---
title: "Maps of the Whole Earth"
book: "Primary & Middle School Earth and Space Sciences"
subject: earth
language: en
chapter: 32
exercises: 12
source: https://one-course.com/books/earth/1/en/chapter/32-maps-of-the-whole-earth
license: CC-BY-NC-SA-4.0
credit: "One Earth and Space Sciences Book, One Course (one-course.com)"
---

# Chapter 32 — Maps of the Whole Earth

On many classroom wall [maps](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), Greenland looks about as big as Africa. On a [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe), Africa is about fourteen times larger: about 29 million square kilometres for the African mainland, against about 2.1 million for Greenland. Both are true pictures of the Earth, made with care. So which one is lying, and why?

**You already know.**

A [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) is a drawing of a place seen from above, smaller than the place, with a [legend](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-legend) and a [scale](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-scale) ([Chapter 4](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#ch-g2-drawing-to-map)). A [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe) is a small model of the round Earth; a [world map](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-world-map) shows the whole Earth flat, in one picture ([Chapter 6](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#ch-g3-continents-and-oceans)). [Parallels](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) and [meridians](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-longitude) give every place its [latitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) and [longitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-longitude) ([Chapter 14](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#ch-g6-latitude-longitude)). [Altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) is the height above [sea level](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude), and a [physical map](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-physical-map) shows the [relief](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-relief) in colours ([Chapter 9](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#ch-g4-world-physical-map)). In physics, you learn that light travels at about $300\,000\,\mathrm{km}$ per second.

## 32.1 Why a flat map has to distort

Try to flatten the peel of an orange on a table: it tears or it stretches. The surface of a sphere cannot be laid flat without changing some lengths. To draw the whole Earth on a sheet, a mapmaker chooses a rule that sends every point of the [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe) to a point of the sheet, and chooses what the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) will keep true, and what it will give up.

**Definition 32.1 (Map projection).**

A *map projection* is a rule that sends every point of the [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe), given by its [latitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) and [longitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-longitude), to a point of a flat [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). On a *Mercator projection*, the [parallels](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) and the [meridians](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-longitude) are straight lines crossing at right angles, and the shape of every small region is kept, but areas are enlarged more and more towards the [poles](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles). On an *equal-area projection*, every region keeps its true area compared with the others, but shapes are bent, more and more towards the edges of the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map).

The figure below draws the same equal circles on the [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe), all of the same size, onto both [maps](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). On the Mercator [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), the circles stay round but grow towards the [poles](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles): at [latitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) $60{}^{\circ}$, their area is four times what it is at the [equator](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-equator), and near Greenland’s middle, at about $72{}^{\circ}$, about ten times. On the equal-area [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), the circles all keep the same area, but those far from the centre are squashed into ovals.

No projection is the best for everything. The [Mercator projection](#def-g9-maps-of-the-earth-projection) was made for sailors: a course that keeps the same compass direction is a straight line on it. To compare the sizes of countries, of forests or of [deserts](https://one-course.com/books/earth/1/en/chapter/11-weather-and-climate#def-g5-weather-and-climate-desert), an equal-area [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) tells the truth. Before trusting a [world map](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-world-map), it is worth asking which projection it uses.

![The same world on two projections. Red: circles of the same size on the globe, centred every 30 of latitude and 60 of longitude. Orange: Greenland; blue: the African mainland. On the Mercator map (left, cut at 80 S and 84 N, since the poles would be infinitely far), the two look about the same size; on the equal-area map (right), Africa is about 14 times larger, as on the globe. Coastlines from Natural Earth.](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/fig-0c4257fb207f.svg)

*The same world on two projections. Red: circles of the same size on the [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe), centred every $30{}^{\circ}$ of [latitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) and $60{}^{\circ}$ of [longitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-longitude). Orange: Greenland; blue: the African mainland. On the Mercator [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) (left, cut at $80{}^{\circ}$ S and $84{}^{\circ}$ N, since the [poles](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles) would be infinitely far), the two look about the same size; on the equal-area [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) (right), Africa is about 14 times larger, as on the [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe). Coastlines from Natural Earth.*

**Example 32.2 (Greenland and Africa).**

Africa’s mainland covers about 29 million $\mathrm{km}^{2}$, Greenland about 2.1 million $\mathrm{km}^{2}$: $29 \div 2.1 \approx 14$. Africa straddles the [equator](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-equator), where the [Mercator projection](#def-g9-maps-of-the-earth-projection) hardly enlarges anything, while most of Greenland lies between about $60{}^{\circ}$ and $84{}^{\circ}$ north, where areas are enlarged from 4 to more than 10 times. On the Mercator [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), the two come out about the same size.

