Docsity
Docsity

Prepare for your exams
Prepare for your exams

Study with the several resources on Docsity


Earn points to download
Earn points to download

Earn points by helping other students or get them with a premium plan


Guidelines and tips
Guidelines and tips

Contour Lines and Profiles in Physical Geography: Understanding Elevation and Landforms, Study notes of Physical Geography

An introduction to contour lines and profiles in physical geography. Students will learn about the characteristics of contour lines, how to interpret contour maps, and how to construct a contour profile. figures and examples to help illustrate the concepts. Materials needed include a pencil and an enlarged section of a topographic map. Students will become familiar with contour lines and their significance in representing elevation and terrain features.

What you will learn

  • What is the elevation at Point C?
  • What is the feature type at Point E?
  • What is the feature type at Point D?
  • What is the elevation at Point A?
  • What is the contour interval of the map section?

Typology: Study notes

2021/2022

Uploaded on 09/27/2022

russel85
russel85 🇬🇧

4.6

(5)

285 documents

1 / 7

Toggle sidebar

This page cannot be seen from the preview

Don't miss anything!

bg1
PHYSICAL GEOGRAPHY GPH111
LAB F - INTRODUCTION TO GEOGRAPHIC TOOLS - CONTOUR LINES
AND PROFILES
Introduction
Topographic maps are distinguished by their ability to show elevation relationships with contour
lines. The brown lines on a topographic map are contour lines, lines representing an
imaginary line on the ground along which all points are at the same elevation. Contour lines
also show the shape of features on the terrain. Given a series of surveyed data points and their
elevations, one can construct a contour map of any known surface. In this exercise the student
will become familiar with contour lines and their characteristics. Students will also use an
enlarged section of the Folsom, New Mexico Quadrangle to “interpret the language of the
contours”, to determine elevations, types of slope and features (landforms) on the map. Lastly,
students will construct a contour profile, or cross section diagram, of a selected map section
Materials needed: pencil, Buffalo Head enlarged section + 2 topographic maps (on reserve)
Part I. Characteristics of Contour Lines
Before beginning, review the following rules or characteristics concerning contour lines.
1. Closely spaced contour lines indicate a steep slope (Figure F-1).
2. Widely spaced contour lines indicate a gentle slope (Figure F-2).
3. Evenly spaced contour lines indicate a uniform slope (Figure F-2), while irregular spacing
indicates an irregular slope (Figure F-1).
4. Contour lines that are widely spaced at the top of the slope and closely spaced at the
bottom of the slope depict a convex slope. Contour lines that are closely spaced at the top
of the slope and widely spaced at the bottom depict a concave slope.
5. Contour lines may lie very close together, may even appear to coalesce. Such lines
indicate a very steep slope or cliff; however, contour lines never cross, merge, touch,
branch or fork.
6. Completely closed contour lines indicate tops of hills, mountains, peaks etc. These
contours would indicate higher elevation than the surrounding area in all directions (Figure
F-3).
7. Bent contour lines indicate a rise in elevation (spur or ridge), or a drop in elevation (valley)
An example of a valley is shown at (Figure F-4).
8. Lines depicting a valley bend up-valley, toward the higher elevation (Figure F-4).
9. Hachure marks within contour lines indicate a significant, closed depression (Figure F-5).
10. Brown is the color used by cartographers for most contour lines. Light brown is used for
intermediate contour lines. Every 4th or 5th contour line (depending on the contour interval)
is an index contour line, is a darker shade of brown and labeled with the appropriate
elevation (Figures F-4, F-5 or F-6). Index contour lines speed the process of interpretation.
11. The vertical distance between adjacent contour lines is known as the contour interval.
This contour interval is given in the marginal data of the map sheet. Unless otherwise
marked, points that lie between contour lines assume a value of one half of the contour
interval of the map.
F-1
pf3
pf4
pf5

Partial preview of the text

Download Contour Lines and Profiles in Physical Geography: Understanding Elevation and Landforms and more Study notes Physical Geography in PDF only on Docsity!

LAB F - INTRODUCTION TO GEOGRAPHIC TOOLS - CONTOUR LINES

AND PROFILES

Introduction

Topographic maps are distinguished by their ability to show elevation relationships with contour lines. The brown lines on a topographic map are contour lines, lines representing an imaginary line on the ground along which all points are at the same elevation. Contour lines also show the shape of features on the terrain. Given a series of surveyed data points and their elevations, one can construct a contour map of any known surface. In this exercise the student will become familiar with contour lines and their characteristics. Students will also use an enlarged section of the Folsom, New Mexico Quadrangle to “interpret the language of the contours”, to determine elevations, types of slope and features (landforms) on the map. Lastly, students will construct a contour profile, or cross section diagram, of a selected map section

Materials needed: pencil, Buffalo Head enlarged section + 2 topographic maps (on reserve)

Part I. Characteristics of Contour Lines

Before beginning, review the following rules or characteristics concerning contour lines.

  1. Closely spaced contour lines indicate a steep slope (Figure F-1).
  2. Widely spaced contour lines indicate a gentle slope (Figure F-2).
  3. Evenly spaced contour lines indicate a uniform slope (Figure F-2), while irregular spacing indicates an irregular slope (Figure F-1).
  4. Contour lines that are widely spaced at the top of the slope and closely spaced at the bottom of the slope depict a convex slope. Contour lines that are closely spaced at the top of the slope and widely spaced at the bottom depict a concave slope.
  5. Contour lines may lie very close together, may even appear to coalesce. Such lines indicate a very steep slope or cliff; however, contour lines never cross, merge, touch, branch or fork.
  6. Completely closed contour lines indicate tops of hills, mountains, peaks etc. These contours would indicate higher elevation than the surrounding area in all directions (Figure F-3).
  7. Bent contour lines indicate a rise in elevation (spur or ridge), or a drop in elevation (valley) An example of a valley is shown at (Figure F-4).
  8. Lines depicting a valley bend up-valley , toward the higher elevation (Figure F-4).
  9. Hachure marks within contour lines indicate a significant, closed depression (Figure F-5).
  10. Brown is the color used by cartographers for most contour lines. Light brown is used for intermediate contour lines. Every 4th^ or 5 th^ contour line (depending on the contour interval) is an index contour line, is a darker shade of brown and labeled with the appropriate elevation (Figures F-4, F-5 or F-6). Index contour lines speed the process of interpretation.
  11. The vertical distance between adjacent contour lines is known as the contour interval. This contour interval is given in the marginal data of the map sheet. Unless otherwise marked, points that lie between contour lines assume a value of one half of the contour interval of the map.

Part I. Elevations, Slopes and Features (Landforms) Shown With Contour Lines

Figure F-1: Steep, Irregular Slope Figure F-2: Gentle, Uniform Slope

Figure F-3: Peak Figure F-4: Valley

Figure F-5: Closed Depression Figure F-6: Saddle

Part III. Constructing a Contour Profile

The identification of landforms from an examination of the contour lines is adequate for many purposes, but when precision is demanded, a contour profile (Fig F-7) is usually necessary. Constructing a contour profile employs the same graphing skills learned in the first lab exercise (Line Graph) and provides additional information about complex landforms, slopes, trafficability and intervisibility between points on the terrain.

Fig F-7: Contour Profile

Based on the demonstration of the procedure for constructing a contour profile, construct a profile of the area between Points H and I on the Buffalo Head map below. Use the graph paper on page F-7. The X-axis (horizontal axis) represents the true length of the line connecting points H and I.

Graph paper for Buffalo Head Contour Profile