











Meteoraspis dis
Vendor: Fossil Soup
SKU Number: SQ6632414
Meteoraspis dis. from the Middle Cambrian, Weeks Formation, House Range, Millard County, Utah.
This is a rare example that is not often found available on the open market. Meteoraspis sp. is characterized by having 13 thoracic segments and a pygidium with small spines.
Fossil size:
Length: 3.5 cm
Width: 2.3 cm
Matrix size:
Length: 11.5 cm
Width: 8.0 cm
Height: 4.0 cm
This is a very high-end trilobite for the very discerning collector. Very likely the only one currently being offered!!!
Full dimensions are listed below.
Vendor: Fossil Soup
SKU Number: SQ6632414
Meteoraspis dis. from the Middle Cambrian, Weeks Formation, House Range, Millard County, Utah.
This is a rare example that is not often found available on the open market. Meteoraspis sp. is characterized by having 13 thoracic segments and a pygidium with small spines.
Fossil size:
Length: 3.5 cm
Width: 2.3 cm
Matrix size:
Length: 11.5 cm
Width: 8.0 cm
Height: 4.0 cm
This is a very high-end trilobite for the very discerning collector. Very likely the only one currently being offered!!!
Full dimensions are listed below.
Additional Information
This ancient arthropod was a bottom-dweller, likely a deposit feeder that moved slowly across the seafloor, sifting through the mud and sediment to find organic particles to eat. The specimen in the post capture the stunning contrast of its dark, finely textured exoskeleton against the light, reddish-brown limestone matrix. This beautiful trilobite offers a rare glimpse into a moment in time over half a billion years ago. Found in Utah's Fossil-Rich Weeks Formation This location is a Konservat-Lagerstätte, a rare fossil site preserving both hard-shelled and delicate, soft-bodied organisms. The trilobites were likely buried rapidly by a storm or high-salinity event in a shallow sub-tidal environment, perfectly preserving them for us to find today.
The Weeks Formation is located in the central House Range of western Utah. Its stratigraphic position is:
- It conformably overlies the Marjum Formation
- It is conformably overlain by the Orr Formation
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