## 32.2 Scale

A [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) of a [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) or a town is so small a piece of the Earth that the projection hardly matters. What matters is how much smaller than the ground the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) is.

**Definition 32.3 (Numerical scale and scale bar).**

The *numerical scale* of a [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) is a ratio such as $1 : 25\,000$: one centimetre on the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) stands for $25\,000$ centimetres on the ground, and the same for any unit. A *scale bar* is a ruler drawn on the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), marked with the distances on the ground.

**Method 32.4 (Using a numerical scale).**

1. Measure the distance on the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) , in centimetres.
2. Multiply it by the number after the colon: the result is the distance on the ground, in centimetres.
3. Convert: divide by 100 for metres, by $100\,000$ for kilometres.

**Example 32.5 (A walk on a 1:25 0001 : 25\,0001:25000 map).**

On a [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) at $1 : 25\,000$, a footpath measures $6\,\mathrm{cm}$. On the ground, it is $6 \times 25\,000 = 150\,000$ cm, that is $1500\,\mathrm{m}$ or $1.5\,\mathrm{km}$. Each centimetre of the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) stands for $250\,\mathrm{m}$.

The [scale bar](#def-g9-maps-of-the-earth-numerical-scale) has one advantage over the [numerical scale](#def-g9-maps-of-the-earth-numerical-scale): when a [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) is enlarged or shrunk on a screen or a copier, the bar is enlarged or shrunk with it and stays right, while the ratio printed in the corner becomes wrong.

## 32.3 The topographic map

A [physical map](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-physical-map) shows the [relief](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-relief) with colours. A [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) of a small area shows it far more precisely, with lines.

**Definition 32.6 (Topographic map).**

A *topographic map* is a detailed [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) of a small area, at a [scale](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-scale) such as $1 : 25\,000$ or $1 : 50\,000$, that shows the shape and the height of the ground, with the [rivers](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water), roads, paths, buildings and woods.

**Definition 32.7 (Contour line and contour interval).**

A *contour line* is a line on a [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) joining points of the ground at the same [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude). The *contour interval* is the difference in [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) between two neighbouring contour lines; it is the same all over the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map).

Imagine a [hill](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) sliced by horizontal planes, one every $100\,\mathrm{m}$. Each slice cuts the [hill](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) along a closed line; seen from above, these lines are the [contour lines](#def-g9-maps-of-the-earth-contour).

![A hill sliced every 100\, m (a sketch). Seen from above, each slice gives a closed contour line around the summit. Where the slope is steep (east), the lines are close together; where it is gentle (west), they are far apart.](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/fig-1d4d0cbeef48.svg)

*A [hill](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) sliced every $100\,\mathrm{m}$ (a sketch). Seen from above, each slice gives a closed [contour line](#def-g9-maps-of-the-earth-contour) around the summit. Where the slope is steep (east), the lines are close together; where it is gentle (west), they are far apart.*

A [topographic map](#def-g9-maps-of-the-earth-topographic-map) is read with a few rules.

- [Contour lines](#def-g9-maps-of-the-earth-contour) never cross: a point has only one [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) .
- The closer the [contour lines](#def-g9-maps-of-the-earth-contour) , the steeper the slope; far apart, the ground is gentle; no line at all, it is nearly flat.
- Closed lines nested inside one another, rising inwards, mark a [hill](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) ; its top is often marked by a dot with its [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) , a *spot height* .
- Where a [contour line](#def-g9-maps-of-the-earth-contour) crosses a [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) , it bends upstream, in a V that points towards the head of the [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) .
- Every fifth line, the *index contour* , is drawn thicker and labelled with its [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) .

The slope of the ground between two points is the rise divided by the horizontal distance, often written as a percentage. On the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) below, going north from the [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water), the $200\,\mathrm{m}$ and $400\,\mathrm{m}$ contours on line C–D are about $0.75\,\mathrm{km}$ apart: the slope is about $200 \div 750
\approx 0.27$, or $27\,\%$.

