Look at the layers
of the structure.
They are one on top of the other. How do you think they formed? Hint - remember sedimentary rock. |
A place called Smoky Hill
Chalk in Kansas used to be covered
by a huge sea.
What
do see through
the middle of North America? Between 87 and 82 million
|
This shallow ocean
was home to a variety of marine animals which are now
extinct. These included
giant clams, rudists, crinoids, squid, ammonites,
numerous sharks and bony
fish, turtles, plesiosaurs, mosasaurs ,
Pteranodons and even several
species of marine birds. Although it seems
unlikelythat you would find
dinosaur fossils in the middle of the Western
Interior Sea, a number of
them (mostly hadrasaurs) have been collected from
the Smoky Hill Chalk, and
their remains have been well documented. The bodies
of these dinosaurs must
have somehow floated hundreds of miles into the seaway before sinking to
the bottom. It's possible that they died during a catastrophic flood
and were carried out to
sea on a large, tangled mat of trees and other vegetation.
Over a period of about five
million of years, the remains of many of these animals
were preserved as fossils
in the soft, chalky mud of the sea bottom. When this mud was compressed
under thousands of feet overlying shale, it became a layer of chalk that
is more than 600 feet thick. Most of the massive chalk formation that once
covered Kansas, however,
has been eroded away over the last 60 million years and
is now exposed only in a
relatively small area in the northwest corner of the State.
This part of Kansas is now
known as the Smoky Hills.
During the last one hundred
years or so, the Smoky Hill Chalk has been the source
of thousands of fossil specimens,
many of which are on exhibit today in museums around the world.
Some giant clams:
Inoceramus
grandis - A common, giant
bivalve in the lower Smoky Hill chalk. (About 18 inches in diameter) How large is this clam
shell?
|
3. Platyceramus platinus:
A very large
clam shell that occurs throughout the
chalk, sometimes reaching
more than four feet in diameter. As the name implies,
these shells are flat and
often very thin. While alive, the interior served as shelter
for schools of small fish
which are sometimes preserved inside as fossils pressed
into the shell (near the
middle of the chalk).
How large is this clam
shell fossil?
What is sometimes found
preserved as a fossil inside?
Smoky Hill Chalk today:
The
Smoky Hills change from east to west. The eastern hills are capped with
sandstone. This means the top layer of rock is sandstone with other layers,
or beds, of rock underneath.
The sandstone was formed from sediment carried by rivers into the shallow seas from the east. Mushroom Rocks, in Ellsworth County in central Kansas, are concretions of Dakota Formation sandstone, originally deposited during the Cretaceous Period, about 100 million years ago. |
When the seas dried up in
the western part of the Smoky Hills region, thick layers of sediment were
left behind. The sediment
was later buried between 1,000 and 2,000 feet underground and formed into chalk. Some areas of the chalk bed were later exposed by erosion. Today, much of the chalk at the surface has been eroded away by water. In some areas, tall, steep-sided chalk formations were left standing after |
Where would you expect
to find the most primitive and oldest fossils? Would they
be at the lowest layers
or at the top layers of sedimentary rock formations.
Why?
Why are most fossils the remains of animals who lived in or near the water?
Look at some pictures of sedimentary structures: https://www.angelfire.com/nj/PflommScience/sedstruct1.html
Material courtesy of Oceans
of Kansas
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