORATORY TWO GEOLOGIC STRUCTURES EARTH AND ENVIRONMENT THROUGH TIME LABORATORY- EES 1005 LABORATORY TWO GEOLOGIC STRUCTURES Introduction Structural geology is the study of the ways in which rocks or sediments are arranged and deformed

More information

Topographic Maps Practice Questions and Answers Revised October 2007

Topographic Maps Practice Questions and Answers Revised October 2007 Topographic Maps Practice Questions and Answers Revised October 2007 1. In the illustration shown below what navigational features are represented by A, B, and C? Note that A is a critical city in defining

More information

CK-12 Earth Science For High School Workbook

CK-12 Earth Science For High School Workbook CK-12 Earth Science For High School Workbook Say Thanks to the Authors Click http://www.ck12.org/saythanks (No sign in required) www.ck12.org To access a customizable version of this book, as well as other

More information

not to be republished NCERT MAJOR LANDFORMS OF THE EARTH

not to be republished NCERT MAJOR LANDFORMS OF THE EARTH 6 You must have seen some of the landform features as shown in the Figure 6.1 below. You will notice that the surface of the earth is not the same everywhere. The earth has an infinite variety of landforms.

More information

The concepts developed in this standard include the following: Oceans cover about 70% of the surface of the Earth.

The concepts developed in this standard include the following: Oceans cover about 70% of the surface of the Earth. Name Date Grade 5 SOL 5.6 Review Oceans Made by SOLpass - www.solpass.org solpass100@comcast.net Reproduction is permitted for SOLpass subscribers only. The concepts developed in this standard include

More information

Small Dam Hazard Assessment Inventory

Small Dam Hazard Assessment Inventory Small Dam Hazard Assessment Inventory What would happen if your dam were to fail? This is a question that most dam owners hope they will never have to answer. However it is a question you, as a responsible

More information

Chapter 4: Representation of relief

Chapter 4: Representation of relief Introduction To this point in our discussion of maps we have been concerned only with their planimetric properties, those relating to the location of features in two-dimensional space. But of course we

More information

Description of Simandou Archaeological Potential Model. 13A.1 Overview

Description of Simandou Archaeological Potential Model. 13A.1 Overview 13A Description of Simandou Archaeological Potential Model 13A.1 Overview The most accurate and reliable way of establishing archaeological baseline conditions in an area is by conventional methods of

More information

Using Google Earth to Explore Plate Tectonics

Using Google Earth to Explore Plate Tectonics Using Google Earth to Explore Plate Tectonics Laurel Goodell, Department of Geosciences, Princeton University, Princeton, NJ 08544 laurel@princeton.edu Inspired by, and borrows from, the GIS-based Exploring

More information

WHAT MAPS SHOW US Maps do 4 things:

WHAT MAPS SHOW US Maps do 4 things: WHAT MAPS SHOW US Maps show us a range of features, for example: Landforms: Settlement: Communication: Land Use: Geology: Other Info: - hills - valleys - mountains - isolated dwellings - farms - villages

More information

Plate Tectonics. Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics. And I am Buddy Zed s mascot

Plate Tectonics. Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics. And I am Buddy Zed s mascot Plate Tectonics Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics And I am Buddy Zed s mascot Continental Drift Alfred Wegener proposed that continents were not always where

More information

Earth Science & Environmental Science SOL

Earth Science & Environmental Science SOL Earth Science & Environmental Science SOL THE SOL FOR GRADE 6 The Virginia Science SOL for Grades K 6 are organized according to a set of strands, with the SOL in each strand developed progressively through

More information

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

6. Base your answer to the following question on the graph below, which shows the average monthly temperature of two cities A and B. 1. Which single factor generally has the greatest effect on the climate of an area on the Earth's surface? 1) the distance from the Equator 2) the extent of vegetative cover 3) the degrees of longitude

More information

GY301 Geomorphology Fluvial Erosion Landforms

GY301 Geomorphology Fluvial Erosion Landforms Introduction Running water is by far the most important erosional agent on Earth. Even in arid climates, it is the primary agent of erosion. This is evident from the abundance of stream beds found throughout

More information

TECTONICS ASSESSMENT

TECTONICS ASSESSMENT Tectonics Assessment / 1 TECTONICS ASSESSMENT 1. Movement along plate boundaries produces A. tides. B. fronts. C. hurricanes. D. earthquakes. 2. Which of the following is TRUE about the movement of continents?

