What's below the tip of the iceberg? - Camille Seaman

Have you ever heard the term,

"tip of the iceberg"?

You know that icebergs are mostly underwater,

their immense bulk hidden beneath the water.

But why is that so?

Well, the density of pure ice

is less than that of sea water.

Usually only 1/9 of the volume of an iceberg

is above the water.

The shape of the underwater portion

is difficult to discern

by looking at the above-surface portion.

This has led to the expression,

"tip of the iceberg."

Here are some thing you might not know

about the icy islands.

The life of an iceberg

begins many thousands of years

before it reaches the ocean.

Unlike sea ice or pack ice,

which form when the ocean freezes,

glaciers are made of fresh water.

For thousands of years,

these glaciers build layer upon layer of ice,

constantly compressing,

moving,

adding snow,

compressing,

and moving again

as they inch along like a frozen river.

It is the force of gravity

that pulls them towards the sea,

where a glacier may calve off to become an iceberg

or continue to spread up as an ice shelf

or an ice tongue.

Once an iceberg breaks away

from the glacier or ice shelf,

it will usually live for three to six years,

floating around, carried by the currents

and tidal movements of the ocean.

As it floats along,

it is battered by waves,

melts,

and smashes into land

and sometimes other icebergs.

Some icebergs are so unstable

that they have more dramatic ends,

heaving up,

collapsing,

and sometimes even exploding.

And as they fall apart,

many icebergs make all sorts of strange sounds.

When a piece of iceberg melts,

it makes a fizzing sound,

called Bergie Seltzer.

This sound is made when the water-ice interface

reaches compressed air bubbles trapped in the ice.

As this happens, each bubble bursts,

making a popping sound.

There are six official size classifications for icebergs.

The smallest icebergs are called growlers.

They can be up the size of your car

and are very dangerous for ships and boats

because usually they sit just at the waterline

where they are not easy to spot.

Next are the bergy bits

- yes, that is their scientific name -

which can be up to the size of your home.

The other four sizes are small,

medium,

large,

and very large.

So just how big is a very large iceberg?

Officially, any iceberg looming larger

than 270 feet high above sea level

and 670 feet long

is considered very large.

That's 27 stories of looming, blue ice.

And how do icebergs get that blue color anyways?

When snow on the glacier

is compressed over many hundreds of years,

the weight of the snow

forces the air bubbles out of the ice,

creating pure ice with very little air trapped inside.

This compression is seen

when the glacier calves,

creating a blue iceberg.

An iceberg that has not experienced

as much compression

and has a large amount of air and surface edges

reflects light as white.

Although they form in far northern or southern areas,

icebergs can float thousands of miles.

An iceberg from the Arctic floated

as far south as Bermuda.

Antarctic icebergs are mostly trapped

in the Circumpolar Current,

never giving them a chance to float north.

However, they have been known to interrupt

shipping lanes between Australia,

South America,

and South Africa.

For all their travelling,

many people think

that these slabs of ice are barren of life,

but these seemingly sterile ice slabs

also harbor their own complex ecosystems

and they shape the ecosystems

that they pass through.

They become mobile, floating ecosystems.

Even in the coldest seas,

icebergs are always melting,

at least a little bit.

This melting has a major impact

on the ocean around an iceberg.

The fresh water from the berg

creates a pool of fresh water

that can extend a nautical mile away from the iceberg.

This water is colder than the surrounding sea water,

and the temperature variation creates thermal currents

in the vicinity of the iceberg.

Life thrives on and around an iceberg.

Young icefish hide in small ice holes to avoid predators,

while a variety of invertebrates,

like jellyfish and siphonophores,

congregate in the area.

Many of them come to feed on krill,

tiny shrimp-like creatures.

Snow petrels nest on the icebergs

and feed on the sea life nearby.

Whales and seals and penguins seem to like them too.

And even now that you know all this,

we're still at the tip of the iceberg.

There are all sorts of things

we don't know about icebergs.

Perhaps you'll be the one to see a little deeper.