**Method 32.8 (Drawing a topographic profile).**

1. Draw the line of the profile on the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) , from one end (C) to the other (D).
2. Lay the straight edge of a strip of paper along the line; mark C, D, and every point where the line crosses a [contour line](#def-g9-maps-of-the-earth-contour) , with its [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) .
3. Draw a horizontal axis as long as C–D (the distances) and a vertical axis of [altitudes](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) .
4. Carry each mark to the graph, at its distance from C and at its [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) , and join the points with a smooth curve: rounded on [hill](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) tops, flat along a [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) floor.

![Top: a topographic map of part of the Varden Hills at 1 : 50\,000 (1 cm on the map for 500\, m on the ground). Contour interval 50\, m; the index contours, thicker, are at 250 and 500\, m. The river flows east along a flat valley floor. Bottom: the topographic profile along C–D, from south to north; the dots are the points where C–D crosses a contour line (the vertical scale is stretched three times).](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/fig-dfba95c35426.svg)

*Top: a [topographic map](#def-g9-maps-of-the-earth-topographic-map) of part of the Varden Hills at $1 : 50\,000$ (1 cm on the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) for $500\,\mathrm{m}$ on the ground). [Contour interval](#def-g9-maps-of-the-earth-contour) $50\,\mathrm{m}$; the index contours, thicker, are at 250 and $500\,\mathrm{m}$. The [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) flows east along a flat [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) floor. Bottom: the topographic profile along C–D, from south to north; the dots are the points where C–D crosses a [contour line](#def-g9-maps-of-the-earth-contour) (the vertical scale is stretched three times).*

## 32.4 Satellite images of the Earth

On 23 July 1972, a rocket launched the first satellite built to study the Earth’s surface, later called Landsat 1. Circling the Earth 14 times a day at $917\,\mathrm{km}$, from [pole](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles) to [pole](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles), it passed over the same place every 18 days and, in six years, took images of about three quarters of the Earth’s surface. Landsat satellites have imaged the land without a break ever since.

**Definition 32.9 (Remote sensing and satellite image).**

*Remote sensing* is the observation of the Earth from a distance, from aircraft or from satellites, by measuring the light and other radiation that the surface sends back. A *satellite image* is a picture of part of the Earth built from these measurements.

A satellite camera sees more than our eyes: it also measures infrared light, which is invisible. Shown in colours on the image (a *false-colour* image), the infrared reveals plants, wet ground or bare [rock](https://one-course.com/books/earth/1/en/chapter/5-stones-pebbles-and-sand#def-g3-stones-pebbles-sand-rock). Images of the same place taken years apart show how a [coast](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water), a forest, a [glacier](https://one-course.com/books/earth/1/en/chapter/27-ice-on-earth#def-g8-ice-on-earth-glacier) or a town changes ([Chapter 27](https://one-course.com/books/earth/1/en/chapter/27-ice-on-earth#ch-g8-ice-on-earth)).

![The delta of the river Lena, in Siberia, where it meets the Arctic Ocean: a false-colour Landsat image of 27 February 2000, made with shortwave infrared, infrared and red light. The many channels of the river show in blue. USGS EROS Data Center, via NASA Visible Earth (public domain, via Wikimedia Commons).](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/img-720300eeeeeb.jpg)

*The [delta](https://one-course.com/books/earth/1/en/chapter/10-water-shapes-the-land#def-g5-water-shapes-the-land-delta) of the [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) Lena, in Siberia, where it meets the Arctic [Ocean](https://one-course.com/books/earth/1/en/chapter/3-water-on-earth#def-g2-water-on-earth-ocean): a false-colour Landsat image of 27 February 2000, made with shortwave infrared, infrared and red light. The many channels of the [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) show in blue. USGS EROS Data Center, via NASA Visible Earth (public domain, via Wikimedia Commons).*

## 32.5 Satellite positioning

A phone or a car can tell where it is to within a few metres, almost anywhere on the Earth. It does not see the satellites; it listens to them.

**Definition 32.10 (Satellite positioning).**

*Satellite positioning* is finding a position on the Earth from the distances to several satellites whose positions are known. A receiver computes each distance from the time a signal from the satellite takes to reach it.

