Image 1: Close up of fossilized dinosaur foot prints from Dinosaur Ridge, CO. 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.
Image 2: Two images. Left: Outcropping of rock that has been tipped up as the Rockies were formed. Second: Fossilized dinosaur prints. 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 and 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 quite a bit more to see (including modern rabbits).
Image 3: Dinosaur footprints. An insert image shows one of the larger Iguanodon tracks with three kids hands in it for scale. 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 in the inset, with kids’ hands for scale.
Image 4: Various animal burrows from a shallow-water deposit near the dinosaur trackways. Shown here are various animal burrows from a shallow-water deposit near the dinosaur trackways (with an interpretive sign 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.
Image 5: Two pictures. Top: Burrowed rock shows burrows from big and small animals. Bottom: Heavily burrowed area buried by a moderately burrowed area. 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).
Image 6: Close up of a rock showing a rippled layer covered up by another rippled layer. 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.)
Image 7: Close up of a rock showing a rippled layer covered up by another rippled layer. 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.
Image 8: Dinosaur tracks. As interesting as ripples and burrows may be, most people go to Dinosaur Ridge to see dinosaur tracks.
Image 9: Three close ups of 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.
Image 10: Two images. Left: Dinosaur bone still in the rock. Right: Layered rock with a orange ayer in the middle. The yellow-orange-ish layer is volcanic ash, from a very large eruption nearby, which is sandwiched between more-ordinary sedimentary rocks.
Image 11: Dr. Alley standing next to an edge-on dinosaur track. 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.
Image 12: Edge-on dinosaur track.
Image 13: Another Edge-on dinosaur track. Matt Spencer with dinosaur track, Dinosaur Ridge, near Denver. The next picture is a close-up with this track outlined.
Image 14: close up of the previous edge on dinosaur track with the track outlined.
Image 15: Previous image turned upside down showing what a dino footprint would look like if the rock turned upside down. 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.
Image 16: Mountain goat. 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 65 million years later. The giant meteorite that killed the dinosaurs left their “jobs” open to others, and evolution filled those jobs with the creatures we now know and enjoy.