More information

Laboratory 6: Topographic Maps

Laboratory 6: Topographic Maps Name: Laboratory 6: Topographic Maps Part 1: Construct a topographic map of the Egyptian Pyramid of Khafre A topographic map is a two-dimensional representation of a three-dimensional space. Topographic

More information

6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes

6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes Name: Date: 1. The road shown below was suddenly broken by a natural event. 3. The convergence of two continental plates would produce Which natural event most likely caused the crack in the road? island

More information

720 Contour Grading. General. References. Resources. Definitions

720 Contour Grading. General. References. Resources. Definitions 720 Contour Grading General Contour grading directs water to a desired point, prevents erosion, provides noise deflection, provides visual fit of the facility into the landscape, and protects desirable

More information

NATURAL REGIONS OF KENTUCKY

NATURAL REGIONS OF KENTUCKY NATURAL WONDERS As you travel around Kentucky taking pictures, you are excited by what you see. Kentucky offers diverse and amazing sights. The Six Regions In the West, you see the Mississippi River, the

More information

ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE. GRADE 6 SCIENCE Post - Assessment

ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE. GRADE 6 SCIENCE Post - Assessment ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE GRADE 6 SCIENCE Post - Assessment School Year 2013-2014 Directions for Grade 6 Post-Assessment The Grade 6 Post-Assessment is

More information

Stage 4. Geography. Blackline Masters. By Karen Devine

Stage 4. Geography. Blackline Masters. By Karen Devine 1 Devine Educational Consultancy Services Stage 4 Geography Blackline Masters By Karen Devine Updated January 2010 2 This book is intended for the exclusive use in NSW Secondary Schools. It is meant to

More information

LEARNING THE LANDFORMS Grade Level: Third Presented by: Elizabeth Turcott, Endeavor Charter Academy, Springfield, Michigan Length of Unit: 14 lessons

LEARNING THE LANDFORMS Grade Level: Third Presented by: Elizabeth Turcott, Endeavor Charter Academy, Springfield, Michigan Length of Unit: 14 lessons LEARNING THE LANDFORMS Grade Level: Third Presented by: Elizabeth Turcott, Endeavor Charter Academy, Springfield, Michigan Length of Unit: 14 lessons I. ABSTRACT This unit develops an understanding of

More information

FUNDAMENTALS OF LANDSCAPE TECHNOLOGY GSD Harvard University Graduate School of Design Department of Landscape Architecture Fall 2006

FUNDAMENTALS OF LANDSCAPE TECHNOLOGY GSD Harvard University Graduate School of Design Department of Landscape Architecture Fall 2006 FUNDAMENTALS OF LANDSCAPE TECHNOLOGY GSD Harvard University Graduate School of Design Department of Landscape Architecture Fall 2006 6106/ M2 BASICS OF GRADING AND SURVEYING Laura Solano, Lecturer Name

More information

1. You are about to begin a unit on geology. Can anyone tell me what geology is? The study of the physical earth I.

1. You are about to begin a unit on geology. Can anyone tell me what geology is? The study of the physical earth I. PLATE TECTONICS ACTIVITY The purpose of this lab is to introduce the concept of plate tectonics and the formation of mountains. Students will discuss the properties of the earth s crust and plate tectonics.

More information

Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: Water in Earth s Processes. (Approximate Time: 5-6 Weeks)

Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: Water in Earth s Processes. (Approximate Time: 5-6 Weeks) The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are

More information

How Did These Ocean Features and Continental Margins Form?

