Dinosaurs: What They Stepped In

Slides:



Advertisements
Similar presentations
The people Look for some people. Write it down. By the water
Advertisements

Vertebrate History in Rocks
The Ocean Floor Anything which looks like this is a link to the next page! Next.
SUCCESS Pull out planners Absent students will be taking their quizzes = – NO TALKING.
Table of Contents Fossils The Relative Age of Rocks Radioactive Dating
Fossils & History of the Earth
Landforms of the United States Brenda Davis June 2010.
Landforms of the United States
Cross bedding and other indicators in sedimentary rocks What is so important about understanding how these sedimentary rocks look the way they do?
A Trip Through Geologic Time
HISTORY OF LIFE Chapter 14. The Record of Life Ch. 14, Sec 1.
Unit 11 – Living on Earth I: Evolution and Extinction Dinosaurs: Where They Lived, and How They Died Photos by R. Alley or as indicated. The Green River.
10/10/09. Sedimentary rocks are layered rocks. The gray on the bottom is the oldest part of the rock. Sandstone transformed into brown rock. The rocks.
Earth’s History Section 4.1
Earth History: Record in the Rocks The geologic history of Earth can be “read” from rocks if you know what to look for. In this presentation, you will.
I am ready to test!________ I am ready to test!________
Fossils. How a Fossil Forms  Most fossils from when living things die and are buried by sediments.  The sediments slowly harden into rock and preserve.
Earth’s History But…there is no book! Oh…rats…. Why do we want to know Earth’s History? Catastrophic Events –If it has happened before, can it happen.
Unit 2 – Making Mountains – Death Valley Geosc. 10 Death Valley Take a stroll through one of the lowest pieces of land in the Western Hemisphere (282 feet.
Unit 7 – Bear Meadows, The Rockies and Greenland What do Rocky Mountain, Bear Meadows, and Greenland have in common? Hint: It’s cold up there on top of.
Evolution and Fossils.
Unit 8 – Coasts and Sea-level Changes (Cape Cod & Acadia) Sept. 18, 1999 Landsat.
Grade 5 – Unit 6, Lesson 2 Lesson Synopis In this lesson, students will focus on how fossils are evidence of past life rather than creating models of fossils.
Madison Bryce 1. Dinosaur National Park Dinosaur National Park is a desert located within both Colorado and Utah. With its amazing wall full of the coolest.
How a Fossil Forms - Fossils
Unit 11 – Living on Earth I: Evolution and Extinction Florissant Fossil Beds National Monument-- Gnattily dressed Photos by National Park Service (indicated)
SOLHEIMAJÖKULL FROM 1998 TO Solheimajökull is an outlet glacier from the Mýrdalsjökull ice cap. Under the ice cap is the volcano Katla which erupts.
Fossil and Soil Review Fossils #1Fossils #2Fossils #3Fossils and SoilSoil
Unit 9 – Which Way Up? Sedimentary rocks, Waterton Lakes-Glacier International Peace Park. Colored lines follow a folded layer. Right-side-up at the green.
The WORLD according to Gary Parker! OR… How to misrepresent the evidence, invent “facts”, and totally mislead people! Especially Children! 
Sight Words.
Fossils Links to the past. What is a fossil? A fossil is any evidence that life once existed. This includes: –Footprints –Marks and Impressions –Parts.
High Frequency Words.
What is a fossil? What do fossils tell us?
Fossils.
What is Evolution? Unit 6: Seventh Grade.
Understanding Geologic History What is it and Why do we care?
Geological Features of the Earth How do natural processes affect geologic features? How do natural processes affect geologic features?
Earth’s Past. Determining Relative age Relative age – the age of the object in relation to the age of other objects – No actual age in years given Law.
Looking at Fossils Chapter 3 Section 4 p Vocabulary:
Ch. 6-1 Fossil Evidence of Evolution
By:Taya Howell. What Is a Fossil? Fossil- remains or impression can be a shell, bone, hole, or a footprint Process of Fossils Dead organisms Mussels and.
Monday, May 2 nd Big Idea: What are fossils? Daily target: I can examine fossils and interpret evolution and time periods. Homework: Hand adaptation (5/3)
Geologic Time Scale. Measuring Time The Earth has existed for 4.6 billion years The Earth has existed for 4.6 billion years The geologic time scale divides.
Created By Sherri Desseau Click to begin TACOMA SCREENING INSTRUMENT FIRST GRADE.
Mississippi River Valley Fossils Around the Twin Cities Summit Avenue and Great River Blvd, St. Paul.
Fossil and Extinction What are the Different Types of Fossils and How Do They Show Evidence of Evolution and Extinction?
By: Julian Koolen. About Dinosaur Ridge Dinosaur Ridge is a museum in Morrison, Colorado where tourists can view footprints of dinosaurs and learn about.
Landforms of the United States
Earth Formation & Early History
Fossils.
Geologic Time Scale.
Chapter 9 Study Notes A View of Earth’s Past.
Geologic Time Scale.
Ocean Floor.
Write the landform beneath the picture
Deeper, and Deeper, and Deeper
Geological time, Fossils, & Dinosaurs
Landforms of the United States
Precambrian Era Paleozoic Era Mesozoic Era Cenozoic Era
Unit 10 Lesson 2 What Was Ancient Earth Like?
Have a seat quickly and quietly
Unit 2, Lesson 2 Earth’s History
Mar 4, The Earths Beginning million years ago - Precambrian Era
The. the of and a to in is you that with.
The of and to in is you that it he for was.
Read the phrases before the slide changes for fluency practice.
Chapter 9: A View into Earth’s Past
Looking at Fossils Chapter 3 Section 4 p Vocabulary:
Presentation transcript:

Dinosaurs: What They Stepped In A Virtual Tour of Dinosaur Ridge All pictures in this show are by Dr. Alley unless noted; some of the pictures here feature PSU graduate and noted scientist Matt Spencer.

Dinosaur Ridge, just west of Denver, Colorado, is part of the Morrison Fossil Area National Natural Landmark as designated by the National Park Service. In the Cretaceous Period of the Mesozoic Era, about 100 million years ago, the area that is now the Ridge sat on the edge of the great Interior Seaway that extended eastward across Kansas, and connected the Gulf of Mexico with the Arctic Ocean. Sediments were deposited, hardened, then tipped up (picture at right) as the Rockies were raised just to the west. The dinosaur trackway (lower right) is the big attraction at the Ridge, although there is lots more to see (including modern rabbits).

The dinosaur tracks really are spectacular The dinosaur tracks really are spectacular. Various dinosaurs walked across the muddy surface, probably heading for a water hole. The little sign (bottom of the picture on the left) points to a three-toed Ornithomimus track. A picture of one of the larger Iguanodon tracks is shown below, with kids’ hands for scale (from the Friends of Dinosaur Ridge web site http://www.dinoridge.org/gallery/full36.html)

Shown here are various animal burrows from a shallow-water deposit near the dinosaur trackways (with an interpretive sign below to give you an idea of the scale). Modern muds similar to these are commonly burrowed by creatures looking for food or avoiding enemies. After a mud layer is deposited, it usually takes a while for the mud to stabilize, and critters to move in and burrow the heck out of the mud, as seen here.

A careful examination of the burrowed rocks from the previous picture shows that various critters were stirring the mud, including big ones (pink arrow) and little ones (blue arrow). Not every layer gets burrowed--if there is too little oxygen to support critters, or too little for critters to eat, or the layer is buried too rapidly, then burrowing may be restricted or absent. Here, the heavily burrowed layer (far right, green arrow) is buried under a moderately burrowed layer covered with ripple marks (the two red arrows in the upper left of the picture point along ripple-mark crests). In turn, the rippled layer was buried by another layer, which was buried by another… (see next slide).

The previous slide showed a burrowed layer buried beneath a rippled layer. Here, a different rippled layer was covered up by yet another rippled layer. (If you don’t see it, the next slide adds some annotations to help.)

In case you didn’t see the features in the previous slide, the solid pink line divides the layer on the bottom (which in the picture is to the upper right) from the layer on top (which in the picture is to the lower left). The crests of two ripples on the layer on the bottom are marked by the light-blue dot-dash lines, and the crests of five ripples on the layer on the top are marked by the dark-blue dotted lines.

As interesting as ripples and burrows may be, most people go to Dinosaur Ridge to see dinosaur tracks.

And, here are a few more pictures of the main trackway at Dinosaur Ridge. Many more trackways have been reported along the Front Range near Denver, and there are other tracks at Dinosaur Ridge in other rock layers (some coming later in this show), but this is the easiest one to see.

There is even more interesting stuff at Dinosaur Ridge There is even more interesting stuff at Dinosaur Ridge. On the left is a dinosaur bone, still in the rock (lens cap for scale). Above, the yellow-orange-ish layer is volcanic ash, from some very large and nearby eruption, sandwiched between more-ordinary sedimentary rocks.

On the other side of Dinosaur Ridge from the “main” trackway seen earlier, you can see dinosaur tracks edge-on, such as this one indicated by Dr. Alley. The next picture includes an outline of the track.

“Artistic” rendition of dinosaur pulling foot out of mud after making track at Dinosaur Ridge, near Denver.

Matt Spencer with dinosaur track, Dinosaur Ridge, near Denver Matt Spencer with dinosaur track, Dinosaur Ridge, near Denver. The next picture is a close-up with this track outlined.

Close-up of previous picture, with dinosaur track outlined.

Dinosaurs didn’t walk on the ceiling Dinosaurs didn’t walk on the ceiling. We just turned the previous picture upside-down, but if you found a track this way in nature, you should conclude that the rock has been turned upside-down.

A long and fascinating story links the dinosaurs tromping on mud when Denver was a coastal city, and this mountain goat looking down toward Denver from Mt. Evans. The giant meteorite 65 million years ago that killed the dinosaurs opened their “jobs” to others, and evolution filled those jobs with the creatures we now know and enjoy.