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Climate 101: Glaciers | National Geographic


glaciers have been shaping our world for

glaciers have been shaping our world for millions of years but as climate change

millions of years but as climate change

millions of years but as climate change warms the planet glaciers are

warms the planet glaciers are

warms the planet glaciers are disappearing

disappearing

disappearing not only altering the landscapes they

not only altering the landscapes they

not only altering the landscapes they leave behind but changing our oceans

leave behind but changing our oceans

leave behind but changing our oceans weather and life on Earth as we know it

weather and life on Earth as we know it

weather and life on Earth as we know it a glacier is a huge mass of ice that

a glacier is a huge mass of ice that

a glacier is a huge mass of ice that moves slowly over land glaciers can be

moves slowly over land glaciers can be

moves slowly over land glaciers can be classified into two general groups

classified into two general groups

classified into two general groups alpine glaciers and ice sheets alpine

alpine glaciers and ice sheets alpine

alpine glaciers and ice sheets alpine glaciers form on mountain sides and move

glaciers form on mountain sides and move

glaciers form on mountain sides and move downwards through valleys sometimes they

downwards through valleys sometimes they

downwards through valleys sometimes they create valleys by pushing dirt soil and

create valleys by pushing dirt soil and

create valleys by pushing dirt soil and other materials out of their way these

other materials out of their way these

other materials out of their way these glaciers are found on every continent

glaciers are found on every continent

glaciers are found on every continent except Australia ice sheets

except Australia ice sheets

except Australia ice sheets unlike alpine glaciers are not limited

unlike alpine glaciers are not limited

unlike alpine glaciers are not limited to mountainous areas they form broad

to mountainous areas they form broad

to mountainous areas they form broad domes and spread out from their centres

domes and spread out from their centres

domes and spread out from their centres in all directions as ice sheets spread

in all directions as ice sheets spread

in all directions as ice sheets spread they cover everything around them with a

they cover everything around them with a

they cover everything around them with a thick blanket of ice including valleys

thick blanket of ice including valleys

thick blanket of ice including valleys planes and even entire mountains the

planes and even entire mountains the

planes and even entire mountains the largest ice sheets are called

largest ice sheets are called

largest ice sheets are called continental glaciers they cover vast

continental glaciers they cover vast

continental glaciers they cover vast areas including most of Antarctica and

areas including most of Antarctica and

areas including most of Antarctica and the island of Greenland glaciers can

the island of Greenland glaciers can

the island of Greenland glaciers can form over years when more snow piles up

form over years when more snow piles up

form over years when more snow piles up and melts soon after falling the snow

and melts soon after falling the snow

and melts soon after falling the snow begins to become denser and more tightly

begins to become denser and more tightly

begins to become denser and more tightly packed when new snow falls and buries

packed when new snow falls and buries

packed when new snow falls and buries the previous year’s snow the bottom

the previous year’s snow the bottom

the previous year’s snow the bottom layer becomes even more compressed the

layer becomes even more compressed the

layer becomes even more compressed the dense grainy ice that has survived one

dense grainy ice that has survived one

dense grainy ice that has survived one year’s melt cycle is called fern when

year’s melt cycle is called fern when

year’s melt cycle is called fern when the ice grows thick enough the fern

the ice grows thick enough the fern

the ice grows thick enough the fern grains fuse into a huge mass called

grains fuse into a huge mass called

grains fuse into a huge mass called glacial ice the glacier may begin to

glacial ice the glacier may begin to

glacial ice the glacier may begin to move under its own weight through a

move under its own weight through a

move under its own weight through a process called compression melting

process called compression melting

process called compression melting as they move glaciers erode or wear away

as they move glaciers erode or wear away

as they move glaciers erode or wear away the land beneath and around them when

the land beneath and around them when

the land beneath and around them when glaciers began their latest retreat less

glaciers began their latest retreat less

glaciers began their latest retreat less than 20,000 years ago they left behind

than 20,000 years ago they left behind

than 20,000 years ago they left behind many landscape features such as lakes

many landscape features such as lakes

many landscape features such as lakes valleys and mountains glaciers provide

valleys and mountains glaciers provide

valleys and mountains glaciers provide people with many useful resources

people with many useful resources

people with many useful resources glacial till provides fertile soil for

glacial till provides fertile soil for

glacial till provides fertile soil for growing crops and deposits of sand and

growing crops and deposits of sand and

growing crops and deposits of sand and gravel are used to make concrete and

gravel are used to make concrete and

gravel are used to make concrete and asphalt many rivers are fed by the

asphalt many rivers are fed by the

asphalt many rivers are fed by the melting ice of glaciers the most

melting ice of glaciers the most

melting ice of glaciers the most important resource provided by glaciers

important resource provided by glaciers

important resource provided by glaciers is freshwater Earth’s average

is freshwater Earth’s average

is freshwater Earth’s average temperature has been increasing

temperature has been increasing

temperature has been increasing dramatically for more than a century

dramatically for more than a century

dramatically for more than a century glaciers can act as indicators of global

glaciers can act as indicators of global

glaciers can act as indicators of global warming and climate change

warming and climate change

warming and climate change in several ways melting ice sheets

in several ways melting ice sheets

in several ways melting ice sheets contribute to rising sea levels as ice

contribute to rising sea levels as ice

contribute to rising sea levels as ice sheets in Antarctica and Greenland melt

sheets in Antarctica and Greenland melt

sheets in Antarctica and Greenland melt they raise sea levels adding fresh water

they raise sea levels adding fresh water

they raise sea levels adding fresh water to the ocean every day the loss of

to the ocean every day the loss of

to the ocean every day the loss of glacial ice also reduces the amount of

glacial ice also reduces the amount of

glacial ice also reduces the amount of fresh water available for plants and

fresh water available for plants and

fresh water available for plants and animals on land large editions of fresh

animals on land large editions of fresh

animals on land large editions of fresh water change the ocean ecosystem as well

water change the ocean ecosystem as well

water change the ocean ecosystem as well as ocean currents

as ocean currents

as ocean currents additionally less salt in the ocean

additionally less salt in the ocean

additionally less salt in the ocean could disturb the Gulf Stream

could disturb the Gulf Stream

could disturb the Gulf Stream drastically changing the weather on land

drastically changing the weather on land

drastically changing the weather on land as well since glaciers are so sensitive

as well since glaciers are so sensitive

as well since glaciers are so sensitive to climate change the increased speed of

to climate change the increased speed of

to climate change the increased speed of glacier melt is an early warning system

glacier melt is an early warning system

glacier melt is an early warning system for the rest of the planet

for the rest of the planet

for the rest of the planet and if global warming goes unchecked

and if global warming goes unchecked

and if global warming goes unchecked many if not all alpine glaciers could

many if not all alpine glaciers could

many if not all alpine glaciers could disappear completely

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