How Did These Ocean Features and Continental Margins Form? 298 10.14 INVESTIGATION How Did These Ocean Features and Continental Margins Form? The terrain below contains various features on the seafloor, as well as parts of three continents. Some general observations

More information

Remote Sensing, GPS and GIS Technique to Produce a Bathymetric Map

Remote Sensing, GPS and GIS Technique to Produce a Bathymetric Map Remote Sensing, GPS and GIS Technique to Produce a Bathymetric Map Mark Schnur EES 5053 Remote Sensing Fall 2007 University of Texas at San Antonio, Department of Earth and Environmental Science, San Antonio,

More information

Crossing the Pacific Bathymetry

Crossing the Pacific Bathymetry Crossing the Pacific Bathymetry Summary What is really under the salt water in our worldwide oceans? This four-part activity will guide students to explore, investigate, and analyze our mysterious ocean

More information

Focus On You Photography TRT from Brockway Summit to Watson Lake

Focus On You Photography TRT from Brockway Summit to Watson Lake Tahoe Rim Trail (TRT) From Hwy 267 (Brockway Summit) west to Watson Lake (Strong Intermediate Advanced) This trail is very demanding. It is almost 2100 ft. of climbing. The trail is up and down, up and

More information

Tectonic plates have different boundaries.

Tectonic plates have different boundaries. KEY CONCEPT Plates move apart. BEFORE, you learned The continents join and break apart The sea floor provides evidence that tectonic plates move The theory of plate tectonics helps explain how the plates

More information

The Next Generation Science Standards (NGSS) Correlation to. EarthComm, Second Edition. Project-Based Space and Earth System Science

The Next Generation Science Standards (NGSS) Correlation to. EarthComm, Second Edition. Project-Based Space and Earth System Science The Next Generation Science Standards (NGSS) Achieve, Inc. on behalf of the twenty-six states and partners that collaborated on the NGSS Copyright 2013 Achieve, Inc. All rights reserved. Correlation to,

More information

Index. protection. excavated drop inlet protection (Temporary) 6.50.1 6.51.1. Block and gravel inlet Protection (Temporary) 6.52.1

Index. protection. excavated drop inlet protection (Temporary) 6.50.1 6.51.1. Block and gravel inlet Protection (Temporary) 6.52.1 6 Index inlet protection excavated drop inlet protection (Temporary) 6.50.1 HARDWARE CLOTH AND GRAVEL INLET PROTECTION Block and gravel inlet Protection (Temporary) sod drop inlet protection ROCK DOUGHNUT

More information

Rocks and Minerals What is right under your feet?

Rocks and Minerals What is right under your feet? Rocks and Minerals What is right under your feet? Name: 1 Before you start What do you already know? What is the difference between a rock and a mineral? What are the three categories of rocks? 1. 2. 3.

More information

Curriculum Map Earth Science - High School

Curriculum Map Earth Science - High School September Science is a format process to use Use instruments to measure Measurement labs - mass, volume, to observe, classify, and analyze the observable properties. density environment. Use lab equipment

More information

Layers of the Earth and Plate Tectonics

Layers of the Earth and Plate Tectonics Layers of the Earth and Plate Tectonics Objectives: explain various ways the earth can be changed by natural forces define the term Geology define the terms Crust, Mantle, Outer Core and Inner Core classify

More information

Motion & The Global Positioning System (GPS)

Motion & The Global Positioning System (GPS) Grade Level: K - 8 Subject: Motion Prep Time: < 10 minutes Duration: 30 minutes Objective: To learn how to analyze GPS data in order to track an object and derive its velocity from positions and times.

More information

Plan Plus Volume 1 No 1 2002 (117-123)

Plan Plus Volume 1 No 1 2002 (117-123) Plan Plus Volume 1 No 1 2002 (117-123) APPLICATION OF GIS (GEOGRAPHIC INFORMATION SYSTEM) FOR LANDSLIDE HAZARD ZONATION AND MAPPING DISASTER PRONE AREA: A STUDY OF KULEKHANI WATERSHED, NEPAL Purna Chandra

More information

Earth Coordinates & Grid Coordinate Systems

Earth Coordinates & Grid Coordinate Systems Earth Coordinates & Grid Coordinate Systems How do we model the earth? Datums Datums mathematically describe the surface of the Earth. Accounts for mean sea level, topography, and gravity models. Projections

More information

Module 2 Educator s Guide Investigation 3

Module 2 Educator s Guide Investigation 3 What similar physical processes occur on both Earth and Mars? Investigation Overview Could life exist on Mars? This is a question that humans have wondered about for centuries. What physical processes