The American system, GPS, keeps at least 24 working satellites at an [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) of about $20\,200\,\mathrm{km}$. Each circles the Earth twice a day, in six orbits spread around the planet, so that from almost any point on the Earth at least four satellites are in view. A signal from $20\,200\,\mathrm{km}$ away, travelling at the speed of light, arrives after $20\,200 \div
300\,000 \approx 0.067$ s: the receiver measures this time and turns it into a distance.

How do distances give a position? Picture the idea on a flat [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). If the receiver is $5\,\mathrm{km}$ from beacon A, it lies somewhere on a circle of radius $5\,\mathrm{km}$ around A. If it is also $10\,\mathrm{km}$ from B, it lies on both circles: at one of the two points where they cross. A third distance, $5\,\mathrm{km}$ from C, picks the right one. In space, the circles become spheres, and one more satellite is needed for the same reason.

![Positioning on a flat map (a sketch; grid in kilometres not drawn). The receiver R is 5\, km from A, 10\, km from B and 5\, km from C. The circles around A and B cross at R and at a false point F; only R also lies on the circle around C.](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/fig-fee85d5720f3.svg)

*Positioning on a flat [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) (a sketch; grid in kilometres not drawn). The receiver R is $5\,\mathrm{km}$ from A, $10\,\mathrm{km}$ from B and $5\,\mathrm{km}$ from C. The circles around A and B cross at R and at a false point F; only R also lies on the circle around C.*

![](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/img-b3765bfdac54.jpg)

![](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/img-f2e811edb0d5.jpg)

*A GPS satellite in orbit, as an artist pictured it. NASA (public domain, via Wikimedia Commons).*

*A surveyor fixes the position of a point with a satellite receiver on a tripod (an illustration).*

## 32.6 Exercises

**Exercise 32.1 ★.**

Give the word for each description. (a) A rule that sends each point of the [globe](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-globe) to a point of a flat [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). (b) A line joining points at the same [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude). (c) A ratio such as $1 : 50\,000$. (d) The difference in [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) between two neighbouring [contour lines](#def-g9-maps-of-the-earth-contour). (e) Observing the Earth from a distance, for example from a satellite.

**Solution of Exercise 32.1.**

(a) A [map projection](#def-g9-maps-of-the-earth-projection). (b) A [contour line](#def-g9-maps-of-the-earth-contour). (c) A [numerical scale](#def-g9-maps-of-the-earth-numerical-scale). (d) The [contour interval](#def-g9-maps-of-the-earth-contour). (e) [Remote sensing](#def-g9-maps-of-the-earth-remote-sensing).

**Exercise 32.2 ★.**

Convert each [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) distance into a distance on the ground, in metres or kilometres. (a) $4\,\mathrm{cm}$ on a $1 : 25\,000$ [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). (b) $3\,\mathrm{cm}$ on a $1 : 50\,000$ [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). (c) $2.5\,\mathrm{cm}$ on a $1 : 1\,000\,000$ [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). (d) On a $1 : 25\,000$ [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), how many centimetres stand for $1\,\mathrm{km}$?

**Solution of Exercise 32.2.**

(a) $4 \times 25\,000 = 100\,000$ cm $= 1\,\mathrm{km}$. (b) $3 \times
50\,000 = 150\,000$ cm $= 1.5\,\mathrm{km}$. (c) $2.5 \times 1\,000\,000
= 2\,500\,000$ cm $= 25\,\mathrm{km}$. (d) $1\,\mathrm{km} = 100\,000$ cm; $100\,000 \div 25\,000 = 4\,\mathrm{cm}$.

**Exercise 32.3 ★.**

True or false? Correct the false sentences. (a) A [world map](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-world-map) can show the whole Earth without distorting anything. (b) On a Mercator [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), Greenland looks bigger than it is. (c) On an equal-area [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), shapes are kept everywhere. (d) A [scale bar](#def-g9-maps-of-the-earth-numerical-scale) stays right when a [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) is enlarged on a copier.

**Solution of Exercise 32.3.**

(a) False: a sphere cannot be flattened without distorting lengths, so every [world map](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-world-map) distorts something. (b) True. (c) False: an equal-area [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) keeps areas, but bends shapes, especially near its edges. (d) True.

**Exercise 32.4 ★.**

On a [topographic map](#def-g9-maps-of-the-earth-topographic-map), (a) what does it mean when [contour lines](#def-g9-maps-of-the-earth-contour) are very close together? (b) far apart? (c) What do closed [contour lines](#def-g9-maps-of-the-earth-contour) rising inwards show? (d) Why can two [contour lines](#def-g9-maps-of-the-earth-contour) never cross?

