File:Eubrontes giganteus (dinosaur footprint) (Longmeadown Formation, Upper Triassic to Lower Jurassic; Mt. Tom Dinosaur Tracksite, Connecticut River Valley, Massachusetts, USA).jpg
![File:Eubrontes giganteus (dinosaur footprint) (Longmeadown Formation, Upper Triassic to Lower Jurassic; Mt. Tom Dinosaur Tracksite, Connecticut River Valley, Massachusetts, USA).jpg](https://upload.wikimedia.org/wikipedia/commons/thumb/6/60/Eubrontes_giganteus_%28dinosaur_footprint%29_%28Longmeadown_Formation%2C_Upper_Triassic_to_Lower_Jurassic%3B_Mt._Tom_Dinosaur_Tracksite%2C_Connecticut_River_Valley%2C_Massachusetts%2C_USA%29.jpg/492px-thumbnail.jpg?20210810154627)
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[edit]DescriptionEubrontes giganteus (dinosaur footprint) (Longmeadown Formation, Upper Triassic to Lower Jurassic; Mt. Tom Dinosaur Tracksite, Connecticut River Valley, Massachusetts, USA).jpg |
English: Eubrontes giganteus Hitchcock, 1845 - theropod dinosaur footprint (~30-35 cm across at its widest) in fine-grained sandstone from the Mesozoic of Massachusetts, USA.
Trace fossils are any indirect evidence of ancient life. They refer to features in rocks that do not represent parts of the body of a once-living organism. Traces include footprints, tracks, trails, burrows, borings, and bitemarks. Body fossils provide information about the morphology of ancient organisms, while trace fossils provide information about the behavior of ancient life forms. Interpreting trace fossils and determination of the identity of a trace maker can be straightforward (for example, a dinosaur footprint represents walking behavior) or not. Sediments that have trace fossils are said to be bioturbated. Burrowed textures in sedimentary rocks are referred to as bioturbation. Trace fossils have scientific names assigned to them, in the same style & manner as living organisms or body fossils. The dinosaur footprint shown here is in an outcrop of terrestrial siliciclastic sedimentary rocks of Late Triassic to Early Jurassic age that fill old rift valleys in Pennsylvania and adjacent states in eastern America. The rift basins formed when the ancient Pangaea supercontinent attempted to break apart, but failed. A successful breakup of Pangaea occurred during the Jurassic. Stratigraphy: Longmeadow Formation, Newark Supergroup, Upper Triassic to Lower Jurassic Locality: Mt. Tom Dinosaur Tracksite, north of Holyoke, Connecticut River Valley of Massachusetts, USA |
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Source | https://www.flickr.com/photos/47445767@N05/15353015480/ |
Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/15353015480. It was reviewed on 10 August 2021 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
10 August 2021
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current | 15:46, 10 August 2021 | ![]() | 589 × 718 (491 KB) | Ser Amantio di Nicolao (talk | contribs) | Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/15353015480/ with UploadWizard |
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Orientation | Normal |
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Horizontal resolution | 576 dpi |
Vertical resolution | 576 dpi |
Software used | Adobe Photoshop CS2 Macintosh |
File change date and time | 20:57, 19 January 2014 |
Color space | sRGB |
Image width | 589 px |
Image height | 718 px |
Date and time of digitizing | 15:57, 19 January 2014 |
Date metadata was last modified | 15:57, 19 January 2014 |