More information

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

FOR TEACHERS ONLY. The University of the State of New York REGENTS HIGH SCHOOL EXAMINATION PHYSICAL SETTING/EARTH SCIENCE FOR TEACHERS ONLY PS ES The University of the State of New York REGENTS HIGH SCHOOL EXAMINATION PHYSICAL SETTING/EARTH SCIENCE Tuesday, June 22, 2010 9:15 a.m. to 12:15 p.m., only SCORING KEY AND RATING

More information

Educator s Guide to Learning about Mexico Using Google Earth

Educator s Guide to Learning about Mexico Using Google Earth Educator s Guide to Learning about Mexico Using Google Earth Overview: Students will research the physical features of Mexico using Google Earth to learn about Mexico s oceans, gulfs, bays, lagoons, rivers,

More information

Using LIDAR to monitor beach changes: Goochs Beach, Kennebunk, Maine

Using LIDAR to monitor beach changes: Goochs Beach, Kennebunk, Maine Geologic Site of the Month February, 2010 Using LIDAR to monitor beach changes: Goochs Beach, Kennebunk, Maine 43 o 20 51.31 N, 70 o 28 54.18 W Text by Peter Slovinsky, Department of Agriculture, Conservation

More information

CITY UTILITIES DESIGN STANDARDS MANUAL

CITY UTILITIES DESIGN STANDARDS MANUAL CITY UTILITIES DESIGN STANDARDS MANUAL Book 2 (SW) SW9 June 2015 SW9.01 Purpose This Chapter provides information for the design of open channels for the conveyance of stormwater in the City of Fort Wayne.

More information

Climates are described by the same conditions used to describe

Climates are described by the same conditions used to describe 58 The Causes of Climate R E A D I N G Climates are described by the same conditions used to describe weather, such as temperature, precipitation, and wind. You now know that oceans have an important effect

More information

1 Branches of Earth Science

1 Branches of Earth Science CHAPTER 1 1 Branches of Earth Science SECTION The World of Earth Science BEFORE YOU READ After you read this section, you should be able to answer these questions: What are the four major branches of Earth

More information

The Water Cycle Now You See It, Now You Don t

The Water Cycle Now You See It, Now You Don t The Water Cycle Now You See It, Now You Don t Unit: Salinity Patterns & the Water Cycle l Grade Level: Elementary l Time Required: Introduction - 30 min. - Activity as groups 45min Wrap Up 20 min l Content

More information

SESSION 8: GEOGRAPHIC INFORMATION SYSTEMS AND MAP PROJECTIONS

SESSION 8: GEOGRAPHIC INFORMATION SYSTEMS AND MAP PROJECTIONS SESSION 8: GEOGRAPHIC INFORMATION SYSTEMS AND MAP PROJECTIONS KEY CONCEPTS: In this session we will look at: Geographic information systems and Map projections. Content that needs to be covered for examination

More information

SLOPE AND TOPOGRAPHY

SLOPE AND TOPOGRAPHY SLOPE AND TOPOGRAPHY What are Slope and Topography? Slope and topography describe the shape and relief of the land. Topography is a measurement of elevation, and slope is the percent change in that elevation

More information

Field Methods in Environmental Science

Field Methods in Environmental Science Field Methods in Environmental Science A Field Camp Experience in West Virginia Geography 418 Fall 2014 (August 11 22) Measuring stream profiles on the South Branch Potomac Course Description Geography

More information

The Ice Age By: Sue Peterson

The Ice Age By: Sue Peterson www.k5learning.com Objective sight words (pulses, intermittent, isotopes, chronicle, methane, tectonic plates, volcanism, configurations, land-locked, erratic); concepts (geological evidence and specific

More information

Environmental Case Study Decatur, Georgia, DeKalb County A Suburban Creek Resists Channelization

Environmental Case Study Decatur, Georgia, DeKalb County A Suburban Creek Resists Channelization Introduction A visual examination of Doolittle Creek in a highly developed suburban county in Georgia yielded telltale signs of a creek whose original streambed had been altered. Examination of official

More information

Flash Flood Science. Chapter 2. What Is in This Chapter? Flash Flood Processes

Flash Flood Science. Chapter 2. What Is in This Chapter? Flash Flood Processes Chapter 2 Flash Flood Science A flash flood is generally defined as a rapid onset flood of short duration with a relatively high peak discharge (World Meteorological Organization). The American Meteorological

