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Collection: MNA 1489, Balakai Point Apache County, Arizona, USA

Age89.3 - 85.8 Ma (Late/Upper Cretaceous)
IntervalMiddle Coniacian
Lat/Long35.9039,-109.871
Co-ordinates derived fromestimated from map
LocationMNA 1489
Mindat.org Region (for given coordinates)Apache County, Arizona, USA
Geographic Scaleoutcrop
Geographic Commentsnear Balakai Point, southeastern-most Black Mesa, Apache Co., AZ. Located at 2200 m elevation on the Navajo Reservation.
FormationToreva
MemberUpper Sandstone
Stratigraphic Scalegroup of beds
Straigraphic Commentstracksite is in the lowermost part of the upper sandstone member (informal unit name)
Lithology Description"In the immediate vicinity of the tracksite, and stratigraphically above it, is an orange-colored, very coarse-grained, cross-bedded sandstone interpreted to be the upper sandstone member...the main tracksite...occurs in a large slab of fine- to medium-grained, well-indurated sandstone, of a generally pinkish color on unweathered surfaces." Upper member described as "arkosic".
Lithologysandstone
Second Lithologysandstone
Environmentfluvial indet.

Recorded Fossils

Accepted NameHierarchyPreservationAge
Chondrichthyes
class
Animalia : Chordata : Chondrichthyesphosphatic
body,trace
89.3 - 85.8 Ma
Late/Upper Cretaceous
Ornithopoda
unranked clade
Animalia : Chordata : Ornithischia : Ornithopodahydroxylapatite
body,trace
89.3 - 85.8 Ma
Late/Upper Cretaceous
Osteichthyes
unranked clade
Animalia : Chordata : Osteichthyesphosphatic
body,trace
89.3 - 85.8 Ma
Late/Upper Cretaceous
Testudines
order
Animalia : Chordata : Reptilia : Testudinesphosphatic
body,trace
89.3 - 85.8 Ma
Late/Upper Cretaceous
Theropoda
unranked clade
Animalia : Chordata : Saurischia : Theropodahydroxylapatite
body,trace
89.3 - 85.8 Ma
Late/Upper Cretaceous
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
 
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