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JurassicherbivoreFossil completeness: excellent

Dryosaurus altus

Pronunciation: DRY-oh-SORE-us AL-tus

A lightly built Late Jurassic herbivore from the Morrison Formation, with long hind limbs, a balancing tail and a small beaked head.

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Dryosaurus altus

The page URL and title are included automatically. Optional contact details are used only to discuss this report. Do not submit private information or precise sensitive fossil-site coordinates.

Last updated 2 August 2026

Field guide

Overview

Dryosaurus altus was a small-bodied dryosaurid ornithopod from the Late Jurassic Morrison Formation of western North America. Its long lower legs and compact torso produced a much lighter build than the contemporary Camptosaurus, while a deep tail helped balance the body during bipedal movement. The front of the mouth formed a toothless beak and the cheek teeth processed vegetation. The holotype includes a partial skeleton and important cranial material, and later discoveries have expanded knowledge of the genus. Some of the most famous skeletons historically displayed as D. altus, however, were separated as Dryosaurus elderae in 2018, so older books and museum labels can combine material that is no longer assigned to the same species.

Its fossils occur between approximately 155 and 145 million years ago. Values shown here are approximate and reflect the current curated seed dataset.

Form and function

Anatomy

The head was small with a beak at the front, leaf-shaped cheek teeth and large eye openings. Short forelimbs ended in five-fingered hands, while the much longer hind limbs had powerful upper segments and elongated feet. Ossified tendons stiffened parts of the back and tail, helping the tail act as a dynamic counterbalance. Unlike hadrosaurs, Dryosaurus lacked a deep dental battery and did not have forelimbs specialized into weight-bearing columns.

  • Small beaked skull with leaf-shaped cheek teeth
  • Five-fingered hands on short forelimbs
  • Long and slender weight-bearing hind limbs
  • Elongated feet suited to efficient bipedal movement
  • Deep balancing tail reinforced by ossified tendons
  • Lightly built torso compared with larger iguanodontians

Evolutionary position

Scientific classification

  1. 1Dinosauriaclade
  2. 2Ornithischiaclade
  3. 3Neornithischiaclade
  4. 4Ornithopodaclade
  5. 5Iguanodontiaclade
  6. 6Dryosauridaefamily
  7. 7Dryosaurusgenus
  8. 8Dryosaurus altusspecies

This simplified classification path shows one placement from Dinosauria to this species. Each step is clickable, and other analyses may support alternative relationships.

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Scale

Size comparison

Scientific record

Discovery and naming

Samuel Wendell Williston found the holotype at Reed's Quarry 5 near Como Bluff, Wyoming, in 1876 during the early years of the Bone Wars. Othniel Charles Marsh described it in 1878 as Laosaurus altus and created the separate genus Dryosaurus in 1894. The holotype, YPM VP 001876, remains in the Yale Peabody Museum. Carnegie Museum expeditions later collected excellent dryosaur material at Dinosaur National Monument, but a 2018 revision distinguished those Utah skeletons as D. elderae rather than D. altus.

Discovery credit: Samuel Wendell Williston.

Naming authors: Othniel Charles Marsh.

Palaeoenvironment

Habitat and behaviour

Dryosaurus inhabited the river channels, floodplains and seasonally dry woodland mosaics of the Morrison Formation. It lived among much larger herbivores including sauropods, stegosaurs and Camptosaurus, as well as predators such as Allosaurus and Ceratosaurus. Its small body likely gave it access to low vegetation and ecological space different from the giant browsers. The map point represents the broad Como Bluff quarry region, not a publicly released excavation coordinate.

Dryosaurus cropped low vegetation with its beak and sliced it with cheek teeth. Long hind limbs and a counterbalancing tail support agile bipedal locomotion, but fossils cannot provide a reliable maximum running speed. Speed was probably useful when avoiding predators, although direct chase evidence is absent. No nest, trackway or mass accumulation securely demonstrates its group size, parental care or migratory behaviour.

Worth knowing

Field notes

  • Its name means tree or oak lizard, referring to a presumed woodland habitat rather than oak-shaped teeth.
  • The type skeleton was discovered near Como Bluff during the Bone Wars era.
  • Dryosaurus had five fingers even though its forelimbs were much shorter than its legs.
  • Ossified tendons helped stiffen the back and tail.
  • Famous Utah fossils once called D. altus are now often classified as Dryosaurus elderae.

Fossil distribution

Fossil locations

Reed's Quarry 5 fossil region

Como Bluff, Albany County, Wyoming, United States

Morrison Formation, upper Brushy Basin Member

regional marker

Markers are deliberately approximate. They identify published fossil areas without exposing sensitive excavation coordinates.

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Fossil specimen record

Museums and research collections

Yale Peabody Museum

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New Haven, Connecticut, United States

Repository of the Dryosaurus altus holotype from Reed's Quarry 5 at Como Bluff. The catalogued partial skeleton is the name-bearing reference for the species and is available through the museum's vertebrate palaeontology collection.

Record type: originalChecked 2 August 2026Institution website

A research repository is not necessarily a public exhibit. Loan and display status can change, so check with the institution before visiting.

Scientific uncertainty

  • Older reconstructions often combine the Wyoming type species with Dinosaur National Monument material reassigned to D. elderae in 2018.
  • The precise age and correlation of individual Morrison Formation quarries remain under study.
  • Body length and mass vary with specimen maturity and with which referred skeletons are accepted as D. altus.
  • Long legs indicate efficient movement but do not establish a numerical top speed.
  • Colour and external soft tissues in the life reconstruction are interpretive.

Evidence

References and sources

  1. 01
    A photo documentation of bipedal ornithischian dinosaurs from the Upper Jurassic Morrison Formation, USA

    Kenneth Carpenter, Peter M. Galton · Geology of the Intermountain West 5, 167-207 · 2018

    Open source
  2. 02
    Dryosaurus altus holotype YPM VP 001876

    Yale Peabody Museum Vertebrate Paleontology Collection

    Open source
  3. 03
    Dryosaurus altus

    Dinosaur National Monument, U.S. National Park Service

    Open source
  4. 04
    Dryosaurus dinosaur directory entry

    Natural History Museum, London

    Open source