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Dinosaur
State Park Arboretum
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This is a great place to take kids and and adults alike. After all, who doesn't love dinosaurs? This park in the Connecticut River Valley was discovered by accident during a construction dig and fortunately, preserved as a State Park for our enlightenemtn and viewing pleasure. There are several trails with tracks around the park that are worth looking at. The main attraction, of course, is the dome shaped arboretum which houses a number of preserved dinosaur prints and has a bunch of instructional material on the geology of Connecticut and how these tracks were preserved. The video's are definately worth watching as well. They are filled with informational gems of the geological variety. There are a number of different preserved dilophosaurus tracks here made by several different dinosaurs. There are four sites which can provide you with a wealth of information on this park: It's Wikipedia entry, the Connecticut DEP entry, Wesleyan University's Dinosaur State Park field trip page and the Official Site.
Instead of repeating all that information here I put together a few pictures and a ditto I hope to hand out to students when I become a teacher. It asks a host of interesting things about Connecticut and makes sure you have a firm grasp on the basic message of Dinosaur State Park. Go to the park with these questions in mind and look for their answers. Of course, my answer key follows the questions here. If you want to learn about the CT River Valley and be able to know why many footprints are preserved in Dinosaur State Park but no bones are, read on. Just remember the store in the arboretum is closed on Monday. That probably means that the exhibit is closed as well and only the trails are open to the public.You don't want to come here just for the trails. The arboretum is awesome.
Dinosaur State Park Worksheet
Geologic Time Walk:
Questions to Answer: [1] Our state has highlands in the east and west with a lower lying river valley in the middle (aka the Connecticut River Valley). Why does CT have the geology that it does? [2] The surface of the earth is always changing. Even the continents are moving at the rate of fingernail growth (2" per year). Around 200 mya what latitude was Connecticut situated at and next to what present day landmass? [3] How does the existence of the CT river valley support the idea of continental drift and plate tectonics? [4] When we step into the sand at an ocean our prints are washed away. Why after millions of years are these footprints there? Hint: What conditions are required for the preservation of a dinosaur track? (give at least 4) [5] The CT river valley in central Connecticut extends from New Haven (southern coast) all the way up into Massachusetts. The footprints tell us that dinosaurs permeated these lands millions of years ago. Why are there lots of footprints at Dinosaur state park but no bones of ancient dinosaurs? Hint: What conditions are required for bone preservation? [6] In Geologic Terms, what is the Connecticut River Valley? [7] What is the difference between a negative and positive print? [8] Dinosaur means "terrible lizard". Why is this a misnomer? [9] At one time some dinosaur experts thought the dinosaurs were slow, stocky, tail dragging beasts (like Godzilla). How do the track-prints at Dinosaur State park allow paleontologists to dispel with such theories? [10] Why would some dinosaurs have slow reaction times? [11] What type of rock
is found in Dinosaur State Park? How old is it and how did it form? PS: Don't forget to check
out the Demonstration room and the full dinosaur skeleton with visible
bones in its ribcage (its lunch!)!
Teacher's Answer Key:
---Tensional forces stretch
and thin the crust
[A3] Rift valley basins are found all the way from Nova Scotia to the Carolinas and similarly in corresponding West African areas. [A4] Footprint preservation requires a number of conditions: ---Good track impressions are
usually found near an ancient shore Lithification is stone making: unconsolidated sediments are compacted (or cemented) into sedimentary rocks. Pangaea the super continent broke and a rift valley formed in Central CT. The surrounding highlands were weathered and eroded sediments down into the river basin which contained water and this made for soft shores. The right conditions were met in certain areas that dinosaurs walked in and these tracks were allowed to briefly dry without disturbance. They were covered by sediments brought from weathering or rising water levels bringing mud. Surface fault eruptions continually reburied material in the rift valley which allowed for the sedimentation of the prints. They were then later found on a construction site in Connecticut. P.S. These tracks were made by a dilophosaurus in case you forgot. [A5] The processes that lead to good track preservation are harmful to bone preservation and vice versa. In other words, good conditions for one are poor conditions for the other. As the answer to question four entails, track print preservation requires slow covering with sedimentation. Good bone preservation required the opposite: ---Rapid burial under thick
deposits (e.g. flash flood of a mountain stream) Thus, conditions for bone formation will not allow track prints to preserve. We could find bones in the CT river valley as it may have flooded and later been buried by surface fault eruptions but they should not be found in the same layer or coincident with track-prints. [A6] A continental rift valley. [A7] A positive print is the depression made by the dinosaur (the indentation). A negative print is the sediment that is pulled out from that print that makes the shape of the print. [A8] Dinosaurs are reptiles, not lizards. [A9] There are no tail indentations anywhere near the track prints. If these dinosaurs dragged their tails then we should see such indentations. Rather, dinosaurs did not walk like Godzilla, but leaned forward a bit with their tails in the air. [A10] Reaction time depends on information being sent to our brain. It would take that information a lot longer to reach the brain of something a third the size of a football field than a human. The horned stegosaurus had the brain the size of a walnut. The herbivorous Brachiosaurus was humungous ( ate giant trees for lunch! ) but had the brain the size of a kitten and a real slow reaction time (maybe a minute). Thus it and most all dinosaurs could easily classify as big dumb dumbs. [A11] The rock is of the east Berlin formation and is about 200 mya. It is sedimentary, being lithified sand and mud that most likely was deposited in the lakes of the river valley/rift valley to the weathering of the eastern and western highlands of Connecticut. |
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Each Foot along the 90 foot walkway represents 50 million years of Geologic Time! |
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You'll find a room filled with informational pictures like these:
It will show you different types of geological features and also yield answers to many questions such as why bones are not found when so many well preserved dinosaur footprints exist here. |
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One of the Crown Jewels of the Information Room: Complete Dinosaur Skeleton with other bones in its ribcage (its lunch!)
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The Arboretum
tracks and exhibit recreations (there is an ancient forest recreation
on the other side).
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One of
the recreated figures.
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Real Dinosaur
Footprints!!!
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Picture
of part of a trail outside.
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