Kirtland Formation facts for kids
Quick facts for kids Kirtland FormationStratigraphic range: Campanian (typically Kirtlandian) 75–73Ma |
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Type | Geological formation |
Sub-units | Hunter Wash, Farmington and De-na-zin Members |
Underlies | Ojo Alamo Formation |
Overlies | Fruitland Formation |
Thickness | 594 m (1,949 ft) |
Lithology | |
Primary | Sandstone |
Other | Shale, mudstone, conglomerate |
Location | |
Coordinates | 36°42′29″N 108°21′00″W / 36.708°N 108.350°W |
Approximate paleocoordinates | 42°36′N 76°18′W / 42.6°N 76.3°W |
Region | ![]() |
Country | ![]() |
Extent | San Juan Basin |
Type section | |
Named for | Kirtland Post Office |
Named by | C.M. Bauer |
Year defined | 1916 |
The Kirtland Formation is a special type of sedimentary rock layer. It was first called the Kirtland Shale. This rock formation is a record of ancient environments. It tells us about the land and life that existed millions of years ago.
Contents
What is the Kirtland Formation?
The Kirtland Formation is made of mud and sand. These materials were left behind by ancient rivers and floods. This happened on a flat coastal plain. This plain was next to an ancient inland sea. This sea covered parts of North America during the late Cretaceous Period.
The Kirtland Formation sits on top of another rock layer called the Fruitland Formation. You can find the Kirtland Formation in the San Juan Basin. This basin is in the states of New Mexico and Colorado in the United States.
How Old is the Kirtland Formation?
Scientists have studied the Kirtland Formation very carefully. They use special methods to find out its age. The bottom part of the Kirtland Formation is about 75 million years old. This part is called the Hunter Wash member.
The Kirtland Formation is divided into different layers, or "members."
- The Hunter Wash member is the oldest, about 75 million years old.
- Above it is the Farmington member, which is about 74 million years old.
- The De-na-zin member is on top of the Farmington member. It is about 73.37 million years old.
- The very top of the De-na-zin member is about 73.04 million years old.
There's also a layer called the Naashoibito member. This layer was once thought to be part of the Kirtland Formation. But now, scientists believe it belongs to the Ojo Alamo Formation, which is a rock layer found above the Kirtland Formation.
How the Kirtland Formation Was Discovered
The Kirtland Formation was first named in 1916. A scientist named C.M. Bauer gave it its name. He named it after the Kirtland Post Office. This was near where he found the rock layers.
Rock Layers of the San Juan Basin
Stratigraphy is the study of rock layers. It helps us understand how different layers formed over time. The image shows how the Kirtland Formation fits with other rock layers in the San Juan Basin.
Amazing Animals from the Kirtland Formation
The Kirtland Formation is famous for its many fossils. These fossils tell us about the animals that lived there millions of years ago. Many of these animals were dinosaurs!
Ancient Crocodilians (Crurotarsans)
Crurotarsans were a group of reptiles that included ancient relatives of crocodiles.
Ancient Crocodilians of the Kirtland Formation | |||
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Genus | Species | Member | Notes |
Brachychampsa | B. montana | De-na-zin | |
Denazinosuchus | D. kirtlandicus | De-na-zin | |
Leidyosuchus | Indeterminate | De-na-zin |
Plant-Eating Dinosaurs (Ornithischians)
Ornithischians were a large group of plant-eating dinosaurs. Many different kinds have been found here.
Plant-Eating Dinosaurs from the Kirtland Formation | |||
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Genus | Species | Member | Notes |
Ahshislepelta | A. minor | Hunter Wash | An armored dinosaur. |
Anasazisaurus | A. horneri | A duck-billed dinosaur. | |
Kritosaurus | K. navajovius | De-na-zin | A duck-billed dinosaur. |
Naashoibitosaurus | N.ostromi | De-na-zin | Another duck-billed dinosaur. |
Nodocephalosaurus | N. kirtlandensis | De-na-zin | An armored dinosaur with a bony head. |
Parasaurolophus | P. tubicen | De-na-zin | A duck-billed dinosaur with a long crest on its head. |
Pentaceratops | P. fenestratus | A horned dinosaur. | |
P. sternbergi | De-na-zin, Hunter Wash | A horned dinosaur, common in the lower parts. | |
Sphaerotholus | S. goodwini | De-na-zin | A dome-headed dinosaur. |
Stegoceras | S. novomexicanum | Hunter Wash | Another dome-headed dinosaur. |
Terminocavus | T. sealeyi | Hunter Wash | A horned dinosaur. |
Navajoceratops | N. sullivani | Hunter Wash | A horned dinosaur. |
Titanoceratops | T. ouranos | Hunter Wash | A very large horned dinosaur. |
Ziapelta | Z. sanjuanensis | Hunter Wash, De-na-zin | An armored dinosaur. |
Flying Reptiles (Pterosaurs)
Pterosaurs were flying reptiles that lived at the same time as dinosaurs.
Flying Reptiles of the Kirtland Formation | ||
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Genus | Species | Member |
Navajodactylus | N. boerei | Hunter Wash Member |
Lizard-Hipped Dinosaurs (Saurischians)
Saurischians include both giant long-necked dinosaurs and meat-eating dinosaurs.
Lizard-Hipped Dinosaurs of the Kirtland Formation | |||
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Genus | Species | Member | Notes |
Alamosaurus | A. sanjuanensis | This dinosaur was once thought to be from Kirtland, but its fossils are actually from the Ojo Alamo Formation. | |
Aublysodon | A. mirandus | This name was used for some teeth, but they are now known to belong to Bistahieversor. | |
Bistahieversor | B. sealeyi | Farmington, Hunter Wash | A large meat-eating dinosaur, a type of tyrannosaur. |
Daspletosaurus | Unnamed | De-na-zin, Farmington, Hunter Wash | Some remains once thought to be Daspletosaurus are now known to be Bistahieversor. |
Ornithomimus | O. sp. | De-na-zin | A fast, ostrich-like dinosaur. |
Saurornitholestes | S. sullivani | De-na-zin | A small, meat-eating dinosaur. |
"Saurornitholestes" | "S." robustus | De-na-zin | This was once thought to be Saurornitholestes, but it's actually another type of small meat-eating dinosaur called a troodontid. |
Troodontidae | Indeterminate | Small, bird-like dinosaurs. | |
Tyrannosauridae | Indeterminate | Large, meat-eating dinosaurs, like T. rex. |
Ancient Turtles
Many types of ancient turtles have been found in the Kirtland Formation.
Turtles of the Kirtland Formation | ||
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Genus | Species | Member |
Basilemys | B. nobilis | De-na-zin |
Denazinemys | D. nodosa | De-na-zin |
Neurankylus | N. baueri | De-na-zin |
Plastomenus | P. robustus | De-na-zin |
Thescelus | T. hemispherica | De-na-zin |
Bony Fish
Fossils of bony fish have also been found.
Bony Fish of the Kirtland Formation | ||
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Genus | Species | Member |
Melvius | M. chauliodous | De-na-zin |
Cartilaginous Fish
These are fish like sharks and rays, whose skeletons are made of cartilage instead of bone.
Cartilaginous Fish of the Kirtland Formation | ||
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Genus | Species | Member |
Myledaphus | M. bipartitus | De-na-zin |
Color key
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Notes Uncertain or tentative taxa are in small text; |
Images for kids
See also
In Spanish: Formación Kirtland para niños