**Solution of Exercise 32.4.**

(a) The slope is steep. (b) The ground is gentle. (c) A [hill](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform), its top inside the smallest line. (d) A point of the ground has only one [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude), so it cannot lie on two lines of different [altitudes](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude).

**Exercise 32.5 ★★.**

On a Mercator [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), areas at [latitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) $60{}^{\circ}$ are enlarged 4 times, and at [latitude](https://one-course.com/books/earth/1/en/chapter/14-latitude-longitude-and-time-zones#def-g6-latitude-longitude-latitude) $30{}^{\circ}$ about 1.33 times, compared with the [equator](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-equator). (a) A [lake](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) of $1000\,\mathrm{km}^{2}$ at $60{}^{\circ}$ N is drawn on the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). A [lake](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) at the [equator](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-equator) drawn with the same size has what true area? (b) Two islands of the same true area lie at $30{}^{\circ}$ and at $60{}^{\circ}$. How many times larger does the second look than the first? (c) Why can the Mercator [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) never show the [poles](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles)?

**Solution of Exercise 32.5.**

(a) At $60{}^{\circ}$ N the [lake](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) is drawn 4 times too large: it looks as large as $4 \times 1000 = 4000\,\mathrm{km}^{2}$. At the [equator](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-equator) areas are not enlarged, so the [lake](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) drawn with the same size has a true area of $4000\,\mathrm{km}^{2}$. (b) $4 \div 1.33 \approx 3$ times larger. (c) Areas, and distances north to south, grow without limit towards the [poles](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles): the [poles](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-poles) would be infinitely far from the [equator](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-equator).

**Exercise 32.6 ★★.**

Use the [topographic map](#def-g9-maps-of-the-earth-topographic-map) of the Varden Hills in this chapter. (a) What is the [contour interval](#def-g9-maps-of-the-earth-contour)? (b) What is the [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) of the summit marked by its spot height, and of the index contour just around it? (c) The [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) flows east. Is the [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) floor higher in the west or in the east of the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map)? (d) Along C–D, north of the [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water), between which [contour lines](#def-g9-maps-of-the-earth-contour) are the lines closest together? What does that tell you about the slope there?

**Solution of Exercise 32.6.**

(a) $50\,\mathrm{m}$. (b) The summit is at $544\,\mathrm{m}$; the index contour around it is the $500\,\mathrm{m}$ line. (c) In the west: a [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) flows downhill, so its floor is lower downstream, to the east. (d) Between about the 300 and the $400\,\mathrm{m}$ lines: there the slope is steepest, gentler both near the [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) floor and near the summit.

**Exercise 32.7 ★★.**

Use the profile C–D in this chapter. (a) At about what [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) are C and D? (b) What is the lowest [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) along the profile, and how far from C is it? (c) How long is the flat [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) floor along C–D? (d) The profile is drawn with its vertical scale stretched three times. Why do mapmakers often do this?

**Solution of Exercise 32.7.**

(a) C at about $400\,\mathrm{m}$, D at about $530\,\mathrm{m}$. (b) About $135\,\mathrm{m}$, about $1.3\,\mathrm{km}$ from C, on the [valley](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) floor. (c) About 0.3 to $0.4\,\mathrm{km}$. (d) The heights are small compared with the distances: without stretching, the [hills](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-landform) would look almost flat.

**Exercise 32.8 ★★.**

On a $1 : 25\,000$ [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), a path crosses the $200\,\mathrm{m}$ contour and then the $300\,\mathrm{m}$ contour, $2\,\mathrm{cm}$ further on. (a) What is the horizontal distance between the two points on the ground? (b) How much does the path climb? (c) What is the slope, as a percentage? (d) Further on, two contours $100\,\mathrm{m}$ apart in [altitude](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) are $4\,\mathrm{cm}$ apart on the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map). Is the path steeper or gentler there? By how much?

**Solution of Exercise 32.8.**

(a) $2 \times 25\,000 = 50\,000$ cm $= 500\,\mathrm{m}$. (b) $300 - 200 =
100\,\mathrm{m}$. (c) $100 \div 500 = 0.2$, a slope of $20\,\%$. (d) Gentler: $4\,\mathrm{cm}$ is $1000\,\mathrm{m}$, so the slope is $100 \div 1000 = 10\,\%$, half as steep.

