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SPEAKER: Hi everybody!
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Today we're going to take a look at
topographic maps, and I'm going to
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teach you how to read them, and we're
going to go through some of the rules
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that will help them make sense.
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So right now you're looking at a
topographic map, and it probably
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looks like a bunch of squiggles and
lines and colours.
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Probably does not make too much sense
to you.
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Here's another topographic map, the same
thing, probably just looks like a bunch of
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brown squiggles with some other colours
thrown in there.
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By the end of the video, hopefully you're
going to be able to look at a map like this
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and you're going to be able to see the
topography, or the shape of the land.
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So a topographic map looks like this one
on the bottom, and basically what they do
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is they are a map that is able to show us
the elevation, the height above sea level,
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and the shape of the land by using these
lines, which are a kind of isoline,
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called contour lines.
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So on the top we have a landscape, you
can see there's a cliff over here, there's
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a hill over here.
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When you know how to read a topographic
map you can actually look at this and
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you can tell that there's a cliff over
here and there's a hill over here.
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Topographic maps have certain features
that you will always see, so let's go
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through 4 of those features.
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The first thing you're going to have to
figure out is what the contour interval is.
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When you look at a topographic map, you'll
notice that not every line is labelled.
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For example, this map, we have 300
labeled, we have 400 labeled.
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Those lines are a little bit darker than
the surrounding lines.
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Those numbered lines are called index
contour lines, the reason they only
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label some of them is because we don't
want the map to be too confusing,
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we don't want numbers everywhere.
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So, the first thing you have to do is
figure out what the contour interval is.
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In other words, what is the difference
between each pair of lines?
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Now, sometimes they'll tell you the
interval in a key under the map, but
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more often than not you're gonna have to
determine it yourself.
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So if we start with this map over here,
again we have 300 and it's
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either meters or feet or kilometers,
we're not sure with this map because it
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doesn't tell us.
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But we have 300 here, we have 400 here.
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So our task is to figure out what the
contour interval is, what are we gonna
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count by to get to 300 to 400?
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Now, hopefully, you're looking at this
and you're realizing, well, it's a
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difference of 100 and it's spread out
over 5 lines, so 100 divided by 5
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is 20.
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So for this map the contour interval
would be 20 units.
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So by units, we mean either miles or
kilometers or meters.
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Let's take a look at this top left map
over here.
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So we're going from 10, and then we're
skipping a line, it's not labeled, then
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we're going to 20.
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So that one's pretty easy, we're
counting by 5's.
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The bottom left map over here, okay, I
see that this contour line is labeled
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as 50, and this contour line up here is
labeled as 100.
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So, again, it goes from 50 to 100, which
is a difference of 50, and it's going
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5 lines between them, so 50 divided by
5 is 10.
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And then on the last map, this one's
pretty easy to figure out.
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We're counting by 25's, so our contour
interval would be 25 whatever unit is
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being used.
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Let's take a look at another map.
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Can you figure out on this map what
the contour interval would be?
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And feel free to pause the video.
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Well hopefully you realized that we're
going from 500 to 600, so we're going
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a difference of 100, and again we're
spreading it out over 5 lines so we're
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counting with an interval of 20 meters.
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Once you know the interval, you can now
figure out the elevation of any of the
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lines that are not labeled.
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So, for example, line A, right over
here, if we're counting by 20's, this
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line would be 540 meters.
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I want you to see if you could figure out
what the elevation of line B would be.
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So think about that for a second.
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And hopefully, you're realizing that
it's 580 meters.
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Okay, so again: contour interval, first
thing you want to figure out.
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The next thing that you'll notice on
most maps is somewhere there will be a
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compass rose, and that's important
because that will show you where North is.
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And normally when we look at a map, North
is usually up, but that is not always
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the case.
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You can see on this map that they're
telling you that north is facing the right
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side of the map, so North is really here
and then South would be over here.
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So you want to look at the compass rose,
you want to figure out where North is,
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where South is.
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So, let's go through some of the rules of
how to read a topographic map, okay.
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Going back to this first map that we
looked at earlier.
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I want you to notice when there's a cliff,
what the contour lines look like.
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So right over here, where the land is
steep, you probably notice that the
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contour lines are very close together,
and that's always going to be the case.
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Rule #1 is the closer the lines are, the
steeper the slope.
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Or, the opposite, the more spread out
the lines are, the gentler the slope.
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We can see on the side of this hill over
here we have a nice flat area, uh,
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right over here, the land is pretty flat
over here and on our contour map we can
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see the lines are spread apart much
further than they were over there.
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Now, on the back of your note sheet
you have this map.
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I want you to go ahead and I want you
to figure out where the steepest
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slope would be on this landscape.
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So we're looking for where the lines are
the closest.
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And pretty easy to see, the lines are the
closest somewhere near the top over here,
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okay, you can see how close together
they are.
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Go ahead and label that on your map,
on the back of your note sheet, that is
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the steepest slope.
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Okay, rule #2 deals with streams and
rivers: when a contour line crosses a
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river or a stream, the contour line
bends and forms a V.
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We can see that, again this is the map on
the back of your sheet, we have this
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middle river over here, and we can
see that, when the contour lines cross
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the river, they are bending and they are
forming V's.
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You always want to look for the V's
because the V's will tell you where the
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water is coming from.
