Badlands Transcript Table
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David Suzuki |
Heidi |
Amanda |
Michael |
Ashley |
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ItÕs amazing how the
landforms here really look like other things other than rocks. Do you notice that sometimes? |
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Yeah |
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Yeah |
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Yeah |
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ItÕs funny |
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As long as youÕve got a
good imagination |
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Well, weÕve noticed that
maybe, yeah, maybe letÕs go down this way. We noticed that the longer youÕre out in the badlands, and
the hotter it is, the more things look like things |
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Yeah-ha-ha-ha. YouÕre imagination gets looser, huh? |
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Well, it does. Some people claim it might be a kind
of hallucination – now watch out for the cactus. When we get around here, you
want to take a look around and see if thereÕs any landforms that look like
something that would be familiar to you, not just like a rock. |
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So what do you think that
landform over there is? Does
this one look, look like anything to you? |
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Hmm. Oh! That rock right there looks like a camel |
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OhÉnoÉ..thatÕs it! We actually have a name for this guy. We call him Fred the camelÉ.see the
humpÉ.see the big droopy lips pointing to the left. And if you look off in the back can you see anything else? |
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? |
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No. |
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IÕll give you a clue. Where are camels found? |
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Egypt. |
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Very good! |
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A pyramid |
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A camel and then a pyramid |
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Very good! |
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Has Fred changed that much
while youÕve been here Heidi? |
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Not that much although he
did get a bit of a facelift, heÕs lost his double-chin. But, uh, weÕre really concerned that
the caprock on the hump of Fred may fall off. That ironstone.
And if that falls off the hump could erode away very quickly. |
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But erosion is natural,
itÕs going to fade away over time. |
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David seems to direct conversation |
Fred is naturally going to
erode away. But if he ever lost his hump, all weÕd do is change his name to
Humphrey the camel. |
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Awwwwwwooooooo |
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Ha ha Ha Ha HA Ha |
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Ha ha |
Ha ha
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Huh ha |
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Child directs convo |
Sometimes it takes a
while. Hmmm Hmmm Hmmm |
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How are these gullies
formed? |
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Well, because there thereÕs
not much plants or because thereÕre not too many plants growing from them, we
donÕt get a nice protective layer and all this very soft sedimentary rock is
exposed every time it rains the outer surface weathers. Do you know how that happens? Have you, do you have any idea how
the weathered surface of a rock |
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By erosion? |
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Well, how does erosion
happen though? |
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By wind or water or ice
when it hits against the stuff it will fall |
By wind or water |
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Water is the key word
here. The rain hits the slopes,
it makes the clay thatÕs in the in the sedimentary rock here expand. And clayÕs a neat little mineral and
nice and flat and forms nice layers and when they rain, when it rains they
absorb the water and they expand and they disorient themselves and when it
stops raining they sort of try to get back into those nice layers, but they
donÕt. And they crumble and
crack. And with the next
rainstorm all that loose crumbled material washes down and washes into a dry
stream channel and washed down in to the Red Deer River and ends up somewhere
in Saskatchewan. And thatÕs how
these badlands form. You can see
all them a stream thatÕs working their way down the hills and thatÕs where
all the rain carries all of that material away |
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And?É.it leaves? |
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Bones and fossils |
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Right! |
So we have that to thank
for finding all the wonderful dinosaur fossils and all the other fossils
here. |
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When people come to
dinosaur provincial park they look around and they see all these hoodoos and
badlands and cactus and grass and they wonder: Gee, what did those dinosaurs eat? ThereÕs hardly anything around here
to eat! And then you have to say
that 75 million years ago things were a lot different. Here, we had rivers, we had forests
from mosses and cattails, very lush, very sub-tropical |
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Look at the ironstones
there |
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IsnÕt that neat? |
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Yeah! They have different
*** you can see |
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Hey look at
this! |
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Oh my gosh, Amada found a
bone! |
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Hey thatÕs great! |
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Good fossil! |
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Looks like a leg bone |
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YouÕre absolutely right
Michael. That is a tibia, which
is this part of the leg, of a duck-billed dinosaur. And if you add that to the foot, maybe give a foot for the
foot, add the tibia, which is a metre long because half of that oneÕs eroded
away, and then add the femur, our thigh bone |
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Look at that |
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What is it? |
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Oh, whatÕs that? |
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I think we made a discovery
here. |
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Hey, thatÕs very good
Amanda. That looks like a
vertebra is it? |
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Mmm hmm. You can see how round it is. ItÕs a vertebrae from the backbone of
a dinosaur. And if you look on
that side, you can even see where his spinal column went through |
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So that could have been the
tail of the animal. |
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It could have been the
caudal vertebrae, the vertebrae from the tail end. You canÕt see where the ribs were fused. |
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What kind of dinosaur do
you think it could be from? |
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Well I know for sure itÕs
from uh uh a plant eater or herbivore. |
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How do you know that? |
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Well you you can take a
look at the structure on the inside. |
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Mmm Hmm |
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