Badlands Transcript Table Format

 

 

 

 

David Suzuki

Heidi

Amanda

Michael

Ashley

 

ItÕs amazing how the landforms here really look like other things other than rocks.  Do you notice that sometimes?

 

 

 

 

 

Yeah

 

 

 

 

 

 

Yeah

 

 

 

Yeah

 

 

ItÕs funny

 

 

 

As long as youÕve got a good imagination

 

 

 

 

 

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

 

 

 

Yeah-ha-ha-ha.  YouÕre imagination gets looser, huh?

 

 

 

 

 

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.

 

 

 

 

So what do you think that landform over there is?  Does this one look, look like anything to you?

 

 

 

 

 

Hmm.  Oh!  That rock right there looks like a camel

 

 

 

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?

 

 

 

 

 

?

 

 

 

 

 

No.

 

IÕll give you a clue.  Where are camels found?

 

 

 

 

 

 

 

 

Egypt.

Very good!

 

 

 

 

 

 

A pyramid

 

 

 

 

A camel and then a pyramid

 

 

Very good!

 

 

 

 

Has Fred changed that much while youÕve been here Heidi?

 

 

 

 

 

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.

 

 

 

But erosion is natural, itÕs going to fade away over time.

 

 

 

 

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.

 

 

 

Awwwwwwooooooo

 

 

 

 

 

Ha ha Ha Ha HA Ha

 

 

 

 

 

Ha ha

Ha ha                            

Huh ha

Child directs convo

 

Sometimes it takes a while.  Hmmm Hmmm Hmmm

 

 

 

 

 

How are these gullies formed?

 

 

 

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

 

 

 

 

 

By erosion?

 

 

 

Well, how does erosion happen though?

 

 

 

 

 

By wind or water or ice when it hits against the stuff it will fall

By wind or water   

 

 

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

 

 

 

And?É.it leaves?

 

 

 

 

 

 

 

Bones and fossils

 

Right!

So we have that to thank for finding all the wonderful dinosaur fossils and all the other fossils here.

 

 

 

 

 

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

 

 

 

 

 

 

Look at the ironstones there

 

 

IsnÕt that neat?

 

 

 

 

 

 

Yeah! They have different *** you can see

 

 

 

Hey look at this!

 

 

 

 

 

 

Oh my gosh, Amada found a bone!

 

Hey thatÕs great!

 

 

 

Good fossil!

 

 

 

 

 

 

Looks like a leg bone

 

 

 

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

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Look at that

 

 

 

 

What is it?

 

 

Oh, whatÕs that?

 

 

 

 

 

I think we made a discovery here.

 

 

 

Hey, thatÕs very good Amanda.  That looks like a vertebra is it?

 

 

 

 

 

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

 

 

 

So that could have been the tail of the animal.

 

 

 

 

 

 

It could have been the caudal vertebrae, the vertebrae from the tail end.  You canÕt see where the ribs were fused.

 

 

 

 

 

 

What kind of dinosaur do you think it could be from?

 

 

Well I know for sure itÕs from uh uh a plant eater or herbivore.

 

 

 

 

How do you know that?

 

 

 

 

 

Well you you can take a look at the structure on the inside.

 

 

 

Mmm Hmm