More information

Mud in the Water. www.agclassroom.org/ok. Oklahoma Academic Standards. Objective. Background. Resources Needed. Activities

Mud in the Water. www.agclassroom.org/ok. Oklahoma Academic Standards. Objective. Background. Resources Needed. Activities Mud in the Water Objective Students will learn about soil erosion and water pollution by building a demonstration model from pop bottles and observing the movement of pollutants from soil into water. Background

More information

Geomorphology is the Study of Landforms. Usually by Erosion, Transportation and Deposition

Geomorphology is the Study of Landforms. Usually by Erosion, Transportation and Deposition Geomorphology is the Study of Landforms and the Processes that t Create Them, Usually by Erosion, Transportation and Deposition Fluvial = running water, rivers and floodplains Glacial = flowing ice in

More information

The rock cycle. Introduction. What are rocks?

The rock cycle. Introduction. What are rocks? The rock cycle This Revision looks at the three types of rock: sedimentary, igneous and metamorphic. It looks at how they are formed, the weathering of rocks and the way one form of rock turns into another,

More information

Rosaly Lopes, Jet Propulsion Laboratory, California Institute of Technology

Rosaly Lopes, Jet Propulsion Laboratory, California Institute of Technology Saturn s Moon Titan: Cassini-Huygens Reveals a New World Rosaly Lopes, Jet Propulsion Laboratory, California Institute of Technology The year 2005 will be remembered in the history of space exploration

More information

Gravitational potential

Gravitational potential Gravitational potential Let s assume: A particle of unit mass moving freely A body of mass M The particle is attracted by M and moves toward it by a small quantity dr. This displacement is the result of

More information

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

What causes Tides? If tidal forces were based only on mass, the Sun should have a tidegenerating What are Tides? Tides are very long-period waves that move through the oceans as a result of the gravitational attraction of the Moon and the Sun for the water in the oceans of the Earth. Tides start in

More information

5 th Grade Science Vocabulary Words

5 th Grade Science Vocabulary Words 5 th Grade Science Vocabulary Words abiotic factor A nonliving part of an ecosystem. acceleration Change in velocity with respect to time. action The force one object applies to a second, as in Newton

More information

Web of Water. Teacher s Guide Webisode 1 Blue Ridge

Web of Water. Teacher s Guide Webisode 1 Blue Ridge Web of Water Teacher s Guide Webisode 1 Blue Ridge Table of Contents About Blue Ridge.... 3 South Carolina Science Standards.. 4 Discussion Questions.. 10 Knowitall Resources....... 13 Credits..... 14

More information

ebb current, the velocity alternately increasing and decreasing without coming to

ebb current, the velocity alternately increasing and decreasing without coming to Slack water (slack tide): The state of a tidal current when its velocity is near zero, especially the moment when a reversing current changes its direction and its velocity is zero. The term is also applied

More information

Benton MacKaye Trail - Section 2. Three Forks (FS 58) to GA. Highway 60. 11.4 miles

Benton MacKaye Trail - Section 2. Three Forks (FS 58) to GA. Highway 60. 11.4 miles General Benton MacKaye Trail - Section 2 Three Forks (FS 58) to GA. Highway 60 11.4 miles This is the longest and most remote section of the Benton MacKaye Trail (BMT) east of GA 5. It follows the Appalachian

More information

How To Read Maps And Aerial Photos

How To Read Maps And Aerial Photos 3 Read Maps and Aerial Photos WRITING SAMPLE (training guide) Stephen X. Arthur, technical writer 2005 www.transcanfilm.com/stephenarthur First draft. Copyright 1996, BC Ministry of Forests / BC Institute

More information

Geologic History Review

Geologic History Review 1. The climate that existed in an area during the early Paleozoic Era can best be determined by studying (1) the present climate of the area (2) recorded climate data of the area since 1700 (3) present

More information

How can you tell rocks apart?

How can you tell rocks apart? How can you tell rocks apart? Grade Range: 4-7 G.L.E Focus: 1.1.5 Time Budget: 1 1.5 hours WASL Vocabulary: Overview: Different rocks have different characteristics because of their minerals, the ways

More information