**Exercise 32.9 ★★.**

Landsat 1 circled the Earth 14 times a day and passed over the same place every 18 days. (a) How many orbits did it make between two passes over the same place? (b) Each orbit took 103 minutes. How long, in hours, are 14 orbits? (c) Built to work one year, it was switched off on 6 January 1978, five and a half years after its launch. How many times its planned life did it work? (d) Give one change on the Earth’s surface that images of the same place taken years apart can show.

**Solution of Exercise 32.9.**

(a) $14 \times 18 = 252$ orbits. (b) $14 \times 103 = 1442$ minutes, about $24\,\mathrm{h}$: a day. (c) $5.5 \div 1 = 5.5$ times. (d) For example: a [glacier](https://one-course.com/books/earth/1/en/chapter/27-ice-on-earth#def-g8-ice-on-earth-glacier) that retreats, a forest cut down, a town that grows, a [coast](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) or a [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) that moves.

**Exercise 32.10 ★★.**

A GPS satellite is about $20\,200\,\mathrm{km}$ away; its signal travels at about $300\,000\,\mathrm{km}$ per second. (a) How long does the signal take to arrive? Write the answer in scientific notation. (b) If a receiver’s clock were wrong by $1 \times 10^{-3}$ s, what error in the distance would that make? (c) What does this tell you about the clocks used in [satellite positioning](#def-g9-maps-of-the-earth-positioning)?

**Solution of Exercise 32.10.**

(a) $20\,200 \div 300\,000 \approx 0.067$ s $= 6.7 \times 10^{-2}$ s. (b) $300\,000 \times 10^{-3} = 300\,\mathrm{km}$. (c) A tiny error of time makes a huge error of distance: the clocks have to be extremely precise.

**Exercise 32.11 ★★★.**

On a flat [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) with a grid in kilometres, beacon A is at $(0, 0)$ and beacon B at $(10, 0)$. A receiver is $6\,\mathrm{km}$ from A and $8\,\mathrm{km}$ from B. (a) Show that the point $(3.6, 4.8)$ is $6\,\mathrm{km}$ from A and $8\,\mathrm{km}$ from B. (b) Give another point at the same distances from A and B. (c) A third beacon C is at $(0, 10)$, and the receiver is about $6.3\,\mathrm{km}$ from it. Which of the two points is the receiver? (d) Why does [satellite positioning](#def-g9-maps-of-the-earth-positioning) need several satellites?

**Solution of Exercise 32.11.**

(a) Distance to A: $\sqrt{3.6^2 + 4.8^2} = \sqrt{12.96 + 23.04} =
\sqrt{36} = 6$; distance to B: $\sqrt{6.4^2 + 4.8^2} = \sqrt{40.96 +
23.04} = \sqrt{64} = 8$. (b) $(3.6, -4.8)$, the mirror image across the line AB. (c) Distance from C to $(3.6, 4.8)$: $\sqrt{3.6^2 + 5.2^2} =
\sqrt{40} \approx 6.3$; to $(3.6, -4.8)$: $\sqrt{3.6^2 + 14.8^2} =
\sqrt{232} \approx 15.2$. The receiver is at $(3.6, 4.8)$. (d) One distance gives a circle (a sphere in space), two give two possible points; another distance is needed to choose.

**Exercise 32.12 ★★★.**

Africa’s mainland covers about 29 million $\mathrm{km}^{2}$ and Greenland about 2.1 million $\mathrm{km}^{2}$. (a) How many times larger is Africa? (b) On a Mercator [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), areas near the middle of Greenland, at about $72{}^{\circ}$ N, are enlarged about 10.5 times. Estimate the area Greenland seems to have. (c) Africa lies across the [equator](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-equator), where areas are enlarged little. Compare your answer to (b) with Africa’s area, and explain the wall [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) of the start of the chapter. (d) Which projection would you choose to show the sizes of the [continents](https://one-course.com/books/earth/1/en/chapter/6-the-globe-continents-and-oceans#def-g3-continents-and-oceans-continent) fairly?