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So the tip of the V shows you the
source of the water.
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So, in this case, the water is coming from
over here, this would be the source.
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And so the water is travelling from this
bottom edge of the map, the river is
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flowing this way towards the ocean.
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and it eventually goes into the ocean,
and that would be called the mouth
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of the stream, or the mouth of the river.
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Let's practice that skill a little bit,
that's an important skill.
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Let's take a look at this map, I want you
to see if you can figure out which way
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Long Creek would be flowing.
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Alright, so hopefully you noticed the
contour lines are bending, they're forming
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V's, and again the tip of the V shows us
the source of the water, so Long Creek is
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basically flowing towards the South,
slightly West, so South-West or South.
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Here's another one, let's look at
Trout Stream over here.
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See if you can figure out which way Trout
Stream would be flowing.
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Alright, again, we look at our contour
lines, they are bending, they are forming
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V's, the tip of the V shows us the source
of the stream, so the water is coming
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from here and it is flowing down this
hill into the river.
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We can see the same thing when we look at
the river.
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If we look at Cedar River we have this
one contour line here that forms a V,
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so we know the river is flowing this
direction towards the lake.
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Okay, so that's how we figure out which
way streams and rivers are flowing.
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Rule #3, you'll notice this landform over
here has 2 hills, when they are put on
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a topographic map, they look like
concentric circles that get smaller
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and smaller inside of each other.
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Rule #3 is that when there are rings of
circles that get smaller and smaller, that
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it represents a hill or a mountain.
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So let's look at the map, again, that's
on the back of your sheet.
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Let's figure out how many hills there are.
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So, I see one over here, so let's go ahead
let's label that somewhere, if I click-
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there we go!
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So there's a hill, can you find any
others?
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Well, you should, there are 2 others.
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We have one hill over here where there are
circles inside of circles.
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We have another one over here.
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This area down here on the bottom
right-hand corner is not a hill because it
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has these little marks on it, which we'll
get to in a couple of minutes.
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Okay, so again, anytime you see circles
within circles, it is a hill or a mountain.
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Now, what we have to do is we have to be
able to figure out how high the top of the
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hill or the mountain is.
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So to do that, what we would do, is we
would look at our map and we'd figure
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out what our contour interval was.
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Now, we looked at this one before.
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So we know that this one is counting by
20's.
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This top contour line is 400, which
means the top of the hill has to be
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higher than 400, but it's not going to
be as high as what the next line would be.
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So the next line, if there was one, would
be 420.
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So the top of this hill is somewhere between
401 and 419 meters, or whatever unit it is.
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So again, it can't be 400 and it can't be
420, it's gotta be in between.
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How about on this map?
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Again, we're counting by 20's, so if this
top line is 600 it means the top of the
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hill has to be somewhere above that, but
lower than what the next line would be.
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So it's got to be somewhere between 601
and 619, okay.
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So rule #4 says: the highest possible
elevation of a hill is just below the value
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of whatever the next contour line would
be, if there was a next contour line.
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So let's figure out what the height of
these hills, okay.
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So let's start with this one over here.
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So this contour line is 300, so let's
figure out what we're counting by.
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So here's 200, here's 300, so we're
counting by 20's.
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So if we come up the hill, so this is 300,
320, 340, 360, 380.
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So this small loop is 380, which means the
top of the hill has to be somewhere
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between 381 and 399, it can't be 400
because if it was 400 we'd have another
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line there, so the highest it could possibly
be is 399 meters.
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If we take a look at this hill we could
figure out the same thing, we could
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figure out the same thing down here.
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So, in this case, here's 200, so the
circle where letter Z is, that's 220.
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The next line would be 240, so the
elevation cant be that high it's got to
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be underneath that. So the highest
would be 239.
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Alright, moving on, rule #5, sometimes
we don't have a hill, sometimes the land
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dips down and forms a depression.
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So this is the top of a volcano, and
there's a crater up here, that's a
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depression, on a contour map we show
depressions by using these little marks
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that are called hachures or hatch marks.
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So, again, we'd find these where there's a
volcanic crater, or maybe where a meteor
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hit the Earth and left a crater.
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So on your map, we see that right over
here we have a depression, so these
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little hatcher marks tell us that the land
is going downwards, okay.
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Now the last rule, the 6th rule, tells us
how we would figure out how deep the
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bottom of the depression is, okay.
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So the first part of the rules says
that when you at a depression,
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the first hachured line,
so the outer circle,
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has the same elevation
as the previous contour line.
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So in other words,
this line over here
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has an elevation of 120 meters.
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So our first line with the
hatcher marks is also 120 meters.
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Then what we do is we
start to go downwards.
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So if this is 120,
it means the next line
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is going down by 20.
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So it is going to be 100.
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To figure out the deepest that this
depression could be,
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what we will do is --
we say 'if there was
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another line, what would that be?'
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So if there was another line
it would be 80.
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But that line is not there.
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So this depression can't go down to 80.
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So it has got to be a little
bit higher than 80.
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So the lowest possible elevation
is just above whatever the next
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contour line would be.
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Alright, so here is another
contour map.
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Hopefully you can use
some of the rules we
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went over and you can
figure out some of the topography.
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Some of the shape of the landscape.
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We are going to be doing
a lot of this in class.
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Have fun!