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dinosaursexcavationsitesfieldworkSeptember 17, 20264 min read

What Is a Dinosaur Quarry? A Site Worked for Years Rather Than Days

By the BrainSnail editorial team. How these articles are written and checked, and how to tell us when one is wrong.

Most fossil finds are isolated and occasionally a site produces bones continuously across decades of excavation. Those quarries supply a disproportionate share of what is known, and working one is closer to a long-running construction project than to the popular image of a dig.

Why some sites keep producing

A productive quarry generally exists because a particular bed accumulated bones in quantity, whether through a mass death, a long period of carcasses collecting at one spot, or water sorting remains into a deposit. Once such a bed is identified, following it laterally produces more material, so a site that yielded one specimen is worth returning to. Access matters as much as richness, since a bed exposed in a cliff face or under thin overburden can be worked while the same bed under a hundred metres of rock cannot. Permission and landholding determine whether work can continue at all, and many important sites sit on public land under permit systems or on private land under agreement. Funding cycles shape the pace, since a season is short and money is annual, and a large quarry may be worked in summers across decades by successive teams, with each season removing overburden, mapping, extracting and backfilling.

How a season runs

The work is systematic and most of it is not extraction:

  • Removing overburden, which is mechanical and frequently involves heavy equipment, and which is the largest single effort at many sites
  • Establishing a grid and mapping every element in three dimensions before anything is lifted, since position is the information that cannot be recovered
  • Careful excavation with hand tools and brushes once bone is reached, with consolidant applied as material is exposed
  • Jacketing in plaster and burlap for transport, with large blocks requiring machinery to move
  • Sampling sediment, collecting microfossils and screening spoil for small material, which is where most of the small vertebrates and plants come from
  • Backfilling and stabilising the site at the end of a season to protect what remains for next year

The famous ones

A handful of quarries have shaped the discipline. The Carnegie Quarry in Utah, worked from 1909 and now enclosed within a building where visitors see bones still in the rock face, supplied specimens to museums across several continents. Dinosaur Provincial Park in Alberta contains a very large number of productive localities within a small area and has produced a substantial fraction of known specimens from its period. The Cleveland-Lloyd Quarry in Utah is unusual for an excess of predators over prey and has been excavated repeatedly with the interpretation revised each time. Bone beds in Montana and Wyoming have supplied the growth series that changed how several groups are understood. Sites in Liaoning, China, preserved feathered dinosaurs in fine-grained lake deposits and transformed the field from the 1990s. Each of these represents an accumulation of effort across generations rather than a single discovery, which is the pattern the popular account of palaeontology rarely conveys.

What is left behind

A quarry raises questions about what should be removed and what should stay. Leaving material in place preserves context and permits future excavation with better techniques, and several sites deliberately retain bone in situ for display and for later work. Removing everything protects it from weathering and from theft, which is a genuine problem at accessible sites, with commercially valuable specimens stolen and sites damaged by unauthorised digging. Public access is a further tension, since visitors support the funding and also damage sites. Legal frameworks differ enormously, with fossils on public land in some countries requiring permits and remaining public property, and with private land ownership in others allowing commercial sale, which is why identical specimens can be scientific material in one jurisdiction and saleable property in the next. That variation drives an international market and creates the situation where scientifically important specimens are auctioned and disappear into private hands, which journals and professional bodies have responded to by refusing to publish descriptions of inaccessible material.

The takeaway

A rich bed followed laterally keeps producing, so productive sites are worked across decades by successive teams rather than excavated once. Removing overburden and mapping positions take more effort than extraction does, and screening spoil produces most of the small animals. Ownership law varies enough that the same specimen is public scientific material in one country and saleable property in another.

Practise this

Questions from How Palaeontology Works

Reading about something is not the same as being able to recall it. These are real questions from the How Palaeontology Works unit in our Dinosaurs & Prehistoric Life track, answers and explanations included. The unit has 107 in total across 18 steps.

  • Choose all that applyLevel 3

    1. Which people shaped early dinosaur science? Pick all that apply.

    • William Bucklandcorrect
    • Gideon Mantellcorrect
    • Mary Anningcorrect
    • Isaac Newton

    Buckland, Mantell, Owen and Anning were all central figures.

  • Choose all that applyLevel 2

    2. Which records are made during excavation? Pick all that apply.

    • Photographs of the bones in placecorrect
    • GPS coordinatescorrect
    • Notes on the rock layercorrect
    • The finder's shoe size

    Photographs, maps, GPS coordinates and notes on the rock layer are all essential.

  • Fact or fibLevel 3

    3. Some fossils are prepared under a microscope with tools as fine as needles.

    Answer: True

    True, especially for tiny or delicate specimens.