**Solution of Exercise 32.12.**

(a) $29 \div 2.1 \approx 14$ times. (b) $2.1 \times 10.5 \approx
22$ million $\mathrm{km}^{2}$. (c) Greenland seems to cover about 22 million $\mathrm{km}^{2}$, close to Africa’s 29 million: on the Mercator wall [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map), the two look about the same size, although Africa is 14 times larger. (d) An [equal-area projection](#def-g9-maps-of-the-earth-projection).

## 32.7 Problem: A footpath across the Varden Hills

**Problem 32.1.**

Weekend problem — planners have drawn a footpath across the Varden Hills on the topographic map; the final answer is the length of the footpath in kilometres and its total climb in metres

The footpath starts at a farm S, goes down to a bridge B over the [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water), then climbs to a shelter W and on to the summit T. Each leg is straight and only goes down or only goes up. The [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) is at $1 : 50\,000$; the [altitudes](https://one-course.com/books/earth/1/en/chapter/9-the-physical-map-of-the-world#def-g4-world-physical-map-altitude) of S, B, W and T are written beside them.

![The footpath S–B–W–T on the topographic map of the Varden Hills (shown here reduced; on the original map at 1 : 50\,000 the legs measure 3.6, 2.5 and 2.35\, cm).](https://one-course.com/images/onecourse/chapters/earth-1/g9-maps-of-the-earth/fig-b4c41e113f97.svg)

*The footpath S–B–W–T on the [topographic map](#def-g9-maps-of-the-earth-topographic-map) of the Varden Hills (shown here reduced; on the original [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) at $1 : 50\,000$ the legs measure 3.6, 2.5 and $2.35\,\mathrm{cm}$).*

**Part I — The route on the map.**

1. At $1 : 50\,000$ , how many metres on the ground does $1\,\mathrm{cm}$ of the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) stand for?
2. On the original [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) , the leg S–B measures $3.6\,\mathrm{cm}$ . How long is it on the ground, in kilometres?
3. The legs B–W and W–T measure $2.5\,\mathrm{cm}$ and $2.35\,\mathrm{cm}$ . How long are they on the ground?
4. In which general direction does the path run from B to T?

**Part II — The climb.**

5. What is the [contour interval](#def-g9-maps-of-the-earth-contour) of the [map](https://one-course.com/books/earth/1/en/chapter/4-from-a-drawing-to-a-map#def-g2-drawing-to-map-map) ?
6. Which leg goes down? By how many metres?
7. By how many metres does the path climb on B–W, and on W–T?
8. What is the average slope of the leg W–T, as a percentage?
9. Why did the planners not draw the path in a straight line from S to T?

**Part III — The walk.**

10. Suppose a walker covers $4\,\mathrm{km}$ an hour on the flat and needs one more minute for every $10\,\mathrm{m}$ of climb. How long does the whole walk take?
11. Another walker follows the footpath the other way, from T to S. How many metres does she climb?
12. What is the total length of the footpath, in kilometres, and its total climb, in metres?

**Solution of Problem 32.1.**

**1.** $50\,000$ cm $= 500\,\mathrm{m}$.

**2.** $3.6 \times 500 = 1800\,\mathrm{m} = 1.8\,\mathrm{km}$.

**3.** B–W: $2.5 \times 500 = 1250\,\mathrm{m}$; W–T: $2.35 \times 500
\approx 1180\,\mathrm{m}$.

**4.** Towards the north-east.

**5.** $50\,\mathrm{m}$.

**6.** S–B goes down: $296 - 143 = 153\,\mathrm{m}$.

**7.** B–W: $335 - 143 = 192\,\mathrm{m}$; W–T: $544 - 335 =
209\,\mathrm{m}$.

**8.** $209 \div 1180 \approx 0.18$, about $18\,\%$.

**9.** A straight line from S to T would cross the [river](https://one-course.com/books/earth/1/en/chapter/2-landscapes-around-us#def-g1-landscapes-around-us-water) where there is no bridge; the path goes down to the bridge at B.

**10.** $1.8 + 1.25 + 1.18 \approx 4.2\,\mathrm{km}$ at $4\,\mathrm{km}$ an hour: about 63 minutes; climb $192 + 209 = 401\,\mathrm{m}$: about 40 minutes more. In all, about 1 h 43 min.

**11.** From T she goes down to B, then climbs from B up to S: $296 -
143 = 153\,\mathrm{m}$.

**12.** Length: $1.8 + 1.25 + 1.18 \approx \textbf{4.2 km}$; total climb: $192 + 209 = \textbf{401 m}$.