
How
Our Island Was Made
Our
island is really just the top of some mountains. There are all of these
mountain ranges that run north and south along our side of America. See
on the map if it is showing now. One of the mountain ranges is partly covered
by the ocean. This is called the Insular Range. Insular
just means islands and so it is the tops of these mountains that make up
all the islands you see along the coast.
Why
We Have So Many Mountains
Scientists
that study the earth are called geologists. Geologists think they know
why we have so many mountains. They think that the center of the earth
is melted rock and that there are hard plates of the earth's crust floating
and moving around on it. In some places those plates bump into each other.
This is what they think is happening on the west coast of America. This
makes two kinds of mountains.
Folded
Mountains
When two
plates meet they push into each other and the weaker one begins to fold
and bend. The heavier one begins to slide under the lighter one.It looks
a bit like this.


When
the heavy plate goes under, it makes the plate on top get folds and wrinkles.
You can try this by sliding a hard book under the edge of a table cloth
or the blanket on your bed. See how the softer thing makes folds? Well
if those folds are softer rock and very big, then you get mountains. When
you pushed your book under, did you notice since your push was all from
one side, the wrinkles or folds in the cloth all went one way....well that
is what happened here. The push is like this -----> against the
coast so the wrinkles or mountains all go from north to south.
Volcanoes
The plate
that is trying to get under the other one must go deeper and deeper into
the earth and as it does that it starts to get hot and melt. You can guess
what happens then! A volcano! Again see the pictures.
Another
kind of mountain!
Ice
About
18,000 years ago there was an Ice Age and big glaciers covered most of
this continent. We still have a glacier near where I live. Here it is.
It is called the Comox Glacier. It looks like this even on our hot summer
days.
Glaciers
scrape at the sides of the mountains and make them very steep and jagged
like this.
We have
a lot of sharp jagged mountains like this on our island now that most of
the glaciers are melted.
Do you remember that I explained
that we live near a place where one part of the earth's crust is pushing
under another part like this:
Well you
must remember these are great hunks of rock not nice smooth dinner plates.
They are rough. That means sometimes they get stuck. They just keep pushing
together and the mountains bulge up a bit till suddenly they get unstuck....When
you push a big piece of furniture and it finally moves, it is a jerky move,
right? Well that is what happens when a plate that has been stuck suddenly
moves. All the earth on top of it shakes...We call it an earthquake.
Have
you head of big earthquakes knocking down buildings? Well that is not all
they knock down. On Vancouver Island we do not have many big buildings
but we have some big mountains. Earthquakes have knocked down pieces of
our mountains sometimes. This is Mt. Colonel Foster. See the funny looking
section on the right hand side. That is a landslide. A whole hunk of the
mountain got shaken loose and fell down in a heep of rubble.
Water
Did you
know that water can wear away stone and rock? It happens very slowly but
in time where the waves have come crashing in against the side of a mountain
the bits of rock break off and finally a cliff is formed. Some rocks are
harder than others. If there is a softer section the waves will wash that
part away faster and so you might get a cave or funny looking little bowls
in the rock. In this picture the rocky shore looks a bit like the pictures
you see of the moon up close. See the cave starting to form?
More
on Geological Formation
Earth
Quake Activity in the B.C. South West
© 1998 vanisle@oocities.com
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