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9

Introduction

I

cebergs are bits of glaciers that have broken off into the sea. An iceberg has over

twice as much ice under the water.

Under the Ice

The great land masses of the northern

hemisphere

form the

edges of the Arctic Ocean, with North America to one side,

and Eurasia on the other. The gaps are nearly filled by

islands such as Greenland and Spitzbergen. The North

Atlantic and Bering Strait are the only way in by ship. Early

explorers in small wooden vessels braved these passages.

In 1977, a Russian nuclear-powered icebreaker was

able to push its way right across the Arctic Ocean, smashing

a track through the sea ice and reaching the North Pole.

Submarines have traveled beneath the ice, surfacing near

the North Pole through cracks in the ice.

T

he Arctic Ocean is covered by sea ice most of the year. This ice is always moving

and cracks suddenly open or close.

Lines on the Earth

The globe can be divided up by lines

encircling the Earth starting at the

Equator, which is exactly around the

middle, and going north and south.

These are called lines of latitude. And

it can be divided by lines running from

the North Pole to the South Pole. These

are lines of longitude. The point where

lines of longitude and latitude cross

gives an exact description of a position

on the globe.

Latitude was known to early Greek

and Arab navigators. They made simple

devices to measure the angle of the

Sun above the horizon at midday.

A calculation showed how many degrees

they were away from the Equator. The

Equator is 0° and if you travel north

your latitude gradually increases to 90°

at the North Pole. For each degree you

travel about 68 miles (110 km).

Confusingly, the same thing happens

when you travel south from the Equator.

Latitude must always have north (N) or

south (S) added to show which side of

the Equator you are. So, London is

51°N, and the North Pole 90°N. But

Sydney, Australia, is 33°S, and the

South Pole 90°S.

To work out the exact position,

degrees are broken down into

minutes

.

Just as there are 60 minutes in an hour,

so there are 60 minutes in a degree.

L

ines of latitude and longitude on the globe.